天然气地球科学 ›› 2009, Vol. 20 ›› Issue (3): 446–453.doi: 10.11764/j.issn.1672-1926.2009.03.446

• 煤层气 • 上一篇    下一篇

焦作煤田煤储层物性特征及控气因素

张小东, 刘炎昊, 张子戌, 王利丽, 刘浩   

  1. 1.河南理工大学能源科学与工程学院,河南 焦作 454000;
    2.河南理工大学资源环境学院,河南 焦作  454000
  • 收稿日期:2008-11-06 修回日期:2009-03-05 出版日期:2009-06-10 发布日期:2009-06-10
  • 通讯作者: 张小东z_wenfeng@163.com. E-mail:z_wenfeng@163.com.
  • 基金资助:

    国家自然科学基金项目(编号:40602017);国家重点基础研究发展规划(“973”)项目(编号:2006CB202204);河南理工大学博士基金项目(编号:648513)联合资助.

Coal Reservoir Properties and Coalbed Gas Controlling Factors of  Jiaozuo Coalfield

ZHANG Xiao-Dong, LIU Tan-Hao, ZHANG Zi-Qu, WANG Li-Li, LIU Gao   

  1. 1.School of Energy Science and Engineering,Henan Polytechnic University,Jiaozuo 454000,China;
    2.School of Resources and Environment, Henan Polytechnic University, Jiaozuo 454000, China
  • Received:2008-11-06 Revised:2009-03-05 Online:2009-06-10 Published:2009-06-10

摘要:

根据以往资料和实验测试结果,研究了焦作煤田主力煤层二1煤层的储层结构、渗透性、吸附性等物性特征及分布规律,采用定性与定量相结合的方式,对煤层含气性的变化规律及控制因素进行了探讨。研究认为:焦作煤田二1煤层微孔含量最高,其次是过渡孔,而大中孔含量要低得多,具有很强的吸附能力和较强的扩散能力,但渗流或层流能力很弱;煤层渗透率较低,且随着埋深的增加而减小,但地质构造对煤层渗透性具有一定的影响,并且研究区内煤层压裂处理渗透性可明显改善;煤层顶、底板岩性为煤层气体提供了良好的保存条件,而有效埋深、断裂构造对本区煤层含气性具有重要的控制作用。随着有效埋深的增加,含气量先是急剧增大,到了一定阶段后,增大趋势变缓,之间具有对数正相关关系;向斜轴部煤层气含量高于两翼,而背斜则呈现相反的趋势;区域大断裂带附近以及多组断裂的交会部位,煤层含气量往往较低。

关键词: 焦作煤田, 煤层气, 储层物性, 含气性, 影响因素

Abstract:

Based on measures on coal samples and the relative previous data, the property of fracture and pore structure, permeability and adsorption of the Ⅱ1 coalbed methane reservoir in the Jiaozuo coalfield were systematically studied. The gas-bearing change law and the influence factors on gas-bearing properties were discussed using qualitative and quantitative analyses. The study shows, micropores are the major pore, transitional pores are the second and macropores are far less in the Ⅱ1 coal, thus for the kind of coal, the adsorption capacity is very high, the diffusibility is a little strong, but the capacity of seepage and laminar flow is very weak. The permeability coefficient is low and decreases with the burial depth of the coalbed, and the permeability also is influenced by the geo-structure and can be improved under hydraulic fracturing. The roof and floor of the Ⅱ1 coalbed provide favorable gas\|preservation conditions, and the effective burial depth and faults structure are also the major factors causing gas-bearing change in the Ⅱ1 coal. The effective burial depth and gas-content is in positive correlation. The gas content in the axial part of the syncline is greater than that in the wings, and the relation is the very opposite in the anticlines. The gas content is often low near the regional faults or in the intersection part of the regional faults.

Key words: Jiaozuo coalfield, Coalbed methane, Coal reservoir properties, Gas-bearing properties, Influence factors.

