Agroforestry for Improving Soil Health and Land Productivity...Ranjith Udawatta. The world would...
Transcript of Agroforestry for Improving Soil Health and Land Productivity...Ranjith Udawatta. The world would...
Agroforestry for
Improving Soil
Health and Land
Productivity
Ranjith Udawatta
The world would still
need 974 more calories
per person each day in
2050 even if all the food
produced in 2009 were
distributed to all people
in 2050
A huge calory need and uneven food distribution
Challenge Produce more
and high quality food
Middle class expansion (next 20 yrs)
73% more meat by 20502 billion in 2010 --- 4.9 billion in 2030
Brookings Institute
Meat consumption, Soil and Water
3
6
9
1950 60 70 80 90 00
Oz/day/person
3 billion People * 4 oz/day
750,000,000 lb meat/day
~1500 lb/animal
500,000 animals/day
Water need for 1lb
Beef 1850, chicken 519, bread 193 gal
USDA/Economic Research Service, www.ers.usda.gov
Challenge
Land Limitation/Productivity
Cynthia Nickerson, Robert Ebel, Allison Borchers, and Fernando Carriazo. 2011. Major Uses of
Land in the United States, 2007. USDA. Economic Information Bulletin 89
41 million ac Ag
land in US
1982-2007
7% more by 2030
1200 m2
0.3 ac
Actual soil erosion
rates are greater than
the upper limit of
tolerable soil erosion.
Erosion from Midwest cropland is
up to 12 times higher than the
federal government’s estimates.
Economists put the cost of soil
erosion between $60 and $100
billion per year.
Problems
Cox et al. 2011 Losing Ground. Environmental Working Group.
Actual soil erosion rates for tilled, arable land in
Europe are, on average, 3 to 40 times greater
than the upper limit of tolerable soil erosion.
Types of Soil Degradation FAO, 2015
(Global Assessment of Soil Degradation (GLASOD) evaluate 13 types of soil degradation)
1. Water erosion (topsoil loss and mass movement, including rill and gully formation)
2. Wind erosion (topsoil loss, terrain deformation– primarily dune activity)
3. Overblowing (surface burial from aeolian deposition)
4. Loss of nutrients
5. Loss of organic matter
6. Salinization
7. Acidification
8. Pollution
9. Compaction
10. Physical degradation
11. Waterlogging
12. Subsidence of organic soils
13. Water Scarcity
Water Quality
Water Body Total size Assessed(% of total)
Impaired(% of assessed)
Rivers 3,533,205 miles 16% 44%
Lakes 41.7 million acres 39% 64%
Estuaries 87,791 square miles 29% 30%
USEPA, 2013
Soil Erosion and Productivity
Al-Kaisi 2001. Soil erosion and crop productivity:
topsoil thickness
13%
30%
Stocking 2003. Tropical soils and
food security: The next 50 years.
Science, 302:1356-1359.
Problems
Agricultural output gains have shifted from input intensification in
1960s -1980s to efficiency gains in recent years
(rate of output growth, % per year)
WRR, 2013-14 World Resources Institute
Need to pay more attention on increase of efficiency
Efficiency Gains:
Selection of correct cultivar
Site specific management (land preparation,
efficient planting/seeding, fertilization,
irrigation, chemical application,… harvest)
Use of efficient equipment
Provide required input at the right time
Incorporation of weather data for management
decision
AGROFORESTRY
“Intensive land-use management
that Optimizes the benefits
(physical, biological, ecological,
economic, social) from biophysical
Interactions created when trees
and/or shrubs are Intentionally
Integrated combined with crops
and/or livestock”Gold and Garrett, 2009.
Paired watershed at Greenley Center Grazed Pasture watersheds at HARC
Google image 2014Google image 2015
Approximate study site location in Missouri and 0.5 m interval contour lines on
watersheds. Gray bands represent location of contour grass buffers on contour
strip watershed, agroforestry buffers on agroforestry watershed and grass
waterways on all three watersheds.
West Center East
1991-1997
2002
2005
2007
1999
2012
Soil Erosion and Nutrient Loss
Udawatta et al. 2002 and 2011. J Environ. Qual. 31:1214-1225 40:800-806.
