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Title: Fingerprinting groundwater salinity sources in the Gulf Coast Aquifer System, USA

Journal Article · · Hydrogeology Journal
;  [1];  [2]
  1. The University of Texas at Austin, Bureau of Economic Geology, Jackson School of Geosciences (United States)
  2. INTERA Inc. (United States)

Understanding groundwater salinity sources in the Gulf Coast Aquifer System (GCAS) is a critical issue due to depletion of fresh groundwater and concerns for potential seawater intrusion. The study objective was to assess sources of groundwater salinity in the GCAS using ∼1,400 chemical analyses and ∼90 isotopic analyses along nine well transects in the Texas Gulf Coast, USA. Salinity increases from northeast (median total dissolved solids (TDS) 340 mg/L) to southwest (median TDS 1,160 mg/L), which inversely correlates with the precipitation distribution pattern (1,370– 600 mm/yr, respectively). Molar Cl/Br ratios (median 540–600), depleted δ{sup 2}H and δ{sup 18}O (−24.7‰, −4.5‰) relative to seawater (Cl/Br ∼655 and δ{sup 2}H, δ{sup 18}O 0‰, 0‰, respectively), and elevated {sup 36}Cl/Cl ratios (∼100), suggest precipitation enriched with marine aerosols as the dominant salinity source. Mass balance estimates suggest that marine aerosols could adequately explain salt loading over the large expanse of the GCAS. Evapotranspiration enrichment to the southwest is supported by elevated chloride concentrations in soil profiles and higher δ{sup 18}O. Secondary salinity sources include dissolution of salt domes or upwelling brines from geopressured zones along growth faults, mainly near the coast in the northeast. The regional extent and large quantities of brackish water have the potential to support moderate-sized desalination plants in this location. These results have important implications for groundwater management, suggesting a current lack of regional seawater intrusion and a suitable source of relatively low TDS water for desalination.

OSTI ID:
22780897
Journal Information:
Hydrogeology Journal, Vol. 26, Issue 1; Other Information: Copyright (c) 2018 Springer-Verlag GmbH Germany, part of Springer Nature; Article Copyright (c) 2017 Springer-Verlag GmbH Germany; Country of input: International Atomic Energy Agency (IAEA); ISSN 1431-2174
Country of Publication:
United States
Language:
English