Prediction of carbonate rock facies from core probe permeability measurements and well log data: a case study from carbonate reservoirs, Phu Khanh basin

Hong-Minh Thi Nguyen, H. T. Pham
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Abstract

Probe permeameter (also known as Mini-permeameter) has been widely used in many field and laboratory applications where in-situ measurements and spatial distributions of permeability are needed. Mini-permeameter measurements have become popular techniques for collecting localized permeability measurements in both laboratory and field applications. It is designed to obtain fast, cheap, intensive and non-destructive permeability measurements and to describe the spatial arrangement of permeability. Currently the probe permeability meter is designed and manufactured as a portable air permeability for field applications and to be used in outcrop and core samples. In this instrument, the permeability is measured by air that flows from the samples to be measured into an air chamber through the vacuum created by increasing the volume of the chamber. In carbonate reservoirs, permeability predicted from pure porosity-permeability empirical relationship is often difficult due to complex rock pore systems leading to poor porosity-permeability relations. Once the relationships between permeability and textural rock properties are clearly established in carbonates, they can provide better permeability predictions from porosity data. Rock texture is an important parameter for the understanding of the porosity and permeability characteristics of carbonate reservoirs. In addition to predicting carbonate rock facies from routine core plug porosity and permeability measurements, there is an approach to determine carbonate reservoir facies based on core-plug probe permeability. The results of the probe permeability measurements, in this paper, can be used in combination with the porosity values derived from the well logs to classify and predict rock facies in carbonate cored or uncored reservoirs in Phu Khanh basin.
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利用岩心探头渗透率测量和测井数据预测碳酸盐岩相:以Phu Khanh盆地碳酸盐岩储层为例
探针式渗透率仪(又称微型渗透率仪)已广泛应用于许多需要现场测量渗透率和渗透率空间分布的现场和实验室应用中。在实验室和现场应用中,微型渗透率测量已经成为收集局部渗透率测量的流行技术。它旨在获得快速、廉价、密集和无损的渗透率测量,并描述渗透率的空间分布。目前,探头渗透率计是设计和制造的便携式透气性仪器,用于野外应用,并用于露头和岩心样品。在本仪器中,通过增加气室容积所产生的真空,从待测样品流入气室的空气来测量渗透率。在碳酸盐岩储层中,由于复杂的岩石孔隙系统导致孔渗关系较差,单纯通过孔渗经验关系预测渗透率往往比较困难。在碳酸盐岩中,一旦渗透率与岩石结构性质之间的关系得到明确确立,就可以通过孔隙度数据更好地预测渗透率。岩石结构是认识碳酸盐岩储层孔隙度和渗透率特征的重要参数。除了通过常规岩心塞孔隙度和渗透率测量来预测碳酸盐岩相外,还有一种基于岩心塞探头渗透率来确定碳酸盐岩储层相的方法。探针渗透率测量结果可与测井所得孔隙度值相结合,对Phu Khanh盆地碳酸盐岩有芯或无芯储层进行岩相分类和预测。
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