Runoff
m3ha-1
39
43
48
1
3
5 1
3
5
5
Map of United
States
Profile view of well installation at (HARC)
Well 5 (3.6 m)
Well 1 (12.2 m)
Well 3 (10.7 m)
Ground water flow direction
Buffer
zone
20
LAKE
0
1
2
3
4
5
Co
nce
ntr
atio
n (
mg
L-1
)
NO3-N HARC 1-1
0
1
2
3
4
5
3 7 11 15 19 23 27 31 35 39 43 47 51
Co
nce
ntr
atio
n (
mg
L-1
)
Week of year
NO3-N HARC 1-5
Nitrate and Total NitrogenHARC
1-1
HARC
1-5
HARC
1-3
21
0
2
4
6TN HARC 1-1
0
2
4
6
3 10 17 24 31 38 45 52
Week of year
TN HARC 1-5
22
Well
locationsAverage SD SE
NO3-N
(mg L-1)
TN
(mg L-1)
NO3-N
(mg L-1)
TN
(mg L-1)
NO3-N
(mg L-1)
TN
(mg L-1)
Summit 2.72 3.35 1.11 1.51 0.10 0.19
Mid slope 2.53 2.99 1.25 1.15 0.15 0.26
Foot slope -
with
agroforestry
buffer
0.03 0.10 0.026 0.17 0.003 0.025
Foot slope -
with grass
buffer0.09 0.30 0.052 0.31 0.007 0.046
HARC
1
HARC
5
HARC
3
HARC 1
HARC
5
HARC
3
HARC
1-1
HARC
1-5
HARC
1-3
HARC
2-1HARC
2-5
HARC
2-3
2004 Monthly Precipitation and
Cropping Period
Figure 5.
0
75
150
225
J F M A M J J A S O N D
Pre
cip
itation (
mm
)
2004Corn
5/22/04
Long-term
precipitation
670 mm
(944mm)
Runoff Control
After NRCS, 2002
Reported Effectiveness of Buffer Zone Width for Sediment Reduction in the USA (Earlier studies)
Runoff reduction varies with buffer width and ranged between 40 and 100%
Wider the better
Liu et al., 2008. Major factors influencing the efficacy of
vegetated buffers on sediment trapping: a review and
analysis. J. Environ. Qual. 37, 1667-1674
Buffer width and water quality
Mayer et al., 2005. Riparian Buffer Width, Vegetative
Cover, and Nitrogen Removal Effectiveness: A Review
of Current Science and Regulations EPA/600/R-
05/118. October 2005
Riparian Forest Buffer
Planned combinations of trees, shrubs, grasses, forbs & bioengineered structures designed to mitigate the impact of land-use on a stream or lake.
4 year old RFB
Native Grass
Shrubs Trees
Four-zone riparian buffer and environmental benefits and associated
buffer widths. Different widths for different pollutants.
Naiman, R., H. Decamps, and M. McClain. Riparia. 2005, Elsevier
Image taken March 23, 1992
Image taken February 23, 1995
Image taken August 13, 2009
APEX Model Assessment of
Environmental Benefits of
Agroforestry/Grass Buffers
MODEL SIMULATIONAPEX
TopographyManagement
Soil Data
0
400
800
1200
1600
1991 1993 1995 1997 1999 2001 2003 2005
Precipitation
Measured
Data
Simulations Crop and buffer
areas were
simulated as
separate subareas.
Model calibration:
using agroforestry
buffer (grass and
tree) watershed
data (1998-2008, 43
events).
Model validation:
using grass buffer
watershed data.
