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Author Adolph, G.; Römer, T.; Külls, C.
Title (up) Deriving complex groundwater age structure by combining age dating and analytic element modelling Type Conference Article
Year Publication G-DAT 2008-Leipzig Abbreviated Journal
Volume Issue Pages 12
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Call Number THL @ christoph.kuells @ Adolph2008deriving Serial 55
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Author Baram, S.; Ronen, Z.; Kurtzman, D.; Külls, C.; Dahan, O.
Title (up) Desiccation-crack-induced salinization in deep clay sediment Type Journal Article
Year 2013 Publication Hydrology and Earth System Sciences Abbreviated Journal
Volume 17 Issue 4 Pages 1533
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Publisher Copernicus GmbH Place of Publication Editor
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Call Number THL @ christoph.kuells @ Baram2013desiccation Serial 21
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Author Adolph, G.; KÜlls, C.; Willscheid, A.
Title (up) Determination and validation of age structures as an improved measure of hydrological dynamics Type Conference Article
Year 2007 Publication Geophysical Research Abstracts Abbreviated Journal
Volume 9 Issue 08013 Pages
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Call Number THL @ christoph.kuells @ Adolph2007determination Serial 58
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Author Zaeri, A.; Mohammadi, Z.; Rezanezhad, F.
Title (up) Determining the source and mechanism of river salinity: An integrated regional study Type Journal Article
Year 2023 Publication Journal of Hydrology: Regional Studies Abbreviated Journal
Volume 47 Issue Pages 101411
Keywords River salinity, Salinization mechanism, Isotope, Halite brine, River sinuosity
Abstract Study region Zohreh River Basin, Southwest Iran Study focus The salinity of Zohreh River sharply increases in three salinity zones (SZs) along the river named SZ1, SZ2 (the focus of this study), and SZ3. Determining the salinity sources and salinization mechanism using an integrated approach including geological, hydrochemical, isotopic, geophysical, river sinuosity and hydrocarbon analysis are the main objectives of this study. The study focuses on the combination of evidence of regional-scale (i.e., river sinuosity and seismic data) and small-scale (i.e., drilling core analysis). New hydrologic insights for the region Among several known sources of river salinity, it was found that the water quality of the Zohreh River is mainly threatened by the salt-bearing Gachsaran Formation and oil-field brine. It is concluded that halite brine and oil-field brine simultaneously cause the salinization in SZ2, and their contributions were delineated to be 95% and 5%, respectively. The lack of reliable geological evidence to support halite dissolution in surficial layers by circulating waters suggests the possibility of a deep source of halite brine in SZ2. The results revealed that deep halite brine of the salt layers of Gachsaran Formation is mainly responsible for the salinization of SZ2. The mechanism of deep brine penetration to the river through the hidden fault failures detected by the combination of river sinuosity analysis and geophysical data for the first time.
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ISSN 2214-5818 ISBN Medium
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Call Number THL @ christoph.kuells @ Zaeri2023101411 Serial 251
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Author Külls, C.J.; Ritter, M.
Title (up) Deuterium excess anomaly of precipitation in Svalbard Type Conference Article
Year 2010 Publication American Geophysical Union Abbreviated Journal
Volume 2010 Issue Pages 51
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Call Number THL @ christoph.kuells @ Kuells2010deuterium Serial 50
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