Dataset Information

Fate of Arsenic during Red River Water Infiltration into Aquifers beneath Hanoi, Vietnam.

ABSTRACT: Recharge of Red River water into arsenic-contaminated aquifers below Hanoi was investigated. The groundwater age at 40 m depth in the aquifer underlying the river was 1.3 ± 0.8 years, determined by tritium-helium dating. This corresponds to a vertical flow rate into the aquifer of 19 m/year. Electrical conductivity and partial pressure of CO₂ (P_CO₂) indicate that water recharged from the river is present in both the sandy Holocene and gravelly Pleistocene aquifers and is also abstracted by the pumping station. Infiltrating river water becomes anoxic in the uppermost aquifer due to the oxidation of dissolved organic carbon. Further downward, sedimentary carbon oxidation causes the reduction of As-containing Fe-oxides. Because the release of arsenic by reduction of Fe-oxides is controlled by the reaction rate, arsenic entering the solution becomes highly diluted in the high water flux and contributes little to the groundwater arsenic concentration. Instead, the As concentration in the groundwater of up to 1 ?M is due to equilibrium-controlled desorption of arsenic, adsorbed to the sediment before river water started to infiltrate due to municipal pumping. Calculations indicate that it will take several decades of river water infiltration to leach arsenic from the Holocene aquifer to below the World Health Organization limit of 10 ?g/L.

SUBMITTER: Postma D

PROVIDER: S-EPMC5290489 | biostudies-literature | 2017 Jan

REPOSITORIES: biostudies-literature

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Fate of Arsenic during Red River Water Infiltration into Aquifers beneath Hanoi, Vietnam.

Postma Dieke D Mai Nguyen Thi Hoa NT Lan Vi Mai VM Trang Pham Thi Kim PT Sø Helle Ugilt HU Nhan Pham Quy PQ Larsen Flemming F Viet Pham Hung PH Jakobsen Rasmus R

Environmental science & technology 20161229 2

Recharge of Red River water into arsenic-contaminated aquifers below Hanoi was investigated. The groundwater age at 40 m depth in the aquifer underlying the river was 1.3 ± 0.8 years, determined by tritium-helium dating. This corresponds to a vertical flow rate into the aquifer of 19 m/year. Electrical conductivity and partial pressure of CO2 (PCO2) indicate that water recharged from the river is present in both the sandy Holocene and gravelly Pleistocene aquifer ...[more]

PMID: 27958705

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Fate of Arsenic during Red River Water Infiltration into Aquifers beneath Hanoi, Vietnam.

Publications

Fate of Arsenic during Red River Water Infiltration into Aquifers beneath Hanoi, Vietnam.

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