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首页> 外文期刊>Journal of Petroleum Science & Engineering >Hydrogeological control and productivity modes of coalbed methane commingled production in multi-seam areas: A case study of the Bide-Santang Basin, western Guizhou, South China
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Hydrogeological control and productivity modes of coalbed methane commingled production in multi-seam areas: A case study of the Bide-Santang Basin, western Guizhou, South China

机译:多层地区煤层气制成的水文地质控制和生产力 - 以南黔西部Bide-Santang盆地案例研究

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摘要

Coalbed methane (CBM) commingled production is an important measure to increase the CBM productivity in multi-seam areas. However, multiple superimposed CBM systems are widely developed in multi-seam areas and the difference in the hydrogeological conditions between CBM systems significantly influences the CBM commingled production. In this study, the Bide-Santang Basin in South China was used as an example and hydrogeological data analysis, production data analysis, and rock and coal sample tests were used to investigate variable hydrogeological conditions of superimposed CBM systems and their implications for the CBM production. The hydrogeochemical closed index (HCI) is proposed based on the ion compositions of the groundwater in the coal-bearing strata, which is a new parameter that can be used for the quantitative discrimination and description of superimposed CBM systems based on the determination of the groundwater environment. The hydrodynamics of the upper CBM system are stronger at a lower HCI value, and thus susceptible to shallow groundwater interference during the CBM production. The predicted daily water production based on the unit water inflow of the pumping test boreholes is generally lower than 1 m(3) /(d.m) when the median depth of the coal seam group exceeds 150 m. When the daily water production per unit drawdown (DWPPUD) of the producing fluid level in the CBM well is less than 1 m(3) /(d.m), high CBM production can be achieved in the well due to the absence of shallow groundwater interference in the Zhucang Syncline. Finally, three productivity modes of CBM commingled production wells in the Bide-Santang Basin were discriminated: shallow groundwater interference wells, high production wells, and fracturing fluid-contaminated wells. Numerical simulation shows that upper CBM system limits the production of middle and lower CBM systems. Suggestions are made for the CBM development in the Bide-Santang Basin based on the variable hydrogeological conditions and in situ stress of the superimposed CBM systems.
机译:混合生产的煤层气(CBM)是增加多煤层中CBM生产率的重要措施。然而,多个叠加的CBM系统在多缝区域中广泛发展,CBM系统之间的水文地质条件的差异显着影响CBM混合的生产。在这项研究中,南方的Bide-Santang盆地被用作示例,水文地质数据分析,生产数据分析和岩石和煤样试验用于调查叠加CBM系统的可变水文地质条件及其对CBM生产的影响。基于燃煤地层中地下水的离子组合物提出了水性化学细胞封闭指数(HCI),这是一种新参数,可用于基于地下水的测定来用于叠加CBM系统的定量辨别和描述环境。上CBM系统的流体动力学在较低的HCI值下更强,因此在CBM生产期间易于浅地下水干扰。当煤层组的中值深度超过150μm时,基于泵送试验钻孔的单位水流入的预测的日常水产通常低于1米(3)/(3)/(3)/(3)。当CBM阱中生产液位的每单位水平的每单位水平(DWPPUD)小于1米(3)/(DM)时,由于没有浅层地下水干扰,可以在井中实现高CBM产生在Zhucang Syncline。最后,歧视了双方桑塘盆地中CBM混合生产井的三种生产力模式:浅层地下水干扰井,高生产井和压裂液污染孔。数值模拟表明,上CBM系统限制了中下CBM系统的生产。基于变量水文地质条件和叠加的CBM系统的原位应力,对双边桑东盆地中的CBM开发进行了建议。

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