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Hwang, Y.; Pigford, T.H.; Lee, W.W.L.; Chambre, P.L.
Lawrence Berkeley Lab., CA (USA)1989
Lawrence Berkeley Lab., CA (USA)1989
AbstractAbstract
[en] A form of colloid migration that can enhance or retard the migration of a dissolved contaminant in ground water is the sorption of the contaminant on the moving colloidal particulate to form pseudocolloids. In this paper we develop analytical solutions for the interactive migration of radioactive species dissolved in ground water and sorbed as pseudocolloids. The solute and pseudocolloids are assumed to undergo advection and dispersion in a one-dimensional flow field in planar fractures in porous rock. Interaction between pseudocolloid and dissolved species is described by equilibrium sorption. Sorbed species on the pseudocolloids undergo radioactive decay, and pseudocolloids can sorb on fracture surfaces and sediments. Filtration is neglected. The solute can decay and sorb on pseudocolloids, on the fracture surfaces, and on sediments and can diffuse into the porous rock matrix. 1 fig
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Jun 1989; 3 p; Winter meeting of the American Nuclear Society; San Francisco, CA (USA); 26-30 Nov 1989; UCB-NE--4156; CONF-891103--41; CONTRACT AC03-76SF00098; Available from NTIS, PC A02/MF A01 as DE90002684; OSTI; INIS; US Govt. Printing Office Dep
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