Scenario analysis% area under buffers and placement
• 20% area in upland contour buffers
• 10% backslope 10% toeslope flat shape buffer
• 10% backslope 10% toeslope v-shape buffer
• 20% toeslope flat shape buffer
• 20% toeslope v-shape buffer
• 20% backslope buffer
Runoff Simulations
0
50
100
1500
3/2
9/9
80
4/0
8/9
80
4/1
5/9
80
4/2
8/9
80
5/0
7/9
80
5/1
2/9
80
5/2
3/9
80
6/0
8/9
80
6/1
5/9
80
6/1
8/9
80
6/2
3/9
80
6/2
9/9
81
0/0
5/9
81
0/1
7/9
81
1/1
0/9
81
2/0
6/9
80
4/1
6/9
90
5/0
5/9
90
5/1
7/9
90
4/2
2/0
10
5/0
6/0
10
5/1
3/0
10
6/0
1/0
10
6/0
6/0
10
5/0
1/0
20
5/0
9/0
20
5/2
5/0
20
6/1
3/0
20
4/3
0/0
30
5/1
0/0
30
9/1
8/0
30
9/2
1/0
30
4/2
0/0
40
5/3
1/0
40
6/1
5/0
40
8/2
8/0
40
6/0
5/0
50
6/0
8/0
50
5/0
6/0
70
4/2
5/0
80
5/1
1/0
80
6/1
8/0
8Ru
no
ff (
mm
)
Storm event
Mearsured runoff Simulated runoff
0
50
100
150
03
/29
/98
04
/08
/98
04
/15
/98
04
/28
/98
05
/07
/98
05
/12
/98
05
/23
/98
06
/08
/98
06
/15
/98
06
/18
/98
06
/23
/98
06
/29
/98
10
/05
/98
10
/17
/98
11
/10
/98
12
/06
/98
04
/16
/99
05
/05
/99
05
/17
/99
04
/22
/01
05
/06
/01
05
/13
/01
06
/01
/01
06
/06
/01
05
/01
/02
05
/09
/02
05
/25
/02
06
/13
/02
04
/30
/03
05
/10
/03
09
/18
/03
09
/21
/03
04
/20
/04
05
/31
/04
06
/15
/04
08
/28
/04
06
/05
/05
06
/08
/05
05
/06
/07
04
/25
/08
05
/11
/08
06
/18
/08
Ru
no
ff (
mm
)
Storm event
Model calibration by agroforestry buffer watershed
Model validation by grass buffer watershed
Performance indicatorsModel output
Model Coefficients
Calibration Validation
Agroforestry buffer WS
Grass buffer WS
Event Runoff
r2 0.82 0.77
NSC 0.80 0.73
Pbias 2.17 7.72
Event sediment
r2 0.39 0.18
NSC 0.28 0.07
Pbias 7.90 -15.59
Event total P
r2 0.61 0.69
NSC 0.55 0.57
Pbias -10.15 15.39
30 year
simulation
Scenario
% Annual Average Reductions
Runoff Sediment TP
AGF CGS AGF CGS AGF CGS
With upland buffers 20 10 58 54 24 20
10% flat toeslope
10% Back slope buffers 21 11 77 76 23 19
10% v-shape toeslope
10% Back slope buffers 22 10 76 75 26 21
20% flat toeslope buffers 16 6 62 61 19 15
20% v-shape toeslope buffers 20 10 63 63 22 18
20% backslope buffers 21 10 56 54 23 19
• APEX model quantified the benefits of
agroforestry and grass buffers and
their different placement shapes and
proportions.
• Buffers reduce 6-22% runoff, 54-77%
sediment, 15-26% TP.
• 10% back-slope 10% toe slope buffers
reduced highest amount of sediments
than other treatments.
• Toeslope buffers were better for
sediment reductions than the
backslope buffers.
Soil Physical PropertiesCores:
0-10
10-20
20-30
30-40
40-50 cm
Bulk density and saturated hydraulic conductivity (Ksat) for row
crop, grass buffer, and agroforestry buffer
treatments by soil depth.
0
10
20
30
40
50
1.0 1.2 1.4 1.6
Bulk Density (g cm-3)
De
pth
(c
m)
Crop
Grass
AGF
0
10
20
30
40
50
0 10 1000
Ksat (mm hr-1)
Dep
th (
cm
)
Crop
Grass
AGF
Seobi et al 2005. Agroforestry influence on soil hydraulic properties. Soil Sci Soc Am J 69:893-901.
