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Land and Soil Issues in Africa:
Disturbance, succession and the promise
of ecological intensification
Tim Crews
The Land Institute
Bamako, Mali, September 4, 2015
Limitations to Productivity
-erosion by wind and water
-profound nutrient limitation
N, P and other elements
-phosphorus fixation on Fe and
Al oxides
-difficulty improving soil organic
matter status
-soil acidity
-low effective rainfall
(loss through runoff and
leaching)
Limitations to Productivity
-erosion by wind and water
-profound nutrient limitation
N, P and other elements
-phosphorus fixation on Fe and
Al oxides
-difficulty improving soil organic
matter status
-soil acidity
-low effective rainfall
(loss through runoff and
leaching)
Limitations to Productivity
-erosion by wind and water
-profound nutrient limitation
N, P and other elements
-phosphorus fixation on Fe and
Al oxides
-difficulty improving soil organic
matter status
-soil acidity
-low effective rainfall
(loss through runoff and
leaching)
Ecosystem Services
Regulating
• Biological pest control
• Pollination
• Nutrient mineralization
(Bommarco et al. 2013)
Driver: Biodiversity
Ecosystem Services
Regulating
• Biological pest control
• Pollination
• Nutrient mineralization
Supporting
• Soil formation and erosion
prevention
• Nutrient retention
• Build soil organic matter
--Soil structure (root
penetration, gas exchange,
water infiltration)
--Carbon storage and ghg
gas regulation
• Water infiltration, storage
and purification(Bommarco et al. 2013)
Driver: ?Driver: Biodiversity
frequencymagnitude
extent
Frequency + Magnitude + Extent
Global median changes in soil depth per year
in millimeters
Native
Ecosystem
No-till
Agriculture
Plowed
Agriculture
MontgomeryPNAS2007
+0.004 -0.065-1.520
Schlesinger1986
Loss of soil carbon to the atmosphere with plow conversion of
perennial plant communities to annual agriculture.
Temperate Grasslands Annual Grains
2.5 m
BNPP: 52, 67% (24-87%)
Annual turnover: 47-58%
Saugier et al. 2001,
Lauenroth and Gill 2003
BNPP: 15%
Annual turnover: 100%
Goudriaan et al. 2001
J. Richardson/J. Glover
Belowground Allocation (% of NPP)
Our food-producing
ecosystem is set back to--and
held--in a very early stage of
secondary succession
Implications?
nitrate leaching
gases (N2,N2O)
30-60% of the nitrogen
fertilizer applied to grain fields
is not taken up by the crop runof
f
“Discontinuous, insufficient or no fertiliser application over a certain
period of time may lead to severe soil degradation through nutrient
depletion and loss of organic matter. ….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.”
Tittonell & Giller 2013
Retro-succession
From secondary towards primary succession
Soils to parent material
Tittonell & Giller 2013
Tittonell & Giller 2013
Improve sustaining and regulating
ecosystem services
Water holding capacity
Aggregate structure
Belowground food web
Nutrient availability
J. Richardson/J. Glover
Soilprotection
Carbonandnutrientretention
Functionsofsoilmicrobiome
Wateruptakeefficiency +
-
S U C C E S S I O N
C entering from photosynthesis kg / m2 / yr
0.25 0.18
C in soil organic matter kg / m2
5.6 21.6
Desert Tundra
R
o
o
t
s
b
u
i
l
d
S
O
M
2011-Nature
Estimates of annual C sequestration from
grassland restoration and cellulosic
biofuel studies
Restored grasslands: 332 kg C ha-1 y-1 (31-13000)
Post & Kwon 2000
Miscanthus biomass 160-820 kg C ha-1 y-1
Mishra et al. 2013
J. Richardson/J. Glover
In the conversion of CRP land into cropland, one tillage
event resulted in the loss of ~8 years of carbon sequestration
being lost compared to no-till (herbicide) conversion
Glover et al. 2010
Relative abundance of nematode trophic groups from Culman et al. 2010
Perennial Hay MeadowAnnual Wheat
Annual sorghum in a very low fertility trial at ICRISAT, Mali
Pigeon pea in a very low fertility trial at ICRISAT, Mali
Using N to go after P?
~45 km north of London, 704mm precip yr-1, 120m elevation
Broadbalk Continuous
Wheat since 1844
Park Grass Hayed
Perennial Meadow
Since 1856
Rothamsted Research
0
2
4
6
8
10
12
14
16
18
0-23 24-46 47-69 70-92
µgPgdw-1soil
Soil depth (cm)
Broadbalk Without Fertilization (nil)
Annual Wheat
0
20
40
60
80
100
120
140
0-10 11-23 24-46 47-69 70-92
Soil depth (cm)
µgPgdw-1soil
Park Grass Without Fertilization (nil)
Perennial Hay
Comparison of resin-available Pi and microbial biomass Po with depth
= resin-available Pi
= microbial biomass Po
Crews & Brookes 2013
0
10
20
30
40
50
60
Active Po
Low Pi
Active cycling Po vs. as proportions of total P
%Pheldinfractions
Perennial
Annual
Perennial
Annual
No P Fertilizer + P Fertilizer
Photo: D. Larson
Udawattaetal.2008
macro-pores created by
large perennial roots
improve infiltration
Greater soil organic matter
contents improves water
storage
Deep roots expands crop
water uptake potential in
time and space
J. Richardson/J. Glover
Translocation of nutrients into
roots, rhizomes and crowns
Nutrient retention by deep roots
SOIL ORGANIC MATTER
• More N & P cycling in and out of
soil organic pools
• Shift in soil microbiome can favor
more efficient mycorrhizae and
N mineralizing microfauna
• Phosphorus stays available in
organic forms rather than
becoming fixed to Fe or Al oxides

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Land and Soil Issues in Africa: Disturbance, succession and the promise of ecological intensification

  • 1. Land and Soil Issues in Africa: Disturbance, succession and the promise of ecological intensification Tim Crews The Land Institute Bamako, Mali, September 4, 2015
  • 2. Limitations to Productivity -erosion by wind and water -profound nutrient limitation N, P and other elements -phosphorus fixation on Fe and Al oxides -difficulty improving soil organic matter status -soil acidity -low effective rainfall (loss through runoff and leaching)
  • 3. Limitations to Productivity -erosion by wind and water -profound nutrient limitation N, P and other elements -phosphorus fixation on Fe and Al oxides -difficulty improving soil organic matter status -soil acidity -low effective rainfall (loss through runoff and leaching)
  • 4.
