2017
DOI: 10.1002/hyp.11309
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Modelling of colloidal particle and heavy metal transfer behaviours during seawater intrusion and refreshing processes

Abstract: The proper management of coastal aquifers commonly requires an understanding of regional mass flow and complete seawater-freshwater circulation. In this study, time series observations of seawater intrusion and refreshing were conducted using a column experiment based on natural flow conditions in coastal groundwater and a sampled medium from a coastal sandy aquifer without chemical treatment. Ranges of hydrodynamic and hydrochemical variables were tested and

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Cited by 10 publications
(3 citation statements)
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“…(1) Particle size difference: the movement of particles in porous media is affected by the particle size itself and the pore size of the media. When encountering pores with diameters smaller than the particles, exclusion effects may occur, causing the particles to be mechanically retarded outside the small pores [ 43 , 44 ]. Therefore, NBC is more prone to migration, due to its smaller particle size, while micrometer-sized bulk BC is more susceptible to exclusion effects, leading to retention in the media.…”
Section: Discussionmentioning
confidence: 99%
“…(1) Particle size difference: the movement of particles in porous media is affected by the particle size itself and the pore size of the media. When encountering pores with diameters smaller than the particles, exclusion effects may occur, causing the particles to be mechanically retarded outside the small pores [ 43 , 44 ]. Therefore, NBC is more prone to migration, due to its smaller particle size, while micrometer-sized bulk BC is more susceptible to exclusion effects, leading to retention in the media.…”
Section: Discussionmentioning
confidence: 99%
“…115 Heterogeneous colloids are composed of various inorganic minerals and organic materials, and the combined effect of IS and grain size affects the stability and related transport behavior of colloids. 116 The transient flow with perturbations in chemistry (e.g., reduction in IS and increases in pH) of porewater results in the rapid release of colloids in the vadose zone. 22,117 It was notable that saline−freshwater interaction and rainfall infiltration in aquifers lead to a decrease in the salinity of porewater, eventually releasing colloids from the solid matrix.…”
Section: Formation and Retention Of Colloidsmentioning
confidence: 99%
“…From acid mine drainage, the Fe­(II) contaminant was oxidized to form Fe­(III)-containing colloids under GTF . Heterogeneous colloids are composed of various inorganic minerals and organic materials, and the combined effect of IS and grain size affects the stability and related transport behavior of colloids …”
Section: Colloid Formation and Transport In The Gtf Zonementioning
confidence: 99%