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Author Edwards, P.J.; Williard, K.W.J.; Schoonover, J.E.
Title Fundamentals of watershed hydrology Type Journal Article
Year 2015 Publication Journal of contemporary water research & education Abbreviated Journal
Volume 154 Issue 1 Pages 3-20
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Publisher Wiley Online Library Place of Publication Editor
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Notes Approved no
Call Number (up) THL @ luqianxue.zhang @ edwards2015fundamentals Serial 101
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Author El-Sayed, S.A.; Ramadan, A.B.; Salama, M.H.; Diab, M.
Title Geochemical and Radiological Characteristics of Harvested Rainwater and Surficial Soil in El-Alamein-Alam El-Rum Area, Western Mediterranean Coastal Zone, Egypt Type Journal Article
Year 2015 Publication Isotope and Radiation Research Abbreviated Journal
Volume 47 Issue 2 Pages 177-198
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Call Number (up) THL @ luqianxue.zhang @ El-Sayed2015 Serial 57
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Author El Mandour, A.; El Yaouti, F.; Fakir, Y.; Zarhloule, Y.; Benavente, J.
Title Evolution of groundwater salinity in the unconfined aquifer of Bou-Areg, Northeastern Mediterranean coast, Morocco Type Journal Article
Year 2007 Publication Environmental Geology Abbreviated Journal
Volume 54 Issue 3 Pages 491-503
Keywords Unconfined aquifer, Groundwater salinity, Seawater intrusion, Nitrate pollution, Lagoon, Morocco  Bou-Areg
Abstract The Bou-Areg plain in the Mediterranean coast at the North-eastern of Morocco is characterized by a semiarid climate. The aquifer consists of two sedimentary formations of Plio-quaternary age: the upper formation of fine silts and the lower one of coarse silts with sand and gravels. The aquifer is underlain by marly bedrock of Miocene age that dips toward the coastal lagoon of Bou-Areg. The

hydrodynamic characteristics vary between 10–4 and 10–3 m/s; and transmissivities range between 10–4 and 10–1 m2 /s. The general direction of flow is SW to NE, toward the lagoon. The aquifer is crossed by the river Selouane, which also ends in the lagoon. The groundwater is characterized by a high salinity that can reach 7.5 g/l. The highest values are observed in the upstream and in the downstream sectors of the aquifer. The temporal evolution of the physicochemical parameters depends on the climatic conditions and

piezometric variations. The analysis of the spatio-temporal distribution of the physico-chemical parameters suggests different sources of groundwater salinization: the seawater intrusion, the influence of marly gypsum-bearing terrains, and the influence of anthropogenic products as the agricultural fertilizers, which cause great nitrate concentrations that vary between 80 and 140 mg/l.
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Publisher Springer Place of Publication Editor
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ISSN 0943-0105 ISBN Medium
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Notes Approved no
Call Number (up) THL @ luqianxue.zhang @ ElMandour2008 Serial 44
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Author Elrashidi, M.A.; Adriano, D.C.; Workman, S.M.; Lindsay, W.L.
Title Chemical equilibria of selenium in soils: a theoretical development1 Type Journal Article
Year 1987 Publication Soil Science Abbreviated Journal
Volume 144 Issue 2 Pages 141-152
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Publisher Lww Place of Publication Editor
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Call Number (up) THL @ luqianxue.zhang @ elrashidi1987chemical Serial 103
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Author Galazoulas, E.C.; Petalas, C.P.
Title Application of multivariate statistical procedures on major ions and trace elements in a multilayered coastal aquifer: the case of the south Rhodope coastal aquifer Type Journal Article
Year 2014 Publication Environmental earth sciences Abbreviated Journal
Volume 72 Issue 10 Pages 4191-4205
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Publisher Springer Place of Publication Editor
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Notes Approved no
Call Number (up) THL @ luqianxue.zhang @ galazoulas2014application Serial 100
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