Agronomy Journal Journal of Natural Resources and Life Sciences Education
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Published online 1 January 2007
Published in Agron J 99:18-26 (2007)
DOI: 10.2134/agronj2005.0352
© 2007 American Society of Agronomy
677 S. Segoe Rd., Madison, WI 53711 USA
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Management Practice Effects on Surface Soil Total Carbon

Differences along a Textural Gradient

X. Hao and A. N. Kravchenko*

Department of Crop and Soil Sciences, Michigan State Univ., East Lansing, MI 48824-1325


Figure 1
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Fig. 1. Relationships between soil total C and clay + silt content at the 0- to 5-cm depth based on combined data from four plots for each treatment fitted with two-segment linear regressions in (a) conventional tillage with conventional chemical inputs (CT), (b) conventional tillage with leguminous cover crops and no chemical inputs (CT-cover), and (c) no-till with conventional chemical inputs (NT) treatments. The dash lines indicate locations of optimal break points from two-segment regressions.

 

Figure 2
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Fig. 2. Relationships between soil total N and clay + silt content at the 0- to 5-cm depth based on combined data from four plots for each treatment fitted with two-segment linear regressions in (a) conventional tillage with conventional chemical inputs (CT), (b) conventional tillage with leguminous cover crops and no chemical inputs (CT-cover), and (c) no-till with conventional chemical inputs (NT) treatments. The dashed lines indicate locations of optimal break points from two-segment regressions.

 





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