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Tittonell & Giller (2013). When yield gaps are poverty traps: The paradigm of ecological intensification in African smallholder agriculture

Page 1

Figures and page graphics, page 1

Field

 

Crops

 

Research

 

143

 

(2013)

 

76–90

Contents

 

lists

 

available

 

at

 

SciVerse

 

ScienceDirect

Field

 

Crops

 

Research

j o u

 

r n a l

 

h

 

o m

 

e p a g e :

 

w w w . e l s e v i e r . c o m / l o c a t e / f c r

When

 

yield

 

gaps

 

are

 

poverty

 

traps:

 

The

 

paradigm

 

of

 

ecological

 

intensification

 

in

African

 

smallholder

 

agriculture

Pablo

 

Tittonell

a

,

∗

,

 

Ken

 

E.

 

Giller

b

a

Farming

 

Systems

 

Ecology,

 

Wageningen

 

University,

 

P.O.

 

Box

 

563,

 

6700

 

AN

 

Wageningen,

 

The

 

Netherlands

b

Plant

 

Production

 

Systems,

 

Wageningen

 

University,

 

P.O.

 

Box

 

430,

 

6700AK

 

Wageningen,

 

The

 

Netherlands

a

 

r

 

t

 

i

 

c

 

l

 

e

 

i

 

n

 

f

 

o

Article

 

history:

Received

 

23

 

May

 

2012

Received

 

in

 

revised

 

form

 

5

 

October

 

2012

Accepted

 

10

 

October

 

2012

Keywords:

Cereal

 

yields

Cassava
Highland

 

banana

Grain

 

legumes

Boundary

 

line

 

analysis

Soil

 

organic

 

matter

Soil

 

degradation

Non-responsive

 

soils

a

 

b

 

s

 

t

 

r

 

a

 

c

 

t

Yield

 

gaps

 

are

 

pervasive

 

in

 

African

 

smallholder

 

agriculture,

 

and

 

are

 

large

 

for

 

almost

 

all

 

crops

 

in

 

all

 

regions.

There

 

is

 

consensus

 

that

 

poor

 

soil

 

fertility

 

and

 

nutrient

 

availability

 

are

 

the

 

major

 

biophysical

 

limitations

to

 

agricultural

 

production

 

in

 

the

 

continent.

 

We

 

identify

 

two

 

major

 

yield

 

gaps:

 

(1)

 

the

 

gap

 

between

 

actual

yields

 

(

Y

A

)

 

and

 

the

 

water-limited

 

yield

 

potential

 

(

Y

w

),

 

which

 

is

 

the

 

maximum

 

yield

 

achievable

 

under

 

rain-

fed

 

conditions

 

without

 

irrigation

 

if

 

soil

 

water

 

capture

 

and

 

storage

 

is

 

optimal

 

and

 

nutrient

 

constraints

 

are

released,

 

and

 

(2)

 

The

 

gap

 

between

 

Y

A

,

 

and

 

a

 

locally

 

attainable

 

yield

 

(

Y

L

)

 

which

 

corresponds

 

to

 

the

 

water

and

 

nutrient-limited

 

yields

 

that

 

can

 

be

 

measured

 

in

 

the

 

most

 

productive

 

fields

 

of

 

resource

 

endowed

 

farm-

ers

 

in

 

a

 

community.

 

Estimates

 

of

 

these

 

two

 

yield

 

gaps

 

are

 

given

 

for

 

major

 

crops,

 

together

 

with

 

a

 

framework

for

 

how

 

yield

 

gaps

 

can

 

be

 

estimated

 

in

 

a

 

pragmatic

 

way

 

for

 

different

 

farming

 

systems.

 

The

 

paradigm

of

 

ecological

 

intensification

 

which

 

focuses

 

on

 

yield

 

potential,

 

soil

 

quality

 

and

 

precision

 

agriculture

 

is

explored

 

for

 

the

 

African

 

context.

 

Our

 

analysis

 

suggests

 

that

 

smallholder

 

farmers

 

are

 

unable

 

to

 

benefit

from

 

the

 

current

 

yield

 

gains

 

offered

 

by

 

plant

 

genetic

 

improvement.

 

In

 

particular,

 

continued

 

cropping

without

 

sufficient

 

inputs

 

of

 

nutrients

 

and

 

organic

 

matter

 

leads

 

to

 

localised

 

but

 

extensive

 

soil

 

degrada-

tion

 

and

 

renders

 

many

 

soils

 

in

 

a

 

non-responsive

 

state.

 

The

 

lack

 

of

 

immediate

 

response

 

to

 

increased

 

inputs

of

 

fertiliser

 

and

 

labour

 

in

 

such

 

soils

 

constitutes

 

a

 

chronic

 

poverty

 

trap

 

for

 

many

 

smallholder

 

farmers

 

in

Africa.

 

This

 

necessitates

 

a

 

rethink

 

for

 

development

 

policy

 

aimed

 

to

 

improve

 

productivity

 

and

 

address

problems

 

of

 

food

 

insecurity.

©

 

2012

 

Elsevier

 

B.V.

 

1.

 

Introduction

The

 

concept

 

of

 

ecological

 

intensification

 

was

 

coined

 

by

 

Cassman

(1999)

 

to

 

define

 

the

 

set

 

of

 

principles

 

and

 

means

 

necessary

 

to

increase

 

primary

 

productivity

 

in

 

the

 

major

 

cereal

 

agroecosystems

of

 

the

 

world.

 

Emphasis

 

was

 

placed

 

on

 

increasing

 

the

 

yield

 

ability

of

 

major

 

crops

 

and

 

narrowing

 

yield

 

gaps

 

through

 

implementing

forms

 

of

 

precision

 

agriculture,

 

relying

 

on

 

scientific

 

breakthroughs

in

 

the

 

field

 

of

 

plant

 

physiology,

 

crop

 

ecophysiology

 

and

 

soil

 

science.

Later

 

reinterpretations

 

of

 

this

 

concept,

 

particularly

 

in

 

the

 

con-

text

 

of

 

European

 

agriculture

 

(e.g.,

 

Bonny,

 

2011;

 

Malezieux,

 

2012

),

attached

 

a

 

definition

 

that

 

borders

 

those

 

of

 

organic

 

or

 

ecological

farming.

 

Ecological

 

intensification

 

is

 

now

 

understood

 

as

 

a

 

means

 

of

increasing

 

agricultural

 

outputs

 

(food,

 

fibre,

 

agro-fuels

 

and

 

environ-

mental

 

services)

 

while

 

reducing

 

the

 

use

 

and

 

the

 

need

 

for

 

external

inputs

 

(agrochemicals,

 

fuel,

 

and

 

plastic),

 

capitalising

 

on

 

ecological

processes

 

that

 

support

 

and

 

regulate

 

primary

 

productivity

 

in

 

agroe-

cosystems.

 

Yet,

 

little

 

has

 

been

 

written

 

on

 

how

 

to

 

achieve

 

this.

 

Single

∗

Corresponding

 

author.

E-mail

 

address:

 

pablo.tittonell@wur.nl

(P.

 

Tittonell).

efforts

 

addressing

 

the

 

various

 

challenges

 

facing

 

current

 

agriculture

have

 

been

 

often

 

done

 

in

 

isolation

 

rather

 

than

 

holistically.

 

These

observations

 

have

 

prompted

 

Doré

 

et

 

al.

 

(2011)

 

to

 

propose

 

new

sources

 

of

 

knowledge

 

and

 

methods

 

in

 

agronomy

 

to

 

strengthen

 

the

ecological

 

intensification

 

of

 

current

 

agriculture.

The

 

ecological

 

intensification

 

of

 

agriculture

 

has

 

seldom

 

been

addressed

 

in

 

the

 

context

 

of

 

the

 

smallholder

 

farming

 

systems

that

 

characterise

 

rural

 

Africa.

 

There

 

is

 

no

 

doubt

 

of

 

the

 

concept’s

relevance

 

to

 

guide

 

farming

 

systems

 

design

 

in

 

the

 

African

 

con-

text:

 

producing

 

more

 

with

 

less

 

external

 

input,

 

while

 

keeping

 

a

healthy

 

environment

 

that

 

provides

 

multiple

 

services.

 

However,

in

 

view

 

of

 

the

 

importance

 

of

 

agriculture

 

for

 

rural

 

livelihoods

 

and

national

 

economies

 

the

 

‘intensification’

 

component,

 

whether

 

eco-

logical

 

or

 

not

 

has

 

been

 

sensed

 

as

 

most

 

urgent

 

for

 

Africa.

 

The

need

 

to

 

intensify

 

African

 

agriculture

 

has

 

recently

 

led

 

agricultural

research

 

for

 

development

 

in

 

a

 

somehow

 

opposite

 

direction,

 

pro-

moting

 

the

 

use

 

of

 

mineral

 

fertilisers,

 

hybrid

 

seeds,

 

new

 

crops,

irrigation,

 

herbicide-based

 

no-till

 

systems,

 

genetically

 

modified

cultivars

 

or

 

mechanisation

 

as

 

means

 

to

 

increase

 

productivity

 

(e.g.,

http://www.agra.org

).

 

The

 

sustainable

 

intensification

 

of

 

agricul-

ture

 

through

 

technologies

 

that

 

rely

 

on

 

substantial

 

investment

 

in

inputs

 

has

 

been

 

seriously

 

hampered

 

by

 

poorly

 

developed

 

input

 

and

0378-4290 ©

 

2012

 

Elsevier

 

B.V.

 

http://dx.doi.org/10.1016/j.fcr.2012.10.007

Open access under 

CC BY-NC-ND license.

Open access under 

CC BY-NC-ND license.

Page 2

Figures and page graphics, page 2

P.

 

Tittonell,

 

K.E.

 

Giller

 

/

 

Field

 

Crops

 

Research

 

143

 

(2013)

 

76–90

 

77

output

 

markets

 

(

Dorward

 

et

 

al.,

 

1998

),

 

but

 

often

 

also

 

by

 

the

 

poor

performance

 

of

 

technologies

 

in

 

the

 

African

 

context

 

or

 

their

 

inade-

quacy

 

to

 

fit

 

within

 

local

 

smallholder

 

systems

 

(e.g.,

 

Giller

 

et

 

al.,

 

2009,

2011

).

Thus,

 

whether

 

deliberately

 

or

 

not,

 

much

 

of

 

African

 

agriculture

has

 

remained

 

rather

 

‘ecological’.

 

Basic

 

supportive

 

and

 

regulatory

ecological

 

processes

 

steered

 

through

 

local

 

lay

 

knowledge

 

still

 

con-

stitute

 

the

 

backbone

 

of

 

smallholder

 

agriculture

 

in

 

many

 

places.

But

 

despite

 

the

 

genuine

 

attractiveness

 

that

 

surrounds

 

traditional

systems

 

and

 

local

 

practices,

 

their

 

inability

 

to

 

sustain

 

Africa’s

 

food

sufficiency

 

is

 

self-evident.

 

Yet,

 

there

 

are

 

reasons

 

to

 

believe

 

that

supportive

 

and

 

regulatory

 

ecological

 

mechanisms

 

that

 

farmers

 

are

able

 

to

 

master

 

can

 

lead

 

to

 

synergetic

 

responses

 

of

 

agricultural

 

sys-

tems

 

to

 

external

 

inputs

 

(e.g.,

 

Lahmar

 

et

 

al.,

 

2012

).

 

This

 

forms

 

the

basis

 

for

 

the

 

design

 

of

 

integrated

 

approaches

 

to

 

soil

 

fertility,

 

pest

or

 

crop

 

management

 

that

 

build

 

on

 

local

 

knowledge.

 

A

 

large

 

body

of

 

evidence

 

shows

 

that

 

labour,

 

water

 

or

 

nutrient

 

use

 

efficiencies

are

 

enhanced

 

through

 

the

 

implementation

 

of

 

such

 

knowledge-

intensive

 

approaches

 

(e.g.,

 

Khan

 

et

 

al.,

 

2010;

 

Vanlauwe

 

et

 

al.,

 

2010;

Altieri

 

et

 

al.,

 

2012

).

Cassman

 

(1999)

 

distinguished

 

between

 

strategies

 

necessary

for

 

ecological

 

intensification

 

under

 

unfavourable

 

(mostly

 

rain-

fed)

 

and

 

favourable

 

environments,

 

focusing

 

mostly

 

on

 

the

 

latter.

He

 

postulated

 

that

 

the

 

ecological

 

intensification

 

of

 

agriculture

 

in

unfavourable

 

rain-fed

 

environments,

 

where

 

lack

 

of

 

water

 

would

be

 

the

 

primary

 

constraint,

 

would

 

depend

 

on

 

reducing

 

the

 

reliance

on

 

subsistence

 

cereal

 

production,

 

integration

 

with

 

livestock

 

enter-

prises,

 

greater

 

crop

 

diversification

 

and

 

agroforestry

 

practices

 

that

may

 

ensure

 

higher

 

economic

 

value

 

and

 

soil

 

conservation.

 

Although

some

 

of

 

these

 

principles

 

may

 

be

 

relevant

 

for

 

the

 

rain-fed

 

pro-

duction

 

environments

 

that

 

predominate

 

in

 

sub-Saharan

 

Africa,

closer

 

examination

 

is

 

necessary.

 

For

 

example,

 

crop

 

productivity

 

in

many

 

parts

 

of

 

Africa

 

is

 

limited

 

primarily

 

by

 

nutrient

 

rather

 

than

water

 

availability;

 

smallholder

 

cereal

 

production

 

is

 

often

 

oriented

to

 

both

 

consumption

 

and

 

the

 

market;

 

the

 

integration

 

of

 

cropping

and

 

livestock

 

activities

 

is

 

already

 

a

 

common

 

denominator

 

to

 

many

of

 

these

 

systems;

 

in

 

densely

 

populated

 

regions

 

green

 

manures

or

 

agroforestry

 

do

 

not

 

always

 

fit

 

the

 

needs

 

and

 

possibilities

 

of

smallholders;

 

and

 

so

 

on.

 

Where

 

natural

 

resources

 

have

 

become

degraded,

 

farmers

 

may

 

be

 

caught

 

in

 

poverty

 

traps

 

(

Marenya

 

and

Barrett,

 

2007

),

 

where

 

response

 

to

 

inputs

 

is

 

poor

 

and

 

follows

 

an

‘S-shaped’

 

curve

 

(

De

 

Wit,

 

1992,

 

1994

).

 

Africa

 

needs

 

a

 

‘uniquely

African’

 

strategy

 

for

 

the

 

sustainable

 

intensification

 

of

 

its

 

agricul-

ture

 

(cf.

 

Tittonell

 

et

 

al.,

 

2011

),

 

capitalising

 

on

 

ecological

 

processes

and

 

ensuring

 

efficient

 

use

 

of

 

scarce

 

external

 

inputs.

This

 

paper

 

examines

 

current

 

yield

 

gaps

 

in

 

Africa

 

and

 

the

opportunities

 

and

 

challenges

 

that

 

lay

 

ahead

 

for

 

the

 

ecological

intensification

 

of

 

smallholder

 

agriculture,

 

placing

 

emphasis

 

on

 

the

efficient

 

use

 

of

 

the

 

abiotic

 

resources:

 

light,

 

water

 

and

 

nutrients.

 

We

draw

 

on

 

a

 

wide

 

range

 

of

 

experiences

 

from

 

Southern,

 

East,

 

Central

and

 

West

 

Africa.

 

We

 

postulate

 

that

 

current

 

approaches

 

to

 

the

 

eco-

logical

 

intensification

 

of

 

smallholder

 

agriculture

 

in

 

Africa:

 

(i)

 

may

be

 

deterred

 

by

 

inherent

 

characteristics

 

of

 

these

 

agroecosystems,

(ii)

 

lack

 

biophysical

 

references

 

and

 

suitable

 

technical

 

means

 

that

embrace

 

local

 

preferences

 

and

 

knowledge,

 

(iii)

 

should

 

not

 

overlook

the

 

integrated

 

nature

 

of

 

smallholder

 

systems

 

(e.g.,

 

crop-livestock

interactions,

 

communally

 

owned

 

resources,

 

etc.)

 

in

 

which

 

decisions

are

 

made

 

at

 

scales

 

higher

 

than

 

the

 

field

 

plot,

 

and

 

(iv)

 

will

 

not

 

be

achieved

 

without

 

prior

 

efforts

 

to

 

restore

 

productivity

 

of

 

already

degraded

 

land.

 

The

 

three

 

pillars

 

that

 

Cassman

 

(1999)

 

identified

for

 

the

 

ecological

 

intensification

 

of

 

cereal

 

production,

 

namely

 

yield

potential,

 

soil

 

quality

 

and

 

precision

 

agriculture

 

are

 

first

 

analysed

for

 

their

 

specificities

 

and

 

suitability

 

in

 

the

 

African

 

context.

