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Sun, Q,Ding, SM,Zhang, LP,Chen, MS,Zhang, CS
2017
August
Chemosphere
A millimeter-scale observation of the competitive effect of phosphate on promotion of arsenic mobilization in sediments
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()
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Phosphate Arsenic Iron Sediment ZrO-Chelex DGT High resolution THIN-FILMS TECHNIQUE IRON-COUPLED INACTIVATION MIXED BINDING GEL DIFFUSIVE GRADIENTS HIGH-RESOLUTION IN-SITU VIVIANITE FORMATION ADSORBED ARSENATE RIVER SEDIMENTS PHOSPHORUS
180
285
294
A millimeter-scale investigation is key to the understanding of the competitive effects of phosphate(P) on arsenic(As) mobility in sediments by taking the great biogeochemical heterogeneity of the sediments into consideration. In this study, a microcosm experiment was performed in this aspect using high-resolution dialysis and diffusive gradients in thin films (DGT) to simultaneously measure dissolved and labile P, As, and iron (Fe) in sediments, respectively. With the increase of P content in water from 0.02 mg L-1 to 0.20 and 2.4 mg L-1, consistent release of As from sediments was observed. The concentrations of DGT-labile As increased significantly especially in the upper sediment layer (up to 12 times of the 0.02 mg P L-1 treatment) due to the competition of phosphate, which corresponded well to the increase in DGT-labile P. There was limited increase in dissolved P and As contents due to the buffering provided by sediment solids, while the concentrations of both dissolved and DGT-labile Fe in sediments decreased. A stoichiometric calculation showed that 47% and 8% of the added P were removed through Fe(II) precipitation for the 0.20 and 2.4 mg P L-1 treatments, respectively, which greatly suppressed the release of As induced by P competition for the 0.20 mg P L-1 treatment. The DGT-induced fluxes in sediments (DIFS) modeling showed an increase in solid resupply to pore water As from elevation of water P through the increases of the desorption rate constant from 5.4 to 31( x 10(-7)) s(-1) and the sorption rate constant from 1.8 to 22( x 10(-4)) s(-1). (C) 2017 Elsevier Ltd. All rights reserved.
10.1016/j.chemosphere.2017.04.010
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