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Published online 25 January 2008
Published in Soil Sci Soc Am J 72:285-294 (2008)
DOI: 10.2136/sssaj2007.0113
© 2008 Soil Science Society of America
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Estimating Regional Changes in Soil Carbon with High Spatial Resolution

Tristram O. Westa,*, Craig C. Brandta, Bradly S. Wilsonb, Chad M. Hellwinckelb, Donald D. Tylerc, Gregg Marlanda, Daniel G. De La Torre Ugarteb, James A. Larsond and Richard G. Nelsone

a Environmental Sciences Division, Oak Ridge National Lab., Oak Ridge, TN 37831-6335
b Agricultural Policy Analysis Center, Univ. of Tennessee, Knoxville, TN 37996-4519
c Biosystems Engineering and Soil Science Dep., Univ. of Tennessee, Knoxville, TN 37996-4531
d Dep. of Agricultural Economics, Univ. of Tennessee, Knoxville, TN 37996-4518
e Engineering Extension, Kansas State Univ., Manhattan, KS 66506-2508


Figure 1
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Fig. 1. Historical adoption of tillage practices in the United States. Data are from the Conservation Technology Information Center (2004).

 

Figure 2
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Fig. 2. Adjustment factor for C accumulation rates (Table 1) as a function of initial or baseline soil C. Analysis based on data compiled by Tan et al. (2006).

 

Figure 3
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Fig. 3. Integration of field, inventory, and remote sensing data used in the development of this C accounting framework. The (a) National Land Cover Data (NLCD) land use classes, (b) State Soil Geographic database (STATSGO) map units, and (c) county Federal Information Program Service values were integrated into (d) one composite layer that summarizes the unique combinations of the three values. Annual adoption rates (e) of different tillage intensities (from Conservation Technology Information Center [CTIC] data) were applied to the area of respective crop types (from National Agricultural Statistics Service [NASS] data). The new data set was combined with C dynamics derived from field experiments (f) using initial soil C values (b) to estimate changes in soil C that were then distributed across areas of respective cropland classes in the NLCD (a). A final spatial data set (g) of estimated C flux was generated.

 

Figure 4
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Fig. 4. Comparison of National Land Cover Data (NLCD) cropland area and National Agricultural Statistics Service (NASS) cropland area aggregated to the NLCD land use categories.

 

Figure 5
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Fig. 5. Estimated soil C content for the Mid-Continent Intensive (MCI) region in 1990. Soil C content is based on historical tillage and cropping practices. The spatial resolution of 900 m2 coincides with land use categories delineated by the National Land Cover Data (Vogelmann et al., 2001).

 

Figure 6
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Fig. 6. Cumulative changes in soil C from 1991 to 2000 caused by changes in tillage intensity and crop rotation for the Mid-Continent Intensive (MCI) region. The magnified area is an enhanced view of Wayne County, Iowa. Wayne County includes a diverse set of cropping practices, tillage intensities, and soil types, and illustrates a range of soil C gain and loss at a 900-m2 resolution within a 10-yr period.

 





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