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Bacterial and Fungal Cell-Wall Residues in Conventional and No-Tillage Agroecosystems

Georg Guggenbergera, Serita D. Freyb, Johan Sixc, Keith Paustianc and Edward T. Elliottc

a Lehrstuhl für Bodenkunde und Bodengeographie, Universität Bayreuth, 95440 Bayreuth, Germany
b School of Natural Resources, 2021 Coffey Road, Ohio State University, Columbus, OH 43210-1085 USA
c Natural Resource Ecology Lab., Colorado State Univ., Fort Collins, CO 80523 USA



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Fig. 1 Ratios of glucosamine to muramic acid for the conventional ({square}) and no-tillage soils ({blacksquare}) at Mandan, ND, Stratton, CO, Bushland, TX, Sidney, NE, Manhattan, KS, and Lexington, KY. Mean values with standard errors are shown, n = 3. Pairs of bars with the same letter signify no sigificant difference at P < 0.05 between the two cropping systems

 


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Fig. 2 Scatter plot of the microbial biomass versus the amino sugar content in conventional ({circ}) and no-tillage (•) soils at Mandan, ND, Stratton, CO, Bushland, TX, Sidney, NE, Manhattan, KS, and Lexington, KY. Mean values with standard errors are shown, n = 3. The solid line represents the functional relation between both sets of parameter with its slope and its intercept

 


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Fig. 3 Concentration of SOM present as total amino sugars (A) and glucosamine (B) as related to the TOC content in conventional ({square}) and no-tillage soils ({blacksquare}) at Mandan, ND, Stratton, CO, Bushland, TX, Sidney, NE, Manhattan, KS, and Lexington, KY. Mean values with standard errors are shown, n = 3. Pairs of bars with the same letter signify no sigificant difference at P < 0.05 between the two cropping systems

 


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Fig. 4 Ratios of glucosamine to muramic acid for the aggregate-size classes <53 µm ({square}), 53 to 250 mm (), 250 to 2000 mm (), and 2000 yo 8000 mm ({blacksquare}) of the conventional (CT) and no-tillage soils (NT) at Sidney, NE and Lexington, KY. Mean values with standard errors are shown, n = 3. Pairs of bars with the same letter signify no sigificant difference at P < 0.05 between the aggregate-size classes. Values of the NT treatment with * are significantly different than corresponding values of the CT plots at P < 0.05

 


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Fig. 5 Concentration of SOM present as total amino sugars (A) and glucosamine (B) as related to the TOC content in the aggregate-size classes <53 µm ({square}), 53 to 250 mm (), 250 to 2000 mm (), and 2000 to 8000 mm ({blacksquare}) of the conventional (CT) and no-tillage soils (NT) at Sidney, NE and Lexington, KY. Mean values with standard errors are shown, n = 3. Pairs of bars with the same letter signify no sigificant difference at P < 0.05 between the aggregate-size classes. Values of the NT treatment with * are significantly different than corresponding values of the CT plots at P < 0.05

 





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The SCI Journals Agronomy Journal Crop Science
Journal of Natural Resources
and Life Sciences Education
Vadose Zone Journal
Journal of Plant Registrations Journal of
Environmental Quality
The Plant Genome
Copyright © 1999 by the Soil Science Society of America.