| Records |
| Author |
Deverel, S.J.; Fujii, R. |
| Title |
Chemistry of trace elements in soils and ground water |
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Journal Article |
| Year |
1990 |
Publication |
Agricultural salinity assessment and management |
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Pages  |
64-90 |
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American Society of Civil Engineers New York |
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THL @ luqianxue.zhang @ deverel1990chemistry |
Serial |
69 |
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| Author |
Bazrafshan, O.; Moradi, M.; Farokhzadeh, B. |
| Title |
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. |
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1(2) |
Issue |
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Pages |
62-69 |
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CUT @ phaedon.kyriakidis @ Bazrafshan2017 |
Serial |
155 |
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| Author |
Arslan*, H. |
| Title |
Spatial and temporal mapping of groundwater salinity using ordinary krigingand indicator kriging: The case of Bafra Plain, Turkey |
Type |
Journal Article |
| Year |
2012 |
Publication |
Agric. Water Manag. |
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113 |
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Pages |
57-63 |
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CUT @ phaedon.kyriakidis @ Arslan2012 |
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135 |
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| Author |
Pearce, C.R.; Parkinson, I.J.; Gaillardet, J.; Chetelat, B.; Burton, K.W. |
| Title |
Characterising the stable (δ88/86Sr) and radiogenic (87Sr/86Sr) isotopic composition of strontium in rainwater |
Type |
Journal Article |
| Year |
2015 |
Publication |
Chemical Geology |
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| Volume |
409 |
Issue |
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Pages |
54-60 |
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Elsevier |
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THL @ luqianxue.zhang @ pearce2015characterising |
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96 |
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| Author |
Zhao, Q.; Su, X.; Kang, B.; Zhang, Y.; Wu, X.; Liu, M. |
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A hydrogeochemistry and multi-isotope (Sr, O, H, and C) study of groundwater salinity origin and hydrogeochemcial processes in the shallow confined aquifer of northern Yangtze River downstream coastal plain, China |
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Journal Article |
| Year |
2017 |
Publication |
Applied Geochemistry |
Abbreviated Journal |
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| Volume |
86 |
Issue |
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Pages |
49-58 |
| Keywords |
Coastal confined groundwater, Salinity, Hydrogeochemcial processes, Multiple environmental tracers |
| Abstract |
Economically developed coastal areas have a high water demand, and their groundwater resources can be threatened by salinization. Many methods and tracers have been used to discriminate the source of salinization because a single method does not yield reliable results. In this paper, the shallow confined coastal plain aquifer, north of the downstream Yangtze River in China, is used as a case study to investigate the origin of the salinity and the relevant geochemical processes for this aquifer. Multiple environmental tracers of major ions, minor ions (Br−, I−), and isotopes (18O, 2H, 13C, 87Sr, 3H, 14C) were used so as to provide reliable conclusions. The TDS distribution of the aquifer has an increasing trend, from below 500 mg/L in the inland areas to more than 20,000 mg/L around the southeast coastline. The water chemical type evolves from HCO3-Ca to Cl-Na as the TDS increases. The results suggest that the groundwater salinity is influenced by seawater intrusion. The seawater proportions in the groundwater samples range from 0.07% to 94.41% and show the same spatial distribution pattern as TDS. The 3H and 14C values show that the highest salinity was mainly caused by a seawater transgression around 6000a B.P. The aquifer is also affected by other hydrogeochemical processes: base exchange has enriched Ca2+ and depleted K+ and Na+, sulfate reduction has reduced the concentration of SO42− and enriched HCO3−, and iodine-rich organic matter decomposition has enriched the concentration of I−. The iodine enrichment also suggests paleo-seawater intrusion. In addition, the precipitation of carbonate minerals has decreased the concentration of Ca2+, Mg2+, and HCO3−, albeit to a limited extent. |
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0883-2927 |
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no |
| Call Number |
THL @ christoph.kuells @ Zhao201749 |
Serial |
182 |
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