影响沁南—中南煤层气井解吸压力的地质因素及其作用机制  

Geological factors affecting desorption pressure of CBM wells in the southern and central-southern Qinshui Basin and their influencing mechanism

作　　者：朱庆忠 张小东[2,3] 杨延辉 胡修凤 张永平 杨艳磊 陈龙伟 ZHU Qingzhong;ZHANG Xiaodong;YANG Yanhui;HU Xiufeng;ZHANG Yongping;YANG Yanlei;CHEN Longwei(Exploration and Development Research Institute of Huabei Oilfield Company,PetroChina,Renqiu 062552,China;School of Energy Science and Engineering,Henan Polytechnic University,Jiaozuo 454000,China;Collaborative Innovation Center of Coalbed Methane(Shale Gas)in Central Plains Economic Zone,Jiaozuo 454000,China)

机构地区：[1]中国石油华北油田分公司勘探开发研究院,河北任丘062552 [2]河南理工大学能源科学与工程学院,河南焦作454000 [3]中原经济区煤层气(页岩气)协同创新中心,河南焦作454000

出　　处：《中国石油大学学报（自然科学版）》2018年第2期41-49,共9页Journal of China University of Petroleum(Edition of Natural Science)

基　　金：国家科技重大专项(2011ZX05061);国家自然科学基金项目(41372162)

摘　　要：以沁南的郑庄-樊庄区块和沁中南的长治-安泽区块为研究区,依据煤层气地质背景和气井排采资料,对各区块煤层气井的解吸压力分布特征以及引起区块间解吸压力差异的主要因素进行研究。结果表明:沁南的郑庄-樊庄区块西、北部煤层气井的实际解吸压力明显高于东南部、中部;沁中南的长治-安泽区块,解吸压力总体呈东西两翼低中部高的条带状展布;实际解吸压力和临界解吸压力的对应关系一定程度上与煤级有关;煤级,灰分含量及煤体结构的差异是盆地南部与中南部解吸压力差异的主要原因,地质构造、埋深是沁水盆地南部煤层气井解吸压力局部性变化的主要因素,而埋深、地应力是沁水盆地中南部煤层气井解吸压力区内差异的主要因素。Based on geological settings of coalbed methane(CBM)and production data of CBM wells,which were obtained from the Zhengzhuang-Fanzhuang block and the Changzhi-Anze block in the southern and south-central regions of the Qinshui coal basin,respectivly,the distribution law-s of desorption pressure of CBM wells between different CBM blocks were analyzed,and the main influencing factors on the difference of desorption pressure were investigated.The results show that the actual desorption pressure of CBM wells in the west and north of the Zhengzhuang-Fanzhuang block is greater than that in the southeast and the central.For the Changzhi-Anze block,the desorption pressure in the east and west is lower than that in the central,showing a banding distribution.The relationship between the critical desorption pressure calculated by the adsorption theory and the actual desorption pressure obtained from CBM wells is inlluenced by coal ranks to some extent.Those factors,including the coal rank,the ash content and the deformation degree of coal body,result in the differences of actual desorption pressure between the southern part and the central-southern part in the Qinshui coal basin.In addition,our study suggests that geological structure and buried depth of coal seam are the main factors controlling the local changes of desorption pressure for the Zhengzhuang-Fanzhuang block,while buried depth of coal seam and in-situ stress are the principal factors for the Changzhi-Anze block.

关 键 词：沁水盆地 煤层气 解吸压力 地质因素 

分 类 号：P618.11[天文地球—矿床学]