岩性油气藏 ›› 2018, Vol. 30 ›› Issue (1): 140149.doi: 10.3969/j.issn.1673-8926.2018.01.014
李闽, 王浩, 陈猛
LI Min, WANG Hao, CHEN Meng
摘要: 明确可动流体含量、分布及影响因素是有效评价致密储层开发潜能的基础。选取准噶尔盆地芦草沟组21块致密砂岩样品,采用核磁共振T2谱分析和离心实验相结合的方法,测量岩样在不同含水饱和度下的核磁共振T2谱,并辅以铸体薄片和扫描电镜技术分析储层可动流体含量差异的影响因素。结果表明:储层岩样核磁共振T2谱主要呈现为5种形态,复杂的储层微观特征和孔喉结构均是导致核磁共振T2谱形态多样的主要原因;储层建立束缚水饱和度的最佳离心力是400~450 psi,计算得到可动流体饱和度为29.44%~68.92%,平均值为46.69%,不同岩样可动流体含量和分布均有明显差异,可动流体分布的有效孔喉半径下限约为50 nm,储层主流喉道半径为70~200 nm;可动流体含量和物性参数之间的关系表明,对于物性较差的储层,渗透率是决定可动流体含量的主要因素,但对于物性较好的储层,渗透率对可动流体含量的影响较小;孔隙类型、形状及表面粗糙程度均会影响储层束缚水含量和分布;储层次生孔隙的发育程度及分布、孔喉半径大小及连通性、黏土矿物的充填程度及产状和裂缝的发育情况都会对可动流体含量产生影响。该研究成果可为致密储层开发潜力评价提供依据。
中图分类号:
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