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Comparison of Soil Carbohydrate in Several Prairie and Forest Soils by Gas‐Liquid Chromatography
Author(s) -
Folsom B. L.,
Wagner G. H.,
Scrivner C. L.
Publication year - 1974
Publication title -
soil science society of america journal
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.836
H-Index - 168
eISSN - 1435-0661
pISSN - 0361-5995
DOI - 10.2136/sssaj1974.03615995003800020027x
Subject(s) - monosaccharide , soil water , rhamnose , xylose , arabinose , chemistry , carbohydrate , environmental chemistry , total organic carbon , galactose , soil science , geology , organic chemistry , fermentation
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.