SSSAJ Journal of Natural Resources and Life Sciences Education
HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
 QUICK SEARCH:   [advanced]


     


Published in Soil Sci Soc Am J 38:305-309 (1974)
© 1974 Soil Science Society of America
677 S. Segoe Rd., Madison, WI 53711 USA
This Article
Right arrow Full Text (PDF)
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Services
Right arrow Similar articles in this journal
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Right arrow reprints & permissions
Citing Articles
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Folsom, B. L.
Right arrow Articles by Scrivner, C. L.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Folsom, B. L.
Right arrow Articles by Scrivner, C. L.
Agricola
Right arrow Articles by Folsom, B. L.
Right arrow Articles by Scrivner, C. L.

Comparison of Soil Carbohydrate in Several Prairie and Forest Soils by Gas-Liquid Chromatography1

B. L. Folsom, G. H. Wagner and C. L. Scrivner2

ABSTRACT

Soil carbohydrate in thirteen different profiles was investigated using gas-liquid chromatography to identify and determine quantities of monosaccharides released by acid hydrolysis. Total quantities of monosaccharides extracted by sulfuric acid were positively correlated with organic carbon for the soils studied. Differences in monosaccharide determined for the various profiles related to the influence of native vegetation and parent material. Generally high concentrations of monosaccharides occurred in the Al horizons of forested soils, while the prairie soils which had thicker surface layers contained the larger total quantities. Total monosaccharides accounted for from 9 to 24% of organic carbon. Where the influence of vegetation and parent material on development was similar for a sequence of soils, those showing a greater degree of weathering had a lower proportion of the organic carbon occurring as saccharides. Glucose, galactose, and mannose were the predominant sugars in all soils and glucose was always present in the greatest amount. Appreciable quantities of arabinose and xylose were present in all soils, and small amounts of rhamnose, fucose, and ribose were found. Changes in distribution of the various monosaccharides with depth in the profile were noted, the most consistent of which was that the amount of mannose relative to total measured carbohydrate increased with depth. There were proportionately more pentoses than hexoses in the prairie soils than the forest soils.


NOTES

1 Contribution from the Dep. of Agronomy, Missouri Agr. Exp. Sta. Missouri Journal Series no. 6782. Approved by the Director.

2 Graduate Research Assistant. presently at Texas A & M, and Professors, respectively.

Received for publication July 6, 1973. Accepted for publication November 27, 1973.







HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
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 © 1974 by the Soil Science Society of America.