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Restoration of Microbial Residues in Soils of the Conservation Reserve Program

W. Amelung*,a, J. M. Kimbleb, S. Samson-Liebigb and R. F. Follettc

a Inst. of Soil Science and Soil Geography, Univ. of Bayreuth, D-95440 Bayreuth, Germany
b Natural Resources Conservation Service, 100 Centennial Mall North, Lincoln, NE 68516
c USDA-ARS, Soil-Plant-Nutrient Research, 301 S. Howes St., P.O. Box E, Fort Collins, CO 80522-0470



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Fig. 1. Average N (left black bars) and amino sugar concentration (right lined bars) in the surface soil (0–5 cm) of the prairie, Conservation Reserve Program (CRP) and cropland fields under study. Different letters (a–b, c–e) indicate significant difference among land-use systems at the P < 0.05 level of probability using ANOVA and the respective relative concentrations (normalized to N or the amino sugar content of the prairie) as input parameters.

 


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Fig. 2. Relative increase in the ratio of glucosamine to galactosamine in the surface soil (0–5 cm) after long-term cropping of the prairie.

 


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Fig. 3. Changes in the ratio of glucosamine to muramic acid with land use as related to bulk density (0–5 cm).

 





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The SCI Journals Agronomy Journal Crop Science
Journal of Natural Resources
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Vadose Zone Journal
Journal of Plant Registrations Journal of
Environmental Quality
The Plant Genome
Copyright © 2001 by the Soil Science Society of America.