1994
DOI: 10.2475/ajs.294.5.529
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A coupled model for transport of multiple chemical species and kinetic precipitation/dissolution reactions with application to reactive flow in single phase hydrothermal systems

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Cited by 796 publications
(616 citation statements)
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“…An alternative expression for computing reactive surface area is given by Steefel and Lasaga (1994) 135) where A • mα and φ • m are the initial surface area and volume fraction of the mineral, respectively. In the case of secondary minerals that are not initially present and where no precursor mineral occurs with a non-zero volume fraction, both Eqns.…”
Section: Reactive Surface Area Evolutionmentioning
confidence: 99%
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“…An alternative expression for computing reactive surface area is given by Steefel and Lasaga (1994) 135) where A • mα and φ • m are the initial surface area and volume fraction of the mineral, respectively. In the case of secondary minerals that are not initially present and where no precursor mineral occurs with a non-zero volume fraction, both Eqns.…”
Section: Reactive Surface Area Evolutionmentioning
confidence: 99%
“…In a dual permeability (fracture-matrix) system, the surface area of the fracture in contact with the mobile fluid phase, A F (in units of m 2 fracture m −3 medium) is (Steefel and Lasaga, 1994) 138) where ϕ F is the fracture porosity and δ is the fracture aperture. To calculate the amount of mineral surface area present along the fracture, one can use the volume fraction of the primary dissolving phase as an estimate of the fraction of the fracture surface made up of that mineral…”
Section: Reactive Surface Area Evolutionmentioning
confidence: 99%
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“…Expressions for nonisothermal multiphase flow are given in Pruess (1987) and Pruess et al (1999). The transport equations are written in terms of total dissolved concentrations of chemical components, which are concentrations of the basis species plus their associated aqueous secondary species (Yeh and Tripathi, 1991;Steefel and Lasaga, 1994;Walter and others, 1994;Lichtner, 1996;and Xu and Pruess, 2001). If kinetically-controlled reactions occur between aqueous species, then additional ordinary differential equations need to be solved to link the total concentrations of the primary species with the evolving concentrations of the secondary species (Steefel and MacQuarrie, 1996).…”
Section: Governing Equationsmentioning
confidence: 99%