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摘要:
To determine the effect of dissolution on pore network development in carbonate rocks, dissolution experiments, X-Ray microtomography, and thin section analysis were conducted on argillaceous limestone and grain limestone samples at different temperatures and constant pH, HCl concentration. The relationship between Ca^2+ concentration and time was revealed through the experiments;pore size distribution before and after dissolution indicate that there is no correlation between the temperature and pore size variation, but pore size variation in grain limestone is more significant, indicating that the variation is mainly controlled by the heterogeneity of the rock itself(initial porosity and permeability) and the abundance of unstable minerals(related to crystal shape, size and mineral type). At different temperatures, the two kinds of carbonate rocks had very small variation in pore throat radius from 0.003 mm to 0.040 mm, which is 1.3 to 3.5 times more, 1.7 on average of the original pore throat radius. Their pore throat length varied from 0.05 mm to 0.35 mm. The minor changes in the pore throat radius, length and connectivity brought big changes to permeability of up to 1 000×10^-3 μm^2.
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篇名 Static dissolution-induced 3D pore network modification and its impact on critical pore attributes of carbonate rocks
来源期刊 石油勘探与开发:英文版 学科 工学
关键词 3D PORE networks CARBONATE ROCKS PORE structure MUDSTONE grainstone ACIDIZING dissolution X-Ray micro tomography
年,卷(期) 2019,(2) 所属期刊栏目
研究方向 页码范围 374-383
页数 10页 分类号 TE
字数 语种
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研究主题发展历程
节点文献
3D
PORE
networks
CARBONATE
ROCKS
PORE
structure
MUDSTONE
grainstone
ACIDIZING
dissolution
X-Ray
micro
tomography
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研究去脉
引文网络交叉学科
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期刊影响力
石油勘探与开发:英文版
双月刊
2096-4803
10-1529/TE
北京市海淀区学院路20号
80-232
出版文献量(篇)
331
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0
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