Insights into arsenic retention dynamics of Pleistocene aquifer sediments by in situ sorption experiments. (1st February 2018)

• Record Type: Journal Article
• Authors: Neidhardt, Harald; Winkel, Lenny H.E.; Kaegi, Ralf; Stengel, Caroline; Trang, Pham T.K.; Lan, Vi M.; Viet, Pham H.; Berg, Michael
• Is Part Of: Water research. Volume 129(2018)
• Page Start: 123
• Page End: 132
• Publication Date: 2018-02-01
• Subjects: Arsenic behavior -- In situ sorption isotherm -- Reducing conditions -- Iron oxyhydroxides -- Groundwater -- Arsenic remobilization; Water -- Pollution -- Research -- Periodicals; 363.7394
• DOI: 10.1016/j.watres.2017.11.018
• Languages: English
• ISSNs: 0043-1354

Abstract

Abstract: The migration of arsenic (As) enriched groundwater into Pleistocene aquifers as a consequence of extensive groundwater abstraction represents an increasing threat to the precious water resources in Asian delta regions. Pleistocene aquifer sediments are typically rich in FeIII-(hydr)oxides and are capable to adsorb high amounts of As. This results in a pronounced accumulation of As in Pleistocene aquifers, where high As groundwater infiltrates from adjacent Holocene aquifers. However, As retention by Pleistocene aquifers over long-term time scales remains largely unknown. We studied As sorption in situ by placing natural Pleistocene sediments and pure mineral phases directly inside groundwater monitoring wells at a study site near Hanoi (Vietnam). This in situ exposure allows for constant flushing of the samples with unaltered groundwater and the establishment of undisturbed sorption equilibria similar to those in local aquifer sediments, which is not readily attainable in traditional laboratory sorption experiments. The groundwaters in our experimental wells were characterized by different As concentrations (0.01–6.63 μmol/L) and redox states, reaching from suboxic to anoxic conditions (Eh of +159 to −4 mV). Results show that adsorption is the dominant As retention mechanism, independent from the respective groundwater chemistry (i.e. concentrations of dissolved P, HCO3 − and Si). Whilst most of the As sorbed within the first week, sorption further increased slowly but consistently by 6–189%, respectively, within six months. Hence, the As sorption behavior of Pleistocene aquifer sediments should be determined over longer periods to avoid an underestimation of the As sorption capacity. Accompanying desorption experiments revealed that about 51% of the sorbed As was remobilized within six months when exposed to low As groundwater. We therefore conclude that a considerable proportion of the As accumulated in the aquifer sediments is prone to remobilization once the As concentrations in migrating groundwater decline. Remobilization of As should be considered in local water management plans to avoid contamination of precious groundwater resources with this As legacy. Graphical abstract: Highlights: As sorption to Pleistocene sediments increased within six months in situ exposure. A high proportion of As sorbed by Pleistocene aquifer sediments was remobilized. Sorption of As by Pleistocene sediments mainly controlled by surface adsorption. As adsorption near-linear over a wide range of As concentrations and redox states.