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When
yield
gaps
are
poverty
traps:
The
paradigm
of
ecological
intensification
in
African
smallholder
agriculture
Pablo
Tittonell
,
Ken
E.
Giller
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
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.,
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.
address:
(P.
Tittonell).
efforts
addressing
the
various
challenges
facing
current
agriculture
have
been
often
done
in
isolation
rather
than
holistically.
These
observations
have
prompted
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.,
).
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.
P.
Tittonell,
K.E.
Giller
/
Field
Crops
Research
143
(2013)
76–90
77
output
markets
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.,
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.,
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.,
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
where
response
to
inputs
is
poor
and
follows
an
‘S-shaped’
curve
(
Africa
needs
a
‘uniquely
African’
strategy
for
the
sustainable
intensification
of
its
agricul-
ture
(cf.
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
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
2.
The
pillars
of
ecological
intensification
following
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
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
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
(
genetic
progress
through
plant
breeding
played
a
central
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
:
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.,
In
this
paper
we
refer
to
the
water-limited
yield
potential
(
Y
w
)
as
defined
by
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
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
There
is
consensus
that
nutrient
supply,
rather
than
water,
is
the
main
yield-limiting
factor
in
sub-Saharan
Africa
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
(
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
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.,
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.,
Such
an
exercise
is
illustrated
in
for
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
(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
(
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
(
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
(
cutting
through
one
of
the
areas
of
highest
agricultural
potential
in
sub-Saharan
Africa.
2.1.3.
Non-cereal
crops
Although
the
analysis
of
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
(
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
and
as
high
as
75–90
t
ha
−
1
in
Colombia
or
India
(
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,
at
establishing
yield
thresholds
with
respect
to
soil
indicators
such
as
exchangeable
K
(
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
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
)
(
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
(
Using
the
boundary
line
approach
(
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
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.,
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.
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
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.,
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
(
However,
less
than
5%
of
banana
farmers
in
Uganda
use
any
type
of
mineral
fertiliser
(
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,
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.
One
of
the
weakest
points
in
the
calcula-
tion
of
nutrient
balances
is
the
estimation
of
flows
that
are
difficult
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.
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
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
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
Northwest
Tanzania
Banana-based
farming
systems
Kibanja
(banana)
18
26
−
8
Partial
balance
using
NUTMON
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
Sole
maize
(burning)
0
118
−
120
Southern
Mali
Cereal/cotton/pastoral
systems
Village
settlings
58
45
−
15
Complete
balance
using
NUTMON
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.
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
(
For
instance,
N
losses
by
leaching
assumed
by
different
authors
in
African
conditions
were
widely
variable:
8–15
kg
N
ha
−
1
year
−
1
10
kg
N
ha
−
1
year
−
1
11–26
kg
ha
−
1
year
−
1
(
or
36–153
kg
N
ha
−
1
year
−
1
Estimations
remain
uncertain,
and
may
often
lack
quantitative
rigour
(
Nonetheless,
the
work
of
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.,
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
(
Ghana
and
Uganda
(
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.,
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
(
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:
organic
fertilisers,
or
both
combined
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
(
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
(
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
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
(
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.
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
P.
Tittonell,
K.E.
Giller
/
Field
Crops
Research
143
(2013)
76–90
83
Fig.
6.
Cattle
densities
in
sub-Saharan
Africa
(World
Resources
Institute;
).
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
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.,
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
(
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
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
(
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
(
Thus
the
resulting
differences
in
yields
are
due
to
gradients
of
management
inten-
sity
rather
than
soil
fertility
alone
(
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.
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
and/or
with
micro-dosing
and
point-placed
application
of
nutrient
sources
Point
(iii)
deserves
most
attention
in
the
context
of
yield
gaps
and
their
biophysical
causes.
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
(
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.
an
example
of
soil
fertility
zoning
across
farm
types
in
the
vicinities
of
Murewa,
Zimbabwe
(
From
this
data
it
is
possible
to
roughly
assume
that
all
households
in
the
poorest
resource
categories
farm
on
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.,
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.,
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
(
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.,
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
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
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
actual
and
attainable
yields.
A
coarse
but
useful
first
approximation
to
average
crop
yields
per
country
is
the
FAOStat
database.
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.
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,
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.,
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
:
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
(
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.
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.
or
to
the
95th
percentile
yield
in
a
farmer
yield
survey
(cf.
Digital
soil
maps,
if
sufficiently
accurate,
could
provide
the
input
required
to
charac-
terise
soil
properties
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
(
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
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
to
the
water-
and
nutrient-limited
yield
level
defined
by
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
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.
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.
This
information,
together
with
knowledge
about
major
biotic
constraints
(weeds,
pest
and
diseases
–
cf.
exam-
ple
of
highland
banana
in
Section
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.
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.
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
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
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
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.
Degraded
and
poorly
responsive
soils
cover
large
areas
of
Africa,
and
represent
the
majority
of
poor
farmers’
fields
in
certain
regions
(cf.
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
(
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.
A
sound
understanding
and
accurate
mea-
surements
of
yield
variability
is
essential
for
estimating
yield
gaps
(cf.
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
(
Discussing
the
choice
of
maize
cultivars
with
local
farm-
ers,
that
grain
yield
was
pondered
against
other
criteria
such
as
the
amount
of
fod-
der
biomass
harvestable,
yield
reliability
under
water,
nutrient
or
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
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’
– 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.,
)
need
con-
comitant
attention
to
restoration
of
exhausted
soils
to
a
healthy
and
responsive
state
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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