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Toward Sustainable Nitrogen and
Carbon Cycling on Diversified
Horticulture Farms Serving Community
Food Systems
Krista L. Jacobsen, Debendra Shresta, Department of Horticulture, University of
Kentucky
Ole Wendroth*, Department of Plant and Soil Sciences, University of Kentucky
John Schramski, College of Engineering, University of Georgia
*presenting author
2013-67019-21403
Introduction
 Project Background & Context
 Project overview
 Highlights from one of the field experiments
 Overview of modeling objectives and goals
Background and Context
 Small- and medium-scale, diversified farms are important
sources of agricultural products for the local and regional food
movement
 Local food purchases are increasingly valued by the public for
perceptions of healthier products due to “freshness,”
conservation of local farm lands, and/or supporting local farmers
(Onozaka et al, 2010)
 Horticultural crops are a large part of this market
 Fruits, vegetables and nuts were 70% of local food sales in 2007
(Low & Vogel, 2011).
 Diversification into horticultural crops serving local markets is a
global trend for small-holder farmers (Weinberger and Lumpkin,
2007), as horticultural crops are typically higher in value per unit
area than cereals (USDA-NASS, 2009)
Background and Context
 However, much of what we know about C and N cycling in agroecosystems
comes from agronomic systems, less research in horticulture systems (e.g.
West & Post, 2002; Ma & Shaffer, 2001)
 Further, production practices are highly variable, with little standard rotation
varying degree of intensity
Example: A lower input
system, with no
supplemental irrigation,
“living mulch” between
rows, and seasonal
production
Example: Green bean
production in a high tunnel
system, with drip
supplemental irrigation,
intense-tillage, in a year-
round production system
Project Objectives
 Broadly, to improve our understanding of how intensification on diversified
horticulture-based farms influences (1) nitrogen availability, efficiency, and
retention and (2) soil carbon dynamics in labile carbon pools.
Project Objectives:
 Specifically…
 (i) In addition to C and N dynamics, we are also seeking to better understand the net
effects of intensification on whole system C balances using Energy Returned on Energy
Invested (akin to life cycle analysis) approaches.
 More on this next year…
Project Objectives
 Specifically…
(ii) to compare the nitrogen dynamics and key loss pathways in five farming
systems, including four organic systems, representing a gradient of
intensification (characterized by quantity of inputs, and the frequency of tillage
and fallow periods)
Project Objectives:
 Specifically…
 (iii) to identify the sensitivity of a model to measured parameters to describe the key
plant growth and soil processes.
Soil input:
Soil hydraulic properties
Status of soil moisture and
different C- and N-
fractions
Plant input:
Growth status, root
development
-30
-20
-10
0
10
20
30
0
1
2
3
4
5
AirTemp(°C)
Precipitation(inch)
Precipitati
on (Inch)
0
200
400
600
800
TOTALFLUX(MGCO2M-2HR-1
CO2 FLUX
Extensive Organic system Conventional system Stationary Organic High Tunnel system
-100
-50
0
50
100
150
200
250
300
350
400
N2OFLUXUGM-2HR-1
N2O FLUX
Extensive Organic system Conventional system Stationary Organic High Tunnel system
First results on GHG fluxes in different horticultural systems
New RZWQM GHG Submodel (Fang et al., 2015)
N2O emission (N2O_nit) from DAYCENT, fixed proportion of
nitrification (Rnit) modified by a soil water factor (FSW_Nit) (Gillette et
al., 2017) with WFPS as the water-filled pore space
nitNitSWNitnit RFFr  _ON_2 _ON 2
04.1
04.14.0
_



WFPS
WFPS
F NitSW
denDenONden RFrON  __2 2
New: diffusion factor for taking into account N2O diffusion across
different soil depths.
09/01/2009 02/28/2010 08/27/2010 02/23/2011 08/22/2011
0
50
100
150
PRECIPITATION(mm)
-15
-5
5
15
25
35
Tavg
PRECIP.
AIR-TEMP.