  • 5. Limitations to Productivity -erosion by wind and water -profound nutrient limitation N, P and other elements -phosphorus fixation on Fe and Al oxides -difficulty improving soil organic matter status -soil acidity -low effective rainfall (loss through runoff and leaching)
  • 6.
  • 7. Ecosystem Services Regulating • Biological pest control • Pollination • Nutrient mineralization (Bommarco et al. 2013) Driver: Biodiversity
  • 8. Ecosystem Services Regulating • Biological pest control • Pollination • Nutrient mineralization Supporting • Soil formation and erosion prevention • Nutrient retention • Build soil organic matter --Soil structure (root penetration, gas exchange, water infiltration) --Carbon storage and ghg gas regulation • Water infiltration, storage and purification(Bommarco et al. 2013) Driver: ?Driver: Biodiversity
  • 9.
  • 12. Global median changes in soil depth per year in millimeters Native Ecosystem No-till Agriculture Plowed Agriculture MontgomeryPNAS2007 +0.004 -0.065-1.520
  • 13. Schlesinger1986 Loss of soil carbon to the atmosphere with plow conversion of perennial plant communities to annual agriculture.
  • 14. Temperate Grasslands Annual Grains 2.5 m BNPP: 52, 67% (24-87%) Annual turnover: 47-58% Saugier et al. 2001, Lauenroth and Gill 2003 BNPP: 15% Annual turnover: 100% Goudriaan et al. 2001 J. Richardson/J. Glover Belowground Allocation (% of NPP)
  • 15. Our food-producing ecosystem is set back to--and held--in a very early stage of secondary succession Implications?
  • 16. nitrate leaching gases (N2,N2O) 30-60% of the nitrogen fertilizer applied to grain fields is not taken up by the crop runof f
  • 17. “Discontinuous, insufficient or no fertiliser application over a certain period of time may lead to severe soil degradation through nutrient depletion and loss of organic matter. ….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.” Tittonell & Giller 2013 Retro-succession From secondary towards primary succession Soils to parent material
  • 20. Improve sustaining and regulating ecosystem services Water holding capacity Aggregate structure Belowground food web Nutrient availability J. Richardson/J. Glover
  • 22. C entering from photosynthesis kg / m2 / yr 0.25 0.18 C in soil organic matter kg / m2 5.6 21.6 Desert Tundra
  • 24. Estimates of annual C sequestration from grassland restoration and cellulosic biofuel studies Restored grasslands: 332 kg C ha-1 y-1 (31-13000) Post & Kwon 2000 Miscanthus biomass 160-820 kg C ha-1 y-1 Mishra et al. 2013 J. Richardson/J. Glover
  • 25. In the conversion of CRP land into cropland, one tillage event resulted in the loss of ~8 years of carbon sequestration being lost compared to no-till (herbicide) conversion
  • 26. Glover et al. 2010 Relative abundance of nematode trophic groups from Culman et al. 2010 Perennial Hay MeadowAnnual Wheat
  • 27. Annual sorghum in a very low fertility trial at ICRISAT, Mali
  • 28. Pigeon pea in a very low fertility trial at ICRISAT, Mali Using N to go after P?
  • 29.
  • 30. ~45 km north of London, 704mm precip yr-1, 120m elevation Broadbalk Continuous Wheat since 1844 Park Grass Hayed Perennial Meadow Since 1856 Rothamsted Research
  • 31. 0 2 4 6 8 10 12 14 16 18 0-23 24-46 47-69 70-92 µgPgdw-1soil Soil depth (cm) Broadbalk Without Fertilization (nil) Annual Wheat 0 20 40 60 80 100 120 140 0-10 11-23 24-46 47-69 70-92 Soil depth (cm) µgPgdw-1soil Park Grass Without Fertilization (nil) Perennial Hay Comparison of resin-available Pi and microbial biomass Po with depth = resin-available Pi = microbial biomass Po Crews & Brookes 2013
  • 32. 0 10 20 30 40 50 60 Active Po Low Pi Active cycling Po vs. as proportions of total P %Pheldinfractions Perennial Annual Perennial Annual No P Fertilizer + P Fertilizer
  • 35. macro-pores created by large perennial roots improve infiltration Greater soil organic matter contents improves water storage Deep roots expands crop water uptake potential in time and space
  • 36. J. Richardson/J. Glover Translocation of nutrients into roots, rhizomes and crowns Nutrient retention by deep roots SOIL ORGANIC MATTER • More N & P cycling in and out of soil organic pools • Shift in soil microbiome can favor more efficient mycorrhizae and N mineralizing microfauna • Phosphorus stays available in organic forms rather than becoming fixed to Fe or Al oxides