碳纤维
土壤水分
总有机碳
土壤有机质
有机质
环境化学
土壤碳
燃烧
环境科学
碳酸盐
化学
土壤科学
材料科学
有机化学
复合材料
复合数
作者
D. W. Nelson,L. E. Sommers
出处
期刊:Soil Science Society of America book series
日期:2013-07-16
卷期号:: 961-1010
被引量:9564
标识
DOI:10.2136/sssabookser5.3.c34
摘要
Total carbon (C) in soils is the sum of both organic and inorganic C. Organic C is present in the soil organic matter fraction, whereas inorganic C is largely found in carbonate minerals. The wet combustion analysis of soils by chromic acid digestion has long been a standard method for determining total C, giving results in good agreement with dry combustion. Methods for total C are basic for many of the procedures used to determine organic C in soils. In contrast to noncalcareous soils, inorganic C must be removed from calcareous or limed soils before the analysis if wet or dry combustion techniques are used to directly measure the organic C present. The organic matter content of soil may be indirectly estimated through multiplication of the organic C concentration by the ratio of organic matter to organic C commonly found in soils.
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