 

This

 

is

followed

 

by

 

an

 

estimate

 

of

 

the

 

average

 

yield

 

gap

 

of

 

major

 

crops

 

in

the

 

continent,

 

attempting

 

to

 

distinguish

 

between

 

yield

 

gaps

 

caused

by

 

resource

 

availability

 

from

 

gaps

 

caused

 

by

 

access

 

to

 

technology.

Fig.

 

1.

 

Average

 

cereal

 

productivity

 

and

 

fertiliser

 

use

 

intensity

 

(total

 

fertiliser

 

use

over

 

area

 

cropped)

 

at

 

national

 

level

 

for

 

selected

 

countries

 

between

 

1961

 

and

 

2008.

Source

:

 

FAOstat.

We

 

conclude

 

by

 

proposing

 

a

 

framework

 

for

 

yield

 

gap

 

assessment

in

 

African

 

agriculture

 

based

 

on

 

biophysical

 

drivers,

 

with

 

the

 

aim

 

of

contributing

 

to

 

the

 

delineation

 

of

 

a

 

worldwide

 

yield

 

gap

 

atlas

 

(

van

Ittersum

 

et

 

al.,

 

2013

).

2.

 

The

 

pillars

 

of

 

ecological

 

intensification

 

following

Cassman

 

(1999)

2.1.

 

Yield

 

potential

Food

 

production

 

in

 

sub-Saharan

 

Africa

 

is

 

not

 

keeping

 

pace

with

 

population

 

growth.

 

Sub-Saharan

 

Africa

 

has

 

the

 

lowest

 

land

and

 

labour

 

productivity

 

rates

 

in

 

the

 

world,

 

with

 

annual

 

growth

in

 

cereal

 

yields

 

averaging

 

only

 

10

 

kg

 

grain

 

ha

−

1

yr

−

1

–

 

about

 

1%

(

http://www.earthtrends.wri.org

).

 

While

 

cereal

 

yields

 

in

 

most

 

of

the

 

developed

 

and

 

developing

 

world

 

increased

 

steadily

 

during

 

the

last

 

50

 

years,

 

yields

 

in

 

African

 

countries

 

hovered

 

around

 

1

 

t

 

ha

−

1

or

 

less

 

(

Fig.

 

1

A).

 

Similarly,

 

the

 

average

 

yield

 

of

 

tuber

 

crops

 

(cas-

sava,

 

sweet

 

potato,

 

yam,

 

etc.)

 

is

 

the

 

lowest

 

in

 

the

 

world

 

(around

8

 

t

 

ha

−

1

),

 

increasing

 

at

 

a

 

rate

 

of

 

50

 

kg

 

ha

−

1

yr

−

1

or

 

0.6%

 

over

 

the

same

 

period.

 

Counting

 

growth

 

in

 

harvested

 

area

 

as

 

well,

 

food

 

pro-

duction

 

in

 

sub-Saharan

 

Africa

 

increases

 

at

 

an

 

annual

 

rate

 

of

 

ca.

 

2%,

while

 

population

 

growth

 

rates

 

average

 

3%.

 

If

 

Africa

 

seeks

 

to

 

rely

 

on

agriculture

 

for

 

economic

 

development,

 

an

 

annual

 

increase

 

of

 

4–7%

in

 

food

 

production

 

is

 

required

 

(

Breman

 

and

 

Debrah,

 

2003

).

 

Techno-

logical

 

progress

 

in

 

tropical

 

agriculture

 

in

 

combination

 

with

 

more

favourable

 

socio-economic

 

contexts

 

allowed

 

food

 

production,

 

and

particularly

 

cereal

 

yields

 

to

 

increase

 

substantially

 

in

 

Latin

 

Amer-

ica

 

and

 

Asia

 

during

 

the

 

last

 

two

 

to

 

three

 

decades.

 

Although

 

much

of

 

such

 

yield

 

increase

 

may

 

be

 

explained

 

by

 

increased

 

input

 

use

(

Fig.

 

1

B),

 

genetic

 

progress

 

through

 

plant

 

breeding

 

played

 

a

 

central

Page 3

Figures and page graphics, page 3

78

 

P.

 

Tittonell,

 

K.E.

 

Giller

 

/

 

Field

 

Crops

 

Research

 

143

 

(2013)

 

76–90

Fig.

 

2.

 

A

 

representation

 

of

 

yield-defining,

 

yield-limiting

 

and

 

yield-reducing

 

factors

 

determining

 

respectively

 

the

 

potential,

 

attainable

 

and

 

actual

 

yield

 

levels.

 

Factors

 

were

grouped

 

into

 

varietal

 

characteristics

 

(G),

 

uncontrolled

 

environment

 

(E)

 

and

 

management

 

(M)

 

to

 

illustrate

 

the

 

increasing

 

importance

 

of

 

the

 

latter

 

as

 

one

 

moves

 

from

 

potential

to

 

actual

 

yields.

From

:

 

Tittonell

 

(2009)

.

role

 

(Hall,

 

this

 

volume).

 

As

 

the

 

yield

 

ability

 

of

 

major

 

crop

 

varieties

available

 

for

 

tropical

 

environments

 

keeps

 

rising,

 

the

 

stagnating

average

 

yield

 

observed

 

in

 

most

 

African

 

countries

 

means

 

that

 

yield

gaps

 

are

 

widening

 

across

 

the

 

continent.

(Theoretical)

 

potential

 

yields

 

in

 

sub-Saharan

 

Africa,

 

those

 

that

may

 

be

 

achieved

 

under

 

no

 

water

 

or

 

nutrient

 

constraints,

 

vary

 

for

the

 

various

 

cereal

 

crops

 

and

 

their

 

cultivars

 

and

 

are

 

defined

 

chiefly

by

 

latitude,

 

altitude

 

and

 

cloud

 

cover.

 

Potential

 

yields

 

can

 

be

 

calcu-

lated

 

using

 

simulation

 

models

 

that

 

input

 

the

 

length

 

of

 

the

 

growing

season,

 

diurnal

 

and

 

nocturnal

 

air

 

temperatures,

 

day

 

length

 

and

the

 

total

 

amount

 

of

 

solar

 

radiation

 

received

 

during

 

a

 

season

 

by

 

a

given

 

cultivar

 

(e.g.,

 

Thornton

 

et

 

al.,

 

2009

).

 

In

 

this

 

paper

 

we

 

refer

 

to

the

 

water-limited

 

yield

 

potential

 

(

Y

w

)

 

as

 

defined

 

by

 

van

 

Ittersum

et

 

al.

 

(2013)

,

 

which

 

is

 

the

 

maximum

 

yield

 

achievable

 

under

 

rain-

fed

 

conditions

 

without

 

irrigation

 

if

 

soil

 

water

 

capture

 

and

 

storage

is

 

optimal

 

and

 

nutrient

 

constraints

 

are

 

eliminated.

 

The

 

attainable

yield

 

level

 

following

 

the

 

classical

 

definition

 

of

 

production

 

situa-

tions

 

by

 

De

 

Wit

 

(1992)

,

 

corresponds

 

to

 

water

 

and

 

nutrient-limited

yields.

 

Here,

 

we

 

propose

 

an

 

adaptation

 

of

 

this

 

to

 

the

 

African

 

situ-

ation

 

by

 

defining

 

a

 

locally

 

attainable

 

yield

 

level

 

(

Y

L

),

 

which

 

is

 

the

maximum

 

yield

 

achievable

 

by

 

resource

 

endowed

 

farmers

 

in

 

their

most

 

productive

 

fields.

 

Two

 

yield

 

gaps

 

can

 

be

 

then

 

calculated:

 

a

yield

 

gap

 

1,

 

between

 

Y

W

and

 

Y

L

,

 

and

 

a

 

yield

 

gap

 

2,

 

between

 

Y

L

and

actual

 

farmers

 

yield

 

levels

 

(

Y

A

).

2.1.1.

 

The

 

(G

 

×

 

E

 

×

 

M)

FS

interaction

Taking

 

de

 

Wit’s

 

definitions,

 

the

 

relative

 

importance

 

of

 

manage-

ment

 

decisions

 

with

 

respect

 

to

 

the

 

genotype

 

or

 

the

 

uncontrolled

environment

 

increases

 

as

 

we

 

move

 

from

 

yield-defining

 

to

 

yield-

reducing

 

factors,

 

from

 

potential

 

to

 

attainable

 

and

 

actual

 

yields

(

Fig.

 

2

).

 

There

 

is

 

consensus

 

that

 

nutrient

 

supply,

 

rather

 

than

 

water,

is

 

the

 

main

 

yield-limiting

 

factor

 

in

 

sub-Saharan

 

Africa

 

(

Penning

de

 

Vries

 

and

 

Ditèye,

 

1991;

 

Breman

 

and

 

Debrah,

 

2003

).

 

However,

whilst

 

fertiliser

 

use

 

has

 

expanded

 

in

 

some

 

countries

 

such

 

as

 

Kenya,

it

 

remains

 

anecdotal

 

in

 

many

 

parts

 

of

 

the

 

continent.

 

Where

 

land

 

is

not

 

limiting,

 

the

 

area

 

cultivated

 

is

 

a

 

more

 

important

 

determinant

of

 

household

 

food

 

security

 

than

 

the

 

yield

 

per

 

unit

 

area.

 

In

 

such

cases,

 

farmers

 

often

 

prioritise

 

investments

 

to

 

hire

 

labour

 

or

 

ox-

ploughing

 

rather

 

than

 

purchasing

 

fertilisers

 

or

 

improved

 

seeds

 

to

intensify

 

production

 

(

Tittonell

 

et

 

al.,

 

2010a

).

 

Cultivating

 

large

 

areas

with

 

limited

 

labour

 

available

 

often

 

leads

 

to

 

late

 

planting,

 

exposing

bare

 

soil

 

to

 

the

 

first

 

torrential

 

rains

 

of

 

the

 

season,

 

or

 

to

 

late

 

or

 

ineffi-

cient

 

weeding

 

during

 

the

 

season.

 

In

 

some

 

cases,

 

however,

 

extended

periods

 

of

 

sowing

 

may

 

be

 

a

 

strategy

 

to

 

deal

 

with

 

erratic

 

rainfall,

minimising

 

the

 

risk

 

of

 

complete

 

crop

 

failure

 

in

 

space

 

and

 

time

(

Milgroom

 

and

 

Giller,

 

2013

).

 

Thus

 

probably

 

more

 

than

 

anywhere

else,

 

potential

 

yields

 

under

 

African

 

smallholder

 

conditions

 

are

 

the

result

 

of

 

a

 

tight

 

interaction

 

between

 

the

 

genotype,

 

the

 

environment

and

 

the

 

local

 

farming

 

practice

 

(i.e.,

 

FS

 

in

 

the

 

G

 

×

 

E

 

×

 

M

 

model).

2.1.2.

 

Local

 

reference

 

yields

Although

 

it

 

may

 

be

 

hard

 

to

 

estimate

 

the

 

achievable

 

yields

 

of

local

 

varieties

 

under

 

local

 

circumstances

 

and

 

management

 

prac-

tices,

 

approximations

 

are

 

necessary

 

in

 

order

 

to

 

quantify

 

current

yield

 

gaps.

 

An

 

example

 

is

 

the

 

use

 

of

 

boundary-line

 

analysis

 

(e.g.,

Shatar

 

and

 

McBratney,

 

2004

)

 

of

 

large

 

yield

 

datasets

 

across

 

sites,

seasons

 

and

 

management

 

practices.

 

Boundary

 

lines

 

may

 

reveal

 

ceil-

ing

 

yields

 

for

 

a

 

given

 

crop

 

in

 

a

 

certain

 

environment.

 

Ceiling

 

yields

may

 

sometimes

 

represent

 

the

 

maximum

 

achievable

 

yields

 

under

farmer

 

management,

 

or

 

locally

 

attainable

 

yield

 

Y

L

,

 

or

 

be

 

close

 

to

the

 

water-limited

 

yield

 

potential

 

Y

W

when

 

yields

 

are

 

measured

under

 

controlled

 

conditions.

 

An

 

alternative

 

is

 

to

 

use

 

simulation

models

 

to

 

establish

 

the

 

reference

 

yield

 

Y

W

,

 

or

 

an

 

approxima-

tion

 

to

 

the

 

locally

 

attainable

 

(water

 

and

 

nutrient-limited)

 

yield

 

Y

L

when

 

proper

 

model

 

calibration

 

and

 

validation

 

are

 

possible

 

(e.g.,

Affholder

 

et

 

al.,

 

2013

).

 

Such

 

an

 

exercise

 

is

 

illustrated

 

in

 

Fig.

 

3

A

 

for

Page 4

Figures and page graphics, page 4

P.

 

Tittonell,

 

K.E.

 

Giller

 

/

 

Field

 

Crops

 

Research

 

143

 

(2013)

 

76–90

 

79

Fig.

 

3.

 

(A)

 

On-farm

 

maize

 

biomass

 

yields

 

in

 

farmers’

 

fields

 

(current

 

practice)

 

and

in

 

researcher-managed

 

micro-plots

 

established

 

on

 

the

 

same

 

fields

 

with

 

or

 

without

mineral

 

fertilisers

 

(NPK,

 

control),

 

and

 

yields

 

simulated

 

for

 

each

 

field

 

with

 

the

 

model

DYNBAL

 

(

Tittonell

 

et

 

al.,

 

2006

);

 

(B)

 

means

 

and

 

standard

 

deviations

 

in

 

each

 

case

(first

 

column

 

from

 

the

 

left

 

is

 

average

 

simulated

 

yields);

 

(C)

 

comparing

 

average

 

grain

yields

 

on-farm

 

(current

 

practice

 

and

 

researcher-managed)

 

against

 

yields

 

obtained

 

in

nearby

 

experimental

 

stations

 

(control,

 

NPK),

 

with

 

the

 

observations

 

grouped

 

accord-

ing

 

to

 

proximity

 

to

 

two

 

stations

 

located

 

in

 

lower

 

and

 

higher

 

potential

 

agro-ecological

zones

 

(AEZ)

 

in

 

western

 

Kenya.

maize

 

(

Zea

 

mays

 

L.)

 

grown

 

in

 

the

 

highlands

 

of

 

Kenya,

 

using

 

above-

ground

 

biomass

 

as

 

a

 

measure

 

of

 

productivity

 

(harvest

 

indices

 

were

highly

 

variable

 

under

 

farmer

 

management).

 

Simulated

 

water

 

and

nutrient-limited

 

biomass

 

yields

 

(corresponding

 

to

 

Y

L

)

 

are

 

plotted

against

 

soil

 

organic

 

carbon

 

together

 

with

 

biomass

 

yields

 

measured

on

 

farmers’

 

fields

 

under

 

their

 

own

 

management

 

(current

 

practice)

and

 

under

 

researcher

 

management

 

with

 

(NPK)

 

or

 

without

 

(control)

fertilisers.

 

Soil

 

C

 

(0–20

 

cm)

 

is

 

used

 

here

 

as

 

a

 

surrogate

 

of

 

inherent

and

 

current

 

soil

 

fertility,

 

with

 

soil

 

clay

 

contents

 

varying

 

from

 

18

to

 

44%,

 

altitude

 

from

 

1100

 

to

 

2100

 

masl

 

and

 

rainfall

 

from

 

1300

 

to

1900

 

mm

 

in

 

the

 

study

 

area.

Across

 

this

 

environmental

 

range,

 

the

 

simulated

 

attainable

biomass

 

yields

 

varied

 

from

 

ca.

 

5

 

to

 

20

 

t

 

ha

−

1

(15.5

 

on

 

average),

 

and

the

 

respective

 

gaps

 

between

 

2

 

and

 

15

 

t

 

ha

−

1

under

 

farmer

 

prac-

tices,

 

between

 

0

 

and

 

14

 

in

 

control

 

plots,

 

and

 

between

 

0

 

and

 

8

 

t

 

ha

−

1

with

 

a

 

full

 

NPK

 

fertiliser

 

application.

 

The

 

average

 

response

 

to

 

a

full

 

NPK

 

fertilisation

 

was

 

in

 

the

 

order

 

of

 

5.3

 

t

 

ha

−

1

of

 

aboveground

biomass.

 

It

 

is

 

striking

 

that

 

researcher-managed

 

plots

 

receiving

 

no

fertilisers

 

yielded

 

on

 

average

 

better

 

than

 

the

 

same

 

fields

 

under

farmer

 

management,

 

which

 

may

 

include

 

using

 

organic

 

and/or

mineral

 

fertilisers.

 

The

 

effect

 

of

 

germplasm

 

was

 

more

 

difficult

to

 

unravel,

 

given

 

that

 

the

 

hybrid

 

used

 

under

 

research

 

manage-

ment

 

was

 

also

 

often

 

seen

 

in

 

farmers’

 

fields.

 

When

 

examining

grain

 

yields

 

(

Fig.

