成都地铁龙泉山隧道浅层天然气分布特征及运移规律研究

Research on the Distribution Characteristics and Migration Law of Shallow Natural Gas of Longquanshan Tunnel on Chengdu Metro

  • 摘要: 成都地铁龙泉山隧道浅层天然气储气层为侏罗系沙溪庙组砂岩储层,其分布特征主要受卧龙寺向斜、龙泉驿背斜及马鞍山断层构造控制。文章结合地质钻孔检测结果进行分析表明,龙泉山隧道浅层天然气与砂岩层相关性明显,其运移规律为主要沿砂岩储层及断层破碎带运移至隧道开挖空间,并据此划分为“两高、三低”风险区段设防;全隧道瓦斯集中分布在三处地质构造附近,尤其在卧龙寺向斜西翼深部砂岩地层显示浓度高值。

     

    Abstract: The shallow natural gas bearing reservoir of the Longquanshan tunnel of Chengdu metro is the sand? stone reservoir of Jurassic Shaximiao formation, and its distribution characteristics are affected by the Wolongmiao syncline, Longquanyi anticline and Ma′anshan fault structure. Based on an analysis of the geological drilling test, it is found that the shallow natural gas of Longquanshan tunnel has close correlation with sandstone bed, natural gas migrates from the sandstone reservoir and fractured zone of fault to the tunnel excavation space, and the preventive measures are designed based on two areas of high gas risks and three areas of low gas risks; the gas is mainly distributed at the place nearby the three geological structures, especially the gas concentration is high at the deep sandstone stratum of the west wing of Wolongmiao syncline.

     

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