دورية أكاديمية
Quantifying focused groundwater recharge induced by irrigation surface water reservoirs in crystalline basement areas for complementary irrigation
العنوان: | Quantifying focused groundwater recharge induced by irrigation surface water reservoirs in crystalline basement areas for complementary irrigation |
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المؤلفون: | Bambara, Apolline, Orban, Philippe, Ouedraogo, I., Hallot, Eric, Guyon, F., Zangré, A., Brouyère, Serge |
المساهمون: | UEE - Urban and Environmental Engineering - ULiège |
المصدر: | Water (Switzerland), 12 (10), 1-23 (2020-10) |
بيانات النشر: | MDPI AG, 2020. |
سنة النشر: | 2020 |
مصطلحات موضوعية: | Groundwater water balance, Hydrochemistry, Piezometry, Recharge, Surface water reservoir, Chemical analysis, Economics, Groundwater resources, Irrigation, Surface waters, Textures, Underground reservoirs, Water management, Water supply, Watersheds, Crystalline basement, Ground water recharge, Physico-chemical analysis, Regional groundwater, Sediment textures, Socio-economic development, Spatiotemporal analysis, Sub-saharan africa, Recharging (underground waters), Burkina Faso, Engineering, computing & technology, Geological, petroleum & mining engineering, Ingénierie, informatique & technologie, Géologie, ingénierie du pétrole & des mines |
الوصف: | Through the practice of irrigation, surface water reservoirs (SWRs) contribute to the socio-economic development and food production activities of populations in Sub-Saharan Africa (SSA). However, they tend to dry up prematurely. One solution to circumvent these irrigation water shortages is to ensure their conjunctive use with groundwater. The objective of this study is to better understand the contribution of SWRs to groundwater recharge and to determine if groundwater may be considered as a complementary local resource for irrigation. The study was carried out on two watersheds in Burkina Faso, Kierma and Mogtedo. The spatiotemporal analysis of piezometric and SWRs level records coupled with physico-chemical analyses of water was used to characterize exchanges between SWRs and groundwater. The regional groundwater recharge at the scale of the watersheds was assessed. At the SWRs scale, a water balance methodology was developed and used to estimate focused recharge. The results show that SWRs interact almost continuously with groundwater and contribute focused recharge. The magnitude of this recharge is a function of the geological context and the sediment texture of the SWRs. It is estimated at 5 mm/day in Kierma and 4 mm/day in Mogtédo. These values are higher than the natural recharge estimated at 0.2 mm/day in Kierma and 0.1 mm/day in Mogtédo. Additionally, the values of hydraulic conductivity are between 0.01 and 2 m/day in Kierma and between 1 × 10−4 and 0.2 m/day in Mogtédo. These conductivities could allow pumping in large-diameter hand-dug wells with a significant yield between 0.5 and 120 m3 /day in Kierma and between 0 and 10 m3 /day in Mogtédo to palliate the early drying up of the SWRs. © 2020 by the authors. Licensee MDPI, Basel, Switzerland. Caractérisation des conditions hydrogéologiques des nappes alluviales en amont des retenues d'eau d'irrigation |
نوع الوثيقة: | journal article http://purl.org/coar/resource_type/c_6501 article peer reviewed |
اللغة: | English |
Relation: | urn:issn:2073-4441 |
DOI: | 10.3390/w12102880 |
URL الوصول: | https://orbi.uliege.be/handle/2268/254603 |
حقوق: | open access http://purl.org/coar/access_right/c_abf2 info:eu-repo/semantics/openAccess |
رقم الأكسشن: | edsorb.254603 |
قاعدة البيانات: | ORBi |
DOI: | 10.3390/w12102880 |
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