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Tziritis, D.E.; Fidelibus, M.D.; Guler, C.; Külls, C.; Sachsamanoglou, K. |
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An integrated hydrogeochemical approach to identify multiple salinization sources of a coastal aquifer (Rhodope, Northern Greece) |
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2022 |
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2022 Goldschmidt Conference |
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THL @ christoph.kuells @ tziritis2022integrated |
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213 |
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Author |
Külls, C.; Bassukas, D. |
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Title |
Groundwater salinization dynamics-an isotope approach |
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2022 |
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EGU General Assembly Conference Abstracts |
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22 |
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THL @ christoph.kuells @ kulls2022groundwaterb |
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214 |
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Külls, C. |
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Title |
Grundwasserqualität im Abstrom der Deponie Ihlenberg |
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2024 |
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THL @ christoph.kuells @ kulls2024grundwasserqualitat |
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226 |
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Ola, I.; Drebenstedt, C.; Burgess, R.M.; Allan, I.J.; Hoth, N.; Külls, C. |
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Title |
Application of Low Density Polyethylene (LDPE) Passive Samplers for Monitoring PAHs in Groundwater |
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2024 |
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THL @ christoph.kuells @ ola2024application |
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228 |
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Author |
Edmunds, W.M. |
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Title |
Bromine geochemistry of british groundwaters |
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Journal Article |
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Year |
1996 |
Publication |
Mineralogical Magazine |
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60 |
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399 |
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275-284 |
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\textlessp\textgreater The concentrations of Br in potable groundwaters in the United Kingdom range from 60 to 340 µg 1 \textlesssup\textgreater-1\textless/sup\textgreater . The occurrence of Br is described in terms of the Br/Cl weight ratio which enables small changes in bromide concentrations to be assessed in terms of salinity. Median values of Br/Cl in groundwaters range from 2.60 to 5.15 × 10 \textlesssup\textgreater−3\textless/sup\textgreater compared with a sea water ratio of 3.47× 10 \textlesssup\textgreater−3\textless/sup\textgreater . In recent shallow groundwaters the Br/Cl ratio is rather variable in response to a range of natural and anthropogenic inputs (marine and industrial aerosols, industrial and agricultural chemicals including road salt). Some slight enrichment in Br/Cl also occurs naturally during infiltration as a result of biogeochemical processes. \textless/p\textgreater |
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0026-461x |
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THL @ christoph.kuells @ Edmunds1996 |
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20 |
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