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Hydrogeochemical and multi-tracer investigations of arsenic-affected aquifers in semi-arid West Africa

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【作者】 Anja BretzlerLucien StolzeJulien NikiemaFranck LalanneElaheh GhadiriMatthias S.BrennwaldMassimo RolleMario Schirmer

【Author】 Anja Bretzler;Lucien Stolze;Julien Nikiema;Franck Lalanne;Elaheh Ghadiri;Matthias S.Brennwald;Massimo Rolle;Mario Schirmer;Eawag,Swiss Federal Institute of Aquatic Science and Technology;Centre d’Hydrogéologie et de Géothermie (CHYN), Université de Neuchatel;Technical University of Denmark (DTU);Université Ouaga I Pr.Joseph KI-ZERBO;Institut International d’Ingénierie de l’Eau et de l’Environnement (2iE);ETH Zürich, Department of Environmental System Sciences;

【通讯作者】 Anja Bretzler;

【机构】 Eawag,Swiss Federal Institute of Aquatic Science and TechnologyCentre d’Hydrogéologie et de Géothermie (CHYN), Université de NeuchatelTechnical University of Denmark (DTU)Université Ouaga I Pr.Joseph KI-ZERBOInstitut International d’Ingénierie de l’Eau et de l’Environnement (2iE)ETH Zürich, Department of Environmental System Sciences

【摘要】 The semi-arid Sahel regions of West Africa rely heavily on groundwater from shallow to moderately deep(<100 m b.g.l.)crystalline bedrock aquifers for drinking water production.Groundwater quality may be affected by high geogenic arsenic(As)concentrations(>10μg/L)stemming from the oxidation of sulphide minerals(pyrite,arsenopyrite)in mineralised zones.These aquifers are still little investigated,especially concerning groundwater residence times and the influence of the annual monsoon season on groundwater chemistry.To gain insights on the temporal aspects of As contamination,we have used isotope tracers(noble gases,3H,stable water isotopes(2 H,18O))and performed hydrochemical analyses on groundwater abstracted from tube wells and dug wells in a small study area in southwestern Burkina Faso.Results revealed a great variability in groundwater properties(e.g.redox conditions,As concentrations,water level,residence time)over spatial scales of only a few hundred metres,characteristic of the highly heterogeneous fractured underground.Elevated As levels are found in oxic groundwater of circum-neutral pH and show little relation with any of the measured parameters.Arsenic concentrations are relatively stable over the course of the year,with little effect seen by the monsoon.Groundwater residence time does not seem to have an influence on As concentrations,as elevated As can be found both in groundwater with short(<50 a)and long(>103 a)residence times as indicated by 3He/4He ratios spanning three orders of magnitude.These results support the hypothesis that the proximity to mineralised zones is the most crucial factor controlling As concentrations in the observed redox/pH conditions.The existence of very old water portions with residence times>103 years already at depths of<50 m b.g.l.is a new finding for the shallow fractured bedrock aquifers of Burkina Faso,suggesting that overexploitation of these relatively low-yielding aquifers may be an issue in the future.

【Abstract】 The semi-arid Sahel regions of West Africa rely heavily on groundwater from shallow to moderately deep(<100 m b.g.l.)crystalline bedrock aquifers for drinking water production.Groundwater quality may be affected by high geogenic arsenic(As)concentrations(>10μg/L)stemming from the oxidation of sulphide minerals(pyrite,arsenopyrite)in mineralised zones.These aquifers are still little investigated,especially concerning groundwater residence times and the influence of the annual monsoon season on groundwater chemistry.To gain insights on the temporal aspects of As contamination,we have used isotope tracers(noble gases,3H,stable water isotopes(2 H,18O))and performed hydrochemical analyses on groundwater abstracted from tube wells and dug wells in a small study area in southwestern Burkina Faso.Results revealed a great variability in groundwater properties(e.g.redox conditions,As concentrations,water level,residence time)over spatial scales of only a few hundred metres,characteristic of the highly heterogeneous fractured underground.Elevated As levels are found in oxic groundwater of circum-neutral pH and show little relation with any of the measured parameters.Arsenic concentrations are relatively stable over the course of the year,with little effect seen by the monsoon.Groundwater residence time does not seem to have an influence on As concentrations,as elevated As can be found both in groundwater with short(<50 a)and long(>103 a)residence times as indicated by 3He/4He ratios spanning three orders of magnitude.These results support the hypothesis that the proximity to mineralised zones is the most crucial factor controlling As concentrations in the observed redox/pH conditions.The existence of very old water portions with residence times>103 years already at depths of<50 m b.g.l.is a new finding for the shallow fractured bedrock aquifers of Burkina Faso,suggesting that overexploitation of these relatively low-yielding aquifers may be an issue in the future.

【基金】 provided by the Swiss Agency for Development and Cooperation (SDC) through the "Programme 3E" (contract no.81016359);the Information Management System on Geogenic Contaminants, GAP (contract no.81025383)
  • 【文献出处】 Geoscience Frontiers ,地学前缘(英文版) , 编辑部邮箱 ,2019年05期
  • 【分类号】P641.3
  • 【被引频次】1
  • 【下载频次】7
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