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Groundwater arsenic concentrations in Vietnam controlled by sediment age

Abstract

Arsenic contamination of groundwater continues to threaten the health of millions of people in southeast Asia. The oxidation of organic carbon, coupled to the reductive dissolution of arsenic-bearing iron oxides, is thought to control the release of sediment-bound arsenic into groundwater. However, the cause of the high spatial variability in groundwater arsenic concentrations—which can range from 5 to 500 μg l−1 within distances of a few kilometres—has been uncertain. Here, we combine measurements of sediment age, organic-matter reactivity and water chemistry at four locations along a cross-section of the arsenic-contaminated Red River floodplain in Vietnam to determine the origin of variations in groundwater arsenic concentrations. The burial age of the aquifer sediments, determined using optical stimulated luminescence, ranged from 460 years near the course of the present-day river to 5,900 years at the margin of the floodplain. The groundwater arsenic content and the reactivity of sedimentary organic carbon, determined using radiotracer measurements of the rate of methanogenesis, declined with sediment age. The sedimentary pools of both iron and arsenic also declined with the burial age of the sediments. We suggest that the age of aquifer sediments is a key determinant of groundwater arsenic concentrations.

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Figure 1: The location of sites on the alluvial floodplain of the Red River near Dan Phuong, 30 km northwest of Hanoi, Vietnam.
Figure 2: The groundwater chemistry at the four field localities given in Fig. 1.
Figure 3: The release of arsenic and iron from aquifer sediments during dissolution experiments.
Figure 4: The relation between arsenic and iron released from the sediments in the experiments of Fig. 3.

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Acknowledgements

D. D. Nhan made facilities available to do radiotracer work at the Institute for Nuclear Sciences and Technology. H. T. Tuoi, N. T. T. Trang, N. T. H. Mai, C. T. M. Trang and N. N. Khue did chemical analytical work in the field and the laboratory. H. V. Hoan and V. V. Hung supported the field work and sediment coring. The project received financial support as a research capacity building grant from DANIDA.

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Authors and Affiliations

Authors

Contributions

D.P. and F.L. conceived the project. R.J. oversaw and organized the radiotracer work. N.T.T. carried out the radiotracer and leaching experiments. P.T.K.T. and P.H.V. organized the water sampling and analysis, P.Q.N. advised on hydrogeology and organized the drilling, coring and hydrogeological field work together with T.V.L. F.L. was responsible for water dating and the hydrogeological interpretation. A.S.M. carried out the sediment dating. R.J., F.L. and D.P. analysed and interpreted the data. D.P. wrote the paper.

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Correspondence to Dieke Postma.

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The authors declare no competing financial interests.

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Postma, D., Larsen, F., Thai, N. et al. Groundwater arsenic concentrations in Vietnam controlled by sediment age. Nature Geosci 5, 656–661 (2012). https://doi.org/10.1038/ngeo1540

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