Palaeo-hydrogeological control on groundwater As levels in Red River delta, Vietnam

Abstract

To study the geological control on groundwater As concentrations in Red River delta, depth-specific groundwater sampling and geophysical logging in 11 monitoring wells was conducted along a 45 km transect across the southern and central part of the delta, and the literature on the Red River delta's Quaternary geological development was reviewed. The water samples (n=30) were analyzed for As, major ions, Fe 2+ , H 2 S, NH 4 , CH 4 , δ 18 Ο and 8D, and the geophysical log suite included natural gamma-ray, formation and fluid electrical conductivity. The SW part of the transect intersects deposits of grey estuarine clays and deltaic sands in a 15-20 km wide and 50-60m deep Holocene incised valley. The NE part of the transect consists of 60-120 m of Pleistocene yellowish alluvial deposits underneath 10-30m of estuarine clay overlain by a 10-20m veneer of Holocene sediments. The distribution of δ 18 O-values (range -12.2‰ to -6.3%o) and hydraulic head in the sample wells indicate that the estuarine clay units divide the flow system into an upper Holocene aquifer and a lower Pleistocene aquifer. The groundwater samples were all anoxic, and contained Fe 2+ (0.03-2.0mM), Mn (0.7-320μM), SO 4 (<2.1μM-0.75mM), H 2 S (<0.1-7.0μM), NH 4 (0.03-4.4 mM), and CH 4 (0.08-14.5 mM). Generally, higher concentrations of NH 4 and CH 4 and low concentrations of SO 4 were found in the SW part of the transect, dominated by Holocene deposits, while the opposite was the case for the NE part of the transect. The distribution of the groundwater As concentration (<0.013-11.7 μM; median 0.12 μM (9μg/L)) is related to the distribution of NH 4 , CH 4 and SO 4 . Low concentrations of As (≤0.32μM) were found in the Pleistocene aquifer, while the highest As concentrations were found in the Holocene aquifer. PHRE-EQC-2 speciation calculations indicated that Fe 2+ and H 2 S concentrations are controlled by equilibrium for disordered mackinawite and precipitation of siderite. An elevated groundwater salinity (Cl range 0.19-65.1 mM) was observed in both aquifers, and dominated in the deep aquifer. A negative correlation between aqueous As and an estimate of reduced SO 4 was observed, indicating that Fe sulphide precipitation poses a secondary control on the groundwater As concentration.