09/01/2009 02/28/2010 08/27/2010 02/23/2011 08/22/2011
0.00
0.04
0.08
0.12
0.16
0.20
N2O-FLUX(kgN/ha/day)
N2O-MEASURED
N2O SIMULATED
CROP (WHEAT)
n = 30
09/01/2009 02/28/2010 08/27/2010 02/23/2011 08/22/2011
Date
0.0
0.1
0.2
0.3
0.4
0.5
SWC(cm3
cm-3
)
SWC 0-10 cm
6/1/2010 8/1/2010 10/1/2010 12/1/2010 1/31/2011 4/2/2011 6/2/2011
0
40
80
DAILYPRECIP.
(mm)
-10
10
30
AIRTEMP.(C)
PREC.
AIR-TEMP.
6/1/2010 8/1/2010 10/1/2010 12/1/2010 1/31/2011 4/2/2011 6/2/2011
5
7
9
SWS0-30cm
(cm)
-10
10
30
SOILTEMP.(C)
SWS SOIL TEMP.
6/1/2010 8/1/2010 10/1/2010 12/1/2010 1/31/2011 4/2/2011 6/2/2011
0
10
20
qCO2
(mgm-2
min-1
)
0.0
0.5
1.0
1.5
CVqCO2
qCO2 CVqCO2
6/1/2010 8/1/2010 10/1/2010 12/1/2010 1/31/2011 4/2/2011 6/2/2011
0
5
10
15
NUGGETC0
(mgm-2
min-1
)2
0
50
100
150
200
250
RANGEa(m)
NUGGET C0qCO2
RANGE aqCO2
6/1/2010 8/1/2010 10/1/2010 12/1/2010 1/31/2011 4/2/2011 6/2/2011
DATE
0.0
0.5
1.0
C0/(C+C0)
0
10
20
STDqCO2
NUGGET/SILL qCO2
STD qCO2
RESULTS
• Temporal stability of CO2 flux
• rank relationship to surface soil water storage
• What are the main drivers of CO2 flux
6/1/2010 8/31/2010 11/30/2010 3/1/2011 5/31/2011
DATE OF MEASUREMENT
-1.0
-0.5
0.0
0.5
1.0
SPEARMANRANKCORRELATIONrs
qCO2
qCO2 - WS0-30
JUNE 08, 2010
6/1/2010 8/1/2010 10/1/2010 12/1/2010 1/31/2011 4/2/2011 6/2/2011
5
7
9
SWS0-30cm
(cm)
-10
10
30
SOILTEMP.(C)
SWS SOIL TEMP.
CO2 flux Pattern Development and Dependence on Soil Moisture during
one year.
6/1/2010 8/31/2010 11/30/2010 3/1/2011 5/31/2011
DATE OF MEASUREMENT
-1.0
-0.5
0.0
0.5
1.0
SPEARMANRANKCORRELATIONrs
qCO2
qCO2 - WS0-30
JUNE 08, 2010
6/1/2010 8/1/2010 10/1/2010 12/1/2010 1/31/2011 4/2/2011 6/2/2011
5
7
9
SWS0-30cm
(cm)
-10
10
30
SOILTEMP.(C)
SWS SOIL TEMP.
