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Kisi, O.; Ardiçlio\uglu, M.; Hadi, A.M.W.; Kuriqi, A.; Kulls, C. |
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Title |
Estimation of mean velocity upstream and downstream of a bridge model using metaheuristic regression methods |
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2023 |
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Water Resources Management |
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37 |
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14 |
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5559-5580 |
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Springer Netherlands Dordrecht |
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THL @ christoph.kuells @ kisi2023estimation |
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223 |
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Kisi, O.; Heddam, S.; Parmar, K.S.; Yaseen, Z.M.; Kulls, C. |
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Title |
Improved monthly streamflow prediction using integrated multivariate adaptive regression spline with K-means clustering: implementation of reanalyzed remote sensing data |
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2024 |
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Stochastic Environmental Research and Risk Assessment |
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38 |
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6 |
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2489-2519 |
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Springer Berlin Heidelberg Berlin/Heidelberg |
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THL @ christoph.kuells @ kisi2024improved |
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221 |
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Wigley, T.M.L.; Plummer, L.N. |
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Title |
Mixing of carbonate waters |
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Journal Article |
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Year |
1976 |
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Geochimica et Cosmochimica Acta |
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40 |
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9 |
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989-995 |
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When mineral solutions of different compositions are mixed, the molalities and activities of individual ions in the mixture are often non-linear functions of their end-member values. This non-linearity is particularly significant in determining mineral saturation levels. Mixtures of saturated solutions may be either undersaturated or supersaturated depending on the end-member compositions and the physical conditions in which end-members and their mixtures exist. In carbonate solutions important non-linear effects occur due to redistribution of carbonate species. In extreme cases this causes mixture pH to be below both the end-member pH values. A simple but precise computer program (WATMIX) has been developed for calculating mixture composition for closed and open system mixing of arbitrary end-members. A number of mixing examples are considered which allow one to isolate three important processes leading to non-linear behaviour: the algebraic effect, the δPCO2 effect, and the ionic strength effect. |
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0016-7037 |
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THL @ christoph.kuells @ Wigley1976 |
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40 |
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Wen, H.; Carignan, J. |
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Reviews on atmospheric selenium: emissions, speciation and fate |
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2007 |
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Atmospheric environment |
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41 |
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34 |
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7151-7165 |
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Elsevier |
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THL @ luqianxue.zhang @ wen2007reviews |
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97 |
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Author |
Magaritz, M.; Nadler, A.; Kafri, U.; Arad, A. |
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Title |
Hydrogeochemistry of continental brackish waters in the southern Coastal Plain, Israel |
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1984 |
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Chemical Geology |
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42 |
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1 |
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159-176 |
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The southern Coastal Plain in Israel incorportates a transitional fringe of the desert in which three different chemical types of groundwater are found: (1) near-surface waters from springs along the Besor River course: (2) shallow- to moderate-depth waters from the slightly westward-dipping Pleistocene coastal aquifer (this aquifer, which consists of sandstone layers of the Kurkar Group, is recharged in the Coastal Plain); and (3) deep waters of the westward-dipping Upper Cretaceous Judea Group carbonates, which are recharged in the mountains in the east. A thick aquiclude of Upper Cretaceous-Tertiary rocks separates the Judea Group aquifer from the overlying coastal aquifer in the southern Coastal Plain. Isotopically light oxygen and depleted deuterium characterize the Judea Group waters, as expected from high-altitude recharge. The isotopic composition of the Coastal Plain waters is variable, but for the most part enriched in 18O and D. Within the southern Coastal Plain aquifer a southern subgroup comprises waters more depleted in heavy isotopes than those of either the northern or eastern subgroups. The Besor waters are isotopically similar to the Judea Group waters, reflecting their origin in the mountain region, and flow through the surficial river gravels and sands. It is suggested that leakage of the Besor waters into the underlying southern Coastal Plain aquifer results in mixing of the two water types. The most prominent chemical feature characterizing the groundwater of the southern Coastal Plain is Na+Cl− \textgreater 1. This Na+Cl− ratio can be maintained only by a continuous input from a non-marine source of Na. The most plausible source of this Na is the dissolution of feldspar derived from the windblown loess deposits which cover the area and/or leaching of trona minerals found in the unsaturated zone, combined with base-exchange processes. |
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0009-2541 |
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THL @ christoph.kuells @ Magaritz1984 |
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31 |
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