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Method for determining the degree of development of organic matter in geologic sediments
Method for determining the degree of development of organic matter in geologic sediments
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机译:确定地质沉积物中有机质发展程度的方法
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摘要
A sample of the studied sediments is heated in a non-oxidizing atomosphere. The organic material of the sediment is then pyrolyzed and the released products are oxidized. The sulfur content of the sulfur compounds produced by this oxidation is continuously measured in relation with the temperature in the form of an electric signal. The overall sulfur content of the sample is utilized in combination with a parameter characterizing the sample to determine the degree of evolution of the organic material in the sediment.
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