非常规天然气

深部煤层气成藏条件特殊性及其临界深度探讨

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  • 1.中国矿业大学资源与地球科学学院/煤层气资源与成藏过程教育部重点实验室; 江苏省煤基CO2捕集与地质储存重点实验室,江苏 徐州 221116;2.中国石油勘探开发研究院廊坊分院,河北 廊坊 065007
申建(1983-),男,四川遂宁人,讲师,博士,主要从事煤层气地质研究.E-mail:cumthenjian@126.com.

收稿日期: 2014-03-04

  修回日期: 2014-05-07

  网络出版日期: 2014-09-10

基金资助

国家重大科技专项(编号:2011ZX05033-3);国家自然科学基金项目(编号:41302131,41362009);中央高校基本科研业务费专项基金(编号:2012QNB32)|江苏省煤基CO2捕集与地质储存重点实验室开放基金项目(编号:2012KF04)联合资助.

 

 

 

Properties of Deep Coalbed Methane Reservoir-forming Conditions and Critical Depth Discussion
 

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  • (1.School of Resources and Geoscience/Key Laboratory of CBM Resources and Reservoiring Process/The Key Laboratory of Coal-based CO2 Capture and Geological Storage,China University of Mining and Technology,Xuzhou 221116, China; 2.Langfang Branch of China Petroleum Exploration and Development Research Institute,Langfang 065007, China)

Received date: 2014-03-04

  Revised date: 2014-05-07

  Online published: 2014-09-10

摘要

深煤层概念及其评价指标的科学界定,是推动深部煤层气基础理论研究的基础。基于对地应力、含气性、储层物性及岩石力学性质等随煤层埋深变化特征的分析结果显示:相对浅部,深部煤孔隙结构变化小,中孔—微孔比例趋于均一;煤层含气量与埋深之间存在一个“临界深度”,超过此埋深之后含气量随埋深进一步增大而趋于降低;渗透率的常用对数与埋深呈线性负相关关系,暗示深部煤储层趋于致密化;深部围压正效应和温度负效应强弱相互转换,煤岩弹性模量随着埋深增加存在“拐点”。构建了基于地应力、饱和含气量、渗透率等深煤层界定指标体系。以沁水盆地为例,将该盆地深煤层界定在750m以深。即在此深度以深,煤层气成藏特征开始发生转换,其开发须针对储层特性变化采取相应的措施。

本文引用格式

申建,秦勇,傅雪海,陈刚,陈润 . 深部煤层气成藏条件特殊性及其临界深度探讨[J]. 天然气地球科学, 2014 , 25(9) : 1470 -1476 . DOI: 10.11764/j.issn.1672-1926.2014.09.1470

Abstract

Concept and evaluation indices of deep coalbed are essential for motivating deep coalbed methane research.Based on the analysis of ground stress,pore properties,gas content,reservoir physical and mechanical properties,it has shown that variations of proportion of different pore types of deep coal are very small,especially for mesopore to micropore.With the increase of coal burial depth,gas content increases firstly and then decreases.The inflexion point from gas content increasing to decreasing is defined as “critical depth”,and that is,the gas content decreases when the burial depth is deeper than the critical depth.Decimal logarithm of permeability is linearly negatively related to burial depth,which means that permeability of deep coal is probably very low.Elasticity modulus of coal are positively related to confining pressure and negatively related to temperature,and it also suggests that there is an “inflexion point” in the relation curve between elasticity modulus and burial depth.In further,indices of ground stress,saturated gas content,permeability were constructed to define the critical depth.Taking the Qinshui Basin as an example,the critical burial depth of deep coalbed is at 750m through calculations of the indices.It is suggested that reservoir condition changes a lot compared to shallow coalbed,and corresponding measures must be taken in coalbed methane development.

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