Multi-scale X-ray tomography analysis of carbonate porosity

被引:32
|
作者
Hebert, V. [1 ]
Garing, C. [1 ]
Luquot, L. [1 ]
Pezard, P. A. [1 ]
Gouze, P. [1 ]
机构
[1] Univ Montpellier 2, CNRS, INSU, UMR 5243, F-34095 Montpellier, France
关键词
UPPER MIOCENE; TRANSPORT-PROPERTIES; REACTIVE FLUID; PORE STRUCTURE; CLASSIFICATION; PERMEABILITY; ROCKS; HETEROGENEITY; EVOLUTION; LIMESTONE;
D O I
10.1144/SP406.12
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
The porosity (from values of,1% up to more than 50%, with a mean value of 36.5%) and permeability (from very low values to 20.4 D, with a mean value around 800 mD) of 38 plugs, with a diameter 40 mm, have been measured. These plugs were taken approximately every 1.5 m along a 100 m-long core, sampling a series of reefal carbonate platform lithofacies. A non-unique relationship between porosity and permeability is obtained. In addition, the porosity was measured from processing X-ray micro-tomography images with resolutions ranging from 0.42 to 190.0 mm and sampling volumes ranging from less than 1 mm 3 to few cm 3. Depending on the structure of the pore network, the computed porosity is, in some cases, controlled by the X-ray image resolution and the sampled volume. While high resolution is required to image micro-porous material, large samples with lower resolution images are necessary for identifying distributed vugs and millimetre-scale structures. This study shows that multi-resolution X-ray micro-tomography is an effective tool for characterizing the multi-scale pore structure of carbonate rocks and understanding how it may control key petrophysical parameters such as porosity and permeability.
引用
收藏
页码:61 / 79
页数:19
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