6/1/2010 8/31/2010 11/30/2010 3/1/2011 5/31/2011
DATE OF MEASUREMENT
-1.0
-0.5
0.0
0.5
1.0
SPEARMANRANKCORRELATIONrs
qCO2
qCO2 - WS0-30
JUNE 21, 2010
6/1/2010 8/31/2010 11/30/2010 3/1/2011 5/31/2011
DATE OF MEASUREMENT
-1.0
-0.5
0.0
0.5
1.0
SPEARMANRANKCORRELATIONrs
qCO2
qCO2 - WS0-30
JULY 06, 2010
6/1/2010 8/31/2010 11/30/2010 3/1/2011 5/31/2011
DATE OF MEASUREMENT
-1.0
-0.5
0.0
0.5
1.0
SPEARMANRANKCORRELATIONrs
qCO2
qCO2 - WS0-30
JULY 19, 2010
6/1/2010 8/31/2010 11/30/2010 3/1/2011 5/31/2011
DATE OF MEASUREMENT
-1.0
-0.5
0.0
0.5
1.0
SPEARMANRANKCORRELATIONrs
qCO2
qCO2 - WS0-30
AUG. 02, 2010
6/1/2010 8/31/2010 11/30/2010 3/1/2011 5/31/2011
DATE OF MEASUREMENT
-1.0
-0.5
0.0
0.5
1.0
SPEARMANRANKCORRELATIONrs
qCO2
qCO2 - WS0-30
AUG. 16, 2010
6/1/2010 8/31/2010 11/30/2010 3/1/2011 5/31/2011
DATE OF MEASUREMENT
-1.0
-0.5
0.0
0.5
1.0
SPEARMANRANKCORRELATIONrs
qCO2
qCO2 - WS0-30
SEP. 02, 2010
6/1/2010 8/31/2010 11/30/2010 3/1/2011 5/31/2011
DATE OF MEASUREMENT
-1.0
-0.5
0.0
0.5
1.0
SPEARMANRANKCORRELATIONrs
qCO2
qCO2 - WS0-30
SEP. 16, 2010
6/1/2010 8/31/2010 11/30/2010 3/1/2011 5/31/2011
DATE OF MEASUREMENT
-1.0
-0.5
0.0
0.5
1.0
SPEARMANRANKCORRELATIONrs
qCO2
qCO2 - WS0-30
SEP. 30, 2010
6/1/2010 8/31/2010 11/30/2010 3/1/2011 5/31/2011
DATE OF MEASUREMENT
-1.0
-0.5
0.0
0.5
1.0
SPEARMANRANKCORRELATIONrs
qCO2
qCO2 - WS0-30
OCT. 15, 2010
6/1/2010 8/31/2010 11/30/2010 3/1/2011 5/31/2011
DATE OF MEASUREMENT
-1.0
-0.5
0.0
0.5
1.0
SPEARMANRANKCORRELATIONrs
qCO2
qCO2 - WS0-30
OCT. 28, 2010
6/1/2010 8/31/2010 11/30/2010 3/1/2011 5/31/2011
DATE OF MEASUREMENT
-1.0
-0.5
0.0
0.5
1.0
SPEARMANRANKCORRELATIONrs
qCO2
qCO2 - WS0-30
NOV. 11, 2010
6/1/2010 8/31/2010 11/30/2010 3/1/2011 5/31/2011
DATE OF MEASUREMENT
-1.0
-0.5
0.0
0.5
1.0
SPEARMANRANKCORRELATIONrs
qCO2
qCO2 - WS0-30
NOV. 25, 2010
6/1/2010 8/31/2010 11/30/2010 3/1/2011 5/31/2011
DATE OF MEASUREMENT
-1.0
-0.5
0.0
0.5
1.0
SPEARMANRANKCORRELATIONrs
qCO2
qCO2 - WS0-30
DEC. 31, 2010
6/1/2010 8/31/2010 11/30/2010 3/1/2011 5/31/2011
DATE OF MEASUREMENT
-1.0
-0.5
0.0
0.5
1.0
SPEARMANRANKCORRELATIONrs
qCO2
qCO2 - WS0-30
JAN. 31, 2011
6/1/2010 8/31/2010 11/30/2010 3/1/2011 5/31/2011
DATE OF MEASUREMENT
-1.0
-0.5
0.0
0.5
1.0
SPEARMANRANKCORRELATIONrs
qCO2
qCO2 - WS0-30
FEB. 15, 2011
6/1/2010 8/31/2010 11/30/2010 3/1/2011 5/31/2011
DATE OF MEASUREMENT
-1.0
-0.5
0.0
0.5
1.0
SPEARMANRANKCORRELATIONrs
qCO2
qCO2 - WS0-30
MAR. 01, 2011
6/1/2010 8/31/2010 11/30/2010 3/1/2011 5/31/2011
DATE OF MEASUREMENT
-1.0
-0.5
0.0
0.5
1.0
SPEARMANRANKCORRELATIONrs
qCO2
qCO2 - WS0-30
MAR. 17, 2011
6/1/2010 8/31/2010 11/30/2010 3/1/2011 5/31/2011
DATE OF MEASUREMENT
-1.0
-0.5
0.0
0.5
1.0
SPEARMANRANKCORRELATIONrs
qCO2
qCO2 - WS0-30
MAR. 28, 2011
6/1/2010 8/31/2010 11/30/2010 3/1/2011 5/31/2011
DATE OF MEASUREMENT
-1.0
-0.5
0.0
0.5
1.0
SPEARMANRANKCORRELATIONrs
qCO2
qCO2 - WS0-30
APR. 13, 2011
6/1/2010 8/31/2010 11/30/2010 3/1/2011 5/31/2011
DATE OF MEASUREMENT
-1.0
-0.5
0.0
0.5
1.0
SPEARMANRANKCORRELATIONrs
qCO2
qCO2 - WS0-30
APR. 28, 2011
6/1/2010 8/31/2010 11/30/2010 3/1/2011 5/31/2011
DATE OF MEASUREMENT
-1.0
-0.5
0.0
0.5
1.0
SPEARMANRANKCORRELATIONrs
qCO2
qCO2 - WS0-30
JUNE 08, 2011
Conclusions
 GHG fluxes and relevant soil state variables (moisture,
nitrogen) measured over two seasons.
