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Author Hanshaw, B.B.; Back, W.
Title Deciphering hydrological systems by means of geochemical processes Type Journal Article
Year 1985 Publication Hydrological Sciences Journal Abbreviated Journal
Volume (up) 30 Issue 2 Pages 257-271
Keywords
Abstract The distribution of permeability and chemical character of groundwater in carbonate aquifers is significantly influenced by the many diagenetic processes

and reactions that occur in the early development of these rocks. Many of these diagenetic processes occur in the transition zone formed as the carbonate sediments emerge from the marine environment and become fresh-water aquifers. Analyses of trace elements and isotopes

indicate that calcite cements and dolomites are formed in this groundwater mixing zone. Reverse reactions such as mineral dissolution and dedolomitization occur in carbonate aquifer systems. The geochemical reactivity of the fresh-water/salt-water mixing zone results from the nonlinearity of geochemical parameters as a function of ionic strength and causes extensive dissolution in coastal carbonate rocks. Interpretation of geochemical reactions and isotopic composition of groundwater provides a method to determine hydrological parameters

such as porosity, hydraulic conductivity, and groundwater flow rates. This geochemical method is largely independent of the more conventional approach of determining these parameters by an evaluation of physical properties of aquifer systems.
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ISSN 0262-6667 ISBN Medium
Area Expedition Conference
Notes Approved no
Call Number THL @ christoph.kuells @ Hanshaw1985 Serial 25
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Author Pezzarossa, B.; Piccotino, D.; Petruzzelli, G.
Title Sorption and desorption of selenium in different soils of the Mediterranean area Type Journal Article
Year 1999 Publication Communications in soil science and plant analysis Abbreviated Journal
Volume (up) 30 Issue 19-20 Pages 2669-2679
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Publisher Taylor & Francis 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 @ pezzarossa1999sorption Serial 76
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Author Adnan, R.M.; Dai, H.-L.; Kisi, O.; Heddam, S.; Kim, S.; Kulls, C.; Zounemat-Kermani, M.
Title Modelling biochemical oxygen demand using improved neuro-fuzzy approach by marine predators algorithm Type Journal Article
Year 2023 Publication Environmental Science and Pollution Research Abbreviated Journal
Volume (up) 30 Issue 41 Pages 94312-94333
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Publisher Springer Berlin Heidelberg Berlin/Heidelberg Place of Publication Editor
Language Summary Language Original Title
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Notes Approved no
Call Number THL @ christoph.kuells @ adnan2023modelling Serial 218
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Author Kisi, O.; Ajri, S.; Jörgens, K.C.; Karande, A.; Kraus, S.; Naumann, B.; Nierman, K.; Seel, W.; Kulls, C.
Title Comments on “Splitting tensile strength prediction of sustainable high-performance concrete using machine learning techniques” by Wu, Yangi et al., https://doi. org/10.1007/s11356-022-22048-2 Type Journal Article
Year 2023 Publication Environmental Science and Pollution Research Abbreviated Journal
Volume (up) 30 Issue 50 Pages 109854-109855
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Publisher Springer Berlin Heidelberg Berlin/Heidelberg Place of Publication Editor
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Notes Approved no
Call Number THL @ christoph.kuells @ kisi2023comments Serial 222
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Author Liu, Y.; Jin, M.; Wang, J.
Title Insights into groundwater salinization from hydrogeochemical and isotopic evidence in an arid inland basin Type Journal Article
Year 2018 Publication Hydrological Processes Abbreviated Journal
Volume (up) 32 Issue 20 Pages 3108-3127
Keywords deuterium excess, groundwater salinization, Northwest China, Manas River basin, stable isotopes
Abstract Abstract In the Manas River basin (MRB), groundwater salinization has become a major concern, impeding groundwater use considerably. Isotopic and hydrogeochemical characteristics of 73 groundwater and 11 surface water samples from the basin were analysed to determine the salinization process and potential sources of salinity. Groundwater salinity ranged from 0.2 to 11.91 g/L, and high salinities were generally located in the discharge area, arable land irrigated by groundwater, and depression cone area. The quantitative contributions of the evaporation effect were calculated, and the various groundwater contributions of transpiration, mineral dissolution, and agricultural irrigation were identified using hydrogeochemical diagrams and δD and δ18O compositions of the groundwater and surface water samples. The average evaporation contribution ratios to salinity were 5.87% and 32.7% in groundwater and surface water, respectively. From the piedmont plain to the desert plain, the average groundwater loss by evaporation increased from 7% to 29%. However, the increases in salinity by evaporation were small according to the deuterium excess signals. Mineral dissolution, transpiration, and agricultural irrigation activities were the major causes of groundwater salinization. Isotopic information revealed that river leakage quickly infiltrated into aquifers in the piedmont area with weak evaporation effects. The recharge water interacted with the sediments and dissolved minerals and subsequently increased the salinity along the flow path. In the irrigation land, shallow groundwater salinity and Cl− concentrations increased but not δ18O, suggesting that both the leaching of soil salts due to irrigation and transpiration effect dominated in controlling the hydrogeochemistry. Depleted δ18O and high Cl− concentrations in the middle and deep groundwater revealed the combined effects of mixing with paleo-water and mineral dissolution with a long residence time. These results could contribute to the management of groundwater sources and future utilization programs in the MRB and similar areas.
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Call Number THL @ christoph.kuells @ doi:10.1002/hyp.13243 Serial 178
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