Colloid Mobilization in a Fractured Soil: Effect of Pore-Water Exchange between Preferential Flow Paths and Soil Matrix
Mohanty SK, Saiers JE, Ryan JN. Colloid Mobilization in a Fractured Soil: Effect of Pore-Water Exchange between Preferential Flow Paths and Soil Matrix. Environmental Science And Technology 2016, 50: 2310-2317. PMID: 26829659, DOI: 10.1021/acs.est.5b04767.Peer-Reviewed Original ResearchMeSH KeywordsBromidesColloidsElectric ConductivityHydrogen-Ion ConcentrationOsmolar ConcentrationPorositySoilSolutionsWaste Disposal, FluidWaterWater MovementsConceptsPreferential flow pathsSoil matrixExchange of waterRelease of colloidsColloid mobilizationIntact soil coresIonic strengthFlow pathsPore water exchangeContaminated soil matrixPore water chemistrySoil coresSoil heterogeneitySoil colloidsColloid-associated contaminantsEffluent colloid concentrationsWater chemistryCertain ionic strengthPore waterRainfall solutionsSoilDifferent ionic strengthsFractured soils