A Holistic Approach Management Zones

8/14/2014
Precision Management of
Nutrients, Water, & Seeds:
A Holistic Approach
To identify and demonstrate the most
productive,
efficient,
profitable
and
sustainable variable rate-water, -nutrient
and –seed management strategies for
precision crop management
Raj Khosla
Colorado State University
Info Ag 2014
St. Louis, MO
Holistic crop management approach
Management Zones
Active remote-sensing
(micro-management)
A sub-region of a field that expresses
a homogeneous combination of yield
limiting factors
Management zones
(macro-management)
R. Khosla, Colorado State University
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8/14/2014
Management Zones
Management Zones…
1. Bare soil imagery
• Soil organic matter
• Moisture content and
• Other stable soil properties (bulk density, texture, compaction, etc)
Management Zones…
Management Zones…
2. Field topography
3. Farmer’s experience
Elevation map
Grain yields are correlated with topography
R. Khosla, Colorado State University
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8/14/2014
Management Zones…
Management Zones…
The three data layers
3. Farmer’s experience
Aerial Imagery
Topography
Farmer’s experience
• Previous management
• Familiarity with field
• Intuition
• Observations
• History of land use
• Tillage
• Pests and weeds
are stacked as GIS layers
to delineate the zone
Traits such as dark color, lowlying topography, and historic
high yields were designated as a
zone of potentially high
productivity or high zone
Low
Productivity
(Zone 3)
High
Productivity
(Zone 1)
Medium
Productivity
(Zone 2)
Mean grain yield across MZs
12
12
8
4
0
9
6
3
0
Low
Medium
High
Management zones
Overall findings
20
Grain yield (Mg ha -1)
Grain yield (Mg ha -1)
Grain yield (Mg ha -1)
16
Precision Nutrient Management Across Soil Zones…
has shown to enhance: 15
10
(i) overall grain yield of the field, 5
(ii) nutrient use efficiency, 0
Low
Medium
High
Management zones
Low
Medium
High
Management zones
(iii) net $ returns to farmers and (iv) reduces overall nutrient losses from the field. • What’s the problem?
R. Khosla, Colorado State University
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8/14/2014
Crop Based Management
N Rate (kg ha-1) = (135.3 x (NDVIRef. / NDVITarget)2) – (134.8 x (NDVIRef. / NDVITarget)) + 1
NDVI
0.41
NDVI
0.41
NDVI
0.41
2
N Rate (kg ha-1) = Crop
(135.3properties
x (NDVIRef.
+ Soil
/ NDVI
Properties
Target) ) – (134.8 x (NDVIRef. / NDVITarget)) + 1
NDVI
~96 lb/a
~96 lb/a
Medium
High
0.41
NDVI
~92 lb/a
~144 lb/a
0.41
NDVI
~96 lb/a
~37 lb/a
0.41
Low
Crop Sensing + Soil Sensing
Make better and most efficient nutrient
management decisions
Holistic crop management approach
Fertilizer
Crop sensing
Water
Precision water
management
MZ
R. Khosla, Colorado State University
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8/14/2014
Variability in soil water holding capacity at the field scale
Sand varies from 36 % to 78% (more than double)
Clay varies from 10 to 28 % (almost triple)
Source: http://www.soilsampling.com/services/soil‐characteristics/electrical‐conductivity‐mapping
A
Is there spatial variability?
B
System dating
to 1905
Sand: 39% 5%
Silt: 55% 75%
Clay: 6% 20%
R. Khosla, Colorado State University
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Precision irrigation based on
FC and MAD
25%
50%
75%
R. Khosla, Colorado State University
Capacitance
8/14/2014
Crop responds to drought stress
Quantifying the spatial variability
of soil moisture content
• How much of the field is
represented by the average?
• Is there a spatial pattern?
• How strong is the temporal
variability?
March
June
Adapted from Tom Trout’s
presentation, USDA-ARS
How much of the field is represented by the average?
1.8
1.6
1.4
1
Stress days (water logged)
1.2
No stress
0.8
0.6
0.4
0.2
Stress days (drought)
0
FC: Field Capacity, MAD: Max Allowable Depletion
Date
6
8/14/2014
Field 3100 at
Agriculture Research, Development and
Education Center of Colorado State University
Source: Timothy Gish, Hydrolab, ARS-USDA
Probe readings
Soil moisture in space
(Data at 42” deep)
0.00
2.25
0 - 8– 484
2.26
– 2.50
8 485
- 9 000
2.51
– 3.00
9 001
- 10 (in/ft)
000
3.01
– 3.50
10 010
- 11 000
3.51
– 4.00
11 010
- 12 000
4.01
– 4.51
12 010
- 13 000
6”
18”
June
July
Aug.
