Biodegradation of low molecular weight organic acids in coniferous forest podzolic soils
By P. Hees, David L. Jones, D. Godbold. 2002
162 citations recorded by the source corpus.
Subfields: Biomaterials, Ecology, Soil Science
View Paper: https://www.semanticscholar.org/paper/49798912a084c948268c7735f8ad7c476685deb7
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In Biomaterials
In Ecology
In Soil Science
Citations in the corpus
- Rhizospheric organic compounds in the soil–microorganism–plant system: their role in iron availability (2014, background): “In addition, molecular size and chemical structure might further influence the degradation rate. van Hees et al. (2002) observed that citrate (a tricarboxylate) was mineralized faster than oxalate (a bicarboxylate) and acetate (a monocarboxylate).”
- Plant and mycorrhizal regulation of rhizodeposition. (2004, background): “…as a result of the constant removal © New Phytologist (2004) www.newphytologist.org New Phytologist (2004) 163 : 459–480 of exudates from the soil solution by either biotic (e.g. soil microbial uptake; Kuzyakov et al ., 2003) or abiotic processes (e.g. sorption; van Hees et al ., 2002, 2003).”
- Fate of low molecular weight organic substances in an arable soil: From microbial uptake to utilisation and stabilisation (2014, background): “Since carboxylic acid utilisation is substrate-controlled (van Hees et al., 2002), we expect divergence in the utilisation of short- and long-chain acids.”