The recharge process in alluvial strip aquifers in arid Namibia and implication for artificial recharge; [Le processus de recharge dans des bandes aquifères alluviales en Namibie aride et son implication pour la recharge artificielle]; [O processo de recarga em aquíferos de depósitos aluvionares nas regiões áridas da Namíbia e suas implicações para recarga artificial]; [El proceso de recarga en los acuíferos de franjas aluviales áridas de Namibia y las implicancias en la recarga artificial]

被引:0
作者
Sarma D. [1 ,2 ]
Xu Y. [1 ,3 ]
机构
[1] Department of Earth Sciences, University of the Western Cape, Cape Town
[2] Namib Hydrosearch CC, Box 11546, Windhoek
[3] College of Water Resources Science and Engineering, Taiyuan University of Technology, Taiyuan
关键词
Alluvial strip aquifers; Arid regions; Artificial recharge; Namibia; Numerical modelling;
D O I
10.1007/s10040-016-1474-z
中图分类号
学科分类号
摘要
Alluvial strip aquifers associated with ephemeral rivers are important groundwater supply sources that sustain numerous settlements and ecological systems in arid Namibia. More than 70 % of the population in the nation’s western and southern regions depend on alluvial aquifers associated with ephemeral rivers. Under natural conditions, recharge occurs through infiltration during flood events. Due to the characteristic spatial and temporal variability of rainfall in arid regions, recharge is irregular making the aquifers challenging to manage sustainably and they are often overexploited. This condition is likely to become more acute with increasing water demand and climate change, and artificial recharge has been projected as the apparent means of increasing reliability of supply. The article explores, through a case study and numerical simulation, the processes controlling infiltration, significance of surface water and groundwater losses, and possible artificial recharge options. It is concluded that recharge processes in arid alluvial aquifers differ significantly from those processes in subhumid systems and viability of artificial recharge requires assessment through an understanding of the natural recharge process and losses from the aquifer. It is also established that in arid-region catchments, infiltration through the streambed occurs at rates dependent on factors such as antecedent conditions, flow rate, flow duration, channel morphology, and sediment texture and composition. The study provides an important reference for sustainable management of alluvial aquifer systems in similar regions. © 2016, Springer-Verlag Berlin Heidelberg.
引用
收藏
页码:123 / 134
页数:11
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