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作 者:陈尚斌[1,2] 夏筱红[1,2] 秦勇[1,2] 付常青[1] 胡琳[1]
机构地区:[1]中国矿业大学资源与地球科学学院,江苏徐州221116 [2]中国矿业大学煤层气资源与成藏过程教育部重点实验室,江苏徐州221116
出 处:《煤炭学报》2013年第5期760-765,共6页Journal of China Coal Society
基 金:国家重点基础研究发展计划(973)资助项目(2012CB214702);江苏高校优势学科建设工程资助项目;国家自然科学基金资助项目(41272155)
摘 要:运用压汞法测定川南龙马溪组页岩气储层孔隙特征,结合有机碳含量(TOC)、矿物成分进行多元回归分析,探讨孔隙主要影响因素,并对孔隙进行分类。结果表明,孔隙度平均为4.71%,发育程度中等;储集空间由超大孔、大孔、中孔、小孔和微孔组成;中孔、小孔和微孔为主要孔径,6~120 nm的孔隙占有重要比例;TOC和脆性矿物对孔隙形成有积极意义,且TOC影响最显著;黏土矿物相反,且其影响程度远小于TOC和脆性矿物含量。基于退汞曲线-TOC成因,将龙马溪组孔隙结构划分为3种类型:Ⅰ型(退汞曲线上凸型,高TOC),Ⅱ型(退汞曲线先凸后凹型,低TOC)和Ⅲ型(退汞曲线凹型,中TOC),其中具有Ⅰ型孔隙结构的页岩气储层为最有利储层。Taking the Longmaxi Formation in the south of Sichuan Basin as an example,this paper discussed the main factors influencing the pore structures,and studied the characteristics and classification of pore structures using the multivariate regression analysis which was determined by mercury injection method,total organic content(TOC) and mineral composition.The findings are as follows:the mean porosity is 4.71%;the reservoir space is a composite of five types of pores including ultra-large hole,macropore,mesopore,pore and micropore.The pore size less than 1 000 nm is mainly mesopore,pore and micropore,especially in 6-120 nm regions for large composition.Multiple regression analysis shows that TOC and fragile mineral content are in favor of the pore formation,while the clay mineral is opposite.The influence of clay minerals is far less than that of TOC and fragile mineral content,and the TOC is the most significant factor for the shale pore.Based on the mercury withdrawal curve shape and the TOC,pore structure types are divided into three categories:Type Ⅰ(the convex part in the mercury withdrawal curve and with high TOC),Type Ⅱ(the concave part in the mercury withdrawal curve and with low TOC),and Type Ⅲ(the concave part in the mercury withdrawal curve and with moderate TOC).TypeⅠpore structure is in most favor of shale gas reservoir.
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