 

3

C),

 

such

 

differences

 

were

 

wider

 

for

 

the

 

fields

grouped

 

in

 

the

 

lower

 

potential

 

zone

 

(dominated

 

by

 

ferric-Acrisols,

1300–1500

 

mm)

 

than

 

in

 

the

 

higher

 

potential

 

zone

 

(Nitosols

 

and

humic-Ferralsols,

 

1500–1900

 

mm).

 

Yields

 

under

 

controlled

 

man-

agement

 

with

 

fertiliser

 

were

 

greater

 

on

 

nearby

 

experimental

stations

 

than

 

in

 

farmer’s

 

fields

 

(although

 

not

 

during

 

the

 

same

 

sea-

son),

 

and

 

such

 

difference

 

was

 

also

 

wider

 

in

 

the

 

high

 

potential

 

zone.

The

 

potential

 

yields

 

simulated

 

with

 

the

 

soil-crop

 

model

 

DYNBAL

(

Tittonell

 

et

 

al.,

 

2006,

 

2007b

)

 

in

 

response

 

to

 

water

 

and

 

nutrient

availability

 

varied

 

between

 

10.8

 

and

 

11.4

 

t

 

ha

−

1

grain

 

(22.6

 

and

24.5

 

t

 

ha

−

1

aboveground

 

biomass)

 

for

 

this

 

environmental

 

range

(

Fig.

 

3

),

 

cutting

 

through

 

one

 

of

 

the

 

areas

 

of

 

highest

 

agricultural

potential

 

in

 

sub-Saharan

 

Africa.

2.1.3.

 

Non-cereal

 

crops

Although

 

the

 

analysis

 

of

 

Cassman

 

(1999)

 

focuses

 

on

 

the

 

yield

potential

 

of

 

major

 

cereal

 

crops,

 

the

 

economy

 

of

 

large

 

areas

 

of

 

sub-

Saharan

 

Africa

 

depends

 

also

 

on

 

other,

 

equally

 

important

 

staple

 

or

cash

 

crops.

 

Yield

 

gaps

 

for

 

cassava

 

(

Manihot

 

esculenta

 

Crantz)

 

grown

in

 

vast

 

areas

 

of

 

medium

 

to

 

marginal

 

agro-ecological

 

potential

 

may

also

 

be

 

analysed

 

with

 

respect

 

to

 

management

 

practices

 

or

 

single

limiting

 

factors,

 

and

 

reference

 

ceiling

 

(rather

 

than

 

potential)

 

yields

be

 

derived

 

through

 

boundary

 

line

 

analysis

 

(

Fig.

 

4

A).

 

Maximum

 

fresh

root

 

yields

 

obtained

 

on

 

eastern

 

Uganda

 

farms

 

were

 

in

 

the

 

order

 

of

25

 

t

 

ha

−

1

,

 

while

 

yields

 

of

 

50–60

 

t

 

ha

−

1

have

 

been

 

obtained

 

under

experimental

 

conditions

 

in

 

East

 

Africa

 

(

Ntawuruhunga

 

et

 

al.,

 

2006

)

and

 

as

 

high

 

as

 

75–90

 

t

 

ha

−

1

in

 

Colombia

 

or

 

India

 

(

El-Sharkawy,

2004

).

 

Fermont

 

et

 

al.

 

(2009)

 

analysed

 

the

 

yield

 

gap

 

of

 

cassava

 

in

 

the

East

 

African

 

highlands

 

and

 

determined

 

the

 

individual

 

yield

 

gains

and

 

synergies

 

that

 

may

 

be

 

expected

 

from

 

improved

 

agronomy,

cultivar

 

choice

 

or

 

fertiliser

 

use.

 

Although

 

it

 

is

 

generally

 

believed

that

 

cassava

 

responds

 

poorly

 

to

 

fertilisers,

 

this

 

research

 

showed

once

 

again

 

that

 

responses

 

were

 

substantial

 

when

 

proper

 

agronomic

(establishment

 

and

 

weeding)

 

practices

 

were

 

in

 

place.

 

The

 

incre-

mental

 

contribution

 

of

 

these

 

different

 

factors

 

to

 

narrowing

 

the

 

yield

gap

 

on

 

farmers’

 

fields

 

was

 

1.5

 

t

 

ha

−

1

for

 

improved

 

crop

 

implanta-

tion

 

(from

 

an

 

average

 

yield

 

of

 

fresh

 

cassava

 

roots

 

8.6

 

to

 

10.1

 

t

 

ha

−

1

),

3.5

 

t

 

ha

−

1

for

 

improved

 

cultivar

 

choice

 

(from

 

10.1

 

to

 

13.6

 

t

 

ha

−

1

)

and

 

7.2

 

t

 

ha

−

1

with

 

fertiliser

 

use

 

(from

 

13.6

 

to

 

20.8

 

t

 

ha

−

1

).

 

The

choice

 

of

 

cultivars

 

with

 

resistance

 

to

 

cassava

 

mosaic

 

virus

 

was

crucial.

For

 

an

 

indeterminate

 

crop

 

such

 

as

 

cotton

 

(

Gossypium

 

hirsutum

L.),

 

the

 

engine

 

of

 

rural

 

economies

 

across

 

regions

 

of

 

West,

 

Central

and

 

Southern

 

Africa,

 

the

 

relationships

 

between

 

single

 

limiting

 

fac-

tors

 

and

 

yield

 

are

 

more

 

elusive.

 

Examining

 

data

 

from

 

a

 

number

 

of

research

 

trials

 

established

 

across

 

the

 

cotton

 

growing

 

area

 

of

 

south-

ern

 

Mali,

 

Cretenet

 

(1994)

 

arrived

 

at

 

establishing

 

yield

 

thresholds

with

 

respect

 

to

 

soil

 

indicators

 

such

 

as

 

exchangeable

 

K

 

(

Fig.

 

4

B)

 

or

organic

 

C

 

contents,

 

to

 

rainfall

 

or

 

to

 

sowing

 

dates

 

using

 

a

 

similar

boundary-line

 

approach.

 

Cotton

 

has

 

a

 

relatively

 

strong

 

K

 

demand.

A

 

negative

 

K

 

balance

 

of

 

200

 

kg

 

ha

−

1

over

 

a

 

certain

 

period

 

of

 

time,

which

 

corresponds

 

to

 

a

 

change

 

in

 

0.025

 

cmol

(+)

kg

−

1

of

 

K

 

in

 

the

 

first

40

 

cm

 

of

 

the

 

soil,

 

results

 

in

 

a

 

reduction

 

of

 

up

 

to

 

570

 

kg

 

ha

−

1

in

 

the

attainable

 

seed-cotton

 

yield.

 

Each

 

day

 

of

 

delay

 

in

 

the

 

date

 

of

 

plant-

ing,

 

or

 

each

 

day

 

of

 

reduction

 

in

 

the

 

rainy

 

period

 

led

 

to

 

an

 

average

reduction

 

of

 

16

 

kg

 

ha

−

1

in

 

the

 

attainable

 

seed

 

cotton

 

yield,

 

irrespec-

tive

 

of

 

fertiliser

 

use.

 

More

 

difficult

 

to

 

predict

 

in

 

the

 

case

 

of

 

cotton

is

 

the

 

potential

 

quality

 

of

 

the

 

fibre

 

obtained,

 

which

 

has

 

a

 

strong

impact

 

on

 

the

 

price

 

received

 

by

 

the

 

farmer.

The

 

examples

 

above

 

illustrate

 

the

 

use

 

of

 

boundary

 

line

 

analy-

sis

 

to

 

study

 

the

 

effect

 

of

 

single

 

abiotic,

 

yield-limiting

 

factors

 

such

as

 

water,

 

nutrients

 

or

 

dates

 

of

 

planting.

 

Similarly,

 

the

 

method

 

can

be

 

used

 

to

 

study

 

the

 

effect

 

of

 

biotic

 

yield-reducing

 

factors

 

such

as

 

weeds,

 

pest

 

and

 

diseases.

 

The

 

East

 

African

 

highland

 

banana

(

Musa

 

spp.,

 

AAA-EA

 

genome)

 

is

 

a

 

staple

 

crop

 

in

 

large

 

areas

 

of

Burundi,

 

the

 

Democratic

 

Republic

 

of

 

Congo,

 

Rwanda

 

and

 

Uganda.

In

 

a

 

detailed

 

investigation

 

on

 

plots

 

on

 

159

 

smallholder

 

farms

in

 

Uganda,

 

yields

 

of

 

highland

 

banana

 

were

 

significantly

 

greater

Page 5

Figures and page graphics, page 5

80

 

P.

 

Tittonell,

 

K.E.

 

Giller

 

/

 

Field

 

Crops

 

Research

 

143

 

(2013)

 

76–90

0

5

10

15

20

25

30

0.0

 

0.3

 

0.6

 

0.9

 

1.2

 

1.5

 

1.8

 

2.1

C

a

ssava r

oot

 yi

el

d (

t ha

-1

)

On-farm observations

Boundary-line model

0.0

0.6

1.2

1.8

2.4

3.0

3.6

0.0

 

0.1

 

0.2

 

0.3

 

0.4

 

0.5

S

e

ed-

cot

ton yi

el

d (

t ha

-1

)

On-station observations

Boundary-line model

Source: Crétenet (1994)

A

 

B

Banana bunch yield (t ha

-1

)

Nematode root necrosis (%) 

 

Weevils corm damage (%) 

Weed pressure index (%) 

C D E 

Source: Fermont et al. (2009) 

Total soil  N (g kg

-1

 

)  

Exchangeable K (cmol

(+)

 kg

-1

) 

40

20

0

40

20

 

0

40

20

 

0

Source: Wairegi et al. (2010) 

0

 

2.5

 

5

 

7.5

10

 

0

15

30

45

 

0

 

5

10

15

20

Fig.

 

4.

 

Examples

 

of

 

using

 

boundary

 

line

 

analysis

 

to

 

establish

 

ceiling,

 

or

 

locally

 

attainable

 

yields

 

as

 

a

 

function

 

of

 

different

 

explanatory

 

variables.

 

(A)

 

Cassava

 

yield

 

in

 

Uganda

and

 

Kenya

 

against

 

total

 

soil

 

N;

 

(B)

 

Cotton

 

yield

 

in

 

Mali

 

against

 

soil

 

exchangeable

 

K;

 

(C–E)

 

Highland

 

banana

 

yield

 

against

 

different

 

biotic

 

constraints.

 

Boundary

 

line

 

models

fitted

 

to

 

the

 

maxima

 

at

 

each

 

level

 

of

 

the

 

independent

 

variable

 

are

 

represented

 

by

 

(continuous

 

or

 

dashed)

 

lines.

in

 

the

 

Southwest

 

region

 

(20

 

t

 

ha

−

1

year

−

1

)

 

than

 

in

 

the

 

Central

(12

 

t

 

ha

−

1

year

−

1

)

 

and

 

South

 

(10

 

t

 

ha

−

1

year

−

1

)

 

(

Wairegi

 

et

 

al.,

 

2010

)

whereas

 

the

 

estimated

 

national

 

average

 

yield

 

in

 

2007

 

was

 

only

5.5

 

t

 

ha

−

1

year

−

1

(FAOSTAT).

 

On

 

the

 

same

 

farms

 

demonstration

plots

 

yielded

 

3

 

to

 

10

 

t

 

ha

−

1

year

−

1

more

 

when

 

(on

 

average)

 

71

 

N,

 

8

 

P

and

 

32

 

K

 

kg

 

ha

−

1

year

−

1

was

 

applied

 

(

Wairegi

 

et

 

al.,

 

2010

).

 

Using

 

the

boundary

 

line

 

approach

 

(

Fig.

 

4

C–E)

 

they

 

found

 

that

 

the

 

yield

 

gap

expressed

 

as

 

percentage

 

of

 

attainable

 

yield

 

in

 

the

 

Central

 

region

was

 

caused

 

by

 

pests

 

(nematodes

 

10%

 

loss,

 

weevils

 

6%)

 

and

 

subop-

timal

 

crop

 

management

 

(mulch

 

25%)

 

indicating

 

that

 

past

 

research

efforts

 

were

 

mistaken

 

in

 

neglecting

 

abiotic

 

constraints.

2.2.

 

Soil

 

quality

The

 

second

 

pillar

 

of

 

ecological

 

intensification

 

proposed

 

by

Cassman

 

(1999)

 

was

 

the

 

maintenance

 

or

 

improvement

 

of

 

soil

quality,

 

defined

 

as

 

the

 

capacity

 

of

 

soils

 

to

 

sustain

 

biological

 

pro-

ductivity

 

while

 

ensuring

 

environmental,

 

plant

 

and

 

animal

 

health.

Both

 

severe

 

and

 

subtle

 

forms

 

of

 

soil

 

degradation

 

are

 

associated

worldwide

 

with

 

the

 

practice

 

of

 

agriculture,

 

even

 

under

 

favourable

production

 

environments.

 

Four

 

soil

 

degradation

 

phenomena

 

may

be

 

distinguished:

 

water

 

erosion,

 

wind

 

erosion,

 

deterioration

 

of

physical

 

properties,

 

and

 

chemical

 

degradation.

 

The

 

latter

 

includes

nutrient

 

depletion

 

and

 

loss

 

of

 

organic

 

matter,

 

salinisation,

 

acidifica-

tion,

 

and

 

chemical

 

pollution.

 

The

 

relationship

 

between

 

poverty

 

and

land

 

degradation

 

has

 

been

 

highlighted

 

for

 

sub-Saharan

 

Africa

 

(e.g.,

Scherr,

 

2000;

 

Sanchez,

 

2002

),

 

and

 

many

 

of

 

the

 

forms

 

of

 

degrada-

tion

 

listed

 

take

 

place

 

simultaneously

 

in

 

the

 

continent.

 

Rather

 

than

cataloguing

 

the

 

extent

 

of

 

land

 

degradation,

 

as

 

recently

 

done

 

(cf.

Vlek

 

et

 

al.,

 

2008

),

 

we

 

focus

 

on

 

the

 

particularities

 

of

 

the

 

degradation

processes

 

taking

 

place

 

in

 

sub-Saharan

 

Africa,

 

and

 

on

 

their

 

implica-

tions

 

for

 

the

 

design

 

of

 

strategies

 

to

 

rehabilitate

 

degraded

 

land.

 

Soil

nutrient

 

depletion

 

and

 

loss

 

of

 

organic

 

matter

 

are

 

treated

 

as

 

inte-

grative

 

measures

 

of

 

land

 

degradation,

 

which

 

reflect

 

the

 

combined

effect

 

of

 

management

 

practices,

 

inherent

 

soil

 

fertility

 

and

 

other

forms

 

of

 

degradation.

Two

 

decades

 

ago

 

Stoorvogel

 

and

 

Smaling

 

(1990)

 

published

alarming

 

figures

 

on

 

negative

 

nutrient

 

balances

 

at

 

country

 

level

 

for

sub-Saharan

 

Africa.

 

Since

 

then,

 

nutrient

 

balances

 

calculated

 

in

 

dif-

ferent

 

ways

 

have

 

been

 

used

 

extensively

 

as

 

indicators

 

of

 

soil

 

nutrient

depletion

 

and

 

of

 

the

 

long-term

 

sustainability

 

of

 

agricultural

 

sys-

tems

 

at

 

scales

 

ranging

 

from

 

the

 

individual

 

field

 

plot

 

to

 

entire

regions

 

or

 

countries

 

(e.g.,

 

Smaling

 

et

 

al.,

 

1993;

 

Stoorvogel

 

et

 

al.,

1993

).

 

Nutrient

 

balances

 

calculated

 

at

 

regional

 

and/or

 

national

scales

 

provide

 

coarse

 

but

 

relevant

 

information

 

for

 

policy

 

mak-

ers.

 

For

 

example,

 

it

 

was

 

estimated

 

that,

 

every

 

day,

 

up

 

to

 

100

trucks

 

with

 

a

 

payload

 

of

 

6

 

tonnes

 

of

 

cooking

 

bananas

 

enter

 

the

capital

 

city

 

of

 

Uganda,

 

Kampala,

 

representing

 

an

 

annual

 

export

from

 

rural

 

areas

 

of

 

over

 

1.5

 

million

 

kg

 

K

 

and

 

0.5

 

million

 

kg

 

N

 

(

van

Asten

 

et

 

al.,

 

2004

).

 

However,

 

less

 

than

 

5%

 

of

 

banana

 

farmers

 

in

Uganda

 

use

 

any

 

type

 

of

 

mineral

 

fertiliser

 

(

Bekunda

 

and

 

Woomer,

1996

).

 

Estimations

 

of

 

nutrient

 

balances

 

at

 

field

 

scale,

 

by

 

differ-

ent

 

authors

 

and

 

through

 

slightly

 

different

 

methods

 

show

 

almost

always

 

negative

 

values

 

in

 

different

 

African

 

farming

 

systems.

 

For

continuous

 

cereal

 

cropping

 

in

 

the

 

central

 

highlands

 

of

 

Kenya,

 

De

Jager

 

et

 

al.

