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沁水盆地和顺地区煤层气储层物性特征
引用本文:李琼,何建军,曹均. 沁水盆地和顺地区煤层气储层物性特征[J]. 石油地球物理勘探, 2013, 48(5): 734-739
作者姓名:李琼  何建军  曹均
作者单位:1.成都理工大学“地球探测与信息技术”教育部重点实验室,四川成都 610059;2.成都理工大学地球物理学院,四川成都 610059;3.成都理工大学,四川成都 610059
基金项目:国家自然科学基金(41274129);国家科技重大专项(2011ZX05035);成都理工大学地球探测与信息技术教育部重点实验室2011年开放基金联合资助
摘    要:在对沁水盆地和顺地区煤层气有利区带的地质资料进行相关分析基础上,采集了不同煤矿井下煤样和顶板盖层样品并进行了超声波测试,初步形成了在地层温度与压力条件下的煤样采集、样品制备及测试分析等基本岩石物理参数测试技术。应用MTS岩石物理参数测试系统对该区煤样进行岩石物理参数测试,获得该区煤层气有利区带储层岩石物理参数测试数据及其分布范围,表明煤层纵横波速度之间具有良好的线性关系,煤样及盖层样在纵横波衰减方面存在-定的差异。煤层的弹性特征与盖层存在明显差异,并具有较强的各向异性和非线性特征,可为岩石物理模型、实际模型的数值模拟和波场特征分析提供依据,也为煤层气的预测提供了-种途径。

关 键 词:煤层气储层  物性特征  地层温度与压力  岩石物理实验  
收稿时间:2012-10-30

Physical characteristics of coalbed methane reservoir in Heshun Area of Qinshui Basin
Li Qiong,He Jianjun,Cao Jun. Physical characteristics of coalbed methane reservoir in Heshun Area of Qinshui Basin[J]. Oil Geophysical Prospecting, 2013, 48(5): 734-739
Authors:Li Qiong  He Jianjun  Cao Jun
Affiliation:1. Key Laboratory of Earth Exploration and Infor-mation Techniques of the Ministry of Education,Chengdu University of Technology, Chengdu, Si-chuan 610059, China;2. College of Ueophysics, Chengdu University of Technology, Chengdu, Sichuan 610059, China;3. Chengdu University of Technology, Chengdu, Sichuan 610059, China
Abstract:Aiming at a favorable coalbed methane area in Heshun region of Qinshui Basin,we obtain and analyze the related geological data in different coal mines.We also collect coal samples and roof rock samples in downhole.Including to coal samples collection,preparation,testing and analysing technotogy.A basic rock physical parameter experiment testing technology under strata temperature and pressure is initially formed by ultrasonic testing.Using MTS(a rock mechanics test system), we obtain rock physical parameter data in favorable coalbed methane zones,the distribution of coalbed density,and the distribution of P-wave and S-wave velocities.According the analysis,we find a good linear relationship between P-wave velocity and Swave velocity of coal samples.There are some differences in terms of the P-wave and S-wave attenuations between coal samples and roof samples. Between coal seam and cap rock,elastic characteristics are obviously different with stronger anisotropy.These characteristics may lay a foundation for numerical simulations of the rock physical model and wave field characteristics analysis.It may also provide a tool to predict coalbed methane.
Keywords:coalbed methane reservoir  physical characteristic  strata temperature and pressure  rock physics testing  
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