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Groundwater extraction, land subsidence, and sea-level rise in the Mekong Delta, Vietnam

478

Citations

23

References

2014

Year

TLDR

Groundwater exploitation drives land subsidence, posing flood risks that are amplified by sea‑level rise, and in the lower Mekong Delta—most of which lies <2 m above sea level—over‑exploitation is causing widespread groundwater level declines. We quantified recent subsidence rates (2006–2010) across the Delta by analyzing 78 ALOS PALSAR interferograms from InSAR. Head levels are falling at ~0.3 m yr⁻¹, causing sediment compaction and land subsidence of ~1.6 cm yr⁻¹, with InSAR confirming 1–4 cm yr⁻¹ across the Delta; if pumping persists, ~0.88 m subsidence and ~0.10 m sea‑level rise by 2050 could add ~1 m of flood hazard by mid‑century.

Abstract

Groundwater exploitation is a major cause of land subsidence, which in coastal areas poses a flood inundation hazard that is compounded by the threat of sea-level rise (SLR). In the lower Mekong Delta, most of which lies <2 m above sea level, over-exploitation is inducing widespread hydraulic head (i.e., groundwater level) declines. The average rate of head decline is ∼0.3 m yr−1, based on time-series data from 79 nested monitoring wells at 18 locations. The consequent compaction of sedimentary layers at these locations is calculated to be causing land subsidence at an average rate of 1.6 cm yr−1. We further measure recent subsidence rates (annual average, 2006–10) throughout the Delta, by analysis of interferometric synthetic aperture radar (InSAR), using 78 ALOS PALSAR interferograms. InSAR-based subsidence rates are 1) consistent with compaction-based rates calculated at monitoring wells, and 2) ∼1–4 cm yr−1 over large (1000s of km2) regions. Ours are the first mapped estimates of Delta-wide land subsidence due to groundwater pumping. If pumping continues at present rates, ∼0.88 m (0.35–1.4 m) of land subsidence is expected by 2050. Anticipated SLR of ∼0.10 m (0.07–0.14 m) by 2050 will compound flood inundation potential. Our results suggest that by mid-century portions of the Mekong Delta will likely experience ∼1 m (0.42–1.54 m) of additional inundation hazard.

References

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