1971
DOI: 10.1097/00010694-197101000-00007
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Microbial Activity in Relation to Soil Humus Formation

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Cited by 195 publications
(74 citation statements)
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“…Previous studies of phenol adsorption on smectite clays have indicated that oxidative polymerization to humic acid-like materials can occur (Thompson and Moll, 1973;Martin and Haider, 1971;Wang et al, 1978;Flaig et al, 1975;Stevenson, 1982). The oxidation process is facilitated by the presence of certain transition metal ions, such as Mn, Fe, and Cu (Larson and Hufnal, 1980;Sawhney, 1985;Fenn et aL, 1973;Shindo and Huang, 1985).…”
Section: Discussionmentioning
confidence: 98%
See 1 more Smart Citation
“…Previous studies of phenol adsorption on smectite clays have indicated that oxidative polymerization to humic acid-like materials can occur (Thompson and Moll, 1973;Martin and Haider, 1971;Wang et al, 1978;Flaig et al, 1975;Stevenson, 1982). The oxidation process is facilitated by the presence of certain transition metal ions, such as Mn, Fe, and Cu (Larson and Hufnal, 1980;Sawhney, 1985;Fenn et aL, 1973;Shindo and Huang, 1985).…”
Section: Discussionmentioning
confidence: 98%
“…Indeed, several of the organic compounds Copyright 9 1988, The Clay Minerals Society classified by the U.S. Environmental Protection Agency as priority pollutants are phenols (Chapman et al, 1982). The fate of phenols in the soil environment and their removal from aqueous waste streams is complicated by their low solubility, ability to ionize, low vapor pressure, and tendency to undergo oxidation and oxidative polymerization to humic and fulvic acid-type products (Thompson and Moll, 1973;Martin and Haider, 1971;Wang et al, 1978;Flaig et al, 1975;Stevenson, 1982). The oxidation processes are facilitated by clays and other mineral surfaces containing redox active metal ions, such as Cu, Fe, and Mn (Larson and Hufnal, 1980;Sawhney, 1985;Fenn et al,, 1973;Shindo and Huang, 1985).…”
Section: Introductionmentioning
confidence: 99%
“…Moreover, compared with NR35, FAs from aeration reactors revealed 20% -50% higher content in carboxylic carbon. The increase in carboxyl carbon was accompanied by the decrease in alkyl carbon and O-alkyl carbon, indicating that the main structural variation in FAs originated from the oxidation of alcohol side chain of lignin structure to yield by carboxylation a COOH group [54].…”
Section: Solid-state 13 C-nmrmentioning
confidence: 98%
“…In contrast, microorganisms have a much narrower C/N ratio, i.e., between 5 and 12, as their cell walls are made from nitrogen containing mucopolysaccharides. Element ratios of organic matter are widely used to track the origin of organic matter (Martin and Haider 1971;Turchenek and Oades 1979;Guggenberger et al 1999;Gleixner et al 2001;Kogel-Knabner 2002).…”
Section: Soil Organic Mattermentioning
confidence: 99%