祁连山冻土区天然气水合物气体组分的气相色谱法测定

贺行良1,2,3,刘昌岭1,2,孟庆国1,2,祝有海4,业渝光1,2,夏 宁1,2. 祁连山冻土区天然气水合物气体组分的气相色谱法测定[J]. 地质通报, 2011, 30(12): 1857-1862.
引用本文: 贺行良1,2,3,刘昌岭1,2,孟庆国1,2,祝有海4,业渝光1,2,夏 宁1,2. 祁连山冻土区天然气水合物气体组分的气相色谱法测定[J]. 地质通报, 2011, 30(12): 1857-1862.
HE Xing-liang1,2,3, LIU Chang-ling1,2, MENG Qing-guo1,2,ZHU You-hai4, YE Yu-guang1,2, XIA Ning1,2. Gas chromatographic method for determination of gas composition from decomposed gas hydrate samples in Qilian Mountain permafrost[J]. Geological Bulletin of China, 2011, 30(12): 1857-1862.
Citation: HE Xing-liang1,2,3, LIU Chang-ling1,2, MENG Qing-guo1,2,ZHU You-hai4, YE Yu-guang1,2, XIA Ning1,2. Gas chromatographic method for determination of gas composition from decomposed gas hydrate samples in Qilian Mountain permafrost[J]. Geological Bulletin of China, 2011, 30(12): 1857-1862.

祁连山冻土区天然气水合物气体组分的气相色谱法测定

Gas chromatographic method for determination of gas composition from decomposed gas hydrate samples in Qilian Mountain permafrost

  • 建立了气相色谱法测定祁连山冻土区天然气水合物C1~C5气体组分的分析方法,对比研究了单点法与多点法校正、外标法与外标归一化法定量,以及顶空法与排水法2种气体收集方式的区别。结果表明:顶空法制备、单点法校正、外标归一化法定量计算为气相色谱法测定天然气水合物气体组分的最佳方法, 方法相对标准偏差(RSD)为0~1.06%,检出限为0.0003%~0.0127%。通过对祁连山冻土区DK-2孔10个天然气水合物样品的测定,发现C1含量为60.64%~78.76%,C2含量为8.99%~13.60%,C3含量为6.58%~21.24%,C4和C5含量较少,可见C2+气体组分含量丰富,具有较低的C1/C2+比值(1.5~3.7),显示出明显的热解气特征。
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刊出日期:  2011-12-15

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