Sept.
30”
42”
54”
R. Khosla, Colorado State University
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8/14/2014
Stability over Time
What are the next steps?
May
1. Delineation of water management zones
r
r
r
r
12 dates
June
r
July
r
r
r
r
Aug.
r
r
r
r
r
r
Correlation Coefficient = r
(0 to 1.0) 0=different, 1.0 = 100% match
0
1
5
10
15
Time interval (weeks)
Temporal variability
May
June
r
r
r
r
July
r
r
Temporal variability
Aug.
r
r
r
r
June
July
r
r
r
May
Aug.
r
r
r
r
r
r
r
r
r
r
r
r
0
1 2
5
10
Time interval (weeks)
R. Khosla, Colorado State University
15
0
1 2
5
10
15
Time interval (weeks)
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8/14/2014
0 .8
0 .6
0.4
0.2
AtAt156”cm
AtAt4518”
cm
AtAt7530”
cm
42”cm
AtAt105
At
54”
At 135 cm
0.0
Average correlation (r)
1 .0
Site 1
0
1 2
5
10
15
Time interval (weeks)
0.5 m (mS/m)
EM38 at 1.0
[ARDEC_April18th2012_vertical_point].[CV_0_5M]
[ARDEC_April18th2012_vertical_point].[CV_1_0M]
0 - 13,4
27,5
- 39,3
13,4 -- 41,2
14,5
39,3
14,5 -- 42,7
15,4
41,2
Effect of VRI on yield
15,4 -- 44,3
16,4
42,7
16,4 -- 46,6
17,4
44,3
17,4 -- 50,3
18,9
46,6
18,9 -- 73,1
40,4
50,3
R. Khosla, Colorado State University
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8/14/2014
150
100
 Strong evidence of spatial and temporal
variability in precision levelled field.
 Identify surrogate data layers to delineate water
50
0
Yield (Bu/ac)
Effect of VRI on yield
management zones
a
a
a
a
ab
ab
b
40%
60%
80%
100%
Percentage of full irrigation
Holistic crop management approach
Variable rate seeding
Fertilizer
VRS based on
Yield map
Crop sensing
MZ
Water
Long-term (> 7 years) yield history
Doerge et al. 2006
Precision water
management
Yield maps are cheap
VR Planting
More profitable when
high variability
Seeds
Lowenberg-DeBoer 1998
R. Khosla, Colorado State University
High
Low
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8/14/2014
Variable rate seeding
Variable rate seeding
Better use of
available resources
Several factors can explain yield
o Intra-crop competition for:
P2O5
K 2O
NO3-
K 2O
P2O5
NO3-
Reduced crop-to-crop
competition
P2O5 K2O
NO3-
K 2O
NO3
P2O5
K 2O
P2O5
NO3
P2O5
K 2O
Soil moisture content
•
Sunlight
o Inter-row moisture
influencing disease
occurrence
NO3-
K 2O
K 2O
K 2O
P- 2O5
NO3-
Nutrients
•
o Crop competition to weeds
NO3-
NO3-
P2O5
-
•
NO3-
P2O5
Cu
P
K
Zn
o Germination rate
P
Mo
N
K
B
Mg
Ca
S
N
Fe
Mn
Cl
o Interplay of all factors
K 2O
P2O5
P2O5
Variable rate seeding
Uniform seed rate
Variable rate seeding
Yield map
Yield map
Example of reasons that could explain antagonist
effect:
•
Crust formation reducing germination rate
•
Limited water holding capacity
Variable seed rate
Increased
Increased
• Fine texture
• Low organic matter content
Decreased
R. Khosla, Colorado State University
• High salinity
Maintaining
population or coupling higher population
with
higherpopulation
irrigation could
Increasing
could have
have been
been aa better
better option
option
Decreased
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8/14/2014
Variable rate seeding
Variable rate seeding
Information from the soil is important
Medium yield
Higher yield
Topography
100
Electric conductivity
150
Yield (bu/ac)
200
Lower yield
Soil survey
Yield (historic)
20000
30000
40000
50000
Plant population (plants/ac)
Holistic crop management approach
Fertilizer
Water
Precision water
management
Crop sensing
MZ
Thank you
VR Planting
[email protected]
Seeds
R. Khosla, Colorado State University
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