Titlebook: Rare Earth Elements in Groundwater Flow Systems; Karen H. Johannesson Book 2005 Springer Science+Business Media B.V. 2005 Aquatic Geochemi

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拋媚眼

Determination of 56 Trace Elements in Three Aquifer- Type Rocks by ICP-MS and Approximation of the elements (REEs) and 42 other trace elements in samples of Paleozoic carbonate, Paleozoic quartzite and shale from southern Nevada, and the U.S. Geological Survey standard for diabase, W-2. The trace elements were determined in the dissolved rock samples by low resolution inductively coupled plasma-

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Rare Earth, Major, and Trace Element Geochemistry of Surface and Geothermal Waters from the Taupo Vharacterized by hydrothermal activity with groundwaters feeding Lake Taupo, Waikato River, and the Wairakei and Wai-O-tapu hydrothermal fields of Rotorua. pH values ranged from near neutral (6.5–7.2) to alkaline (7.3–8.5). Surface water temperatures were between 15–16°C, while geothermal fluid tempe

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Rare Earth Element Contents of High pCO2 Groundwaters of Primorye, Russia: Mineral Stability and Coar East. The gas phase in these waters is dominated by mantle-derived CO. (up to 2.6 atm.), being introduced to shallow groundwaters along major fault systems. The aggressive nature of these moderately acidic groundwaters has led to unusual trace element characteristics with high concentrations of r

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Rare Earth Element Concentrations, Speciation, and Fractionation along Groundwater Flow Paths: The ntral Florida) to study the concentration, speciation, and fractionation of rare earth elements (REE) along the groundwater flow path in each system. Major solutes and dissolved organic carbon (DOC) were also measured in these groundwaters. In the Carrizo aquifer, groundwaters in the recharge zone a

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0921-092X original, peer-reviewed contributions by leading researcher.Rare Earth Elements in Groundwater Flow Systems. is the first volume of its kind entirely focused on the geochemistry of the lanthanide series elements in groundwater/aquifer environments. Consisting of ten chapters, each of which is an or

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Determination of 56 Trace Elements in Three Aquifer- Type Rocks by ICP-MS and Approximation of the light rare earth element oxides on the heavy REEs are discussed. Since the rock type may determine the chemical composition of the associated groundwater, the relative solubilities for the elements under study were approximated for a carbonate system by water-rock concentration ratios.