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Spatial Variation in Corn and Soybean Fields in Central Iowa
Energy Balance and Carbon Dioxide Exchanges
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Authors J.L. Hatfield J.H. Prueger W.P. Kustas
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Background Experiment conducted in central Iowa during 2002 as part of the Soil Moisture experiment (SMEX02) Opportunity to combine a Soil Moisture Atmospheric Coupling Experiment (SMACEX) to quantify the spatial variation in energy balance and carbon dioxide exchanges across a watershed
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Objectives Quantify the differences among energy balance and CO2 exchanges across multiple sites in a corn-soybean area Quantify the differences among sites caused by soil and crop growth differences
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Site Walnut Creek Watershed
5200 ha corn/soybean production area in central Iowa
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Soils within Fields Eight sites were in Clarion soil
Two sites in Nicollet soil Two sites in Webster soil Differences among these soils is due to soil water holding capacity in the upper cm.
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Instrumentation 12 EC 3-D sonic anemometer (CSAT3)
10 Open path CO2/H2O IRGA (LI7500) 2 Open Path H2O (KH20) Data Collection 20 Hz, 20 day times series 30 Minute data, remainder of season
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Ancillary Instrumentation
Net radiation (7-Kipp & Zonen, 7-REBS) Soil heat flux plates with soil T (REBS) Vitel θv sensors Temperature and humidity (Vaisala) Radiometric temperatures (soil & canopy + soil, Apogee)
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Cross-Comparison Location
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Exploratory Equivalence Analysis (are the EC’s equivalent)
Variable June 06 Sept. 17 CV CO2 Yes ~ <09% H ~ <11% LE ~ <10%
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Variation in Precipitation
July Rainfall (mm)
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Variation in Precipitation
Total Rainfall (6/1/02-8/19/02) (cm)
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Energy Balance Closure
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Variation in Net Radiation
Little difference among net radiation across the sites
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Seasonal Variation in Rn - Corn
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Seasonal Variation in Rn - Soybean
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Seasonal Variation in G - Corn
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Seasonal Variation in G- Soybean
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Variation in LE and CO2
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Variation in LE - Soybean
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Variation in Energy Balance Components
Blue- Corn Red- Soybean
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Observations Variation in energy balance components and CO2 among sites was larger than the comparison differences Differences among sites were caused the crop growth due to soil types and soil water availability Variation remained consistent throughout the study period
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Implications Multiple sites provide measure of the differences across soils within a watershed settings Careful selection of sites would be necessary to obtain data typical of regional scale estimates
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