 

(2001)

 

calculated

 

nitrogen

 

balances

 

as

 

negative

 

as

 

−

44

to

 

−

75

 

kg

 

N

 

ha

−

1

year

−

1

,

 

clearly

 

contrasting

 

with

 

the

 

values

 

pre-

sented

 

for

 

other

 

African

 

systems

 

that

 

were

 

calculated

 

using

 

the

same

 

method

 

(cf.

 

Table

 

1

).

 

One

 

of

 

the

 

weakest

 

points

 

in

 

the

 

calcula-

tion

 

of

 

nutrient

 

balances

 

is

 

the

 

estimation

 

of

 

flows

 

that

 

are

 

difficult

Page 6

Figures and page graphics, page 6

P.

 

Tittonell,

 

K.E.

 

Giller

 

/

 

Field

 

Crops

 

Research

 

143

 

(2013)

 

76–90

 

81

Table

 

1

N

 

balances

 

(kg

 

ha

−

1

season

−

1

)

 

at

 

field

 

scale

 

across

 

African

 

farming

 

systems

 

calculated

 

using

 

comparable

 

methods

 

and

 

assumptions.

a

Inputs

 

and

 

outputs

 

consider

 

only

 

those

 

mediated

 

by

 

farmers

 

(e.g.,

 

fertilisers,

 

harvest

 

of

 

crop

residue,

 

etc).

Case

 

study

 

Farming

 

system

 

Variability

 

component

 

Total

 

N

inputs

N

 

removal

in

 

harvest

N

 

balance

 

Calculation

 

procedure

 

Source

Central

 

Zimbabwe

Integrated

 

cereal-livestock

systems,

 

free

 

grazing

Best

 

plots

 

26

 

24

 

−

38

Complete

 

balance

 

using

 

NUTMON

 

Zingore

 

et

 

al.

 

(2007)

Average

 

plots

 

22

 

18

 

−

34

Worst

 

plots

 

5

 

11

 

−

31

Western

 

Kenya

Integrated

 

cereal-livestock

systems,

 

zero

 

grazing

Home

 

gardens

 

28

 

28

 

+21

Complete

 

balance

 

using

 

dynamic

simulation

Tittonell

 

et

 

al.

 

(2005b)

Close

 

fields

43

 

36

 

−

22

Mid-distance

 

fields

11

 

25

 

−

17

Remote

 

fields

4

 

12

 

−

24

Eastern

 

Uganda

 

Cereal-based

 

farming

 

systems

 

(Averaged

 

for

 

a

 

representative

 

farm)

 

86

 

138

 

−

48

 

Complete

 

balance

 

using

 

static

 

model

 

Nkonya

 

et

 

al.

 

(2005)

Northwest

 

Tanzania

Banana-based

 

farming

 

systems

Kibanja

 

(banana)

 

18

 

26

 

−

8

Partial

 

balance

 

using

 

NUTMON

 

Baijukya

 

et

 

al.

 

(2005)

Kikamba-maize

 

4

 

13

 

−

9

Kikamba-S.

 

potato

 

1

 

6

 

−

5

Kikamba-Cassava

 

0

 

2

 

−

2

Northern

 

Ghana

Cereal-based

 

farming

 

systems

Mucuna/maize

 

72.4

 

+26

Complete

 

balance

 

using

 

a

 

modified

NUTMON

Anthofer

 

and

 

Kroschel

 

(2002)

Sole

 

maize

 

(burning)

 

0

 

118

 

−

120

Southern

 

Mali

 

Cereal/cotton/pastoral

 

systems

Village

 

settlings

 

58

 

45

 

−

15

Complete

 

balance

 

using

 

NUTMON

 

Ramisch,

 

2005

Hamlet

 

settlings

81

 

47

 

−

3

Fulawere

 

settlings

 

128

 

41

 

+21

a

When

 

results

 

were

 

presented

 

for

 

farms

 

of

 

different

 

wealth

 

classes,

 

only

 

the

 

middle

 

class

 

farms

 

were

 

considered.

Page 7

Figures and page graphics, page 7

82

 

P.

 

Tittonell,

 

K.E.

 

Giller

 

/

 

Field

 

Crops

 

Research

 

143

 

(2013)

 

76–90

to

 

measure,

 

such

 

as

 

losses

 

by

 

leaching

 

or

 

erosion,

 

or

 

the

 

flows

 

gener-

ated

 

by

 

denitrification,

 

wet/dry

 

deposition

 

and

 

N

2

-fixation

 

(

Faerge

and

 

Magid,

 

2004

).

 

For

 

instance,

 

N

 

losses

 

by

 

leaching

 

assumed

by

 

different

 

authors

 

in

 

African

 

conditions

 

were

 

widely

 

variable:

8–15

 

kg

 

N

 

ha

−

1

year

−

1

(

Grimme

 

and

 

Juo,

 

1985

),

 

10

 

kg

 

N

 

ha

−

1

year

−

1

(

Akonde

 

et

 

al.,

 

1997

),

 

11–26

 

kg

 

ha

−

1

year

−

1

(

Ramisch,

 

2005

)

 

or

36–153

 

kg

 

N

 

ha

−

1

year

−

1

(

Poss

 

and

 

Saragoni,

 

1992

).

 

Estimations

remain

 

uncertain,

 

and

 

may

 

often

 

lack

 

quantitative

 

rigour

 

(

Faerge

and

 

Magid,

 

2004

).

 

Nonetheless,

 

the

 

work

 

of

 

Stoorvogel

 

and

 

Smaling

(1990)

 

was

 

highly

 

influential

 

in

 

bringing

 

attention

 

to

 

the

 

problem

and

 

in

 

prioritising

 

research

 

agendas

 

on

 

soil

 

fertility

 

management.

Fortunately

 

the

 

nutrient

 

balances

 

they

 

predicted

 

were

 

not

 

always

realised,

 

for

 

if

 

they

 

were,

 

agriculture

 

would

 

by

 

now

 

have

 

disap-

peared

 

from

 

one

 

third

 

of

 

the

 

continent.

Soil

 

fertility

 

zoning

 

is

 

a

 

well-known

 

process

 

in

 

the

 

savannah-

derived

 

agroecosystems

 

of

 

West

 

Africa,

 

in

 

which

 

nutrients

 

tend

 

to

be

 

concentrated

 

in

 

the

 

village

 

fields

 

to

 

the

 

detriment

 

of

 

the

 

fertility

of

 

the

 

so-called

 

bush

 

fields

 

(e.g.,

 

Prudencio,

 

1993

).

 

Tittonell

 

et

 

al.

(2005a,b)

 

found

 

a

 

similar

 

relationship

 

between

 

the

 

magnitude

 

and

sign

 

of

 

nutrient

 

balances,

 

as

 

determined

 

by

 

management

 

decisions,

and

 

the

 

creation

 

of

 

patterns

 

of

 

spatial

 

soil

 

heterogeneity

 

within

 

indi-

vidual

 

farms

 

in

 

the

 

highly

 

fragmented

 

landscapes

 

of

 

western

 

Kenya.

Large

 

differences

 

in

 

input

 

use

 

(e.g.,

 

0.7–104

 

kg

 

N

 

ha

−

1

year

−

1

),

 

food

production

 

(e.g.,

 

0.6–2.9

 

t

 

DM

 

ha

−

1

year

−

1

),

 

partial

 

C

 

(e.g.,

 

−

570

to

 

1480

 

kg

 

ha

−

1

year

−

1

)

 

and

 

N

 

(e.g.,

 

−

92

 

to

 

57

 

ha

−

1

year

−

1

)

 

bal-

ances

 

were

 

observed

 

between

 

home-

 

and

 

outfields

 

located

 

less

than

 

50–100

 

m

 

apart,

 

which

 

showed

 

also

 

wide

 

differences

 

in

extractable

 

P

 

(e.g.,

 

2.1–19.8

 

mg

 

kg

−

1

)

 

and

 

exchangeable

 

K

 

(e.g.,

0.14–0.54

 

cmol

(+)

kg

−

1

)

 

contents

 

in

 

their

 

soils.

 

Differential

 

manage-

ment

 

of

 

the

 

various

 

fields

 

of

 

the

 

farm

 

led

 

to

 

the

 

establishment

 

of

gradients

 

of

 

soil

 

fertility,

 

notably

 

decreasing

 

with

 

distance

 

from

the

 

homestead.

 

Farmers

 

tended

 

to

 

allocate

 

their

 

scarce

 

nutrient

and

 

labour

 

resources

 

in

 

the

 

fields

 

they

 

perceived

 

as

 

most

 

fertile

or

 

less

 

risky,

 

or

 

in

 

fields

 

around

 

the

 

homestead

 

where

 

high

 

value

crops

 

were

 

better

 

protected

 

from

 

marauding

 

livestock

 

or

 

theft.

 

A

close

 

interaction

 

was

 

also

 

found

 

between

 

soil

 

fertility

 

gradients

and

 

topography

 

in

 

these

 

highly

 

dissected

 

landscapes,

 

with

 

home-

steads

 

located

 

on

 

the

 

upper

 

positions

 

of

 

the

 

slope.

 

Such

 

interactions

between

 

inherent

 

soil-landscape

 

variability,

 

historical

 

and

 

current

management,

 

nutrient

 

balances

 

and

 

current

 

soil

 

fertility

 

were

 

later

documented

 

for

 

smallholder

 

systems

 

in

 

different

 

parts

 

of

 

Africa;

e.g.,

 

in

 

Zimbabwe

 

(

Zingore

 

et

 

al.,

 

2007

),

 

Ghana

 

(

Adjei-Nsiah,

 

2006

)

and

 

Uganda

 

(

Ebanyat,

 

2009

).

Losses

 

of

 

organic

 

matter

 

from

 

agricultural

 

soils

 

are

 

the

 

result

of

 

the

 

imbalance

 

between

 

inputs

 

as

 

plant

 

litter

 

or

 

animal

 

manure

and

 

outputs

 

through

 

decomposition

 

and

 

soil

 

erosion.

 

This

 

balance

is

 

regulated

 

by

 

environmental

 

conditions,

 

soil

 

type,

 

litter

 

quality

and

 

management

 

practices.

 

Vegetation

 

clearance

 

for

 

cultivation,

 

as

practiced

 

in

 

the

 

African

 

savannahs

 

triggers

 

positive

 

feedback

 

loops

–

 

or

 

vicious

 

cycles

 

–

 

characterised

 

by

 

the

 

disturbance

 

of

 

soil

 

physi-

cal

 

properties,

 

increased

 

erosion,

 

accelerated

 

decomposition

 

rates

and

 

gradually

 

decreasing

 

C

 

inputs

 

to

 

the

 

soil

 

in

 

the

 

form

 

of

 

crop

residues

 

due

 

to

 

declining

 

crop

 

yields

 

(e.g.,

 

Kintché

 

et

 

al.,

 

2010

).

Such

 

process

 

may

 

be

 

counterbalanced

 

by

 

application

 

of

 

organic

 

fer-

tilisers

 

such

 

as

 

animal

 

manures,

 

or

 

further

 

aggravated

 

when

 

crop

residues

 

are

 

removed

 

from

 

the

 

fields

 

or

 

grazed

 

by

 

livestock.

 

The

magnitude

 

of

 

soil

 

carbon

 

losses

 

would

 

vary

 

for

 

different

 

soil

 

types

and

 

environments,

 

and

 

be

 

affected

 

by

 

the

 

characteristics

 

of

 

the

local

 

farming

 

(or

 

natural

 

resource

 

management)

 

system.

 

Abrupt

productivity

 

losses

 

(a

 

fast

 

responding

 

variable)

 

take

 

place

 

during

the

 

first

 

5–10

 

years

 

after

 

woodland

 

clearance,

 

especially

 

on

 

sandy

soils

 

or

 

under

 

intensive

 

double-cropping

 

in

 

areas

 

with

 

a

 

bimodal

rainfall

 

regime

 

(

Fig.

 

5

).

 

During

 

the

 

first

 

decade

 

of

 

maize

 

cultivation

in

 

Gagnoa,

 

Ivory

 

Coast

 

maize

 

yields

 

decreased

 

to

 

about

 

one

 

fifth

of

 

their

 

initial

 

level

 

when

 

no

 

nutrient

 

input

 

was

 

applied,

 

but

 

yields

could

 

be

 

sustained

 

with

 

application

 

of

 

large

 

amounts

 

of

 

mineral

 

and

0

1

2

3

4

5

6

7

1970

197

 

2

197

 

4

197

 

6

197

 

8

198

 

0

Maize yield 

(t 

ha

-1

)

4

6

8

10

12

1970

197

 

2

197

 

4

197

 

6

197

 

8

198

 

0

Soil organic 

C (g kg

-1

)

Control

Comp

 

ost

Miner

 

al fertilisers

Comp

 

ost

 

 + 

 

Fertilis

 

ers

Source: Guibert

 

 (1

 

999)

A

B

Fig.

 

5.

 

Results

 

of

 

the

 

first

 

10

 

years

 

of

 

a

 

long-term

 

trial

 

conducted

 

in

 

Gagnoa,

 

Ivory

Coast

 

illustrating

 

how

 

yield

 

gaps

 

increase

 

in

 

time

 

(years

 

of

 

cultivation)

 

due

 

to

 

soil

fertility

 

depletion

 

when

 

no

 

nutrient

 

inputs

 

are

 

used

 

(control).

 

(A)

 

Maize

 

grain

 

yields;

(B)

 

soil

 

organic

 

carbon.

Source:

 

Guibert

 

(1999)

.

organic

 

fertilisers,

 

or

 

both

 

combined

 

(

Guibert,

 

1999

).

 

Soil

 

organic

carbon

 

(a

 

slow

 

variable)

 

decreased

 

in

 

about

 

20%

 

over

 

the

 

same

period

 

in

 

soils

 

that

 

did

 

not

 

receive

 

organic

 

amendments.

 

These

results

 

and

 

similar

 

ones

 

from

 

long-term

 

experiments

 

in

 

West

 

Africa

indicate

 

that

 

the

 

magnitude

 

of

 

the

 

yield

 

gap

 

increases

 

substantially

after

 

the

 

first

 

five

 

years

 

of

 

cultivation

 

of

 

soils

 

cleared

 

from

 

savannah

vegetation.

Rehabilitating

 

soils

 

that

 

have

 

become

 

degraded

 

often

 

requires

substantial

 

investment.

 

The

 

amounts

 

of

 

manure

 

necessary

 

to

restore

 

productivity

 

of

 

degraded

 

outfields

 

on

 

the

 

granitic

 

sandy

soils

 

of

 

Zimbabwe

 

were

 

as

 

much

 

as

 

17

 

t

 

ha

−

1

year

−

1

,

 

complemented

with

 

100

 

kg

 

ha

−

1

year

−

1

of

 

N

 

as

 

mineral

 

fertiliser

 

(

Zingore

 

et

 

al.,

2007

).

 

Earlier

 

calculations

 

indicated

 

that

 

an

 

equivalent

 

of

 

30

 

ha

of

 

grazing

 

land

 

would

 

be

 

necessary

 

to

 

sustain

 

productivity

 

in

 

one

hectare

 

of

 

cropping

 

land

 

on

 

these

 

soils

 

through

 

annual

 

application

of

 

8

 

t

 

ha

−

1

of

 

manure

 

(

Rodel

 

and

 

Hopley,

 

1973

).

 

Analysis

 

at

 

village

scale

 

indicated

 

that

 

only

 

one

 

third

 

of

 

the

 

village

 

cropland

 

could

be

 

covered

 

with

 

the

 

manure

 

produced

 

with

 

its

 

livestock

 

popula-

tion,

 

in

 

equilibrium

 

with

 

the

 

carrying

 

capacity

 

of

 

local

 

grasslands

(

Zingore

 

et

 

al.,

 

2011

).

 

A

 

quick

 

glance

 

at

 

livestock

 

population

 

densi-

ties

 

in

 

Africa

 

shows

 

that

 

sustaining

 

soil

 

fertility

 

exclusively

 

through

manure

 

applications

 

is

 

not

 

a

 

viable

 

option

 

in

 

most

 

places

 

(

Fig.

 

6

).

Cattle

 

(as

 

much

 

as

 

human

 

population)

 

densities

 

are

 

greatest

 

in

the

 

highland

 

regions,

 

where

 

soils

 

are

 

inherently

 

more

 

fertile

 

and

agriculture

 

most

 

intensive.

 

Although

 

crop

 

productivity

 

may

 

be

 

sus-

tained

 

through

 

use

 

of

 

mineral

 

fertilisers

 

coupled

 

with

 

restitution

 

of

crop

 

residues,

 

this

 

does

 

not

 

appear

 

to

 

be

 

sufficient

 

to

 

maintain

 

the

soil

 

organic

 

matter

 

contents

 

needed

 

(i.e.,

 

soil

 

C

 

output

 

is

 

larger

 

than

C

 

input,

 

resulting

 

in

 

soil

 

C

 

decline

 

–

 

cf.

