天然气中伴生氢气的资源意义及其分布

2014年 36卷 第6期
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Distribution and genesis of hydrogen gas in natural gas
孟庆强 金之钧 刘文汇 胡文瑄 张刘平 朱东亚
Meng Qingqiang Jin Zhijun Liu Wenhui Hu Wenxuan Zhang Liuping Zhu Dongya
中国石化 石油勘探开发研究院, 北京 100083 2. 中国石化 石油勘探开发研究院 沉积构造储层实验室, 北京 100083 3. 山东省沉积成矿作用与沉积矿产重点实验室, 山东 青岛 266510 4. 南京大学 能源科学研究院, 南京 210093 5. 中国科学院 地质与地球物理研究所, 北京 100029
Petroleum Exploration and Product Research Institute, SINOPEC, Beijing 100083, China 2. Laboratory of Sedimentary Structural Reservoir, Petroleum Exploration and Product Research Institute, SINOPEC, Beijing 100083, China 3. Shandong Provincial Key Laboratory ofDepositional Mineralization & Sedimentary Minerals, Qingdao, Shandong 266510, China 4. Institute of Energy Sciences, Nanjing University, Nanjing, Jiangsu 210093, China 5. Institute of Geology and Geophysics, CAS, Beijing 100029, China
在系统调研氢气的分布及成因研究现状的基础上,对济阳坳陷部分油气井中天然气中的氢气含量进行了研究,并对其成因进行了初步划分。济阳坳陷天然气中氢气的含量普遍较低,在有R/Ra测试值的井中,氢气的H2/3He值普遍低于20×106,具有明显的幔源特征。因此,在这些井中,幔源氢气伴随深部流体活动混入了天然气中。
The paper systemically studied the distribution and genesis of hydrogen gas in natural gas all over the world on the basis of former study. The hydrogen gas content was studied for some oil and gas wells in the Jiyang Depression, and their genesis was discussed at the same time. The hydrogen gas content was very low in the Jiyang Depression. The H2/3He value was all lower than 20×106 in the wells which had R/Ra value. It was suggested that the hydrogen gas raised from mantle.
氢气; 伴生; 成因; 幔源; 深部流体; 济阳坳陷;
hydrogen gas; coexistence; genesis; mantle-sourced; deep-derived fluid; Jiyang Depression;
国家自然科学基金项目(41102075,41230312)和山东省沉积成矿作用与沉积矿产重点实验室开放基金(DMSM201004)联合资助。
https://doi.org/10.11781/sysydz201406712