4.7 Article

Hydrochemical characterization, spatial distribution, and geochemical controls on arsenic and boron in waters from arid Arica and Parinacota, northern Chile

Journal

SCIENCE OF THE TOTAL ENVIRONMENT
Volume 806, Issue -, Pages -

Publisher

ELSEVIER
DOI: 10.1016/j.scitotenv.2021.150206

Keywords

Northern Chile; Water quality; Hydrochemical evolution; Arsenic; Boron; Geothermal waters

Funding

  1. National Agency for Research and Development (ANID) /Scholarship Program/DOCTORADO BECAS CHILE 2016/Folio [72170419]
  2. University of Manchester FSE Social Responsibility Fund
  3. Leverhulme Trust [ECF2015-657]
  4. University of Manchester Dame Kathleen Ollerenshaw Fellow-ship
  5. FONDAP [15200001]
  6. ICM [NC130065]
  7. Natural Environment Research Council (NERC)
  8. Isotope Geosciences Facilities Steering Committee (NIGFSC) [IP-1925-0619]

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The study revealed that 72% of collected samples had arsenic levels exceeding the WHO drinking water provisional guideline of 10 µg/L, impacting 44% of the studied waters used for drinking. Elevated salinity (>0.75 mS/cm) affected 80% of sampled waters according to Chilean irrigation guidelines, which were also influenced by high boron (89% > 0.75 mg/L) and arsenic (31% > 50 µg/L).
The livelihood of inhabitants from rural agricultural valleys in the arid Arica and Parinacota Region, northernmost Chile, strongly depends on water from high altitude rainfall and runoff to lower elevation areas. However, elevated arsenic, boron, and other potentially harmful elements compromise water quality, especially in rural areas. Samples (n = 90) of surface, underground, cold, geothermal springs, and treated and raw tap water were studied to assess water quality and to determine the main geochemical controls on water composition, origin, and geochemical evolution along dominant (towpaths. Water from major river basins across the region (Lluta, San Jose, Codpa-Chaca, Camarones and Altiplanicas) were collected for hydrogeochemical analysis of a suite of major and trace elements, delta D and delta O-18. Our new dataset was supplemented by hydrochemical data (n > 1500 data points) from secondary sources. Results show that 72% of the collected samples had As >10 mu g/L (WHO drinking water provisional guideline) and affected 44% of the studied waters used for drinking (n = 32). Based on Chilean irrigation guidelines, elevated salinity (EC > 0.75 mS/cm) affected 80% of sampled waters, which were also impacted by high B (89% > 0.75 mg/L), and As (31% > 50 mu g/L). Water composition was strongly controlled by geothermal water and freshwater mixing in high altitude areas. Magnitude and fate of As and B concentration was determined by the geothermal input type. Highest As (similar to 21 mg/L) was associated with circum-neutral Na-Cl waters in Camarones basin, while lower As (similar to 5 mg/L) with acid SO4 waters in Lluta basin. Additionally, evaporative concentration and sediment-water interactions were shown to control the level of As in surface and groundwaters downstream. This works provides a comprehensive analysis and a conceptual model of geochemical controls on regional water compositions, contributing to better understanding the geochemical processes underpinning the water quality challenges in northern Chile. (C) 2021 Published by Elsevier B.V.

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