 

Fig.

 

5

).

 

As

 

a

 

consequence,

yields

 

often

 

plummet

 

when

 

fertiliser

 

applications

 

are

 

interrupted.

Discontinuous,

 

insufficient

 

or

 

no

 

fertiliser

 

application

 

over

 

a

 

cer-

tain

 

period

 

of

 

time

 

may

 

lead

 

to

 

severe

 

soil

 

degradation

 

through

nutrient

 

depletion

 

and

 

loss

 

of

 

organic

 

matter.

 

When

 

fertiliser

 

or

organic

 

matter

 

applications

 

restart

 

after

 

a

 

certain

 

period

 

of

 

cultiva-

tion

 

without

 

them

 

soils

 

may

 

not

 

respond

 

immediately.

 

Often

 

crop

productivity

 

may

 

not

 

be

 

raised

 

back

 

to

 

the

 

yields

 

attained

 

before

Page 8

Figures and page graphics, page 8

P.

 

Tittonell,

 

K.E.

 

Giller

 

/

 

Field

 

Crops

 

Research

 

143

 

(2013)

 

76–90

 

83

Fig.

 

6.

 

Cattle

 

densities

 

in

 

sub-Saharan

 

Africa

 

(World

 

Resources

 

Institute;

http://www.earthtrends.org

).

 

Denser

 

cattle

 

populations

 

(between

 

20

 

and

 

more

 

than

50

 

cattle

 

per

 

km

2

)

 

are

 

distributed

 

across

 

an

 

east-west

 

band

 

of

 

northern

 

grassland,

and

 

along

 

a

 

northeast-southeast

 

band

 

of

 

eastern

 

grassland.

 

Countries

 

with

 

the

 

high-

est

 

densities

 

include

 

Ethiopia,

 

Kenya,

 

Uganda,

 

Tanzania,

 

Zambia,

 

Zimbabwe,

 

South

Africa,

 

and

 

Madagascar.

fertilisation

 

was

 

interrupted,

 

creating

 

a

 

new

 

system

 

state

 

at

 

lower

equilibrium

 

and

 

consequently

 

a

 

very

 

resilient

 

yield

 

gap

 

(

Tittonell

et

 

al.,

 

2012

).

 

The

 

two

 

states,

 

responsive

 

and

 

non-responsive

 

soils

do

 

not

 

necessarily

 

represent

 

a

 

continuum.

 

Reversibility

 

may

 

be

lost

 

when

 

a

 

certain

 

threshold

 

of

 

soil

 

degradation

 

is

 

surpassed.

 

The

magnitude

 

of

 

the

 

distance

 

between

 

these

 

two

 

alternate

 

states

 

is

known

 

as

 

hysteresis.

 

This

 

is

 

a

 

concept

 

common

 

in

 

ecology,

 

but

 

it

has

 

also

 

been

 

used

 

to

 

characterise

 

phases

 

of

 

land

 

rehabilitation

 

(e.g.,

Lal,

 

1997;

 

Tittonell

 

et

 

al.,

 

2008a

).

 

In

 

the

 

francophone

 

literature,

 

it

has

 

been

 

termed

 

the

 

‘

memoire

 

du

 

sol

’

 

and

 

related

 

to

 

the

 

param-

eters

 

that

 

define

 

response

 

curves

 

to

 

fertilisers

 

by

 

crops

 

(

Cretenet

and

 

Tittonell,

 

2010

).

 

In

 

a

 

long-term

 

experiment

 

in

 

southern

 

Benin

ceiling

 

maize

 

yields

 

fluctuated

 

between

 

3

 

and

 

4

 

t

 

ha

−

1

when

 

large

amounts

 

of

 

mineral

 

and

 

organic

 

fertilisers

 

were

 

applied

 

together,

and

 

crop

 

residues

 

incorporated

 

into

 

the

 

soil

 

every

 

year.

 

Control

yields

 

without

 

fertilisers

 

coupled

 

with

 

residue

 

removal

 

dropped

from

 

about

 

1

 

t

 

ha

−

1

to

 

practically

 

nothing

 

after

 

8

 

years.

 

When

 

the

same

 

fertiliser

 

and

 

residue

 

management

 

regimes

 

were

 

applied

 

to

these

 

control

 

fields

 

from

 

the

 

10th

 

year

 

maize

 

yields

 

recovered

 

grad-

ually,

 

but

 

hardly

 

achieved

 

the

 

ceiling

 

yields

 

after

 

a

 

decade.

 

Current

research

 

aims

 

at

 

characterising

 

the

 

determinants

 

of

 

such

 

soil

 

mem-

ory,

 

and

 

ways

 

to

 

overcome

 

it

 

to

 

ensure

 

hysteretic

 

soil

 

rehabilitation,

for

 

different

 

types

 

of

 

soils

 

and

 

cropping

 

systems.

2.3.

 

Precision

 

agriculture

Precision

 

agriculture

 

was

 

proposed

 

by

 

Cassman

 

(1999)

 

as

 

a

means

 

of

 

ensuring

 

a

 

more

 

efficient

 

use

 

of

 

applied

 

agricultural

inputs,

 

reducing

 

losses

 

and

 

thus

 

environmental

 

pollution.

 

Although

this

 

may

 

seem

 

rather

 

foreign

 

to

 

the

 

reality

 

of

 

subsistence

 

agricul-

ture,

 

smallholder

 

farmers

 

in

 

sub-Saharan

 

Africa

 

practice

 

several

forms

 

of

 

precision

 

agriculture.

 

To

 

start

 

with,

 

farmers

 

recognise

niches

 

of

 

soil

 

fertility

 

to

 

which

 

they

 

ascribe

 

different

 

local

 

names.

Thus

 

the

 

pervasive

 

localised

 

soil

 

heterogeneity

 

is

 

much

 

more

 

than

a

 

curiosity.

 

The

 

efficiency

 

with

 

which

 

nutrients

 

added

 

as

 

fertilizer

or

 

manure

 

are

 

captured

 

and

 

used

 

by

 

crops

 

is

 

strongly

 

reduced

 

by

soil

 

degradation

 

(

Giller

 

et

 

al.,

 

2006;

 

Tittonell

 

et

 

al.,

 

2007a

).

 

Farmers

recognise

 

the

 

existence

 

of

 

soil

 

fertility

 

gradients.

 

They

 

tend

 

to

 

plant

crops

 

earlier

 

and

 

more

 

densely,

 

weed

 

earlier

 

and

 

more

 

frequently,

and

 

apply

 

nutrients

 

as

 

fertilisers

 

and

 

manure

 

to

 

the

 

plots

 

that

 

are

already

 

more

 

fertile

 

(

Tittonell

 

et

 

al.,

 

2005b

).

 

Thus

 

the

 

resulting

differences

 

in

 

yields

 

are

 

due

 

to

 

gradients

 

of

 

management

 

inten-

sity

 

rather

 

than

 

soil

 

fertility

 

alone

 

(

Tittonell

 

et

 

al.,

 

2007b

).

 

Such

decision-making

 

patterns,

 

local

 

soil

 

classification

 

and

 

soil

 

quality

indicators

 

may

 

form

 

the

 

basis

 

of

 

a

 

new

 

form

 

of

 

precision

 

agriculture

adapted

 

to

 

the

 

African

 

smallholder

 

context.

 

To

 

ensure

 

efficiency

this

 

new

 

form

 

of

 

precision

 

agriculture

 

should

 

recognise

 

and

 

target

resources:

(i)

 

To

 

diverse

 

regions

 

and

 

agricultural

 

contexts.

(ii)

 

To

 

diverse

 

rural

 

livelihood

 

systems.

(iii)

 

To

 

agro-ecological,

 

cropping

 

systems

 

and

 

soil

 

fertility

 

niches.

(iv)

 

Through

 

concentration

 

of

 

limited

 

resources

 

in

 

space

 

and

 

time.

(v)

 

In

 

synchrony

 

with

 

crop

 

demands.

Cassman

 

(1999)

 

points

 

out

 

that

 

in

 

most

 

cases

 

technical

 

solutions

are

 

available,

 

but

 

that

 

socio-economic

 

factors

 

deter

 

their

 

imple-

mentation.

 

We

 

listed

 

some

 

of

 

such

 

factors

 

relevant

 

for

 

African

agriculture

 

in

 

the

 

introductory

 

paragraphs,

 

and

 

many

 

publications

deal

 

with

 

issues

 

such

 

as

 

diversity

 

of

 

livelihood

 

strategies,

 

land

tenure,

 

integration

 

of

 

crop-livestock

 

activities,

 

climate

 

change

 

and

other

 

risks.

 

Likewise,

 

there

 

is

 

an

 

important

 

body

 

of

 

literature

 

con-

cerning

 

means

 

to

 

improve

 

the

 

synchrony

 

between

 

crop

 

nutrient

demands

 

and

 

nutrient

 

release

 

from

 

different

 

organic

 

resources

used

 

in

 

Africa

 

(

Myers

 

et

 

al.,

 

1997;

 

Palm

 

et

 

al.,

 

2001;

 

Singh

 

et

 

al.,

2001

),

 

and/or

 

with

 

micro-dosing

 

and

 

point-placed

 

application

 

of

nutrient

 

sources

 

(

Aune

 

and

 

Bationo,

 

2008;

 

Hayashi

 

et

 

al.,

 

2008

).

Point

 

(iii)

 

deserves

 

most

 

attention

 

in

 

the

 

context

 

of

 

yield

 

gaps

and

 

their

 

biophysical

 

causes.

 

Fig.

 

7

 

illustrates

 

the

 

challenges

 

in

moving

 

from

 

recommendations

 

based

 

in

 

on-station

 

trials

 

to

 

deci-

sion

 

rules

 

for

 

niches

 

of

 

soil

 

fertility

 

within

 

heterogeneous

 

farms.

Fertiliser

 

experiments

 

provide

 

information

 

on

 

crop

 

responses

 

to

nutrient

 

inputs.

 

Based

 

on

 

this,

 

a

 

range

 

of

 

sensible

 

input

 

rates

 

can

be

 

identified

 

that

 

ensure

 

biophysically

 

efficient

 

input

 

use,

 

avoiding

negative

 

externalities

 

to

 

the

 

environment.

 

Theory

 

indicates

 

that

 

the

amount

 

of

 

inputs

 

to

 

be

 

added

 

depends

 

on

 

the

 

balance

 

between

 

nec-

essary

 

investments

 

and

 

economic

 

returns

 

(both

 

affected

 

by

 

market

conditions).

 

However,

 

adding

 

nutrient

 

inputs

 

may

 

result

 

in

 

highly

variable

 

crop

 

responses

 

across

 

spatially

 

heterogeneous

 

farms.

 

In

smallholder

 

farms

 

as

 

small

 

as

 

0.5

 

ha

 

efficiencies

 

will

 

vary

 

enor-

mously

 

from

 

poorly

 

responsive

 

fertile

 

fields

 

(normally

 

the

 

home

fields),

 

to

 

responsive

 

or

 

poorly

 

responsive

 

infertile

 

fields

 

(normally

the

 

outfields).

 

Applying

 

nutrient

 

inputs

 

in

 

the

 

most

 

responsive

fields

 

of

 

the

 

farm

 

will

 

ensure

 

most

 

efficient

 

use

 

of

 

them.

 

Fertile

home

 

gardens

 

may

 

be

 

managed

 

with

 

‘maintenance

 

fertilisation’,

whereas

 

poor

 

fields

 

should

 

be

 

rehabilitated

 

with

 

long-term

 

addi-

tions

 

of

 

organic

 

matter

 

before

 

they

 

can

 

respond

 

to

 

nutrient

 

inputs.

This

 

means

 

also

 

that

 

the

 

impact

 

of

 

input

 

use

 

should

 

be

 

analysed

considering

 

time

 

horizons

 

longer

 

than

 

a

 

single

 

season.

A

 

major

 

challenge

 

in

 

designing

 

such

 

forms

 

of

 

precision

 

agricul-

ture

 

resides

 

in

 

identifying

 

these

 

three

 

categories

 

of

 

fields

 

in

 

the

landscape,

 

responsive,

 

non-responsive

 

but

 

productive

 

and

 

non-

responsive

 

degraded.

 

Soil

 

fertility

 

and

 

physical

 

condition

 

are

 

the

result

 

of

 

history

 

of

 

land

 

use

 

and

 

current

 

management,

 

of

 

inherent

geology

 

and

 

geomorphology,

 

and

 

of

 

farmer

 

resource

 

endowment

(

Tittonell

 

et

 

al.,

 

2005a,b

).

 

Ebanyat

 

(2009)

 

documented

 

niche

 

man-

agement

 

of

 

soil

 

fertility

 

by

 

smallholder

 

farmers

 

in

 

eastern

 

Uganda,

where

 

they

 

shifted

 

their

 

kraals

 

(corrals)

 

every

 

number

 

of

 

years

 

to

create

 

islands

 

of

 

fertile

 

soils

 

to

 

grow

 

crops.

 

Finger

 

millet

 

(

Eleusine

coracana

 

(L.)

 

Gaertn.)

 

yields

 

ranged

 

between

 

0.6

 

and

 

2.2

 

t

 

h

−

1

in

old-kraal

 

sites

 

and

 

between

 

0.3

 

and

 

1.4

 

in

 

other

 

fields.

 

Obviously

the

 

presence

 

of

 

old-kraals

 

sites

 

is

 

closely

 

associated

 

with

 

farmer

resource

 

endowment,

 

as

 

only

 

the

 

wealthier

 

farmers

 

in

 

the

 

commu-

nity

 

possess

 

livestock.

 

Table

 

2

 

provides

 

an

 

example

 

of

 

soil

 

fertility

zoning

 

across

 

farm

 

types

 

in

 

the

 

vicinities

 

of

 

Murewa,

 

Zimbabwe

(

Zingore

 

et

 

al.,

 

2011

).

 

From

 

this

 

data

 

it

 

is

 

possible

 

to

 

roughly

 

assume

that

 

all

 

households

 

in

 

the

 

poorest

 

resource

 

categories

 

farm

 

on

Page 9

Figures and page graphics, page 9

84

 

P.

 

Tittonell,

 

K.E.

 

Giller

 

/

 

Field

 

Crops

 

Research

 

143

 

(2013)

 

76–90

In

te

rc

ep

t

Nutrient input

Crop y

ield

ΔY

ΔN

Effi

cie

ncy

Res

p

ons

e

Saturation

Excess

‘Sensible’

 

input rates 

Home fi

 

elds

Middle fi

 

elds

Outfields

Decision

 

 rule

Yield response > 

cost of

 

 fertiliser

NPK

NPK

NPK

NPK

NPK

NPK

NPK

NPK

NPK

NPK

NPK

NPK

Expected response (on-station)

Variable responses (on-farm)

Poorly-responsive fertile fields

Responsive fields

Poorly-responsive infertile fields

Yield wi

tho

u

t 

nu

tri

e

nt in

pu

ts

Nutrient input

Crop y

ield

Market

Fig.

 

7.

 

An

 

illustration

 

of

 

the

 

challenges

 

in

 

moving

 

from

 

recommendations

 

based

 

in

 

on-station

 

trials

 

to

 

decision

 

rules

 

for

 

niches

 

of

 

soil

 

fertility

 

within

 

heterogeneous

 

farms.

The

 

diagram

 

must

 

be

 

read

 

clockwise

 

starting

 

from

 

the

 

top-left

 

corner.

non-responsive

 

soils

 

(zone

 

4).

 

This

 

is

 

however

 

not

 

always

 

the

 

case,

and

 

more

 

complex

 

interactions

 

between

 

soil

 

fertility

 

and

 

resource

endowment

 

have

 

been

 

documented

 

(e.g.,

 

Giller

 

et

 

al.,

 

2011

).

An

 

extra

 

source

 

of

 

complexity

 

that

 

contributes

 

to

 

the

 

existence

of

 

niches

 

for

 

technologies

 

(and

 

also

 

to

 

explain

 

yield

 

gaps)

 

within

smallholder

 

farms

 

is

 

the

 

diversity

 

of

 

cropping

 

systems

 

in

 

space

and

 

time.

 

Intercropping

 

and

 

crop

 

rotations

 

are

 

most

 

common

 

in

traditional

 

agricultural

 

systems

 

in

 

the

 

continent.

 

The

 

residual

 

ben-

efits

 

of

 

N

2

-fixing

 

grain

 

legumes

 

on

 

the

 

yields

 

of

 

subsequent

 

cereals

and

 

other

 

crops

 

are

 

well

 

documented

 

(e.g.,

 

Adjei-Nsiah

 

et

 

al.,

 

2008;

Bationo

 

and

 

Ntare,

 

2000

).

 

Apart

 

from

 

the

 

direct

 

N

 

benefit

 

derived

from

 

the

 

legumes,

 

rotational

 

benefits

 

arise

 

due

 

to

 

other

 

factors

 

such

as

 

suppression

 

of

 

the

 

parasitic

 

“witchweed”

 

or

 

Striga

 

which

 

can

devastate

 

cereal

 

crops

 

(

Franke

 

et

 

al.,

 

2006;

 

Rusinamhodzi

 

et

 

al.,

2012

).

