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Crystallization behavior of solid solutions from aqueous solutions: An environmental perspective
Affiliation:1. Department of Geology, University of Oviedo, C/ Arias de Velasco, s/n, 33005 Oviedo, Spain;2. Institute for Nuclear Waste Disposal, Karlsruhe Institute of Technology, 76021 Karlsruhe, Germany;3. Institute of Energy and Climate Research (IEK-6) – Nuclear Waste Management and Reactor Safety, Research Centre Jülich GmbH, 52425 Jülich, Germany;1. Nagoya City University, 3-1 Tanabe, Mizuho, Nagoya City, Aichi 467-8603, Japan;2. Tokushima University, 2-1 Minamijosanjima, Tokushima City, Tokushima 770-8506, Japan;3. Institute for Materials Research, Tohoku University, 2-1-1 Katahira, Aoba, Sendai City, Miyagi 980-8577, Japan;4. National Institute of Materials Sciences, 1-1, Namiki, Tsukuba City, Ibaraki 305-0044, Japan;1. National Institute of Advanced Industrial Science and Technology (AIST), 16-1 Onogawa, Tsukuba 305-8569, Japan;2. Graduate School of Natural Sciences, Nagoya City University, Yamanohata 1, Mizuho-cho, Mizuho-ku, Nagoya, Aichi 467-8501, Japan;3. Faculty of Science, Hokkaido University, N10 W8, Kita-ku, Sapporo, Hokkaido 060-0810, Japan;4. Computer Center, Gakushuin University, Mejiro 1-5-1, Toshima-ku, Tokyo 171-8588, Japan
Abstract:Aqueous–solid solution (AQ-SS) processes have garnered increasing attention from geochemists and environmental engineers because they play major roles in the fate and transport of elements in Earth surface environments. The reasons for this interest include: (i) the primary crystallization of minerals from multicomponent aqueous solutions leads to the formation of solid solutions in which different ions are substituted for one another in equivalent structural positions; (ii) the interaction between pre-existing minerals and water frequently yields surface precipitation and dissolution–recrystallization processes in which such substituting ions redistribute to adapt to new physicochemical conditions; (iii) the concentrations of specific minor elements in biogenic and abiogenic minerals have been shown to correlate with various parameters characterizing the growth environment (temperature, pH, nutrient levels, salinity, etc.) and the corresponding compositional signatures can be powerful tools in reconstructing the past from the sedimentary record; (iv) the aqueous concentration of heavy metals and other harmful ions can be significantly reduced by their incorporation into the structure of suitable host minerals and as such a ‘reduction of solubility’ can be exploited as a remediation strategy or used to design engineered barriers for the retention of metals, radionuclides, and other industrially generated inorganic wastes. In this review, the thermodynamics driving of AQ-SS processes is presented using examples of environmentally-relevant systems. The reaction pathways in AQ-SS processes depend not only on thermodynamic factors but also on kinetic and mechanistic effects, which operate at different scales in space and time. Examples of such effects include non-equilibrium ion partitioning, surface passivation, and compositional (sectorial, concentric, oscillatory) zoning. Finally, we discuss the contribution of both state-of-the-art characterization techniques and molecular simulation methods for the development of predictive models.
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