Abstract
This research aims to evaluate the effects of pH, including both acidic and neutral conditions to simulate an acid mine environment, on the sorption and transport of As(V) in contaminated groundwater through different reactive materials by using column experiments and mathematical modeling. Six saturated columns were set up to evaluate the migration and removal efficiency of As(V) with three different materials acting as permeable reactive barrier (PRB) media under different pH conditions (pH 4 and pH 7). The reactive materials consisted of pure sand (control column), iron oxide-coated sand (IOCS) and a combination of IOCS and zero-valent iron-coated sand (ZVICS) (ZVICS + IOCS). According to the column experiments, the descending order of removal capacity (mg As/g) for ZVICS + IOCS, IOCS and sand was 0.452 > 0.062 > 0.0027 mg As/g at pH 4 and 0.117 > 0.0077 > 0.0022 mg As/g, respectively, at pH 7. The column experiments showed that the removal and retardation factor (RF) of As(V) generally increased with decreasing pH. The SEM images and the corresponding EDX spectra of acid-washed natural sand, IOCS and ZVICS + IOCS from the columns showed that the peak of As was detectable on the reactive materials. The mechanism of As(V) sorption onto sand at pH 4 and pH 7 corresponded to the uniform (equilibrium) solute transport model, whereas the IOCS and ZVICS + IOCS columns corresponded to the two-site model (TSM) with the Freundlich isotherm. The fraction of instantaneous sites (f) for As(V) sorption onto IOCS and ZVICS + IOCS appeared to decrease with increasing pH, especially for ZVICS + IOCS, which indicates that nonequilibrium sorption/desorption mainly dominated during As(V) migration.
Highlights
This research aims to evaluate the effects of pH, including both acidic and neutral conditions to simulate an acid mine environment, on the sorption and transport of As(V) in contaminated groundwater through different reactive materials by using column experiments and mathematical modeling
In addition to SiO2 (99.50%), the sand primarily consisted of Fe2O3 (0.24%) and Al2O3 (0.10%); iron oxide-coated sand (IOCS) consisted of SiO2 (99.30%), Fe2O3 (0.38%) and Al2O3 (0.11%); and zero-valent iron-coated sand (ZVICS) mostly consisted of SiO2 (99.40%) and Fe2O3 (0.43%)
It is suggested that the removal of As(V) increased with decreasing pH because the pHpzc values of sand, IOCS and ZVICS- IOCS were higher than the acidic pH of pH 4, which led to a positive charge on the surfaces and to the higher removal capacity of As(V) on these reactive materials, mainly through electrostatic sorption
Summary
This research aims to evaluate the effects of pH, including both acidic and neutral conditions to simulate an acid mine environment, on the sorption and transport of As(V) in contaminated groundwater through different reactive materials by using column experiments and mathematical modeling. This study aimed to (a) evaluate As(V) sorption, migration, and removal efficiency in contaminated water with combinations of IOCS and ZVICS, (b) describe the effects of pH conditions on the mechanisms of As(V) migration through columns with different reactive materials, and (c) ascertain the appropriate sorption and transport parameters of equilibrium and/or chemical nonequilibrium models to further explain As(V) transport in different reactive media under acidic mine drainage. Our final findings could be further applied as predictive framework for the in situ site remediation of groundwater contaminated with As(V) in unconfined aquifers in acidic mine environments
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