 GHG flux behavior locally driven (SWC and T influence gas
flux only on a relative not on an absolute basis).
 First steps in modeling N2O fluxes with RZWQM
 Next steps:
• model sensitivity to measured soil parameters
• dynamics at different time-scales
Thank you
to USDA-AFRI for supporting our research.

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Sustainable Nitrogen and Carbon Cycling on Diversified Horticulture Farms

  • 1. Toward Sustainable Nitrogen and Carbon Cycling on Diversified Horticulture Farms Serving Community Food Systems Krista L. Jacobsen, Debendra Shresta, Department of Horticulture, University of Kentucky Ole Wendroth*, Department of Plant and Soil Sciences, University of Kentucky John Schramski, College of Engineering, University of Georgia *presenting author 2013-67019-21403
  • 2. Introduction  Project Background & Context  Project overview  Highlights from one of the field experiments  Overview of modeling objectives and goals
  • 3. Background and Context  Small- and medium-scale, diversified farms are important sources of agricultural products for the local and regional food movement  Local food purchases are increasingly valued by the public for perceptions of healthier products due to “freshness,” conservation of local farm lands, and/or supporting local farmers (Onozaka et al, 2010)  Horticultural crops are a large part of this market  Fruits, vegetables and nuts were 70% of local food sales in 2007 (Low & Vogel, 2011).  Diversification into horticultural crops serving local markets is a global trend for small-holder farmers (Weinberger and Lumpkin, 2007), as horticultural crops are typically higher in value per unit area than cereals (USDA-NASS, 2009)
  • 4. Background and Context  However, much of what we know about C and N cycling in agroecosystems comes from agronomic systems, less research in horticulture systems (e.g. West & Post, 2002; Ma & Shaffer, 2001)  Further, production practices are highly variable, with little standard rotation varying degree of intensity Example: A lower input system, with no supplemental irrigation, “living mulch” between rows, and seasonal production Example: Green bean production in a high tunnel system, with drip supplemental irrigation, intense-tillage, in a year- round production system
  • 5. Project Objectives  Broadly, to improve our understanding of how intensification on diversified horticulture-based farms influences (1) nitrogen availability, efficiency, and retention and (2) soil carbon dynamics in labile carbon pools.
