The objective of this paper is to assess quantitatively the potential recharge of shallow aquifers in the Senegal River delta in context of semi-arid climate, of massive irrigation development and of modification of hydrologic and hydrogeological characters after dams building. Quantitative estimation of recharge potentialities have been based on hydrological balance and groundwater table fluctuation calculations and on isotopic tracers techniques of the water molecule (δ18O, δ2H and 3H). This different methodological approaches used to estimate recharge rates have been useful, valuable and complementary. They give results fairly homogeneous and very interesting with indications accurate enough on recharge rates and on recharge spatio-temporal variations in shallow aquifers in alluvial plain (rate varying between 0-37% of annual rainfall) and dunes formations (rate varying between 0-44% of annual rainfall). Results indicate that recharge variations in term of proportions and of distribution are not only depending of volume and frequency rainfall or groundwater depth but also depending of soil and subsoil surface conditions, human activities (water withdraw, irrigation, market gardening, etc.) and evaporative demand. This recharge knowledge in terms of proportions and distribution in shallow aquifers is often very useful to propose groundwater resources management model and to define strategies to exploit them sustainably especially when groundwater resources are very unproductive and often very salty as in Senegal River delta.
Published in | American Journal of Water Science and Engineering (Volume 5, Issue 2) |
DOI | 10.11648/j.ajwse.20190502.12 |
Page(s) | 47-61 |
Creative Commons |
This is an Open Access article, distributed under the terms of the Creative Commons Attribution 4.0 International License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution and reproduction in any medium or format, provided the original work is properly cited. |
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Copyright © The Author(s), 2019. Published by Science Publishing Group |
Recharge Rate, Hydrological Balance, Groundwater Fluctuation, Isotopic Tracers, Shallow Aquifers, Senegal River Delta Hydrosystem
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APA Style
Moctar Diaw, Ibrahima Mall, Marc Le Blanc, Serigne Faye, Yves Travi. (2019). Quantitative Estimation of Recharge Potentialities of Shallow Aquifers in Senegal River Delta Hydrosystem. American Journal of Water Science and Engineering, 5(2), 47-61. https://doi.org/10.11648/j.ajwse.20190502.12
ACS Style
Moctar Diaw; Ibrahima Mall; Marc Le Blanc; Serigne Faye; Yves Travi. Quantitative Estimation of Recharge Potentialities of Shallow Aquifers in Senegal River Delta Hydrosystem. Am. J. Water Sci. Eng. 2019, 5(2), 47-61. doi: 10.11648/j.ajwse.20190502.12
AMA Style
Moctar Diaw, Ibrahima Mall, Marc Le Blanc, Serigne Faye, Yves Travi. Quantitative Estimation of Recharge Potentialities of Shallow Aquifers in Senegal River Delta Hydrosystem. Am J Water Sci Eng. 2019;5(2):47-61. doi: 10.11648/j.ajwse.20190502.12
@article{10.11648/j.ajwse.20190502.12, author = {Moctar Diaw and Ibrahima Mall and Marc Le Blanc and Serigne Faye and Yves Travi}, title = {Quantitative Estimation of Recharge Potentialities of Shallow Aquifers in Senegal River Delta Hydrosystem}, journal = {American Journal of Water Science and Engineering}, volume = {5}, number = {2}, pages = {47-61}, doi = {10.11648/j.ajwse.20190502.12}, url = {https://doi.org/10.11648/j.ajwse.20190502.12}, eprint = {https://article.sciencepublishinggroup.com/pdf/10.11648.j.ajwse.20190502.12}, abstract = {The objective of this paper is to assess quantitatively the potential recharge of shallow aquifers in the Senegal River delta in context of semi-arid climate, of massive irrigation development and of modification of hydrologic and hydrogeological characters after dams building. Quantitative estimation of recharge potentialities have been based on hydrological balance and groundwater table fluctuation calculations and on isotopic tracers techniques of the water molecule (δ18O, δ2H and 3H). This different methodological approaches used to estimate recharge rates have been useful, valuable and complementary. They give results fairly homogeneous and very interesting with indications accurate enough on recharge rates and on recharge spatio-temporal variations in shallow aquifers in alluvial plain (rate varying between 0-37% of annual rainfall) and dunes formations (rate varying between 0-44% of annual rainfall). Results indicate that recharge variations in term of proportions and of distribution are not only depending of volume and frequency rainfall or groundwater depth but also depending of soil and subsoil surface conditions, human activities (water withdraw, irrigation, market gardening, etc.) and evaporative demand. This recharge knowledge in terms of proportions and distribution in shallow aquifers is often very useful to propose groundwater resources management model and to define strategies to exploit them sustainably especially when groundwater resources are very unproductive and often very salty as in Senegal River delta.}, year = {2019} }
TY - JOUR T1 - Quantitative Estimation of Recharge Potentialities of Shallow Aquifers in Senegal River Delta Hydrosystem AU - Moctar Diaw AU - Ibrahima Mall AU - Marc Le Blanc AU - Serigne Faye AU - Yves Travi Y1 - 2019/06/26 PY - 2019 N1 - https://doi.org/10.11648/j.ajwse.20190502.12 DO - 10.11648/j.ajwse.20190502.12 T2 - American Journal of Water Science and Engineering JF - American Journal of Water Science and Engineering JO - American Journal of Water Science and Engineering SP - 47 EP - 61 PB - Science Publishing Group SN - 2575-1875 UR - https://doi.org/10.11648/j.ajwse.20190502.12 AB - The objective of this paper is to assess quantitatively the potential recharge of shallow aquifers in the Senegal River delta in context of semi-arid climate, of massive irrigation development and of modification of hydrologic and hydrogeological characters after dams building. Quantitative estimation of recharge potentialities have been based on hydrological balance and groundwater table fluctuation calculations and on isotopic tracers techniques of the water molecule (δ18O, δ2H and 3H). This different methodological approaches used to estimate recharge rates have been useful, valuable and complementary. They give results fairly homogeneous and very interesting with indications accurate enough on recharge rates and on recharge spatio-temporal variations in shallow aquifers in alluvial plain (rate varying between 0-37% of annual rainfall) and dunes formations (rate varying between 0-44% of annual rainfall). Results indicate that recharge variations in term of proportions and of distribution are not only depending of volume and frequency rainfall or groundwater depth but also depending of soil and subsoil surface conditions, human activities (water withdraw, irrigation, market gardening, etc.) and evaporative demand. This recharge knowledge in terms of proportions and distribution in shallow aquifers is often very useful to propose groundwater resources management model and to define strategies to exploit them sustainably especially when groundwater resources are very unproductive and often very salty as in Senegal River delta. VL - 5 IS - 2 ER -