多孔介质渗透率的NMR测定  

Measurement of Permeability of Porous Rock Using NMR T_2 Relaxation Distribution

作　　者：彭石林[1] 叶朝辉[1] 刘买利[1] 

机构地区：[1]波谱与原子分子物理国家重点实验室(中国科学院武汉物理与数学研究所),湖北武汉430071

出　　处：《波谱学杂志》2006年第2期271-282,共12页Chinese Journal of Magnetic Resonance

基　　金：中国石油天然气集团公司"九五"重点科技攻关项目(970302)

摘　　要：介绍了利用NMRT2弛豫数据求取岩心物性参数———渗透率的方法.国外学者在分析了大量数据的基础上,建立了3种由T2弛豫数据计算渗透率的模型,分别简称为SDR,Coates-cutoff和Coates-sbvi.其中SDR模型不受束缚水计算方法的影响,但对岩心孔隙中流体的性质很灵敏,比较适合于水基泥浆地层.Coates-cutoff和Coates-sbvi模型对束缚水的计算精度很敏感,可动和不可动流体孔隙体积的测定对渗透率的计算结果影响也很大.此外,这三种模型对于低渗透率岩石的计算误差都较大.通过对不同类型岩心的T2弛豫特性和用常规方法测得的渗透率进行系统分析,在SDR模型的基础上所建立的渗透率测定方法(SDR-REV)有三个可调整参数,计算渗透率适用范围更大,计算的结果与常规实验值更接近.把SDR-REV方法用于砂岩、砾岩、凝灰岩和火成岩四类岩心样品渗透率的测定,说明SDR-REV方法具有更普遍的适用性.特别是对于中国普遍存在的低渗透岩心,测定结果更为准确.The calculation methods for permeability of porous rock from its NMR T2 relaxation distribution are introduced. There are three available models （i. e., SDR, Coates-cutoff and Coates-sbvi model）. The Coates-cutoff model and Coates-sbvi model are very sensitive to the precision of irreducible fluid model, and thus the permeability results calculated by these two models are strongly affected by the precision of moveable/irreducible fluid volume calculation. On the other hand, the SDR model is not affected by irreducible fluid model, but it is sensitive to the property of the fluid in the core＇s pores. Because there is only one variable coefficient in these models, the calculation errors are large when the permeability is very low. We found that the SDR-REV model, developed recently with three variable coefficients, is much suitable for calculating permeability of the core samples with lower permeability.

关 键 词：核磁共振(NMR) T2弛豫 测井 岩心 孔隙度 渗透率 模型拟合 

分 类 号：TE135.1[石油与天然气工程—油气勘探]