Triple Porosity Modelling for the Simulation of Multi-Scale Flow Mechanisms in Shale Reservoirs

来源 :第二届中国纳米地球科学学术研讨会暨2016年纳米地球科学国际学术研讨会 | 被引量 : 0次 | 上传用户:andrew2011
下载到本地 , 更方便阅读
声明 : 本文档内容版权归属内容提供方 , 如果您对本文有版权争议 , 可与客服联系进行内容授权或下架
论文部分内容阅读
  Shale gas reservoir is a typical type of unconventional gas reservoirs,primarily because of the complex flow mechanism from nanoscale to macroscale.A new triple porosity model(M3 model)comprising kerogen system,matrix system and natural fracture system was presented to describe the multi-space scale,multi-time scale,and multi-physics characteristic of gas flows in shale reservoir.Apparent permeability model for real gas transport in nanopores,which incorporate flow regimes effect,was used to address multi-scale flow in shale matrix.Simultaneously,geomechanical effects on permeability evolution was derived to impact into apparent permeability model,which is important to determine shale permeability.This combination of two effects forms a novel multiscale permeability model which covers the main mechanism of permeability evolution.Experiments on coal permeability were conducted to validate this model under various stress conditions.Model results were all in good agreements with the experimental data for coal,as well as for shale samples.The model results used for history matching also showed consistency against gas production data from the Barnett Shale.Finally,we performed sensitivity analysis on the contributions of shale deposits and reservoir permeability in different scales that gives some insight as to their importance.Simulated results showed that the influence of deposits in different porous media on production response reflect at the different stages of gas production.It was also suggested that free gas in matrix contributes the main source of gas production,while natural fracture permeability determines the gas production behavior.
其他文献
  进入新世纪以来,以美国为代表的北美一些国家却在页岩气、页岩油、致密油、致密气、煤层气等非常规油气藏勘探领域取得重大突破,改变了世界油气分布的格局。随着页岩油气勘
  吉木萨尔凹陷位于准噶尔盆地东部的西南段,芦草沟组时期发育一套典型的自生自储式致密油储层。地层岩性主要为一套沉积于咸化湖泊,受机械沉积、化学沉积及生物沉积和热液喷