《微生物矿化》是2009年由科学出版社出版的图书，该书作者是贾蓉芬，高梅影。 该书介绍了生物及微生物矿化的研究历史与未来方向、微生物矿化的基本概念与原理等。
土壤活性有机碳是指土壤中移动快、稳定性差、易氧化、矿化，并对植物和土壤微生物活性较高的那部分碳，常可用水溶性有机碳、微生物量碳和易氧化碳等来进行表征。
Soil labile organic carbon (LOC) refers to the fractions of organic carbons that are easy to move and to be oxidized and mineralized, and they are quite available to plant and soil microorganisms.
微生物不仅使土壤有机质的分解和合成处于相对平衡状态，而且可矿化有机物提高土壤肥力。
Soil microbes can not only sustain the balance of decomposition and composition of soil organic matters, but also improve soil fertility by mineralizing the organic matters.
研究微生物与矿物的相互作用，能够为矿物的风化机理和生物矿化提供一定的理论依据。
The Research of interaction between minerals and microbes can provide theory evidence to weathering mechanism and biomineralization.
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