 

Table

 

3

 

illustrates

 

the

 

effect

 

of

 

intercropping

 

with

 

cowpea

on

 

the

 

yield

 

of

 

maize,

 

which

 

dropped

 

from

 

2.4

 

t

 

ha

−

1

in

 

sole

 

crop-

ping

 

to

 

1.6

 

t

 

ha

−

1

when

 

intercropped

 

at

 

a

 

1:1

 

ratio

 

(in

 

spite

 

of

 

the

fact

 

that

 

the

 

land

 

equivalent

 

ratios

 

were

 

in

 

all

 

cases

 

favourable).

The

 

combination

 

of

 

all

 

these

 

elements

 

means

 

that

 

actual

 

yields

 

in

farmer

 

fields

 

are

 

highly

 

variable,

 

in

 

space

 

and

 

time.

 

Precision

 

agri-

culture

 

needs

 

to

 

consider

 

such

 

variability,

 

as

 

responses

 

to

 

inputs

and

 

technologies

 

and

 

therefore

 

their

 

efficiency

 

are

 

also

 

likely

 

to

vary.

The

 

different

 

factors

 

responsible

 

for

 

yield

 

variability

 

are

interdependent,

 

and

 

their

 

interaction

 

often

 

leads

 

to

 

reinforcing

synergistic

 

effects.

 

We

 

can

 

expect

 

thresholds

 

to

 

exist

 

in

 

relation-

ships

 

between

 

yield

 

and

 

management

 

or

 

soil

 

fertility

 

variables,

leading

 

to

 

non-linearities.

 

Analysis

 

of

 

such

 

interactions

 

requires

application

 

of

 

multivariate

 

analysis

 

methods

 

and

 

an

 

ability

 

to

deal

 

with

 

non-linear

 

relationships.

 

Farm

 

survey

 

data

 

sets

 

that

 

can

be

 

used

 

to

 

determine

 

actual

 

yields

 

are

 

normally

 

characterised

by

 

a

 

mixture

 

of

 

continuous

 

and

 

categorical

 

variables,

 

highly

skewed

 

data,

 

and

 

large

 

numbers

 

of

 

missing

 

observations,

 

adding

to

 

the

 

complexity

 

of

 

the

 

analysis.

 

Classification

 

and

 

regression

tree

 

(CART)

 

analysis

 

has

 

been

 

used

 

to

 

unravel

 

within-farm

 

yield

variability

 

(e.g.,

 

Tittonell

 

et

 

al.,

 

2008b

).

 

Fig.

 

8

 

shows

 

an

 

example

of

 

classification

 

of

 

maize

 

yield

 

data

 

measured

 

in

 

150

 

farmer

 

fields

in

 

western

 

Kenya.

 

From

 

about

 

30

 

possible

 

explanatory

 

variables

describing

 

agro-ecological,

 

soil

 

and

 

management

 

factors

 

only

 

five

were

 

retained

 

in

 

a

 

CART

 

analysis

 

as

 

meaningful:

 

resource

 

use

intensity,

 

plant

 

density,

 

planting

 

dates,

 

total

 

soil

 

N

 

and

 

available

 

P.

The

 

150

 

observations

 

were

 

classified

 

in

 

six

 

homogeneous

 

groups

(Terminal

 

nodes),

 

which

 

can

 

be

 

interpreted:

 

e.g.,

 

fields

 

cropped

with

 

no

 

inputs

 

and

 

planted

 

late

 

were

 

the

 

majority,

 

and

 

these

 

fields

exhibited

 

low

 

to

 

very

 

low

 

soil

 

P

 

availabilities.

 

CART

 

is

 

a

 

powerful

method

 

to

 

categorise

 

yield

 

variability,

 

to

 

estimate

 

actual

 

yields

in

 

yield

 

gap

 

analysis,

 

and

 

to

 

link

 

variability

 

back

 

to

 

its

 

underlying

causes.

3.

 

Yield

 

gaps

 

of

 

major

 

food

 

crops

 

in

 

Africa

Here

 

we

 

provide

 

a

 

first

 

attempt

 

to

 

estimate

 

the

 

current

 

yield

gaps

 

of

 

major

 

food

 

crops

 

in

 

Africa,

 

illustrating

 

with

 

examples

 

the

diversity

 

of

 

factors

 

that

 

should

 

be

 

considered

 

when

 

estimating

 

both

Page 10

Figures and page graphics, page 10

P.

 

Tittonell,

 

K.E.

 

Giller

 

/

 

Field

 

Crops

 

Research

 

143

 

(2013)

 

76–90

 

85

Table

 

2

Description

 

of

 

the

 

different

 

zones

 

of

 

fertility

 

on

 

smallholder

 

farms

 

in

 

Murewa,

 

Zimbabwe;

 

(A)

 

their

 

occurrence

 

and

 

soil

 

properties,

 

and

 

(B)

 

proportion

 

of

 

the

 

area

 

covered

 

by

 

zones

 

of

 

fertility

 

on

 

farms

 

differing

 

in

 

wealth

 

status.

Soil

 

fertility

zoning

Sandy

 

soils

 

Clay

 

soils

Village

 

area

SOC

 

(g

 

kg

−

1

)

 

N

 

(g

 

kg

−

1

)

 

Avail.

 

P

 

(mg

 

kg

−

1

)

 

Village

 

area

SOC

 

(g

 

kg

−

1

)

 

N

 

(g

 

kg

−

1

)

 

Avail.

 

P

 

(mg

 

kg

−

1

)

A

Zone

 

1

Uncultivated

 

woodland

 

soils.

 

Mainly

 

used

as

 

communal

 

grazing

 

lands.

53.6%

 

12

1.2

 

14

14.0%

 

21

1.6

 

18

Zone

 

2

 

Most

 

fertile

 

fields

 

where

 

large

 

amounts

 

of

manure

 

were

 

applied,

 

typical

 

homefields

on

 

wealthier

 

farms.

5.6%

 

8

 

0.8

 

12

 

1.5%

 

16

 

1.2

 

12

Zone

 

3

Fields

 

with

 

moderate

 

fertility

 

where

 

small

amounts

 

of

 

manure

 

were

 

used,

 

mid-fields

and

 

outfields

 

of

 

wealthier

 

farms.

6.1%

 

5

0.6

 

7

1.6%

 

10

 

0.8

 

10

Zone

 

4

 

Fields

 

with

 

low

 

fertility

 

mostly

 

cultivated

with

 

little

 

fertilizer

 

inputs,

 

most

 

fields

 

of

poorer

 

farms

 

and

 

outfields

 

of

 

mid

 

to

wealthier

 

farms.

14.6%

 

3

 

0.3

 

3

 

3.9%

 

7

 

0.5

 

5

Farm

 

type

Area

 

in

 

zone

 

2

 

(%)

Area

 

in

 

zone

 

3

 

(%)

Area

 

in

 

zone

 

4

 

(%)

B

Resource

 

Group

 

1

 

(wealthiest)

32

68

0

Resource

 

Group

 

24

2

2

1

 

37

Resource

 

Group

 

30

 

0

 

100

Resource

 

Group

 

4

 

(poorest)

 

0

 

0

 

100

From

 

Zingore

 

et

 

al.

 

(2007)

.

Table

 

3

Crop

 

yields

 

and

 

land

 

equivalent

 

ratios

 

(LER)

 

for

 

different

 

cowpea-maize

 

intercrops

at

 

Ibadan,

 

Nigeria.

Cowpea:maize
ratio

Yield

 

Relative

 

yield

Cowpea

 

Maize

 

Cowpea

 

Maize

 

LER

(kg

 

ha

−

1

)

 

(kg

 

ha

−

1

)

 

(

Y

c

)

 

(

Y

m

)

 

(

Y

c

+

 

Y

m

)

0:100

 

n/a

 

2439

 

n/a

 

n/a

 

n/a

25:75

181

2158

0.43

0.88

1.31

50:50

 

327

 

1653

 

0.78

 

0.68

 

1.46

75:25

291

 

1167

 

0.70

 

0.48

 

1.18

100:0

 

322

 

n/a

 

n/a

 

n/a

 

n/a

Modified

 

from

 

Olufemi

 

Pitan

 

and

 

Odebiyi

 

(2001)

.

actual

 

and

 

attainable

 

yields.

 

A

 

coarse

 

but

 

useful

 

first

 

approximation

to

 

average

 

crop

 

yields

 

per

 

country

 

is

 

the

 

FAOStat

 

database.

 

Table

 

4

presents

 

a

 

comparison

 

of

 

yield

 

ranges

 

of

 

major

 

food

 

crops

 

reported

in

 

the

 

literature

 

–

 

mostly

 

from

 

on-farm

 

experiments

 

–

 

and

 

the

 

aver-

age

 

country-level

 

yield

 

over

 

the

 

last

 

10

 

years

 

calculated

 

from

 

the

FAO

 

data.

 

In

 

spite

 

of

 

the

 

wide

 

coverage

 

of

 

the

 

country

 

average,

which

 

includes

 

diverse

 

agro-ecological

 

regions

 

and

 

production

 

sit-

uations

 

within

 

each

 

country,

 

its

 

value

 

is

 

not

 

far

 

from

 

the

 

mid-range

yield

 

reported

 

in

 

the

 

scientific

 

literature

 

for

 

crops

 

such

 

as

 

maize,

sorghum

 

or

 

millet,

 

and

 

for

 

some

 

grain

 

legumes.

 

The

 

FAO

 

average

yields

 

for

 

cassava

 

and

 

highland

 

banana

 

are

 

closer

 

to

 

the

 

lower

 

end

of

 

the

 

yield

 

range

 

found

 

in

 

the

 

literature

 

–

 

which

 

is

 

likely

 

to

 

be

 

the

case

 

in

 

reality.

 

Yet,

 

yields

 

from

 

the

 

literature

 

exhibit

 

wide

 

ranges

 

of

variability,

 

which

 

are

 

not

 

uncommon

 

in

 

farmers’

 

fields.

 

Perhaps

 

one

of

 

the

 

most

 

useful

 

elements

 

of

 

the

 

FAO

 

database

 

is

 

the

 

time

 

series,

which

 

provides

 

a

 

rough

 

indication

 

of

 

inter-annual

 

yield

 

variability.

These

 

general

 

trends

 

are

 

only

 

indicative

 

of

 

the

 

magnitude

 

of

yield

 

gaps

 

but

 

say

 

little

 

about

 

their

 

causes

 

and

 

local

 

variation.

 

At

local

 

scale,

 

and

 

based

 

on

 

all

 

the

 

evidence

 

presented

 

in

 

the

 

previous

section,

 

soil

 

fertility

 

gradients

 

must

 

be

 

considered

 

in

 

any

 

yield

 

gap

assessment.

 

Table

 

5

 

presents

 

a

 

first

 

attempt

 

to

 

quantifying

 

maize

yield

 

gaps

 

across

 

soil

 

fertility

 

gradients

 

in

 

regions

 

of

 

countries

where

 

maize

 

is

 

grown

 

and

 

important,

 

using

 

data

 

from

 

a

 

diversity

of

 

(comparable)

 

sources.

 

Locally

 

attainable

 

yields

 

varied

 

between

roughly

 

4

 

and

 

7

 

t

 

ha

−

1

across

 

regions.

 

Average

 

yields

 

in

 

farm-

ers’

 

fields

 

varied

 

widely

 

across

 

soil

 

fertility

 

gradients.

 

On

 

average,

however,

 

relative

 

yields

 

were

 

in

 

the

 

order

 

of

 

40–60%

 

of

 

the

 

locally

attainable

 

yields

 

in

 

the

 

most

 

fertile

 

fields,

 

and

 

in

 

most

 

cases

 

they

ranged

 

between

 

10

 

and

 

20%

 

in

 

poorest

 

fields.

 

Rainfall

 

use

 

efficien-

cies

 

ranged

 

from

 

1

 

to

 

2

 

kg

 

ha

−

1

mm

−

1

on

 

poor

 

fields

 

to

 

more

 

than

5

 

kg

 

ha

−

1

mm

−

1

on

 

fertile

 

fields.

 

These

 

efficiencies

 

are

 

calculated

with

 

respect

 

to

 

seasonal

 

rainfall

 

(note

 

that

 

two

 

cropping

 

seasons

per

 

year

 

are

 

possible

 

in

 

some

 

of

 

these

 

sites).

 

On

 

the

 

basis

 

of

 

a

 

large

number

 

of

 

model

 

simulations,

 

Tittonell

 

et

 

al.

 

(2010b)

 

proposed

 

a

simple

 

equation

 

to

 

estimate

 

water-limited

 

maize

 

yields:

WLY (kg

 

ha

−

1

)

 

=

 

Rainfall

 

(mm)

 

×

 

20

 

(kg

 

ha

−

1

mm

−

1

)

 

×

 

HI

 

(1)

where

 

HI

 

is

 

the

 

crop

 

harvest

 

index

 

or

 

the

 

ratio

 

between

 

grain

 

to

total

 

above-ground

 

biomass.

 

The

 

potential

 

rainfall

 

use

 

efficiency

 

for

biomass

 

production,

 

of

 

20

 

kg

 

ha

−

1

mm

−

1

in

 

this

 

case,

 

is

 

obviously

 

a

rough

 

estimate

 

and

 

a

 

coefficient

 

that

 

can

 

be

 

easily

 

calibrated

 

against

data.

 

When

 

rainfall

 

is

 

800

 

mm

 

(e.g.,

 

NE

 

Zimbabwe)

 

and

 

HI

 

=

 

0.5,

the

 

water

 

limited

 

yield

 

potential

 

of

 

maize

 

would

 

be

 

8

 

t

 

ha

−

1

.

 

Such

yields

 

are

 

rarely

 

realised

 

by

 

smallholders,

 

but

 

may

 

be

 

attainable

in

 

commercial

 

farming.

 

Similar

 

simple

 

equations

 

could

 

be

 

eas-

ily

 

derived

 

for

 

sorghum

 

(e.g.,

 

≈

12

 

kg

 

ha

−

1

mm

−

1

)

 

and

 

millet

 

(e.g.,

≈

10

 

kg

 

ha

−

1

mm

−

1

),

 

and

 

perhaps

 

also

 

for

 

non-cereal

 

crops

 

such

 

as

cassava

 

or

 

banana.

 

The

 

fact

 

that

 

the

 

water

 

limited

 

yield

 

could

 

be

greater

 

for

 

sorghum

 

than

 

for

 

millet

 

does

 

not

 

always

 

reflect

 

what

farmers

 

experience

 

in

 

reality.

 

Particularly

 

in

 

dry

 

environments

millet

 

often

 

yields

 

better

 

than

 

sorghum

 

(e.g.,

 

Murungweni

 

et

 

al.,

submitted

 

for

 

publication

).

Page 11

Figures and page graphics, page 11

86

 

P.

 

Tittonell,

 

K.E.

 

Giller

 

/

 

Field

 

Crops

 

Research

 

143

 

(2013)

 

76–90

Table

 

4

Examples

 

of

 

yield

 

ranges

 

for

 

major

 

food

 

crops

 

on

 

smallholder

 

farmers’

 

fields

 

in

 

four

 

countries

 

of

 

East

 

and

 

Southern

 

Africa.

Crop

 

Yield

 

ranges

 

from

 

literature

 

(t

 

ha

−

1

)

 

Country,

 

region

 

Current

 

yield

 

from

 

FAOstat

Low

 

Medium

 

High

 

(t

 

ha

−

1

)

Cereals

Maize

 

0.57

 

1.30

 

5.67

 

Zimbabwe,

 

central

 

1.51

Sorghum

 

0.11

 

1.03

 

3.92

 

Zimbabwe,

 

North

 

0.94

Millet

 

(pearl)

0.16

 

0.72

 

1.93

 

Zimbabwe,

 

S.

 

East

0.83

Millet

 

(finger)

 

0.29

 

1.49

 

2.15

 

Uganda,

 

East

 

n/a

Legumes

Common

 

bean

 

0.14

 

0.34

 

0.76

 

Kenya,

 

West

 

0.64

Cowpea

 

0.16

 

0.40

 

0.81

 

Kenya,

 

West

 

0.64

Groundnut

 

0.22

 

0.55

 

0.98

 

Zimbabwe,

 

S.

 

East

 

0.79

Soyabean

0.35

 

0.87

 

2.15

 

Malawi,

 

central

0.95

Perennial

 

crops

 

(Fresh

 

weight)

Cassava

 

8.60

 

13.60

 

20.80

 

Uganda,

 

East

 

9.13

Banana

 

5.50

 

9.40

 

38.40

 

Uganda,

 

S.