Soil Pores and Agroforestry
Pore scale (x-ray CT, micro-computed tomography)
Gantzer and Anderson, 2006
Udawatta and Anderson, 2008. Geoderma 145:381-389
Water Stable Aggregate
0
10
20
30
40
Crop Grass Agroforestry Grass
Waterway
Wat
er S
table
Aggre
gat
es (
%)
Udawatta et al., 2008 Applied Soil Ecology 39:153-160
0
10
20
30
40
1-Oct 6-Oct 11-Oct 16-Oct 21-Oct 26-Oct 31-Oct
Date
Pre
cip
itati
on
(m
m)
Daily Precipitation During
October 2004 Recharge Period166 mm
Soil Water Storage
Campbell TDR soil
moisture sensors
were installed on
two transects
Study Design
Buffer
Pin oak
5 cm
10 cm
20 cm
40 cm
Senor depths
Data logger
Sensor locations
Soil Water Recharge (5 and 10 cm depths)
0.00
0.10
0.20
0.30
0.40
0.50
0.60
Oct 7,
6:00
Oct 8,
6:00
Oct 9,
6:00
Oct
10,
6:00
Oct
11,
6:00
Oct
12,
6:00
Oct
13,
6:00
Oct
14,
6:00
Oct
15,
6:00
Oct
16,
6:00
Oct
17,
6:00
Oct
18,
6:00
Oct
19,
6:00
Oct
20,
6:00
Oct
21,
6:00
Oct
22,
6:00
Date and Time
VWC
(cm
cm
-3)
Corn
Tree5 cm Depth
0.00
0.05
0.10
0.15
0.20
0.25
0.30
0.35
0.40
0.45
0.50
Oct 7,
6:00
Oct 8,
6:00
Oct 9,
6:00
Oct
10,
6:00
Oct
11,
6:00
Oct
12,
6:00
Oct
13,
6:00
Oct
14,
6:00
Oct
15,
6:00
Oct
16,
6:00
Oct
17,
6:00
Oct
18,
6:00
Oct
19,
6:00
Oct
20,
6:00
Oct
21,
6:00
Oct
22,
6:00
Date and Time
VWC
(cm
cm
-3)
Corn
Tree10 cm Depth
0
10
20
30
40
1-Oct 6-Oct 11-Oct 16-Oct 21-Oct 26-Oct 31-Oct
Date
Pre
cip
itati
on
(m
m)
Soil Water Recharge (20 and 40 cm depths)
0.00
0.05
0.10
0.15
0.20
0.25
0.30
0.35
0.40
0.45
0.50
Oct 7,
6:00
Oct 8,
6:00
Oct 9,
6:00
Oct 10,
6:00
Oct 11,
6:00
Oct 12,
6:00
Oct 13,
6:00
Oct 14,
6:00
Oct 15,
6:00
Oct 16,
6:00
Oct 17,
6:00
Oct 18,
6:00
Oct 19,
6:00
Oct 20,
6:00
Oct 21,
6:00
Oct 22,
6:00
Date and Time
VW
C (c
m c
m-3
)
Corn
Tree20 cm Depth
0.00
0.05
0.10
0.15
0.20
0.25
0.30
0.35
0.40
0.45
Oct 7,
6:00
Oct 8,
6:00
Oct 9,
6:00
Oct
10,
6:00
Oct
11,
6:00
Oct
12,
6:00
Oct
13,
6:00
Oct
14,
6:00
Oct
15,
6:00
Oct
16,
6:00
Oct
17,
6:00
Oct
18,
6:00
Oct
19,
6:00
Oct
20,
6:00
Oct
21,
6:00
Oct
22,
6:00
Date and Time
VW
C (c
m c
m-3
)
Corn
Tree
40 cm Depth
0
1
2
3
Crop Grass Agroforestry Grass
waterways
So
il C
arb
on
(%
)
0.00
0.05
0.10
0.15
0.20
0.25
So
il N
itro
gen
(%
)
Carbon Nitrogen
Soil Carbon and Nitrogen
Udawatta et al., 2008. Agriculture, Ecosystems and Environment 131:98-104
Carbon SequestrationAGROFORESTRY is recognized as an activity
under Afforestation and Reforestation activities
that have been approved as a GHG mitigation
strategy under the Kyoto Protocol.
Reduction of 1 Pg from soil = 0.47 ppm CO2 to atmosphere
(Lal, 2001).
0
10
20
30
40
50
60
70
Semiarid Subhumid Humid Temperate
Mg
C h
a-1
Average C storage by Agroforestry Practices
Montagnini and Nair 2004
Carbon Sequestration
Agroforestry systems have a greater
Potential to sequester C than pasture
or cropping systems (Sanchez, 2000;
Sharrow and Ismail, 2004; Kirkby and Potvin, 2007).
Alley cropping systems sequester 142 Tg C yr-1.