  • 6. Project Objectives:  Specifically…  (i) In addition to C and N dynamics, we are also seeking to better understand the net effects of intensification on whole system C balances using Energy Returned on Energy Invested (akin to life cycle analysis) approaches.  More on this next year…
  • 7. Project Objectives  Specifically… (ii) to compare the nitrogen dynamics and key loss pathways in five farming systems, including four organic systems, representing a gradient of intensification (characterized by quantity of inputs, and the frequency of tillage and fallow periods)
  • 8. Project Objectives:  Specifically…  (iii) to identify the sensitivity of a model to measured parameters to describe the key plant growth and soil processes. Soil input: Soil hydraulic properties Status of soil moisture and different C- and N- fractions Plant input: Growth status, root development
  • 9. -30 -20 -10 0 10 20 30 0 1 2 3 4 5 AirTemp(°C) Precipitation(inch) Precipitati on (Inch) 0 200 400 600 800 TOTALFLUX(MGCO2M-2HR-1 CO2 FLUX Extensive Organic system Conventional system Stationary Organic High Tunnel system -100 -50 0 50 100 150 200 250 300 350 400 N2OFLUXUGM-2HR-1 N2O FLUX Extensive Organic system Conventional system Stationary Organic High Tunnel system First results on GHG fluxes in different horticultural systems
  • 10. New RZWQM GHG Submodel (Fang et al., 2015) N2O emission (N2O_nit) from DAYCENT, fixed proportion of nitrification (Rnit) modified by a soil water factor (FSW_Nit) (Gillette et al., 2017) with WFPS as the water-filled pore space nitNitSWNitnit RFFr  _ON_2 _ON 2 04.1 04.14.0 _    WFPS WFPS F NitSW denDenONden RFrON  __2 2 New: diffusion factor for taking into account N2O diffusion across different soil depths.
  • 11. 09/01/2009 02/28/2010 08/27/2010 02/23/2011 08/22/2011 0 50 100 150 PRECIPITATION(mm) -15 -5 5 15 25 35 Tavg PRECIP. AIR-TEMP. 09/01/2009 02/28/2010 08/27/2010 02/23/2011 08/22/2011 0.00 0.04 0.08 0.12 0.16 0.20 N2O-FLUX(kgN/ha/day) N2O-MEASURED N2O SIMULATED CROP (WHEAT) n = 30 09/01/2009 02/28/2010 08/27/2010 02/23/2011 08/22/2011 Date 0.0 0.1 0.2 0.3 0.4 0.5 SWC(cm3 cm-3 ) SWC 0-10 cm
  • 12. 6/1/2010 8/1/2010 10/1/2010 12/1/2010 1/31/2011 4/2/2011 6/2/2011 0 40 80 DAILYPRECIP. (mm) -10 10 30 AIRTEMP.(C) PREC. AIR-TEMP. 6/1/2010 8/1/2010 10/1/2010 12/1/2010 1/31/2011 4/2/2011 6/2/2011 5 7 9 SWS0-30cm (cm) -10 10 30 SOILTEMP.(C) SWS SOIL TEMP. 6/1/2010 8/1/2010 10/1/2010 12/1/2010 1/31/2011 4/2/2011 6/2/2011 0 10 20 qCO2 (mgm-2 min-1 ) 0.0 0.5 1.0 1.5 CVqCO2 qCO2 CVqCO2 6/1/2010 8/1/2010 10/1/2010 12/1/2010 1/31/2011 4/2/2011 6/2/2011 0 5 10 15 NUGGETC0 (mgm-2 min-1 )2 0 50 100 150 200 250 RANGEa(m) NUGGET C0qCO2 RANGE aqCO2 6/1/2010 8/1/2010 10/1/2010 12/1/2010 1/31/2011 4/2/2011 6/2/2011 DATE 0.0 0.5 1.0 C0/(C+C0) 0 10 20 STDqCO2 NUGGET/SILL qCO2 STD qCO2
  • 13. RESULTS • Temporal stability of CO2 flux • rank relationship to surface soil water storage • What are the main drivers of CO2 flux
  • 14. 6/1/2010 8/31/2010 11/30/2010 3/1/2011 5/31/2011 DATE OF MEASUREMENT -1.0 -0.5 0.0 0.5 1.0 SPEARMANRANKCORRELATIONrs qCO2 qCO2 - WS0-30 JUNE 08, 2010 6/1/2010 8/1/2010 10/1/2010 12/1/2010 1/31/2011 4/2/2011 6/2/2011 5 7 9 SWS0-30cm (cm) -10 10 30 SOILTEMP.(C) SWS SOIL TEMP. CO2 flux Pattern Development and Dependence on Soil Moisture during one year.
