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Author Xu, J.; Li, W.; Hong, Y.; Wei, C.; Tang, J.
Title A quantitative assessment on groundwater salinization in the Tarim River lower reaches, Northwest China Type Journal Article
Year 2014 Publication Sci. Cold Arid. Reg. Abbreviated Journal
Volume 6(1) Issue Pages (up) 44-51
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Call Number CUT @ phaedon.kyriakidis @ Xu2014 Serial 126
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Author Rajabi, M.M.; Ataie-Ashtiani, B.
Title Sampling efficiency in Monte Carlo based uncertainty propagation strategies: Application in seawater intrusion simulations Type Journal Article
Year 2014 Publication Adv. Water Resour. Abbreviated Journal
Volume 67 Issue Pages (up) 46-64
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Call Number CUT @ phaedon.kyriakidis @ Rajabi2014 Serial 153
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Author Zhao, Q.; Su, X.; Kang, B.; Zhang, Y.; Wu, X.; Liu, M.
Title 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 Type Journal Article
Year 2017 Publication Applied Geochemistry Abbreviated Journal
Volume 86 Issue Pages (up) 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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ISSN 0883-2927 ISBN Medium
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Call Number THL @ christoph.kuells @ Zhao201749 Serial 182
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Author Joseph, J.; Külls, C.; Arend, M.; Schaub, M.; Hagedorn, F.; Gessler, A.; Weiler, M.
Title Application of a laser-based spectrometer for continuous in situ measurements of stable isotopes of soil CO 2 in calcareous and acidic soils Type Journal Article
Year 2019 Publication Soil Abbreviated Journal
Volume 5 Issue 1 Pages (up) 49-62
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Publisher Copernicus Publications Göttingen, Germany Place of Publication Editor
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Call Number THL @ christoph.kuells @ joseph2019application Serial 198
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Author Kurunc, A.; Ersahin, S.; Sonmez, N.K.; Kaman, H.; Uz, I.; Uz, B.Y.; Aslan, G.E.
Title Seasonal changes of spatial variation of some groundwater quality variables in a large irrigated coastal Mediterranean region of Turkey Type Journal Article
Year 2016 Publication Science of the Total Environment Abbreviated Journal
Volume 554 Issue Pages (up) 53-63
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Abstract Soil and groundwater degradations have taken considerable attention, recently. We studied spatial and temporal variations of groundwater table depth and contours, and groundwater pH, electrical conductivity (EC), and nitrate (NO3) content in a large irrigated area in Western Mediterranean region of Turkey. These variables were

monitored during 2009 and 2010 in previously constructed 220 monitoring wells. We analyzed the data by geostatistical techniques and GIS. Spatial variation of groundwater table depth (GTD) and groundwater table contours (GTC) remained similar across the four sampling campaigns. The values for groundwater NO3 content, EC, and pH values ranged from 0.01 to 454.1 g L−1 , 0.06 to 46.0 dS m−1 and 6.53–9.91, respectively. Greatest

geostatistical range (16,964 m) occurred for GTC and minimum (960 m) for groundwater EC. Groundwater NO3 concentrations varied both spatially and temporally. Temporal changes in spatial pattern of NO3 indicated that land use and farming practices influenced spatial and temporal variation of groundwater NO3. Several hot spots occurred for groundwater NO3 content and EC. These localities should be monitored more frequently and

land management practices should be adjusted to avoid soil and groundwater degradation. The results may have important implications for areas with similar soil, land use, and climate conditions across the Mediterranean region.
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Publisher Elsevier Place of Publication Editor
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ISSN 0048-9697 ISBN Medium
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Call Number THL @ luqianxue.zhang @ Kurunc2016 Serial 45
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