王凯,郝少伟,陈瑞杰,等. 五里堠井田煤层气井单相水流阶段合理降幅的确定[J]. 中国矿业,2024,33(3):212-218. DOI: 10.12075/j.issn.1004-4051.20240037
    引用本文: 王凯,郝少伟,陈瑞杰,等. 五里堠井田煤层气井单相水流阶段合理降幅的确定[J]. 中国矿业,2024,33(3):212-218. DOI: 10.12075/j.issn.1004-4051.20240037
    WANG Kai,HAO Shaowei,CHEN Ruijie,et al. Determination of reasonable reduction in single-phase water flow stage of coalbed methane wells in Wulihou Mine Field[J]. China Mining Magazine,2024,33(3):212-218. DOI: 10.12075/j.issn.1004-4051.20240037
    Citation: WANG Kai,HAO Shaowei,CHEN Ruijie,et al. Determination of reasonable reduction in single-phase water flow stage of coalbed methane wells in Wulihou Mine Field[J]. China Mining Magazine,2024,33(3):212-218. DOI: 10.12075/j.issn.1004-4051.20240037

    五里堠井田煤层气井单相水流阶段合理降幅的确定

    Determination of reasonable reduction in single-phase water flow stage of coalbed methane wells in Wulihou Mine Field

    • 摘要: 为了确定煤层气井单相水流阶段的合理降幅,最大化地保证煤层气井的水压传播距离,以五里堠井田煤层气井为研究对象,对研究区地下水势进行计算,拟合得出地下水势与平均日产水量的关系;以研究区地下水势平均值为界限,将研究区地下水势分为高地下水势和低地下水势,分析了高地下水势区、低地下水势区煤层气井产水特征差异。基于地下水势、地层供液指数、单相水流阶段压裂液量返排率的关系,建立了单相水流阶段合理降幅数学模型,研究区排采数据验证了模型的准确性。在此基础上,根据研究区地下水势差异性,预测了相应的单相水流阶段合理降幅范围。研究结果表明:研究区地下水势与平均日产水量为正相关关系,不同水势区煤层气井产水特征差异明显,其中,高地下水势区煤层气井排采初期日产水量增长迅速,排采中后期日产水量衰减明显;低地下水势区煤层气井排采初期日产水量增长较慢,排采中后期日产水量无明显变化。单相水流阶段,随着地下水势的增加,地层供液指数、压裂液返排率也随之增大;不同地下水势区域,单相流阶段合理降幅范围不同。研究区东北部及中部,单相水流阶段合理降幅范围为0.018~0.024 MPa/d;研究区西北部、南部,单相水流阶段合理降幅范围为0.007~0.017 MPa/d。该研究成果为未投产区及相似地质条件下煤层气井单相水流阶段排采制度的制定提供了借鉴与指导。

       

      Abstract: In order to determine the reasonable reduction of the single-phase water flow stage of coalbed methane wells, the water pressure propagation distance of coalbed methane wells is ensured to the maximum. Taking Wulihou coalbed methane well as the research object, the groundwater potential in the study area is calculated, and the relationship between the groundwater potential and the average daily water volume is obtained by fitting. Based on the average value of groundwater potential in the study area, the groundwater potential in the study area is divided into high groundwater potential and low groundwater potential, and the difference of water production characteristics of coalbed methane wells in high and low groundwater potential areas is analyzed. Based on the relationship between groundwater potential, formation liquid supply index and flow back rate of fracturing fluid in the single-phase water flow stage, a mathematical model of reasonable drop in the single-phase water flow stage is established. The accuracy of the model is verified by the production data in the study area. On this basis, according to the difference of groundwater potential in the study area, the reasonable reduction range of the corresponding single-phase water flow stage is predicted. The results show that there is a positive correlation between groundwater potential and average daily water volume in the study area. The water production characteristics of coalbed methane wells in different groundwater potential areas are obviously different. In the high groundwater potential area, the daily water output of coalbed methane wells increase rapidly in the early stage of production and decrease significantly in the middle and later stages of production. In the low groundwater potential area, the daily water volume of coalbed methane wells increase slowly in the early stage of production, and there is no significant change in the middle and later stages of production. In the single-phase water flow stage, with the increase of groundwater potential, the formation liquid supply index and fracturing fluid flowback rate also increase. The reasonable drop range of the single-phase water flow stage is different in different groundwater potential areas. In the northeastern and central part of the study area, the reasonable reduction range of the single-phase water flow stage is 0.018-0.024 MPa/d. In the northwest and south of the study area, the reasonable reduction of the single-phase water flow stage ranges from 0.007 to 0.017 MPa/d. The research results provide reference and guidance for the formulation of the single-phase water flow stage production system of coalbed methane wells in unproduced areas and similar geological conditions.

       

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