(Lal et al., 1999)
C Seq capacity in agroforestry varies from 0.29 to 15.21
Mg C ha-1 yr-1 (landuse, soil, mgt, spp, age, climate,
stand age, aggregates; Nair et al 2009)
Carbon Sequestration:
Corn Soybean Grass
Tree Roots1. Depth2. Volume3. Carbon form (recalcitrant)4. Root exudates (leaching)5. Root Turnover (33% NPP fine root)
6. Associated microbial communities C, exudates, turnover
More
above- and
below-
ground C
in tree
areas
than grass
and crop
areasTrees and perennial vegetation within agriculture help improve SQ, greater C accumulation diverse soil communities and activities Tufekoioglu et al 2003
Fine root
biomass
of trees
and
grasses
were
greater
than
annual
crops
Tufekoioglu et al 1999
Above and belowground biomass and C of 2, 8,
12, and 60 year riparian stand in South Carolina
Giese et al., 2003
Soil C% 4.2 4.7 4 11.4
Distance from trees and by time Alleycropping
Thevathasan and Gordon, 1997
Grazing system: root biomass and root C
Kumar et al., 2010
Above and belowground biomass and C for
shelterbelt species
Kort and Turnock, 1999
Nair, P.K.R., B.M. Kumar, and V.D. Nair. 2009. Agroforestry as a strategy for carbon
sequestration. J Plant Nutrition and Soil Science. 172. 10-23.
164 published manuscripts have been used.
Lack of data and differencesin estimationmethodsaffectedfinaloutcome
A comparison of C sequestration potential for
different management practices
Udawatta, R.P. and S. Jose, 2012. Agroforestry strategies to sequester carbon in temperate North America. Agroforestry Systems 86:225-242.
Riparian buffers
Alley Cropping
Windbreaks
and Silvopasture could sequester
548.4 Tg C year-1
Current US CO2 emission is 6870
million metric tons or 1874 Tg C
Agroforestry can offset current C
emission by 34%
Udawatta, R.P. And S. Jose. 2011. Carbon sequestration potential of agroforestry
practices in temperate North America. 17-42. Advances in Agroforestry. Springer
Organic Matter on Available Water Capacity
Silt loam
OM increase from 1% to 4.5%
AWC doubles!
5.7% 22.9% (% by Vol.)
Data from Soil Survey Investigation Reports
(surface horizons only)
- Sands: FL (n = 20)
- Silt loams: IA, WI, MN, KS (n = 18)
- Silty clay loams: IA, WI, MN, KS (n = 21)
Sands AWC = 3.8 + 2.2 (OM)
r2 = 0.79
Silt loams AWC = 9.2 + 3.7(OM)
r2 = 0.58
Silty clay loams AWC = 6.3 + 2.8 (OM)
r2 = 0.76
Hudson, B. D. 1994. Soil organic matter and available
water capacity. J. Soil Water Conserv. 49(2):189-194.
Soil Enzymes
0
20
40
60
80
100
120
p-n
itro
ple
ny
l p
rod
uct
ion
(μg
/ g
-1d
ry s
oil
h-1
)
0
25
50
75
100
125
p-n
itro
ph
eny
l
pro
du
ctio
n
(μg/
g-1
dry
soil
h-1
)
0
1
2
Crop Grass Agroforestry Grass Waterway
Flo
ure
cein
pro
du
ctio
n
(μg
g-1
dry
so
il h
-1)
0
2
4
6
8
Crop Grass Agroforestry Grass Waterway
Tri
phen
ylf
orm
azan
pro
duct
ion
(μg/
g-1
dry
soil h
-1)
β-glucosidase Glucosaminadase
Dehydrogenase FDA
c b a a
c b a ab b b a
c a b b
Perennial
Vegetation
buffers have
increased
microbial
diversity and
enzyme
activities.
Udawatta et al., 2008. Agriculture, Ecosystems and Environment 131:98-104
21-year old
pecan alley
cropping.
Greater
Enzyme
activity
diversity
in tree rows
than middle
of tree rows
in crop allies.
Mungai, N.W., P.P. Motavalli, R.J. Kremer, and K.A Nelson. 2005. Spatial variation of soil enzyme activities and
microbial functional diversity in temperate alley cropping systems. Biol Fertil Soils 42:129-136.
