1993
DOI: 10.1016/0927-7757(93)80021-6
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A hybrid equilibrium model of solute transport in porous media in the presence of colloids

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Cited by 26 publications
(14 citation statements)
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“…Our colloid-facilitated transport model closely follows development of many similar models (e.g., Corapcioglu and Jiang, 1993;Jiang and Corapcioglu, 1993;Saiers and Hornberger, 1996;van de Weerd and Leijnse, 1997;Bekhit and Hassan, 2005). Major differences in our model include consideration of water contents, water fluxes, and air-water interfacial areas that may change in time and space (i.e., transient variably-saturated water flow), the presence of colloids on the air-water interface, and adjustment of all kinetic rates to the number of colloids present in the system.…”
Section: Colloid-facilitated Solute Transportmentioning
confidence: 99%
“…Our colloid-facilitated transport model closely follows development of many similar models (e.g., Corapcioglu and Jiang, 1993;Jiang and Corapcioglu, 1993;Saiers and Hornberger, 1996;van de Weerd and Leijnse, 1997;Bekhit and Hassan, 2005). Major differences in our model include consideration of water contents, water fluxes, and air-water interfacial areas that may change in time and space (i.e., transient variably-saturated water flow), the presence of colloids on the air-water interface, and adjustment of all kinetic rates to the number of colloids present in the system.…”
Section: Colloid-facilitated Solute Transportmentioning
confidence: 99%
“…Pq•H Thus locally at (x, t) there is no reduction in sorption of C nf = C• to soil, and there is no sorption of C•, to soil, as Cm, = 0. This discussion also holds true if the effective isotherm has the form of (35) in part i related to the modeling assumption of Jiang and Corapcioglu [1993], and the sorption of the carrier is in equilibrium, that is, So = •o (Co). For Co (x, t) --> o• (for fixed (x, t)), we find (part 1, equation (10))…”
Section: *[X T C(x T)] --> P*•f *•F[c(x T)] (6)mentioning
confidence: 66%
“…new terms on the right-hand side, the first is only present for space-dependent 02/0•. Together they can be interpreted as an additional transport term owing to convective transport acting on the carrier-bound HOC mass concentrapore-space reduction due to the sorption of carrier to the soil, as it has also been proposed byCorapcioglu and Jiang [ 1993] andJiang and Corapcioglu [ 1993], leads to the following modifications: In(3)and (4) of part 1, 0 has to be substituted by 0 -[p,•oSo + P,vo •o (Co)]/po, where Po [M L-3] is the density of the carrier DOC. As this may be interpreted as a new, diminished, and (x, !…”
mentioning
confidence: 99%
“…We will discuss the conse-REACTIVE SOLUTE TRANSPORT, 1 quence for the general model in the section "Extensions," in part 2. The model developed by Corapcioglu and Jiang [1993] and Jiang and Corapcioglu [1993] is similar to our model but has various differences. We concentrate on the latter paper, since as an essential difference the first paper considers a kinetic description of the formation of carrier-bound HOC by a linear first-order rate function, that is, instead of (9).…”
Section: Linear Sorption Of Hoc Tomentioning
confidence: 99%