PORE STRUCTURES AND TRANSPORT-PROPERTIES OF SANDSTONE

被引：29

作者：

DAVID, C ^{[1
]}

DAROT, M ^{[1
]}

JEANNETTE, D ^{[1
]}

机构：

[1] CGS,F-67084 STRASBOURG,FRANCE

来源：

TRANSPORT IN POROUS MEDIA | 1993年 / 11卷 / 02期

关键词：

SANDSTONE; PORE STRUCTURE; POROSITY; PERMEABILITY UNDER CONFINING PRESSURES UP TO 100 MPA; ELECTRICAL CONDUCTIVITY;

D O I：

10.1007/BF01059632

中图分类号：

TQ [化学工业];

学科分类号：

0817 ;

摘要：

We report laboratory measurements of pore structure, capillarity, water permeability, and electrical conductivity on Fontainebleau sandstone specimens. Experimental equipment and techniques are described. Water permeability measurements were performed on saturated cores with a 100 MPa permeameter. Various combinations of pore and confining pressures were used and an effective pressure law was determined. In addition, electrical conductivity of samples saturated with KCl brines was measured over a wide range of electrolyte conductivities (10(-3) to 1 S m-1). The well-known relationship F = PHI(-m) fits well our data, and empirical parameters such as the cementation exponent and tortuosity factor are derived. Differences between transport properties of the three types of sandstone are related to the microstructural characteristics of the pore network of each rock.

引用

页码：161 / 177

页数：17

共 24 条

[1] THE EFFECTIVE PRESSURE LAW FOR PERMEABILITY DURING PORE PRESSURE AND CONFINING PRESSURE CYCLING OF SEVERAL CRYSTALLINE ROCKS [J].