Microbially Derived Inputs to Soil Organic Matter: Are Current Estimates Too Low?

有机质 土壤有机质 胡敏 土壤水分 环境化学 环境科学 土壤肥力 生物量(生态学) 土壤生物学 土壤生物多样性 土壤科学 化学 农学 生态学 生物
作者
André J. Simpson,Myrna J. Simpson,Emma Smith,Brian P. Kelleher
出处
期刊:Environmental Science & Technology [American Chemical Society]
卷期号:41 (23): 8070-8076 被引量:496
标识
DOI:10.1021/es071217x
摘要

Soil microbes are central to many soil processes, but due to the structural complexity of soil organic matter, the accurate quantification of microbial biomass contributions continues to pose a significant analytical challenge. In this study, microbes from a range of soils were cultured such that their molecular profile could be compared to that of soil organic matter and native vegetation. With the use of modern NMR spectroscopy, the contributions from microbial species can be discerned in soil organic matter and quantified. On the basis of these studies, the contributions of microbial biomass to soil organic matter appear to be much higher than the 1-5% reported by other researchers. In some soils, microbial biomass was found to contribute >50% of the extractable soil organic matter fractions and approximately 45% of the humin fraction and accounted for >80% of the soil nitrogen. These findings are significant because organic matter is intimately linked to nutrient release and transport in soils, nitrogen turnover rates, contaminant fate, soil quality, and fertility. Therefore, if in some cases soil organic matter and soil organic nitrogen are predominately of microbial origin, it is likely that this fraction, whether in the form of preserved material or living cells, plays an underestimated role in several soil processes.
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