  • 15. 6/1/2010 8/31/2010 11/30/2010 3/1/2011 5/31/2011 DATE OF MEASUREMENT -1.0 -0.5 0.0 0.5 1.0 SPEARMANRANKCORRELATIONrs qCO2 qCO2 - WS0-30 JUNE 08, 2010 6/1/2010 8/1/2010 10/1/2010 12/1/2010 1/31/2011 4/2/2011 6/2/2011 5 7 9 SWS0-30cm (cm) -10 10 30 SOILTEMP.(C) SWS SOIL TEMP. 6/1/2010 8/31/2010 11/30/2010 3/1/2011 5/31/2011 DATE OF MEASUREMENT -1.0 -0.5 0.0 0.5 1.0 SPEARMANRANKCORRELATIONrs qCO2 qCO2 - WS0-30 JUNE 21, 2010 6/1/2010 8/31/2010 11/30/2010 3/1/2011 5/31/2011 DATE OF MEASUREMENT -1.0 -0.5 0.0 0.5 1.0 SPEARMANRANKCORRELATIONrs qCO2 qCO2 - WS0-30 JULY 06, 2010 6/1/2010 8/31/2010 11/30/2010 3/1/2011 5/31/2011 DATE OF MEASUREMENT -1.0 -0.5 0.0 0.5 1.0 SPEARMANRANKCORRELATIONrs qCO2 qCO2 - WS0-30 JULY 19, 2010 6/1/2010 8/31/2010 11/30/2010 3/1/2011 5/31/2011 DATE OF MEASUREMENT -1.0 -0.5 0.0 0.5 1.0 SPEARMANRANKCORRELATIONrs qCO2 qCO2 - WS0-30 AUG. 02, 2010 6/1/2010 8/31/2010 11/30/2010 3/1/2011 5/31/2011 DATE OF MEASUREMENT -1.0 -0.5 0.0 0.5 1.0 SPEARMANRANKCORRELATIONrs qCO2 qCO2 - WS0-30 AUG. 16, 2010 6/1/2010 8/31/2010 11/30/2010 3/1/2011 5/31/2011 DATE OF MEASUREMENT -1.0 -0.5 0.0 0.5 1.0 SPEARMANRANKCORRELATIONrs qCO2 qCO2 - WS0-30 SEP. 02, 2010 6/1/2010 8/31/2010 11/30/2010 3/1/2011 5/31/2011 DATE OF MEASUREMENT -1.0 -0.5 0.0 0.5 1.0 SPEARMANRANKCORRELATIONrs qCO2 qCO2 - WS0-30 SEP. 16, 2010 6/1/2010 8/31/2010 11/30/2010 3/1/2011 5/31/2011 DATE OF MEASUREMENT -1.0 -0.5 0.0 0.5 1.0 SPEARMANRANKCORRELATIONrs qCO2 qCO2 - WS0-30 SEP. 30, 2010 6/1/2010 8/31/2010 11/30/2010 3/1/2011 5/31/2011 DATE OF MEASUREMENT -1.0 -0.5 0.0 0.5 1.0 SPEARMANRANKCORRELATIONrs qCO2 qCO2 - WS0-30 OCT. 15, 2010 6/1/2010 8/31/2010 11/30/2010 3/1/2011 5/31/2011 DATE OF MEASUREMENT -1.0 -0.5 0.0 0.5 1.0 SPEARMANRANKCORRELATIONrs qCO2 qCO2 - WS0-30 OCT. 28, 2010 6/1/2010 8/31/2010 11/30/2010 3/1/2011 5/31/2011 DATE OF MEASUREMENT -1.0 -0.5 0.0 0.5 1.0 SPEARMANRANKCORRELATIONrs qCO2 qCO2 - WS0-30 NOV. 11, 2010 6/1/2010 8/31/2010 11/30/2010 3/1/2011 5/31/2011 DATE OF MEASUREMENT -1.0 -0.5 0.0 0.5 1.0 SPEARMANRANKCORRELATIONrs qCO2 qCO2 - WS0-30 NOV. 25, 2010 6/1/2010 8/31/2010 11/30/2010 3/1/2011 5/31/2011 DATE OF MEASUREMENT -1.0 -0.5 0.0 0.5 1.0 SPEARMANRANKCORRELATIONrs qCO2 qCO2 - WS0-30 DEC. 31, 2010 6/1/2010 8/31/2010 11/30/2010 3/1/2011 5/31/2011 DATE OF MEASUREMENT -1.0 -0.5 0.0 0.5 1.0 SPEARMANRANKCORRELATIONrs qCO2 qCO2 - WS0-30 JAN. 31, 2011 6/1/2010 8/31/2010 11/30/2010 3/1/2011 5/31/2011 DATE OF MEASUREMENT -1.0 -0.5 0.0 0.5 1.0 SPEARMANRANKCORRELATIONrs qCO2 