Academic Journal
Hydrogeochemical and multi-tracer investigations of arsenic-affected aquifers in semi-arid West Africa
| العنوان: | Hydrogeochemical and multi-tracer investigations of arsenic-affected aquifers in semi-arid West Africa |
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| المؤلفون: | Bretzler, Anja, Stolze, Lucien, Nikiema, Julien, Lalann, Franck, Ghadiri, Elaheh, Brennwald, Matthias S., Roll, Massimo, Schirmer, Mario |
| المصدر: | Geoscience Frontiers, 10 (5) |
| بيانات النشر: | Elsevier |
| سنة النشر: | 2019 |
| المجموعة: | ETH Zürich Research Collection |
| مصطلحات موضوعية: | Arsenic, Groundwater chemistry, West Africa, Fractured aquifers, Residence time, Noble gases |
| الوصف: | 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 (>10 μg/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 (2H, 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. |
| نوع الوثيقة: | article in journal/newspaper |
| وصف الملف: | application/application/pdf |
| اللغة: | English |
| Relation: | info:eu-repo/semantics/altIdentifier/wos/000483372500005; http://hdl.handle.net/20.500.11850/361644 |
| DOI: | 10.3929/ethz-b-000361644 |
| الاتاحة: | https://hdl.handle.net/20.500.11850/361644 https://doi.org/10.3929/ethz-b-000361644 |
| Rights: | info:eu-repo/semantics/openAccess ; http://creativecommons.org/licenses/by-nc-nd/4.0/ ; Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 International |
| رقم الانضمام: | edsbas.4DCF4AB4 |
| قاعدة البيانات: | BASE |
| DOI: | 10.3929/ethz-b-000361644 |
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