期刊名称：Science et changements planétaires / Sécheresse
印刷版ISSN：1147-7806
电子版ISSN：1777-5922
出版年度：2008
卷号：19
期号：2
页码：145-151
DOI：10.1684/sec.2008.0132
出版社：John Libbey Eurotext
摘要：Figures See all figures Authors Malika Kili , Bouabid El Mansouri , Jamal Chao Laboratoire des géosciences appliquées, Équipe technologies des ressources en eau, Faculté des sciences de Kénitra, Université Ibn Tofail, BP 133, 14000 Kénitra, Maroc Key words: ground water, Morocco, water balance DOI : 10.1684/sec.2008.0132 Page(s) : 145-51 Published in: 2008 The Gharb plain belongs to one of the largest hydrogeologic basins of Western Morocco. Study of a monthly water balance of the various types of soils compiled over thirteen years made the estimatation of infiltration by deep percolation possible. These evaluations relate to the supply of the shallow water table and the deep confined water under the plain through the permeable coastal zone. The interannual recharge of the latter varies from 0 to 52% compared to the average volume of annual total rainfall received by this area located near the oceanic margin and overexploited due to the development of agriculture confronted with recurring periods of drought.