qCO2 - WS0-30 FEB. 15, 2011 6/1/2010 8/31/2010 11/30/2010 3/1/2011 5/31/2011 DATE OF MEASUREMENT -1.0 -0.5 0.0 0.5 1.0 SPEARMANRANKCORRELATIONrs qCO2 qCO2 - WS0-30 MAR. 01, 2011 6/1/2010 8/31/2010 11/30/2010 3/1/2011 5/31/2011 DATE OF MEASUREMENT -1.0 -0.5 0.0 0.5 1.0 SPEARMANRANKCORRELATIONrs qCO2 qCO2 - WS0-30 MAR. 17, 2011 6/1/2010 8/31/2010 11/30/2010 3/1/2011 5/31/2011 DATE OF MEASUREMENT -1.0 -0.5 0.0 0.5 1.0 SPEARMANRANKCORRELATIONrs qCO2 qCO2 - WS0-30 MAR. 28, 2011 6/1/2010 8/31/2010 11/30/2010 3/1/2011 5/31/2011 DATE OF MEASUREMENT -1.0 -0.5 0.0 0.5 1.0 SPEARMANRANKCORRELATIONrs qCO2 qCO2 - WS0-30 APR. 13, 2011 6/1/2010 8/31/2010 11/30/2010 3/1/2011 5/31/2011 DATE OF MEASUREMENT -1.0 -0.5 0.0 0.5 1.0 SPEARMANRANKCORRELATIONrs qCO2 qCO2 - WS0-30 APR. 28, 2011 6/1/2010 8/31/2010 11/30/2010 3/1/2011 5/31/2011 DATE OF MEASUREMENT -1.0 -0.5 0.0 0.5 1.0 SPEARMANRANKCORRELATIONrs qCO2 qCO2 - WS0-30 JUNE 08, 2011
  • 16. Conclusions  GHG fluxes and relevant soil state variables (moisture, nitrogen) measured over two seasons.  GHG flux behavior locally driven (SWC and T influence gas flux only on a relative not on an absolute basis).  First steps in modeling N2O fluxes with RZWQM  Next steps: • model sensitivity to measured soil parameters • dynamics at different time-scales
  • 17. Thank you to USDA-AFRI for supporting our research.

Notes de l'éditeur

  1. Low, S.A., and S. Vogel. 2011. Direct and intermediated marketing of local foods in the United States, ERR-128, U.S. Department of Agriculture, Economic Research Service, November 2011. Onozaka, Y., G. Nurse, and D.T. McFadden. Local Food Consumers: How motivations and perceptions translate into buying behavior. Choices Magazine 25(1): Weinberger, K. and T.A. Lumpkin, 2007. Diversification into horticulture and poverty reduction: A research agenda. World Development 35(8):1464-1480. US Department of Agriculture, National Agriculture Statistics Service, 2009. Census of Agriculture: Volume 1, U.S. Summary and State Reports. November, 2009. http://www.agcensus.usda.gov/Publications/2007/Full_Report/usv1.pdf .
  2. Ma, L., and M.J. Shaffer, 2001. A review of carbon and nitrogen processes in nine U.S. soil nitrogen dynamics models. In: Modeling Carbon and Nitrogen Dynamics for Soil Management. CRC Press, Boca Raton, FL. p. 55-102 West, T.O. and W.M. Post, 2002. Soil organic carbon sequestration rates by tillage and crop rotation: A global data analysis. Soil Science Society of America Journal 66(6): 1930-1946.