 

West

 

7.78

References

:

 

Zingore

 

(2006)

,

 

Ojiem

 

(2006)

,

 

Fermont

 

(2009)

,

 

Nyombi

 

(2010)

,

 

Murungweni

 

(2011)

,

 

Baudron

 

(2011)

,

 

and

 

Kamanga

 

(2011)

.

4.

 

A

 

framework

 

for

 

yield

 

gap

 

assessments

 

in

 

African

smallholder

 

agriculture

When

 

the

 

intention

 

is

 

to

 

assess

 

yield

 

gaps

 

across

 

countries

 

and

regions

 

in

 

Africa,

 

at

 

least

 

three

 

major

 

sets

 

of

 

biophysical

 

drivers

should

 

be

 

considered

 

(

Fig.

 

9

).

 

First,

 

the

 

climatic

 

zone,

 

as

 

determined

by

 

the

 

length

 

of

 

the

 

growing

 

season,

 

radiation,

 

maximum

 

and

minimum

 

temperatures

 

(altitude)

 

and

 

rainfall

 

(amount

 

and

 

dis-

tribution).

 

This

 

information,

 

together

 

with

 

information

 

on

 

the

 

start

and

 

end

 

of

 

the

 

typical

 

growing

 

season

 

allows

 

estimating

 

a

 

water-

limited

 

yield

 

potential

 

(

Y

W

).

 

This

 

is

 

equivalent

 

to

 

the

 

yield

 

that

 

can

be

 

estimated

 

with

 

Eq.

 

(1)

,

 

or

 

calculated

 

with

 

a

 

simple

 

crop

 

growth

model

 

simulating

 

potential

 

yields,

 

correcting

 

the

 

crop

 

growth

 

rate

by

 

the

 

daily

 

(or

 

seasonal,

 

according

 

to

 

data

 

available)

 

ratio

 

between

actual

 

and

 

potential

 

evapotranspiration,

 

or

 

rainfall

 

vs.

 

potential

evapotranspiration.

 

Note

 

that

 

this

 

calculation

 

does

 

not

 

include

soil

 

hydrological

 

characteristics

 

–

 

which

 

were

 

seldom

 

measured

 

in

African

 

soils

 

–

 

and

 

so

 

the

 

water-limited

 

yield

 

thus

 

calculated

 

may

differ

 

from

 

values

 

cited

 

in

 

literature.

 

This

 

yield

 

level

 

should

 

approx-

imate

 

the

 

maximum

 

yields

 

attainable

 

under

 

controlled

 

conditions

in

 

experimental

 

stations,

 

during

 

a

 

favourable

 

growing

 

season.

The

 

second

 

set

 

of

 

physical

 

drivers

 

corresponds

 

to

 

the

 

dominant

soil

 

types,

 

as

 

determined

 

by

 

their

 

geological,

 

geomorphological

and

 

pedological

 

features.

 

In

 

particular

 

soil

 

texture,

 

soil

 

depth

 

and

field

 

slope

 

play

 

an

 

important

 

role

 

in

 

water

 

capture,

 

retention

 

and

availability

 

to

 

crops.

 

These

 

elements

 

plus

 

the

 

inherent

 

soil

 

fertility

define

 

locally

 

attainable

 

yield

 

levels

 

(

Y

L

),

 

which

 

are

 

also

 

affected

by

 

the

 

characteristics

 

of

 

the

 

cropping

 

system

 

(e.g.,

 

intercropping,

agroforestry,

 

and

 

rotations).

 

This

 

yield

 

level

 

corresponds

 

to

 

the

maximum

 

yield

 

that

 

can

 

be

 

obtained

 

on

 

farmers’

 

fields

 

when

 

man-

agement

 

is

 

optimised

 

(or

 

in

 

researcher-managed

 

on-farm

 

trials

 

–

cf.

 

Tittonell

 

et

 

al.,

 

2008c

),

 

or

 

to

 

the

 

95th

 

percentile

 

yield

 

in

 

a

 

farmer

yield

 

survey

 

(cf.

 

van

 

Ittersum

 

et

 

al.,

 

2013

).

 

Digital

 

soil

 

maps,

 

if

sufficiently

 

accurate,

 

could

 

provide

 

the

 

input

 

required

 

to

 

charac-

terise

 

soil

 

properties

 

(

Minasny

 

and

 

Hartemink,

 

2011

).

 

When

 

data

are

 

available

 

for

 

parameterisation,

 

calibration

 

and

 

testing,

 

this

 

yield

Resource   

use intensity

Split = high/low

(Y = 1

 

.5; n = 151)

Term

 

inal 

node 1

(Y = 1

 

.6; 

n = 21)

Term

 

inal 

node 2

(Y = 2

 

.2; 

n = 15)

Term

 

inal 

node 3

(Y = 0

 

.8; 

n = 39)

Term

 

inal 

node 4

(Y = 1

 

.5; 

n = 51)

Term

 

inal

 

 nod

 

e 5

(Y = 1

 

.9; 

 

n = 17)

Term

 

inal

 

 nod

 

e 6

(Y = 2

 

.5; 

 

n = 8)

Delay in

 

  

planti

 

ng  

Split <= 0.17

(Y = 1

 

.4; n = 126)

Olsen P

Split <= 2.0

(Y = 1

 

.2; 

 

n = 90)

Planting 

density

Split <= 4.4

(Y = 2

 

.1; n = 25)

Total

 

 N

Split <= 1.1

(Y = 1

 

.8; 

 

n = 36)

Key

Split

: cutoff va

 

lue

 

 for the splitting criterion

Y

: average maize grain yi

 

eld for the node

n

: number of

 

 cases in each no

 

de

High

Low

Dense

Sparse

Late

Early

High

Low

High

Low

Fig.

 

8.

 

Results

 

of

 

a

 

classification

 

and

 

regression

 

tree

 

analysis

 

of

 

151

 

maize

 

grain

 

yield

 

observations

 

across

 

60

 

households

 

in

 

Kenya.

 

Of

 

the

 

almost

 

30

 

candidate

 

explanatory

variables

 

included

 

in

 

the

 

analysis

 

(including

 

rainfall),

 

only

 

five

 

were

 

selected:

 

the

 

intensity

 

of

 

nutrient

 

resource

 

use

 

(organic

 

and

 

mineral

 

fertilisers),

 

the

 

planting

 

date

 

and

density,

 

total

 

soil

 

N

 

and

 

extractable

 

P

 

(

Tittonell

 

et

 

al.,

 

2008b

).

Page 12

Figures and page graphics, page 12

P.

 

Tittonell,

 

K.E.

 

Giller

 

/

 

Field

 

Crops

 

Research

 

143

 

(2013)

 

76–90

 

87

Table

 

5

Current

 

average

 

maize

 

grain

 

yields

 

(t

 

ha

−

1

)

 

across

 

soil

 

fertility

 

gradients

 

on

 

smallholder

 

farms,

 

locally

 

attainable

 

yields

 

(maximum

 

yields

 

in

 

on-farm

 

trials

 

or

 

95th

 

percentile

farmers’

 

yields),

 

relative

 

yields

 

and

 

rainfall

 

use

 

efficiency

 

in

 

selected

 

regions

 

of

 

countries

 

where

 

maize

 

is

 

an

 

important

 

staple

 

crop.

Country/region

Agro-ecological

 

niche

Current

 

farmers’

yields

Locally

 

attainable

yield

a

Relative

 

yield

 

(%

 

of

locally

 

attainable)

Rainfall

 

use

 

efficiency

(kg

 

ha

−

1

mm

−

1

)

Kenya,

 

Kakamega

NFS

 

2.8

 

6.9

 

41

 

4.2

RS

1.4

 

20

 

2.1

NPS

 

0.9

 

13

 

1.4

Uganda,

 

Tororo

NFS

 

1.7

 

4.8

 

35

 

3.7

RS

 

1.0

 

21

 

2.2

NPS

0.7

 

15

1.5

Zimbabwe,

 

Murewa

NFS

 

2.1

 

6.2

 

34

 

2.8

RS

 

0.7

 

11

 

0.9

NPS

 

0.2

 

3

 

0.3

Tanzania,

 

Kibera

NFS

 

2.6

 

5.1

 

51

 

2.9

RS

 

1.5

 

29

 

1.7

NPS

0.8

 

16

 

0.9

Mozambique,

 

Manika

NFS

 

2.1

 

6.1

 

34

 

2.7

RS

 

0.9

 

15

 

1.2

NPS

 

0.5

 

8

 

0.8

Ghana,

 

Kumasi

MF

 

1.5

 

4.2

 

36

 

1.7

DS

0.4

 

10

 

0.4

Ivory

 

Coast,

 

Gagnoa

MF

 

3.8

 

6.2

 

61

 

5.8

DS

 

1.6

 

26

 

2.4

Togo,

 

terres

 

de

 

barre

 

(S)

MF

 

1.8

 

3.7

 

49

 

3.5

DS

 

0.3

 

8

 

0.6

Benin,

 

Aplaoué

MF

 

2.1

 

4.5

 

47

 

4.2

DS

 

0.5

 

11

 

1.0

NFS:

 

non-responsive

 

fertile

 

fields;

 

RS:

 

responsive

 

soils;

 

NPS:

 

non-responsive

 

soils;

 

MF:

 

moderately

 

fertile;

 

DS:

 

degraded

 

site

a

In

 

most

 

cases,

 

these

 

correspond

 

to

 

yields

 

in

 

on-farm

 

experiments

 

receiving

 

full

 

fertiliser

 

application

 

rates.

level

 

can

 

be

 

calculated

 

with

 

a

 

crop-soil

 

simulation

 

model

 

as

 

shown

in

 

Fig.

 

3

,

 

equivalent

 

to

 

the

 

water-

 

and

 

nutrient-limited

 

yield

 

level

defined

 

by

 

De

 

Wit

 

(1992)

.

 

This

 

yield

 

level

 

can

 

also

 

be

 

approximated

through

 

boundary

 

line

 

models

 

fitted

 

to

 

data

 

on

 

farmers’

 

yields

 

that

include

 

favourable

 

rainfall

 

years.

 

When

 

boundary

 

lines

 

or

 

95th

 

per-

centile

 

farmer

 

yields

 

are

 

considered,

 

the

 

difference

 

between

 

locally

attainable

 

yields

 

and

 

the

 

water-limited

 

yield

 

potential,

 

or

 

yield

 

gap

1

 

in

 

Fig.

 

9

 

may

 

be

 

partly

 

–

 

and

 

sometimes

 

almost

 

exclusively

 

–

explained

 

by

 

the

 

degree

 

of

 

technology

 

used

 

for

 

crop

 

cultivation,

notably

 

by

 

the

 

use

 

of

 

improved

 

germplasm

 

and/or

 

agrochemicals.

The

 

last

 

set

 

of

 

physical

 

drivers

 

is

 

the

 

most

 

elusive

 

and

 

con-

cerns

 

drivers

 

of

 

yield

 

variability

 

within

 

farms,

 

chiefly

 

soil

 

fertility

gradients.

 

Zones

 

of

 

soil

 

fertility

 

are

 

defined

 

by

 

soil

 

management

 

his-

tory,

 

and

 

reflect

 

the

 

proportion

 

of

 

responsive

 

and

 

non-responsive

Climatic 

determinan

 

ts

Dominant so

 

il 

types

Growing 

season

Cropping 

syst

 

em

Soil fertility 

zoning

Biotic 

constraints

Y

W

: Water-

limited yield 

potent

 

ial

Y

L

: Lo

 

cally 

attainable yiel

 

ds 

Y

A

: Actual

 

 yiel

 

d 

& yi

 

eld

 

 var

 

iability

Maximum yiel

 

ds un

 

der 

control

 

led

 

 condi

 

tio

 

ns 

(on-statio

 

n) in a

 

 go

 

od 

year

Maximum yiel

 

ds in on

 

-

farm experime

 

nts

 

 or 

maximum farme

 

rs’ yiel

 

ds 

in a go

 

od year (boun

 

dary 

models)

Average yiel

 

d in farm

 

ers

 

’

fields and

 

 the

 

ir variabi

 

lity 

in space an

 

d time

Length of

 

 growing season 

Radiat

 

ion and temperatu

 

re 

Rainfa

 

ll total & distributi

 

on

Texture, de

 

pth

 

 & 

 

slo

 

pe 

Permanent limitati

 

ons

 

   

 

 

(e.g. pH, salinit

 

y, stoniness)

Soil condit

 

ion (st

 

ructure –

bulk density), carbon 

stocks,

 

 an

 

d nutrient 

availab

 

ility –

 

extent of

 

 soil 

degradation

Tec

 

hno

 

logy gap?

Resour

 

ce gap?

Data & Maps

 

Auxilia

 

ry 

variables

Referen

 

ce 

yields

Sources o

 

f 

references

Physi

 

cal 

environment

Adapted from Tittone

 

ll

 

(2009)

YG1

YG2

Fig.

 

9.

 

A

 

framework

 

for

 

definition

 

and

 

estimation

 

of

 

reference

 

yields

 

and

 

yield

 

gaps

 

in

 

African

 

smallholder

 

agriculture,

 

indicating

 

minimum

 

data

 

needs

 

and

 

possible

 

sources

of

 

yield

 

references.

 

It

 

is

 

hypothesised

 

that

 

while

 

the

 

yield

 

gap

 

1

 

(YG1)

 

is

 

largely

 

attributable

 

to

 

access

 

to

 

(and

 

availability

 

of)

 

adequate

 

technologies,

 

the

 

yield

 

gap

 

2

 

(YG2)

reflects

 

differences

 

in

 

farmers’

 

resource

 

endowment.

Page 13

Figures and page graphics, page 13

88

 

P.

 

Tittonell,

 

K.E.

 

Giller

 

/

 

Field

 

Crops

 

Research

 

143

 

(2013)

 

76–90

soils

 

in

 

agricultural

 

landscapes.

 

Thus

 

the

 

yield

 

gap

 

cannot

 

be

 

esti-

mated

 

on

 

an

 

aggregated

 

basis

 

without

 

a

 

spatial

 

analysis

 

to

 

estimate

the

 

proportion

 

of

 

fields

 

that

 

are

 

in

 

a

 

degraded

 

state.

 

If

 

detail

 

on

individual

 

farms

 

is

 

aimed

 

for,

 

the

 

granularity

 

of

 

such

 

spatial

 

anal-

ysis

 

should

 

be

 

fine

 

enough

 

to

 

identify

 

small

 

plots

 

of

 

0.2

 

ha

 

or

 

less

given

 

the

 

patchwork

 

patterns

 

of

 

fields

 

found

 

in

 

densely

 

populated

areas.

 

This

 

could

 

be

 

done

 

using

 

kriging

 

methods,

 

although

 

the

 

den-

sity

 

of

 

sampling

 

required

 

may

 

be

 

prohibitive.

 

In

 

view

 

of

 

this,

 

we

recommend

 

using

 

remote

 

sensing

 

techniques

 

to

 

estimate

 

the

 

pro-

portion

 

of

 

different

 

categories

 

of

 

fields

 

(or

 

zones

 

of

 

fertility)

 

within

an

 

area

 

(cf.

 

Table

 

2

).

 

This

 

information,

 

together

 

with

 

knowledge

about

 

major

 

biotic

 

constraints

 

(weeds,

 

pest

 

and

 

diseases

 

–

 

cf.

 

exam-

ple

 

of

 

highland

 

banana

 

in

 

Section

 

2.1

)

 

in

 

a

 

certain

 

location

 

can

 

be

used

 

to

 

estimate

 

actual

 

yields

 

and

 

their

 

variability,

 

not

 

for

 

each

individual

 

farm,

 

but

 

for

 

the

 

entire

 

area

 

(cf.

 

Fig.

 

8

).

 

While

 

yield

 

esti-

mates

 

are

 

still

 

likely

 

to

 

show

 

strong

 

stochasticity,

 

the

 

relevant

 

area

unit

 

to

 

estimate

 

yield

 

gaps

 

is

 

likely

 

to

 

vary

 

across

 

regions

 

depend-

ing

 

on

 

inherent

 

spatial

 

variability

 

and

 

demographic

 

patterns.

 

Well

calibrated

 

simulation

 

models

 

of

 

the

 

cropping

 

system

 

(cf.

 

Fig.

 

3

A),

allowing

 

for

 

correction

 

factors

 

due

 

to

 

weed,

 

pest

 

or

 

disease

 

pres-

sure

 

could

 

be

 

used

 

to

 

estimate

 

actual

 

yields

 

–

 

although

 

obtaining

the

 

necessary

 

data

 

to

 

parameterise

 

such

 

models

 

would

 

be

 

often

more

 

demanding

 

than

 

measuring

 

yields

 

in

 

a

 

rigorously

 

identified

sample

 

of

 

farmers’

 

fields.

For

 

yield

 

gaps

 

to

 

be

 

informative

 

at

 

this

 

scale

 

of

 

analysis

 

it

 

is

not

 

only

 

important

 

to

 

consider

 

average

 

yields

 

in

 

farmers’

 

fields

but

 

also

 

their

 

strong

 

variability

 

in

 

time.

