Salmachi Alireza, Karacan C Özgen
Australian School of Petroleum, University of Adelaide, Adelaide, Australia.
Office of Mine Safety and Health Research, NIOSH, Pittsburgh, PA, USA.
Environ Earth Sci. 2017 Mar;76(5). doi: 10.1007/s12665-017-6505-0. Epub 2017 Feb 27.
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.
煤层气(CBM)井往往会产出大量的水,尤其是当煤层与附近地层存在水力连通性时。生产煤层与相邻地层之间的跨地层流动可能会对生产和环境产生重大影响,影响这些浅层储层生产的经济可行性。这种流动还会影响在开采前从煤层中能够采出的气体量,因此对开采过程中的甲烷控制也有影响。本文的目的是研究外部水源流入煤层对生产性能以及储层变量的影响,这些储层变量包括从生产数据分析得出的割理孔隙度和相对渗透率曲线。构建了一个储层模型来研究当煤层与上覆地层之间存在跨地层流动时煤层气井的生产性能。结果表明,通过生产数据分析计算出的割理孔隙度可能比实际割理孔隙度高出一个多数量级。由于水力连通性,煤层内的含水饱和度在一段时间内变化不大,因此产气峰值会延迟。当上覆地层枯竭时,煤层中的含水饱和度迅速下降。煤层中含水饱和度的快速下降对应着产气的急剧增加。一个重要的结果是,当存在交叉流时,从模拟生产数据得出的气水相对渗透率曲线与初始相对渗透率曲线相比具有明显特征。在交叉流的情况下,相对渗透率曲线的特征是在一定范围的含水饱和度内向下凹且气体渗透率低,随后气水渗透率分别迅速增加。本文所呈现的结果和分析有助于评估跨地层流动对从生产数据分析得出的储层变量的影响,也有助于识别煤层与相邻地层之间的水力连通性。