Soil Enzymes
Lin, C.H., K.W., Goyne, R.J. Kremer, R.N. Lerch, and H.E. Garrett. 2010. Dissipation of sulfamethazine and tetracycline in the root zone of grass and tree species. Journal of Environmental Quality 39:1269-1278
Rhizodegradation of antibiotics
Lin, C.-H., R.N. Lerch, K.W. Goyne, and H.E. Garrett. 2011. Reducing herbicides and veterinary antibiotic losses from agroecosystems using vegetative buffers. J. Environ. Qual. 40:791-799.
Lin, C.-H., R.N. Lerch, K.W. Goyne, and H.E. Garrett. 2011. Reducing herbicides and veterinary antibiotic losses from agroecosystems using vegetative buffers. J. Environ. Qual. 40:791-799.
Chu, B., K.W Goyne, S.H. Anderson, C.H. Lin, and R.P. Udawatta 2010. Veterinary antibiotic sorption to agroforestry buffer, grass buffer, and cropland soils. Agroforestry Systems 79:67-80
Soils under
agroforestry and
grass buffer
exhibit enhanced
sorption of
oxytetracycline
and sulfadimethoxine relative
to cropland.
This suggests that the sorptive
capabilities of buffer soils help
reduce the loss of veterinary
antibiotics from
agroecosystems.
Maintaining an efficient nutrient
cycling improve soil quality and
provides other services
including improved water
quality, food security and
ecosystem services
Lal 2010 Bioscience 60:708-721
Soil Heat Transfer
Adhikari, P., R.P. Udawatta, S.H. Anderson, and C.J. Gantzer. 2014. Soil thermal properties under prairies, conservation buffers,
and corn/soybean land use systems. Soil Science Society of America Journal 78:1977-1986.
Thermal conductivity Thermal diffusivity
Soil Heat Transfer
Adhikari, P., R.P. Udawatta, S.H. Anderson, and C.J. Gantzer. 2014. Soil thermal properties under prairies, conservation buffers,
and corn/soybean land use systems. Soil Science Society of America Journal 78:1977-1986.
Volumetric heat capacity
Significantly lower thermal
conductivity and diffusivity
and higher volumetric heat
capacity were observed
under TP, PF, AGF, and
GB compared with the
COS land use system.
Similarly, these prairies
and conservation buffer
land use systems had
higher SOC and lower BD
than the COS at the 0- to
10- and 10- to 20-cm
depths.
• New Varieties
• Fertilizer
• Pesticide
• Machinery
• Technology
Management
• Physical
• Chemical
• Biological
• Conservation
Soil Quality
• Supply
• Market
• Loans/banks
• Land Reform Policy
Ecosystem
Services
Increased
AG
Production
Food
Security
Pollinators and AgroforestryApproximately 80% of all flowering plant species
are pollinated by animals, mostly insects
Pollinators are needed for 35% of the world's crop
production
Increase the output of 87 of the leading food crops
worldwide
Pollinators are critical to crop production, provides
an essential ecosystem service
Multi spp buffers with native and other plants with
year round flowering
Silvopasture Cattel Weight and IncomeSide-by-side
2 years
Traditional “open” pastures with limited shade
Integrated silvopasture x open pasture where 25% of
the pasture area is silvopasture and 75% of the
pasture area is a traditional open pasture
Cows in the Integrated system
Lost approximately 10%
less weight over winter
Had less stress at calving
Weaned heavier calves
Treatment Cow BW
loss over
winter
(lbs)
Calving
Difficulty
%
Calf
Weaning
Weight
(lbs)
Traditional 231 17 595
Integrated 205 4 650
p value 0.02 0.04 0.01
$ value $16.89 - $25.74
2009 Study $43
Current monitory value is ~$52 per cow calf pair
Silvopasture Profitable Agroforestry
Kallenbach, R. 2009. Agroforestry Comes of Age, Proc North Ame. Agroforestry Conference.
Forage growth begins earlier in the spring and continues later into the fall
Forage yields are higher in the heat of summer
Better quality forage
Optimal distribution (reduce hay need and $)
Reduced Heat stress and better weight gain
$43 (2009) per cow calf pair
Ginseng
Profitable
Agroforestry
At the current
prices, a half
acre could
produce
$100,000 worth
of seeds and
roots over a six
year period, or
over $16,000
per year.
Shiitake
Mushroom
Profitable
Agroforestry
Steve Gabriel, 2015. http://smallfarms.cornell.edu/2015/01/12/mushrooms/
The Center for Agroforestry