 

The

 

method

 

proposed

by

 

Lobell

 

(2013)

 

of

 

comparing

 

the

 

average

 

yield

 

of

 

the

 

last

 

one,

two,

 

three,

 

four

 

and

 

five

 

years

 

to

 

assess

 

yield

 

differences

 

would

be

 

most

 

pertinent

 

here,

 

as

 

this

 

provides

 

a

 

measure

 

of

 

variability.

Lobell’s

 

interpretation

 

does

 

of

 

the

 

resulting

 

patterns

 

of

 

variabil-

ity

 

to

 

infer

 

their

 

possible

 

causes

 

is

 

however

 

questionable.

 

For

instance,

 

if

 

these

 

averages

 

were

 

calculated

 

for

 

the

 

yields

 

in

 

the

control

 

treatment

 

in

 

Fig.

 

5

,

 

their

 

value

 

would

 

vary

 

enormously

depending

 

on

 

the

 

5-year

 

period

 

considered,

 

whether

 

1971–1976,

1973–1978,

 

or

 

1975–1980,

 

while

 

in

 

all

 

these

 

periods

 

the

 

underlying

cause

 

of

 

yield

 

decline

 

was

 

the

 

same.

 

We

 

hypothesise

 

that

 

the

 

gap

between

 

actual

 

and

 

locally

 

attainable

 

yields

 

is

 

largely

 

attributable

to

 

farmer

 

resource

 

endowment

 

and

 

access

 

to

 

nutrient

 

inputs,

 

and

a

 

categorisation

 

of

 

yield

 

ranges

 

across

 

farm

 

types

 

and

 

production

environments

 

will

 

provide

 

very

 

good

 

approximation

 

of

 

this

 

yield

gap

 

and

 

its

 

space-time

 

variability

 

within

 

smallholder

 

African

 

farms.

5.

 

Discussion

 

and

 

conclusions

Yield

 

gaps

 

in

 

African

 

smallholder

 

farming

 

are

 

among

 

the

 

largest

in

 

the

 

world.

 

Given

 

demographic

 

projections

 

that

 

the

 

human

 

pop-

ulation

 

in

 

Africa

 

will

 

grow

 

most

 

rapidly

 

of

 

all

 

continents

 

in

 

the

coming

 

years,

 

there

 

is

 

an

 

urgent

 

need

 

for

 

productivity

 

to

 

increase.

The

 

underlying

 

causes

 

of

 

poor

 

productivity

 

of

 

African

 

agriculture

are

 

diverse,

 

but

 

the

 

challenges

 

faced

 

by

 

farmers

 

often

 

include

 

the

lack

 

of

 

access

 

to

 

agricultural

 

inputs,

 

the

 

intense

 

labour

 

demands

caused

 

by

 

lack

 

of

 

mechanisation,

 

the

 

small

 

size

 

and

 

increasing

 

frag-

mentation

 

of

 

farms

 

and

 

the

 

lack

 

of

 

capital

 

to

 

invest

 

in

 

building

productive

 

soils

 

in

 

harsh

 

environments.

 

Thinking

 

about

 

yield

 

gaps

or

 

yield

 

ceilings

 

makes

 

much

 

sense

 

when

 

examining

 

current

 

yields

in

 

the

 

most

 

productive

 

agroecosystems

 

of

 

the

 

world,

 

where

 

actual

yields

 

are

 

constantly

 

narrowing

 

the

 

gap

 

with

 

respect

 

to

 

the

 

yield

potential.

 

In

 

the

 

case

 

of

 

African

 

smallholder

 

agriculture,

 

we

 

believe

that

 

the

 

concept

 

of

 

yield

 

gaps

 

can

 

be

 

meaningful

 

when

 

at

 

least

 

two

main

 

components

 

of

 

the

 

total

 

absolute

 

gap

 

can

 

be

 

distinguished

and

 

studied

 

separately:

 

(1)

 

the

 

gap

 

between

 

the

 

water-limited

yield

 

potential

 

(

Y

W

)

 

and

 

the

 

locally

 

attainable

 

yield

 

(

Y

L

:

 

or

 

best

yields

 

attained

 

in

 

farmers’

 

fields),

 

which

 

provides

 

a

 

measure

 

of

yield

 

gap

 

attributable

 

largely

 

to

 

access

 

to

 

adequate

 

technologies,

and

 

(2)

 

the

 

gap

 

between

 

Y

L

and

 

the

 

average

 

yields

 

(

Y

A

)

 

farmers

obtain

 

across

 

their

 

heterogeneous

 

farms,

 

which

 

differences

 

across

farms

 

and

 

largely

 

attributable

 

to

 

access

 

to

 

resources.

Given

 

the

 

context

 

of

 

poor

 

agricultural

 

productivity,

 

of

 

about

1

 

Mg

 

ha

−

1

year

−

1

of

 

cereal

 

grain

 

across

 

much

 

of

 

sub-Saharan

 

Africa,

increasing

 

resource

 

use

 

efficiency

 

means

 

increasing

 

crop

 

primary

productivity

 

per

 

unit

 

resource

 

invested.

 

In

 

other

 

terms,

 

radiation

interception

 

in

 

space

 

and

 

time

 

and

 

its

 

conversion

 

through

 

pho-

tosynthesis

 

are

 

the

 

obvious

 

ecological

 

processes

 

that

 

need

 

to

 

be

addressed

 

first.

 

Of

 

the

 

three

 

pillars

 

of

 

ecological

 

intensification

 

pro-

posed

 

by

 

Cassman

 

(1999)

,

 

yield

 

potential,

 

soil

 

quality

 

and

 

precision

agriculture,

 

the

 

second

 

is

 

the

 

most

 

urgent

 

in

 

Africa.

 

Little

 

or

 

no

productivity

 

gain

 

can

 

be

 

expected

 

by

 

raising

 

the

 

yield

 

potential

when

 

current

 

yields

 

fluctuate

 

around

 

only

 

20%

 

of

 

that

 

achievable

(cf.

 

Tables

 

4

 

and

 

5

).

 

Degraded

 

and

 

poorly

 

responsive

 

soils

 

cover

large

 

areas

 

of

 

Africa,

 

and

 

represent

 

the

 

majority

 

of

 

poor

 

farmers’

fields

 

in

 

certain

 

regions

 

(cf.

 

Table

 

2

).

 

Yet

 

poorly

 

responsive

 

soils

are

 

hidden

 

due

 

to

 

the

 

patchwork

 

of

 

productive

 

and

 

unproductive

soils

 

across

 

landscapes,

 

coupled

 

with

 

the

 

location

 

of

 

more

 

fertile

fields

 

closer

 

to

 

roads

 

and

 

homesteads

 

which

 

can

 

mislead

 

those

 

con-

ducting

 

rapid

 

and

 

superficial

 

assessments.

 

The

 

fertilisers

 

that

 

are

generally

 

available

 

simply

 

do

 

not

 

work

 

on

 

degraded

 

soils.

 

Substan-

tial

 

investment

 

to

 

build

 

soil

 

organic

 

matter

 

is

 

needed

 

to

 

restore

such

 

soils

 

to

 

a

 

responsive

 

state.

 

A

 

form

 

of

 

precision

 

agriculture,

 

as

 

a

means

 

of

 

making

 

an

 

efficient

 

use

 

of

 

natural

 

resources

 

and

 

agricul-

tural

 

inputs,

 

can

 

be

 

redefined

 

for

 

Africa

 

as

 

a

 

practical

 

approach

 

for

targeting

 

technologies

 

across

 

scales.

 

There

 

is

 

a

 

need

 

for

 

targeting

 

in

a

 

“best

 

fit”

 

approach

 

from

 

a

 

basket

 

of

 

options,

 

rather

 

than

 

pushing

best-bet

 

approaches

 

or

 

“silver

 

bullet”

 

solutions

 

(

Giller

 

et

 

al.,

 

2011

).

The

 

water-limited

 

yield

 

potential

 

seems

 

to

 

be

 

a

 

more

 

sen-

sible

 

reference

 

to

 

calculate

 

yield

 

gaps

 

than

 

the

 

yield

 

potential

determined

 

by

 

radiation

 

and

 

temperature

 

in

 

such

 

rainfed

 

African

farming

 

systems.

 

However,

 

the

 

use

 

of

 

such

 

theoretical

 

yield

 

lev-

els

 

may

 

yet

 

mask

 

important

 

yield

 

differences

 

within

 

and

 

across

farms.

 

For

 

instance,

 

doubling

 

on-farm

 

cereal

 

yields

 

from

 

0.5

 

to

1

 

t

 

ha

−

1

year

−

1

may

 

have

 

a

 

substantial

 

impact

 

on

 

local

 

livelihoods;

but

 

such

 

changes

 

may

 

be

 

barely

 

detectable

 

when

 

relative

 

yields

are

 

calculated

 

against

 

a

 

yield

 

potential

 

of

 

e.g.,

 

12

 

t

 

ha

−

1

year

−

1

(from

 

4.1

 

to

 

8.3%).

 

Likewise,

 

yield

 

gaps

 

calculated

 

with

 

respect

 

to

yields

 

obtained

 

in

 

experimental

 

stations

 

may

 

also

 

be

 

misleading

as

 

they

 

are

 

often

 

located

 

in

 

the

 

most

 

productive

 

environments,

overestimating

 

attainable

 

yields

 

under

 

farmer

 

conditions.

 

Hence,

we

 

recommend

 

effort

 

should

 

be

 

invested

 

in

 

deriving

 

sound

 

esti-

mates

 

of

 

locally

 

attainable

 

yields,

 

Y

L

,

 

which

 

as

 

the

 

maximum

 

yields

attainable

 

in

 

farmers’

 

fields

 

over

 

years

 

are

 

a

 

more

 

meaningful

 

refer-

ence.

 

We

 

suggest

 

a

 

framework

 

for

 

yield

 

gap

 

analysis

 

that

 

recognises

the

 

heterogeneous

 

farming

 

systems

 

and

 

landscapes

 

of

 

smallholder

agriculture

 

(cf.

 

Fig.

 

9

).

 

A

 

sound

 

understanding

 

and

 

accurate

 

mea-

surements

 

of

 

yield

 

variability

 

is

 

essential

 

for

 

estimating

 

yield

 

gaps

(cf.

 

Fig.

 

8

),

 

and

 

probably

 

more

 

challenging

 

to

 

achieve

 

than

 

esti-

mates

 

of

 

water-limited

 

yield

 

potentials

 

which

 

can

 

be

 

derived

 

using

simulation

 

models.

The

 

importance

 

of

 

genotype

 

×

 

environment

 

interactions

 

is

undeniable,

 

and

 

plant

 

breeding

 

has

 

an

 

important

 

role

 

in

 

enhancing

nutritional

 

quality

 

as

 

well

 

as

 

adaptation,

 

resistance

 

and

 

resilience

in

 

the

 

face

 

of

 

abiotic

 

and

 

biotic

 

stresses.

 

Yet

 

cultivar

 

choices

 

of

sub-Saharan

 

Africa

 

smallholders

 

are

 

also

 

highly

 

influenced

 

by

local

 

food

 

habits,

 

markets

 

and

 

traditions.

 

For

 

instance,

 

some

 

of

the

 

local

 

varieties

 

cultivated

 

in

 

the

 

highlands

 

of

 

Kenya,

 

although

poorly

 

yielding

 

when

 

compared

 

with

 

current

 

tropical

 

hybrids,

 

are

highly

 

appreciated

 

for

 

their

 

early

 

maturity

 

that

 

allows

 

harvesting

green

 

cobs

 

for

 

roasting

 

at

 

a

 

time

 

of

 

food

 

scarcity

 

(

Tittonell

 

et

 

al.,

2010a

).

 

Discussing

 

the

 

choice

 

of

 

maize

 

cultivars

 

with

 

local

 

farm-

ers,

 

Figueroa

 

Gomez

 

de

 

Salazar

 

et

 

al.

 

(2008)

 

found

 

that

 

grain

 

yield

was

 

pondered

 

against

 

other

 

criteria

 

such

 

as

 

the

 

amount

 

of

 

fod-

der

 

biomass

 

harvestable,

 

yield

 

reliability

 

under

 

water,

 

nutrient

 

or

Page 14

Figures and page graphics, page 14

P.

 

Tittonell,

 

K.E.

 

Giller

 

/

 

Field

 

Crops

 

Research

 

143

 

(2013)

 

76–90

 

89

biotic

 

stresses,

 

the

 

size

 

of

 

the

 

cobs

 

or

 

even

 

some

 

aesthetic

 

features

of

 

the

 

cultivar

 

(vigour,

 

colour

 

and

 

height)

 

when

 

maize

 

is

 

grown

around

 

the

 

homesteads.

 

In

 

other

 

regions

 

with

 

prolonged

 

dry

 

sea-

sons,

 

post-harvest

 

storage

 

properties

 

may

 

be

 

more

 

important

 

than

the

 

potential

 

yield

 

of

 

a

 

genotype

 

(

Kydd,

 

1989

).

 

Switching

 

from

 

local

varieties

 

to

 

hybrids

 

is

 

not

 

always

 

seen

 

as

 

the

 

most

 

sensible

 

strategy

in

 

resource-poor,

 

risky

 

environments.

Our

 

analysis

 

suggests

 

that

 

an

 

important

 

fraction

 

of

 

the

 

yield

 

gap

may

 

be

 

reduced

 

through

 

proper

 

agronomic

 

management

 

(planting

dates,

 

spacing,

 

cultivars,

 

early

 

weeding,

 

etc.)

 

even

 

when

 

fertilis-

ers

 

are

 

not

 

applied.

 

Essentially

 

sound

 

agronomic

 

management

 

is

 

a

prerequisite

 

for

 

efficient

 

use

 

of

 

fertilisers

 

and

 

other

 

inputs.

 

Para-

doxically,

 

the

 

lack

 

of

 

investment

 

of

 

farmers’

 

labour

 

in

 

agriculture

may

 

in

 

turn

 

be

 

caused

 

by

 

the

 

lack

 

of

 

agricultural

 

inputs

 

required

to

 

allow

 

efficient

 

returns

 

to

 

labour,

 

and

 

the

 

local

 

soil

 

degradation

that

 

requires

 

large

 

investment

 

to

 

achieve

 

response

 

to

 

inputs

 

of

 

fer-

tilizer

 

and

 

labour

 

– a

 

so-called

 

‘poverty

 

trap’

 

(

Carter

 

and

 

Barrett,

2006;

 

Marenya

 

and

 

Barrett,

 

2007

)

 

– rather

 

than

 

due

 

to

 

lack

 

of

knowledge.

 

This

 

is

 

important

 

for

 

policy

 

setting

 

by

 

governments

and

 

their

 

development

 

funding

 

partners.

 

Actions

 

to

 

implement

 

the

“Abuja

 

declaration”

 

to

 

ensure

 

efficient

 

use

 

of

 

fertilisers

 

and

 

enhance

labour

 

productivity

 

(e.g.,

 

http://www.agra-alliance.org

)

 

need

 

con-

comitant

 

attention

 

to

 

restoration

 

of

 

exhausted

 

soils

 

to

 

a

 

healthy

and

 

responsive

 

state

 

(

Tittonell

 

et

 

al.,

 

2012

).

Due

 

either

 

to

 

resource

 

limitations,

 

to

 

local

 

preferences

 

in

 

the

choice

 

of

 

genotypes,

 

or

 

to

 

access

 

to

 

technologies

 

current

 

agricul-

ture

 

in

 

sub-Saharan

 

African

 

is

 

far

 

from

 

being

 

able

 

to

 

profit

 

from

the

 

ongoing

 

genetic

 

gains

 

in

 

yield

 

potential.

 

Estimating

 

the

 

rela-

tive

 

importance

 

of

 

resource

 

limitations

 

(

Y

L

−

 

Y

A

)

 

versus

 

inadequate

access

 

to

 

technologies

 

(

Y

W

−

 

Y

L

)

 

across

 

agro-ecological

 

zones

 

is

 

a

good

 

initial

 

step

 

to

 

inform

 

strategies

 

aimed

 

at

 

ultimately

 

narrowing

the

 

current

 

yield

 

gaps.

 

However,

 

yield

 

gaps

 

in

 

Africa

 

remain

 

wide

and

 

likely

 

to

 

increase

 

further

 

if

 

soil

 

degradation

 

is

 

not

 

reverted,

keeping

 

poor

 

farmers

 

confined

 

within

 

recurrent

 

poverty

 

traps.

Acknowledgements

We

 

thank

 

Lotte

 

Klapwijk

 

for

 

help

 

with

 

compiling

 

back-

ground

 

data.

 

This

 

research

 

was

 

partially

 

funded

 

by

 

the

 

European

Union

 

through

 

the

 

project

 

ABACO,

 

Agroecology-based

 

aggradation-

conservation

 

agriculture

 

(DCI-FOOD

 

2010/230-178).

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