| 土壤甲烷及其碳同位素地球化学特征 |
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| 引用本文： | 张平中,王先彬.土壤甲烷及其碳同位素地球化学特征[J].沉积学报,1993,11(4):73-77. |
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| 作者姓名： | 张平中 王先彬 |
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| 作者单位： | 中国科学院兰州地质研究所气体地球化学国家重点实验室, 730000 |
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| 摘 要： | 本文重点对我国干旱-半干旱区油气异常区和非油气区地表土壤甲烷的碳同位素组成进行了分析;据此,对土壤、重烃及甲烷的碳同位素地球化学特征进行了讨论。
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| 关 键 词： | 碳同位素 土壤甲烷 温室效应 油气异常 |
Geochemistry Characteristics of Methane in Soils and its Isotope of Carbon |
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| Institution: | Stsre Key Larboratory of Gas Geochemistry, Lanzhou Institute of Geology, Chinese Academy of Sciences, 730000 |
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| Abstract: | This paper has reported primarily the carbon isotope composition of the methane in the soil of the oil/gas anomalous area and that of non-oil /gas area which are situated in arid and semi-arid environments of China. Geochemistry characteristics of methane and heavy hydrocarbons in soils and casbon isotope of the methane are discussed. The following conclusions are drawn: (1)Methane in soils one of important sources of "greenhouse effect" gas - methane. The soil in the arid northern China has good ability to preserve mehtane and heavy hydrocarbons concentration. In the south of China, climate condition make it easy for plant to grow. Because of abundant organic matter and strong biological activity in soils, a great quantity of methane of biological origin existed so it could be produced that a g. owing to poor preservation of methane, compared with that of the northern part of China, the soils in the sourth of China contributed more methane to the atmosphere. (2)Methane in soil of the oil/gas-bearing area is a mixture of methane produced by microbiology and by-migrating to the surface from the underground reservoirs in different proportion. Its contribution of methane to atmosphere is often greater than that of non-oil/gas area. (3)δ13C Values of methane in soil of oil/gas - bearing area are heavier than that of non-oil/gas - bearing, i. e. relatively rich in 13C. There are obvious differences of the δ13C Values of methane in soils between two different areas. (4)δ13C values of methane in soils become heavier because of the surface oxidization and other secondary fractionation. It is valid that the two origin types of methane in soils are judged by δ13C values of methane in soils in association with distribution characteristics of hydrocarbons. |
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