寺河矿区压裂煤储层中裂缝与流动通道模型
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  • 英文篇名:Fracture and flow channel model in fractured coal reservoir of Sihe mining area
  • 作者:肖宇航 ; 王生维 ; 吕帅锋 ; 谷媛媛 ; 董庆祥
  • 英文作者:XIAO Yuhang;WANG Shengwei;LYU Shuaifeng;GU Yuanyuan;DONG Qingxiang;Faculty of Earth Resources,China University of Geosciences(Wuhan);State Key Laboratory of Coal and CBM Co-mining;
  • 关键词:寺河矿区 ; 压裂煤储层 ; 大裂隙系统 ; 空间组合 ; 流动通道模型 ; 流体压降
  • 英文关键词:sihe mining area;;fractured coal reservoir;;major fracture system;;spatial combination;;flow channel model;;pressure drop
  • 中文刊名:ZGKD
  • 英文刊名:Journal of China University of Mining & Technology
  • 机构:中国地质大学(武汉)资源学院;煤与煤层气共采国家重点实验室;
  • 出版日期:2018-07-04 16:34
  • 出版单位:中国矿业大学学报
  • 年:2018
  • 期:v.47;No.225
  • 基金:国家科技重大专项(2016ZX05067-001,2016ZX05043-003)
  • 语种:中文;
  • 页:ZGKD201806015
  • 页数:8
  • CN:06
  • ISSN:32-1152/TD
  • 分类号:152-159
摘要
为阐明流体在压裂煤储层中的流动路径,确立流体的流动通道几何模型,对寺河矿区多口压裂煤层气井进行了跟踪开挖解剖研究,认为压裂煤储层中不同成因裂隙因各自空间尺度、密度、分布特征以及与煤基质的接触面积差异,对流体流动的影响各不相同,裂隙的组合方式控制了压降的传递.研究结果表明:在绝大多数水平铺砂压裂裂缝的最前端,存在一段压开未铺砂的压裂裂缝;在单一煤岩分层中,发育线密度8~11条/5cm的内生裂隙局部密集发育带,线密度3~5条/5cm的气胀节理局部密集发育带,不同煤岩分层内的内生裂隙常被外生裂隙或者气胀节理串联;与压裂裂缝连接的天然裂隙存在明显的压裂液挤压、扩张痕迹.根据裂缝空间分布与组合关系,发现存在由内生裂隙、气胀节理、外生裂隙、压裂裂缝组成的2种基本通道类型.煤基质块中的流体通过内生裂隙密集发育带进入流动通道,气胀节理密集发育带和外生裂隙以及压裂裂缝是流体流动的通道;煤基质块对通道的流体补给速率与通道自身的导流能力,决定了通道内的压降传递效率.
        To clarify the flow path of underground fluid in fractured coal reservoir,and establish a flow channel model,an observation was carried out on the wall surface of underground tunnels near the fractured CBM wells at different locations in Sihe mining area.Because of spatial scale,density,distribution characteristics and contact area with the coal matrix,different types of fractures have different effects on fluid flow in fractured coal reservoir.The combination of fractures controls the transfer of pressure drop.Observation results show that at the front end of the horizontal fracturing fractures supported by fracturing sand,there is a fracturing fracture that is not supported by fracturing sand.There are local dense growth segments of cleats and gas expanding fractures in a single layer of coal rock.Their linear densities are respectively 8—11 strips per five centimetres and 3—5 strips per five centimetres.Cleats in dif-ferent layers of coal are often connected by fractures or gas expanding fractures.Natural fractures connected with fracturing fractures are washed and expanded by fracturing fluid.According to the spatial distribution and combination of fractures,two basic channel models consisting of cleats,gas expanding fractures,fractures and fracturing fractures were proposed.Studies indicate that the dense development of gas expanding fractures,fractures,fracturing fractures are the channel for fluid flow.Fluid replenishment rate from the coal matrix block into the channel and the conductivity of channel itself determine the rate of pressure drop in the channel.
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