利用核磁共振、密度测井和SCAL综合数据评价致密砂岩储层岩石物性第九届中东地球科学会议,2010。

G. Hamada
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引用次数: 0

摘要

许多致密地层非常复杂,产层不同,渗透率不同,通常通过自然压裂来提高。这些储层的复杂性主要归因于:(1)低孔低渗储层;(2)孔隙中存在伊利石、高岭土、云母等粘土矿物。致密砂岩气储层评价是一个难点问题。仅使用常规测井曲线来确定岩石物性是非常复杂的。核磁共振测井不同于传统的中子和密度孔隙度测井。核磁共振信号振幅提供了不受岩性影响和放射源影响的详细孔隙度,弛豫时间提供了其他岩石物理参数,如渗透率、毛管压力、孔隙大小分布和油气识别。单独使用核磁共振或与密度测井和SCAL数据相结合,可以更好地确定致密砂岩储层的岩石物理性质。研究重点是确定致密砂岩储层的3个岩石物性参数:(1)结合密度孔隙度(DMR)确定详细的核磁共振孔隙度。发现DMR孔隙度法是一种气相校正孔隙度、独立相孔隙度模型。(2)核磁共振渗透率(KBGMR)是基于侵入带内气体运动和整体气体体积的动力学概念。结果表明,KBGMR是一种不依赖于相的技术,这是该技术最重要的价值。(3)由松弛时间T2分布得到的毛管压力可用于储层饱和度的测量,特别是在过渡带。结果表明,T2分布的毛细管压力近似假设在考虑气、泥滤液影响的情况下,同样适用于气井。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Petrophysical properties evaluation of tight gas sand reservoirs using integrated data of NMR, density logs and SCAL. 9th Middle East Geosciences Conference, GEO 2010.
Many tight formations are extremely complex, producing from multiple layers with different permeability that is often enhanced by natural fracturing. The complexity of these reservoirs is attributed to: (1) low porosity and low permeability reservoir; and (2) the presence of certain clay minerals like illite, kaolin and micas in pores. Evaluation of tight gas sand reservoirs represents difficult problems. Determination of petrophysical properties using only conventional logs is very complicated. Nuclear magnetic resonance (NMR) logs differ from conventional neutron and density porosity logs. NMR signal amplitude provides detailed porosity free from lithology effects and radioactive sources and relaxation times give other petrophysical parameters such as permeability, capillary pressure, the distribution of pore sizes and hydrocarbon identification. Using of NMR on an individual basis or in combination with density log and SCAL data provides better determination of petrophysical properties of tight gas sand reservoirs. This study concentrates on determination of three petrophysical parameters of tight gas sand reservoirs: (1) Determination of detailed NMR porosity in combination with density porosity, DMR. It is found that DMR porosity method is a gas corrected porosity, and independent facies porosity model. (2) NMR permeability, KBGMR, is based on the dynamic concept of gas movement and bulk gas volume in the invaded zone. It is concluded that KBGMR is a facies independent technique, and this is the most important value of this technique. (3) Capillary pressure derived from relaxation time T2 distribution could be used for formation saturation measurements especially in the transition zone. It is found that the assumptions of capillary pressure approximation from T2 distribution can be applied in gas wells as well with some consideration due to gas and mud filtrate effects.
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