中图分类号: 

  • TE132.2

[1]卢耀东,张小东,高灶其.河南省焦作煤田煤层气资源潜力调查评价报告[R].河南省地质矿产勘查开发局,2008:89-93.
[2]Clarkson C R,Bustin R M. The effect of pore structure and gas pressure upon the transport properties of coal:a laboratory and modeling study 2:Adsorption rate modeling[J].Fuel,1999,78(11):1345-1362.
[3]Karacan T,Okandan E. Fracture/cleat analysis of coals from Zongu1dak Basin(northwestern Turkey) relative to the potential of coalbed methane production[J]. International Journal of Coal Geology,2000,44(2):109-125.
[4] 桑树勋,朱炎铭,张时音,等.煤吸附气体的固气作用机-煤孔隙结构与固气作用[J].天然气工业,2005,25 (1):13-15.
[5]秦勇,宋全友,傅雪海.煤层气与常规油气共采可行性探讨--深部煤储层平衡水条件下的吸附效应[J].天然气地球科学,2005,16(4): 492-498.
[6]苏复义,宁正伟,郭友.豫西石炭-二叠系煤层气资源前景研究[J].石油勘探与开发,2001,28(2):23-25.
[7]宋志敏,孟召平.焦作矿区山西组二1煤层含气量的控制因素探讨[J].中国矿业大学学报,2002,31(2):179-181.
[8]何健坤.焦作矿区构造特征及构造控气作用[J].煤炭学报,1994,19(4):412-421.
[9] 叶建平,秦勇,林大杨.中国煤层气资源[M].徐州:中国矿业大学出版社,1998:124-184.
[10]孙斌,邵龙义,卢霞,等.盘关向斜煤层气成藏条件评价[J].天然气地球科学,2008,19(3):427-433.

 

[1] 任茜莹,代金友,穆中奇. 气藏采收率影响因素研究与启示——以靖边气田A井区为例[J]. 天然气地球科学, 2018, 29(9): 1376-1382.
[2] 吴丛丛,杨兆彪,孙晗森,张争光,李庚,彭辉. 云南恩洪向斜西南区垂向流体能量特征及有序开发建议[J]. 天然气地球科学, 2018, 29(8): 1205-1214.
[3] 邢 舟,曹高社,毕景豪,周新桂,张交东. 南华北盆地禹州地区ZK0606钻孔上古生界煤系烃源岩评价[J]. 天然气地球科学, 2018, 29(4): 518-528.
[4] 段毅,吴应忠,赵阳,曹喜喜,马兰花. 草本沼泽泥炭加水热解产物烃类气体氢同位素特征[J]. 天然气地球科学, 2018, 29(3): 305-310.
[5] 张丹锋,胡文瑞,李莉,侯秀林,吕洲,周杨,张洋,王丽宁. 震动压实作用特征及其油气地质意义[J]. 天然气地球科学, 2018, 29(3): 328-336.
[6] 左罗,蒋廷学,罗莉涛,吴魏,赵昆. 基于渗流新模型分析页岩气流动影响因素及规律[J]. 天然气地球科学, 2018, 29(2): 296-304.
[7] 单衍胜,毕彩芹,迟焕鹏,王福国,李惠. 六盘水地区杨梅树向斜煤层气地质特征与有利开发层段优选[J]. 天然气地球科学, 2018, 29(1): 122-129.
[8] 赵一民,陈强,常锁亮,田忠斌,桂文华. 基于边界要素二分的煤层气封存单元分类与评估[J]. 天然气地球科学, 2018, 29(1): 130-139.
[9] 张洲,王生维,周敏. 基于构造裂隙填图技术的煤储层裂隙发育特征预测与验证[J]. 天然气地球科学, 2017, 28(9): 1356-1362.
[10] 李阳,李树同,牟炜卫,闫灿灿. 鄂尔多斯盆地姬塬地区长6段致密砂岩中黏土矿物对储层物性的影响[J]. 天然气地球科学, 2017, 28(7): 1043-1053.
[11] 王玫珠,王勃,孙粉锦,赵洋,丛连铸,杨焦生,于荣泽,罗金洋,周红梅. 沁水盆地煤层气富集高产区定量评价[J]. 天然气地球科学, 2017, 28(7): 1108-1114.
[12] 郭广山,柳迎红,张苗,吕玉民. 沁水盆地柿庄南区块排采水特征及其对煤层气富集的控制作用[J]. 天然气地球科学, 2017, 28(7): 1115-1125.
[13] 马东民,李沛,张辉,李卫波,杨甫. 长焰煤中镜煤与暗煤吸附/解吸特征对比[J]. 天然气地球科学, 2017, 28(6): 852-862.
[14] 朱学申,梁建设,柳迎红,王存武,廖夏,郭广山,吕玉民. 煤层气井产水影响因素及类型研究——以沁冰盆地柿庄南区块为例[J]. 天然气地球科学, 2017, 28(5): 755-760.
[15] 倪小明, 李志恒,王延斌,吴建光. 沁水盆地中部断层发育区煤层气开发有利块段优选[J]. 天然气地球科学, 2017, 28(4): 602-610.
Viewed
Full text


Abstract

Cited

  Shared   
  Discussed   
No Suggested Reading articles found!