有机质
总有机碳
环境化学
化学
碳纤维
环境科学
有机化学
材料科学
复合数
复合材料
作者
D. W. Nelson,L. E. Sommers
出处
期刊:Agronomy
日期:1982-02-01
卷期号:: 539-579
被引量:8688
标识
DOI:10.2134/agronmonogr9.2.2ed.c29
摘要
Total carbon (C) in soils is the sum of both organic and inorganic C. Most organic C is present in the soil organic matter fraction, whereas inorganic C is largely found in carbonate minerals. This chapter describes two dry combustion and one wet combustion procedures for total C analysis. Not all soils contain inorganic C because of dissolution during soil formation of carbonate minerals originally present in parent material. However, organic C is present in all agricultural soils. Total C determinations for soil involve conversion of all forms of C in soils to CO2 by wet or dry combustion and subsequent quantitation of evolved CO2 by gravimetric, titrimetric, volumetric, spectrophotometric, or gas chromatographic techniques. Because of the problem associated with determining the organic matter content of a soil, it is strongly suggested that investigators determine and report the organic C concentration as a measure of the organic matter in a soil.
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