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Nitrogen isotopic geochemical characteristics of crude oils in several basins of china

Science china Earth Sciences 2005年第8期48卷 1211-1219页

作者： chen chuanping1,{1.,{2., china 2. Huazhong university of Science and Technology, Wuhan 430047, china 3. Nanjing Institute of Soil Science, Chinese Academy of Sciences, Nanjing 2.0008, china jianghan {1. {2. Jingzhou China Huazhong university of Science and Technology Wuhan China Nanjing Institute of Soil Science Chinese Academy of Sciences Nanjing China

Nitrogen isotopic ratios of crude oils with different physical and chemical properties in several basins of china have been measured and their geochemistry has been studied ele-mentally combined with molecular organic geochemistry methods. The data indicate that δ 1.N is in the range of ?6‰-{1.‰. They vary with the oils in different sedimentary types of basins. The oils forming in the limnic environment have lower δ 1.N with the value of about 1.-5‰ whereas the oils in saline or semi-saline environment have higher δ 1.N, with most samples being above 1.‰ and some exceeding 1.‰. The average nitrogen isotopic ratio of oils from the Ordovician formation in the Tarim Basin is the lowest, with most samples having δ 1.N below zero, which reflects possibly the characteristic of the oils originating mainly from the organic matter formed in marine carbonate sedimentary environment. The δ 1.N distribution can be altered by fractionation. It increases obviously because of biodegradation and decreases during hydrocarbon migration. However, the effect of nitrogen isotopic fractionation in the short distance migration is uncon-spicuous.

关键词： nitrogen isotope, crude oil, sedimentary environment, isotopic fractionation, china.

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