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Cross-formational flow of water into coalbed methane reservoirs: controls on relative permeability curve shape and production profile

机译:水向煤层气储层的跨形态流动:相对渗透率曲线形状和生产剖面的控制

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摘要

Coalbed methane (CBM) wells tend to produce large volumes of water, especially when there is hydraulic connectivity between coalbed and nearby formations. Cross-formational flow between producing coal and adjacent formations can have significant production and environmental implications, affecting economic viability of production from these shallow reservoirs. Such flows can also affect how much gas can be removed from a coalbed prior to mining and thus can have implications for methane control in mining as well. The aim of this paper is to investigate the impact of water flow from an external source into coalbed on production performance and also on reservoir variables including cleat porosity and relative permeability curves derived from production data analysis. A reservoir model is constructed to investigate the production performance of a CBM well when cross-formational flow is present between the coalbed and the overlying formation. Results show that cleat porosity calculated by analysis of production data can be more than one order of magnitude higher than actual cleat porosity. Due to hydraulic connectivity, water saturation within coalbed does not considerably change for a period of time, and hence, the peak of gas production is delayed. Upon depletion of the overlying formation, water saturation in coalbed quickly decreases. Rapid decline of water saturation in the coalbed corresponds to a sharp increase in gas production. As an important consequence, when cross-flow is present, gas and water relative permeability curves, derived from simulated production data, have distinctive features compared to the initial relative permeability curves. In the case of cross-flow, signatures of relative permeability curves are concave downward and low gas permeability for a range of water saturation, followed by rapid increase afterward for water and gas, respectively. The results and analyses presented in this work can help to assess the impact of cross-formational flow on reservoir variables derived from production data analysis and can also contribute to identifying hydraulic connectivity between coalbed and adjacent formations.
机译:煤层气(CBM)井往往会产生大量水,尤其是当煤层与附近地层之间存在水力连通时。产煤与相邻地层之间的跨形态流动可能会对生产和环境产生重大影响,从而影响这些浅层储层生产的经济可行性。这样的流量还可能影响开采前可以从煤层中清除多少气体,因此也可能对开采中的甲烷控制产生影响。本文的目的是研究从外部水源流入煤层的水对生产性能以及储层变量的影响,这些变量包括割缝孔隙度和从生产数据分析中得出的相对渗透率曲线。当在煤层和上覆地层之间存在横向变形流时,构造储层模型以研究CBM井的生产性能。结果表明,通过生产数据分析计算得出的割理孔隙度可以比实际的割理孔隙度高一个数量级。由于水力连通性,煤层中的水饱和度在一段时间内不会发生很大变化,因此,瓦斯产生的高峰被延迟了。上层地层耗尽后,煤层中的水饱和度迅速降低。煤层中水饱和度的快速下降对应于天然气产量的急剧增加。重要的结果是,当出现横流时,与初始相对渗透率曲线相比,从模拟生产数据得出的天然气和水的相对渗透率曲线具有鲜明的特征。在错流的情况下,相对渗透率曲线的特征是在一定的水饱和度范围内向下凹且气体渗透率低,随后分别对水和气体快速升高。这项工作中提出的结果和分析可以帮助评估变形流对从生产数据分析中得出的储层变量的影响,还可以帮助确定煤层与相邻地层之间的水力连通性。

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