Effect of Reactive Surface Areas Associated with Different Particle Shapes on Chemical-Dissolution Front Instability in Fluid-Saturated Porous Rocks
Effect of Reactive Surface Areas Associated with Different Particle Shapes on Chemical-Dissolution Front Instability in Fluid-Saturated Porous Rocks
复制标题
与不同颗粒形状相关的反应表面积对流体饱和多孔岩石中化学溶解前沿不稳定性的影响
DOI:
10.1007/s11242-007-9162-z
复制
发表时间:
2008-05
影响因子:
2.7
通讯作者:
赵崇斌
中科院分区:
文献类型:
--
作者:
赵崇斌
In this article, the effect of reactive surface areas associated with different particle shapes on the reactive infiltration instability in a fluid-saturated porous medium is investigated through analytically deriving the dimensionless pore-fluid pressure-gradient of a coupled system between porosity, pore-fluid flow and reactive chemical-species transport within two idealized porous media consisting of spherical and cubic grains respectively. Compared with the critical dimensionless pore-fluid pressure-gradient of the coupled system, the derived dimensionless pore-fluid pressure-gradient can be used to assess the instability of a chemical dissolution front within the fluid-saturated porous medium. The related theoretical analysis has demonstrated that (1) since the shape coefficient of spherical grains is greater than that of cubic grains, the chemical system consisting of spherical grains is more unstable than that consisting of cubic grains, and (2) the instability likelihood of a natural porous medium, which is comprised of irregular grains, is smaller than that of an idealized porous medium, which is comprised of regular spherical grains. To simulate the complicated morphological evolution of a chemical dissolution front in the case of the chemical dissolution system becoming supercritical, a numerical procedure is proposed for solving this kind of problem. The related numerical results have demonstrated that the reactive surface area associated with different particle shapes can have a significant influence on the morphological evolution of an unstable chemical-dissolution front within fluid-saturated porous rocks.
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DOI:
10.1007/978-1-4612-0575-3_12
发表时间:
1998
期刊:
--
影响因子:
--
作者:
B. Reddy
通讯作者:
B. Reddy
DOI:
10.1007/978-0-387-76543-3_4
发表时间:
2008
期刊:
--
影响因子:
--
作者:
B. Straughan
通讯作者:
B. Straughan
影响因子:
1.2
作者:
P. Gow;P. Upton;C. Zhao;K. Hill
通讯作者:
P. Gow;P. Upton;C. Zhao;K. Hill
影响因子:
7.4
作者:
E. C. Childs
通讯作者:
E. C. Childs
影响因子:
1.6
作者:
Chong-bin Zhao;B. Hobbs;H. Muhlhaus;A. Ord;G. Lin
通讯作者:
Chong-bin Zhao;B. Hobbs;H. Muhlhaus;A. Ord;G. Lin