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中国地质学会

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榆林北部气田山2段地层水化学特征与天然气聚集关系

孟旺才, 李云, 付国民, 李晶

孟旺才, 李云, 付国民, 等. 榆林北部气田山2段地层水化学特征与天然气聚集关系[J]. 西北地质, 2018, 51(2): 203-208.
引用本文: 孟旺才, 李云, 付国民, 等. 榆林北部气田山2段地层水化学特征与天然气聚集关系[J]. 西北地质, 2018, 51(2): 203-208.
MENG Wangcai, LI Yun, FU Guomin, et al. Relationship between Chemical Characteristics of Formation Water and Natural Gas Accumulation within Shan 2 Member of Shanxi Formation in North Yulin Gas Field[J]. Northwestern Geology, 2018, 51(2): 203-208.
Citation: MENG Wangcai, LI Yun, FU Guomin, et al. Relationship between Chemical Characteristics of Formation Water and Natural Gas Accumulation within Shan 2 Member of Shanxi Formation in North Yulin Gas Field[J]. Northwestern Geology, 2018, 51(2): 203-208.

榆林北部气田山2段地层水化学特征与天然气聚集关系

基金项目: 

国家示范工程项目“鄂尔多斯盆地大型低渗透岩性地层油气藏开发示范工程”(2011ZX05044)和中国博士后基金“鄂尔多斯盆地南部特低渗储层精细评价及地质模型研究”(20070420489)联合资助

详细信息
    作者简介:

    孟旺才(1968-),男,高级工程师,研究生学历,主要从事石油天然气勘探开发工作。E-mail:642622216@qq.com

  • 中图分类号: P618.130

Relationship between Chemical Characteristics of Formation Water and Natural Gas Accumulation within Shan 2 Member of Shanxi Formation in North Yulin Gas Field

  • 摘要: 通过对榆林北部气田山2段地层水样品测试结果的统计与分析,可知目的层段地层水以偏酸性为主,矿化度较高,以CaCl2水型为主,总体反映了地层水封闭条件较好,处于还原的阻滞-停滞水文地质状态,有利于天然气的聚集与保存。地层水化学特征与天然气藏关系研究表明:地层水总矿化度高值区、CaCl2型水分布区、rNa+/Cl-低值区(<0.5)、rMg2+/Ca2+低值区(<0.1)、r (Cl--Na+)/2Mg2+高值区(>10)等均与天然气富集区有较好的对应关系。
    Abstract: Based on the statistics and analysis of the testing results of formation water samples from the Shan 2 Member of Shanxi Formation in North Yulin, it's known that the formation water of destination layer is mainly acidic and the high mineralized, CaCl2 water type, showing well closed condition of formation water. This formation water is located in the reductive block-stagnation hydrogeology condition, which is conducive to the accumulation and preservation of natural gas. The study of relationship between hydro chemical characteristics and natural gas reservoirs shows that it has a better correspondence with natural gas enrichment area among the total high mineralization degeree of the formation water, the distribution range of CaCl2 type water, the low value area of rNa+/Cl- (<0.5) and rMg2+/Ca2+ (<0.1), as well as the high value area of r(Cl--Na+)/2Mg2+ (>10)l.
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出版历程
  • 收稿日期:  2017-09-10
  • 修回日期:  2018-03-05
  • 网络出版日期:  2022-07-28
  • 发布日期:  2018-06-04

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