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Author Ladouche, B.; Luc, A.; Nathalie, D.
Title Chemical and isotopic investigation of rainwater in Southern France (1996–2002): Potential use as input signal for karst functioning investigation Type Journal Article
Year 2009 Publication Journal of Hydrology Abbreviated Journal
Volume 367 Issue 1-2 Pages 150-164
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Corporate Author Thesis
Publisher Elsevier Place of Publication Editor
Language Summary Language Original Title
Series Editor Series Title Abbreviated Series Title
Series Volume Series Issue Edition (up)
ISSN 0022-1694 ISBN Medium
Area Expedition Conference
Notes Approved no
Call Number THL @ luqianxue.zhang @ Ladouche2009 Serial 58
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Author Al-Khashman, O.A.
Title Chemical characteristics of rainwater collected at a western site of Jordan Type Journal Article
Year 2009 Publication Atmospheric Research Abbreviated Journal
Volume 91 Issue 1 Pages 53-61
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Abstract
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Corporate Author Thesis
Publisher Elsevier Place of Publication Editor
Language Summary Language Original Title
Series Editor Series Title Abbreviated Series Title
Series Volume Series Issue Edition (up)
ISSN 0169-8095 ISBN Medium
Area Expedition Conference
Notes Approved no
Call Number THL @ luqianxue.zhang @ Al-Khashman2009 Serial 59
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Author Mihajlidi-Zelić, A.; Deršek-Timotić, I.; Relić, D.; Popović, A.; Đorđević, D.
Title Contribution of marine and continental aerosols to the content of major ions in the precipitation of the central Mediterranean Type Journal Article
Year 2006 Publication Science of the total environment Abbreviated Journal
Volume 370 Issue 2-3 Pages 441-451
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Abstract
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Corporate Author Thesis
Publisher Elsevier Place of Publication Editor
Language Summary Language Original Title
Series Editor Series Title Abbreviated Series Title
Series Volume Series Issue Edition (up)
ISSN 0048-9697 ISBN Medium
Area Expedition Conference
Notes Approved no
Call Number THL @ luqianxue.zhang @ Mihajlidi-Zelić2006 Serial 60
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Author Guerzoni, S.; Molinaroli, E.; Chester, R.
Title Saharan dust inputs to the W. Mediterranean Sea: depositional patterns, geochemistry and sedimentological implications Type Journal Article
Year 1997 Publication Deep-Sea Res Abbreviated Journal
Volume 44 Issue 3-4 Pages 631-654
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Corporate Author Thesis
Publisher Place of Publication Editor
Language Summary Language Original Title
Series Editor Series Title Abbreviated Series Title
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ISSN ISBN Medium
Area Expedition Conference
Notes Approved no
Call Number THL @ luqianxue.zhang @ Guerzoni1997 Serial 61
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Author Vengosh, A.; Spivack, A.J.; Artzi, Y.; Ayalon, A.
Title Geochemical and boron, strontium, and oxygen isotopic constraints on the origin of the salinity in groundwater from the Mediterranean coast of Israel Type Journal Article
Year 1999 Publication Water Resources Research Abbreviated Journal
Volume 35 Issue 6 Pages 1877-1894
Keywords
Abstract In order to identify the origin of the salinity and formation of saline plumes in the central part of the Mediterranean coastal aquifer of Israel, we determined the elemental and boron, strontium, and oxygen isotopic compositions of fresh and brackish groundwater (C1 up to 1500 mg/L). We distinguish between two key anthropogenic sources: (1) sewage effluents used for irrigation with high Na/C1, SO4/C1, and B/C1 ratios and low Br/C1 ratios relative to seawater ratios, low ;5•B values (0-10%o) and high ;5•80 values (>-4%0); and (2) imported water from the Sea of Galilee that is artificially

recharged tothe aquifer with high Br/C1 (3 x 10 -3) and ;5•80 values (-1%o) and a low 87Sr/86Sr ratio of 0.70753. The brackish groundwater from the saline plumes have relatively low Na/C1 ratios (0.5-0.8) and high Ca/Mg, Mg/C1, and Ca/(SO 4 q- HCO3) (> l) ratios relative to seawater ratios; marine SO4/C1 and Br/C1 ratios;5•B values of 24.8-49.9%0; 18 87 86 ;50 of -2.95%0 to -4.73%0; and Sr/ Sr ratios of 0.708275-0.708532. The composition of most of the investigated groundwater from the saline plumes differs from those of the 87 86 anthropogenic sources, imported water, fresh uncontaminated groundwater (Sr/ Sr of 0.70866, ;5•B of 20-30%o), and saline water from the adjacent Eocene aquitard. Only in ß 18 areas of artificial recharge does local groundwater have high Br/C1 and ;50 values that are typical to the Sea of Galilee. The linear relationships between chloride and most of the ions, including Band Sr, the relatively high ;5•B (>30%0) and low ;5•80 (<-4%0) values, and the chemical signature of the saline plumes (e.g., marine Br/C1 and SO4/C1 ratios), suggest that (1) mixing processes control the chemical composition of the brackish water within the aquifer, and (2) the saline postulated end-member has a chemical composition that resembles modified seawater with a marine and higher ;5•B values, and a 87Sr/86Sr ratio of <0.7083. We propose that most of the salinization phenomena and the formation of saline plumes in the inner parts of the coastal aquifer are derived from upconing of underlying natural saline water bodies and enhanced by overexploitation and draw-down of the overlying fresh groundwater.
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Publisher Wiley Online Library Place of Publication Editor
Language Summary Language Original Title
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ISSN ISBN Medium
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Notes Approved no
Call Number THL @ luqianxue.zhang @ vengosh1999geochemical Serial 62
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