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Author Bazrafshan, O.; Moradi, M.; Farokhzadeh, B.
Title (up) Evaluation of interpolation techniques for the salinity of groundwater in wet and dry seasons (Case Study: Minab Plain, South Coast of Iran) Type Journal Article
Year 2017 Publication J. Hydrosci. Env. Abbreviated Journal
Volume 1(2) Issue Pages 62-69
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Notes Approved no
Call Number CUT @ phaedon.kyriakidis @ Bazrafshan2017 Serial 155
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Author Alexakis, D.; Gotsis, D.; Giakoumakis, S.
Title (up) Evaluation of soil salinization in a Mediterranean site (Agoulinitsa district—West Greece) Type Journal Article
Year 2015 Publication Arabian Journal of Geosciences Abbreviated Journal
Volume 8 Issue 3 Pages 1373-1383
Keywords Agricultural soil . Soil quality . Soil salinization
Abstract Soil salinization is an environmental problem having

significant impacts on the soil–water–plant system. This

problem is more frequent in coastal areas due to seawater

intrusion into the land. Assessing the soil salinization is a

critical issue for the agricultural areas situated in the

Mediterranean basin. This paper examines the deterioration

of soil quality in the cultivated land of a Mediterranean site

(Agoulinitsa district—West Greece). Soil samples were collected

in both pre-irrigation and post-irrigation seasons.

Electrical conductivity (EC), pH and the ions Br−, Ca2+, Cl−,

F−, K+, Li+, Mg2+, Na+, NH4

+, NO2

−, NO3

−, PO4

3− and SO4

2−

were determined by the 1:2 (soil/water ratio on weight basis)

method. The salts which were present in both seasons in the

soils of the area studied are KCl, MgCl2, NaCl, CaSO4 and

K2SO4. The wide spatiotemporal variation of EC in the cultivated

land in both seasons demonstrates that soil salinity is

controlled mainly by seawater intrusion and anthropogenic

factors such as the application of salt-rich water which is

directly pumped from the drainage ditches. Seawater intrusion

provides the affected soil with elevated contents of Ca2+, Cl−,

K+, Mg2+, Na+ and SO4

2−. Classification of the soils by using

criteria given by the literature is discussed. Practices to prevent,

or at least ameliorate, salinization in the cultivated land

of Agoulinitsa district are proposed.
Address
Corporate Author Thesis
Publisher Springer Place of Publication Editor
Language Summary Language Original Title
Series Editor Series Title Abbreviated Series Title
Series Volume Series Issue Edition
ISSN 1866-7511 ISBN Medium
Area Expedition Conference
Notes Approved no
Call Number THL @ luqianxue.zhang @ Alexakis2015 Serial 42
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Author Egbi*, C.D.; Anornu, G.; Appiah‑Adjei, E.K.; Ganyaglo, S.Y.; Dampare, S.B.
Title (up) Evaluation of water quality using hydrochemistry, stable isotopes, and water quality indices in the Lower Volta River Basin of Ghana Type Journal Article
Year 2019 Publication Environ. Dev. Sustain. Abbreviated Journal
Volume 21 Issue Pages 3033-3063
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Notes Approved no
Call Number CUT @ phaedon.kyriakidis @ Egbi2018 Serial 124
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Author El Mandour, A.; El Yaouti, F.; Fakir, Y.; Zarhloule, Y.; Benavente, J.
Title (up) 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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Corporate Author Thesis
Publisher Springer Place of Publication Editor
Language Summary Language Original Title
Series Editor Series Title Abbreviated Series Title
Series Volume Series Issue Edition
ISSN 0943-0105 ISBN Medium
Area Expedition Conference
Notes Approved no
Call Number THL @ luqianxue.zhang @ ElMandour2008 Serial 44
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Author Kloppmann, W.; Petelet-Giraud, E.; Guerrot, C.; Cary, L.; Pauwels, H.
Title (up) Extreme Boron Isotope Ratios in Groundwater Type Journal Article
Year 2015 Publication Procedia Earth and Planetary Science Abbreviated Journal
Volume 13 Issue Pages
Keywords
Abstract Kloppmann, W. , Petelet-Giraud, E. , Guerrot, C. , Cary, L. , & Pauwels, H. (2015). Extreme Boron Isotope Ratios in Groundwater. Procedia Earth and Planetary Science, 13 . doi: 10.1016/j.proeps.2015.07.069
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Publisher Place of Publication Editor
Language Summary Language Original Title
Series Editor Series Title Abbreviated Series Title
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Notes Approved no
Call Number THL @ christoph.kuells @ Serial 193
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