Numerical modeling of non-isothermal quartz dissolution/precipitation in a coupled fracture–matrix system

A numerical model is developed to simulate the combined effect of thermal and reactive solute transport in a coupled fracture–matrix system using dual porosity concepts. The model includes solute dispersion in the fracture, lateral diffusion-limited transport of solutes from the fracture into the re...

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Published inGeothermics Vol. 34; no. 4; pp. 411 - 439
Main Authors Kumar, G. Suresh, Ghassemi, Ahmad
Format Journal Article
LanguageEnglish
Published Oxford Elsevier Ltd 01.08.2005
Elsevier Science
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Abstract A numerical model is developed to simulate the combined effect of thermal and reactive solute transport in a coupled fracture–matrix system using dual porosity concepts. The model includes solute dispersion in the fracture, lateral diffusion-limited transport of solutes from the fracture into the reservoir matrix, lateral conduction-limited thermal flux from the reservoir into the fracture, as well as thermal conduction and dispersion in the fracture. The model is applied to examine the mass of silica dissolved/precipitated along a fracture and to compute the change in fracture aperture. Results show that the maximum increase in the fracture aperture occurs near its inlet. A parametric study indicates that the reservoir thermal conductivity, reservoir porosity, reservoir effective diffusion coefficient, water velocity in the fracture, and the initial fracture aperture have dominant roles in quartz dissolution/precipitation mechanisms.
AbstractList A numerical model is developed to simulate the combined effect of thermal and reactive solute transport in a coupled fracture-matrix system using dual porosity concepts. The model includes solute dispersion in the fracture, lateral diffusion-limited transport of solutes from the fracture into the reservoir matrix, lateral conduction-limited thermal flux from the reservoir into the fracture, as well as thermal conduction and dispersion in the fracture. The model is applied to examine the mass of silica dissolved/precipitated along a fracture and to compute the change in fracture aperture. Results show that the maximum increase in the fracture aperture occurs near its inlet. A parametric study indicates that the reservoir thermal conductivity, reservoir porosity, reservoir effective diffusion coefficient, water velocity in the fracture, and the initial fracture aperture have dominant roles in quartz dissolution/precipitation mechanisms.
Author Ghassemi, Ahmad
Kumar, G. Suresh
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Issue 4
Keywords Thermal transport
Dual porosity
Reactive solute transport
Silica
Fracture aperture
Quartz dissolution/precipitation
diffusion
solutes
porosity
silica
dissolution
reservoirs
quartz
transport
velocity
inlets
precipitation
numerical models
silicates
framework silicates
thermal conductivity
dispersion
fractures
Language English
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Snippet A numerical model is developed to simulate the combined effect of thermal and reactive solute transport in a coupled fracture–matrix system using dual porosity...
A numerical model is developed to simulate the combined effect of thermal and reactive solute transport in a coupled fracture-matrix system using dual porosity...
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SubjectTerms Dual porosity
Earth sciences
Earth, ocean, space
Engineering and environment geology. Geothermics
Exact sciences and technology
Fracture aperture
Geothermics
Quartz dissolution/precipitation
Reactive solute transport
Silica
Thermal transport
Title Numerical modeling of non-isothermal quartz dissolution/precipitation in a coupled fracture–matrix system
URI https://dx.doi.org/10.1016/j.geothermics.2005.04.003
https://search.proquest.com/docview/28573884
Volume 34
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