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Analysis of garnet minerals. (a) The garnet structure along the [001] direction (b) Unit cell of the garnet structure showing the interconnected Ca sites forming a network for Ca diffusion. (c) Detail of the garnet structure showing three edge-sharing Ca dodecahedra. (d) Calculated energy barriers for Ca diffusion in garnet Ca 3 M 2 (SiO 4 ) 3 for M = Cr and Mn. Color code: Ca cyan, Cr/Mn blue, O red.

Analysis of garnet minerals. (a) The garnet structure along the [001] direction (b) Unit cell of the garnet structure showing the interconnected Ca sites forming a network for Ca diffusion. (c) Detail of the garnet structure showing three edge-sharing Ca dodecahedra. (d) Calculated energy barriers for Ca diffusion in garnet Ca 3 M 2 (SiO 4 ) 3 for M = Cr and Mn. Color code: Ca cyan, Cr/Mn blue, O red.

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Rechargeable lithium-ion batteries dominate the consumer electronics and electric vehicle markets. However, concerns on Li availability have prompted the development of alternative high energy density electrochemical energy storage systems. Rechargeable batteries based on a Ca metal anode can exhibit advantages in terms of energy density, safety an...

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... substitutional solid solution series of silicates with the general formula X 3 Y 2 Si 3 O 12 , where X is a divalent cation (Mg, Fe, Mn, and Ca, in the most common species) in 8-fold coordination and Y is a trivalent cation (Al, Fe, and Cr, in the most common species) in 6-fold coordination 36 . The structure of these silicate garnets (Fig. 5a) consists of isolated Si tetrahedra (in grey) sharing corners with the Y octahedra (in blue) to form chains along each of the a axes of a cubic cell. The spaces between chains are occupied by the X cations (in cyan) which are coordinated by eight oxygen atoms forming a triangular dodecahedron (i.e. distorted cube). Each dodecahedron is ...
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... the Y octahedra (in blue) to form chains along each of the a axes of a cubic cell. The spaces between chains are occupied by the X cations (in cyan) which are coordinated by eight oxygen atoms forming a triangular dodecahedron (i.e. distorted cube). Each dodecahedron is linked to other three forming a 3D network of sites in the structure (see Fig. 5b). In addition to these silicate garnets, the garnet supergroup 37 also includes minerals other than silicates and even those in which the anion is not oxygen (mainly OH − groups or, more rarely, F − ). All these minerals, however, are isostructural with the most common rock-forming silicate garnets described ...
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... garnet structure possesses three-dimensional pathways for Ca diffusion; Fig. 5c shows a detail of three interconnected Ca sites. Figure 5d provides the calculated energy landscape for Ca ions hopping from one Ca site to the nearest one. A diffusing Ca ion must move from the initial site across a quadrangular face to fit in a trigonal prismatic (TP) site at the transition state. The calculated Ca-O distances in the ...
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... garnet structure possesses three-dimensional pathways for Ca diffusion; Fig. 5c shows a detail of three interconnected Ca sites. Figure 5d provides the calculated energy landscape for Ca ions hopping from one Ca site to the nearest one. A diffusing Ca ion must move from the initial site across a quadrangular face to fit in a trigonal prismatic (TP) site at the transition state. ...
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... Ằ and r(O 2− ) = 1.4 Ằ, the Ca 2+ ion seems too large for the size of the channel. Regarding the cationic repulsions, although the TP site shares a face with the octahedral chromium, the Ca-Cr 3+ distance is 2.8 Å. This means that the cationic repulsion is lower than in the pyroxene structure, in agreement with its lower energy barrier of 2.07 eV (Fig. 5). However, this barrier is still too high for Ca ...

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... An observation of structural variations associated with the chemical and temperature-driven phase transition is performed on the solid solution series LiFeGe 2 O 6 and NaFeGe 2 O 6 [8]. Some pyroxene materials have shown suitability in Ca-ion and Li-ion batteries [9,10]. Kim et al. [11] have reported the ...
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... Экспериментальные и теоретические данные о стабильности карбонатных соединений при высоком давлении и высокой температуре необходимы для лучшего понимания углеродного цикла Земли и возможности хранения СО 2 . Электронные свойства важны для разработки перезаряжаемых батарей на основе металлического Са анода [8]. Твердые растворы Ca x Cd 1-x CO 3 представляют интерес с точки зрения сорбции для удаления кадмия из водных, морских и подземных вод [9]. ...
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... Computational modeling based on density functional theory (DFT) and classical pair potentials shows that activation energies of Ca ion diffusion in Ca-bearing oxide materials are high, indicating the slow movement of Ca ions. 52,53 For the Ca migration, three main local hops between adjacent Ca sites were identified (refer to Fig. 2). The lowest migration barrier is 4.42 eV (path A) (refer to Table IV). ...
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... Furthermore, calcium-bearing minerals are of interest in the development of electrode materials for rechargeable Ca-ion batteries [9]. Though CaAl 2 Si 2 O 8 was not studied for this purpose yet, theoretical investigation on other Ca-based minerals is available [10][11][12]. ...
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... Other studies have shown that the replacement of Al 3+ in NaAlSi 2 O 6 by Tl 3+ results in the large bandgap reduction (from 5.32 eV to 2.05 eV) which makes this doped pyroxene a potential material in photovoltaics and optoelectronic devices [6]. Some pyroxene structures have shown applicability in Li-ion batteries [7][8][9]. Furthermore, some pyroxene structures have exhibited exotic properties have recently renewed interest in the magnetic aspect of pyroxenes, such as multiferroicity [10][11][12], ferrotoroidicity [13], spin-singlet ground states [14,15] which can lead to phosphorescence and spin-Peierls transition which leads to a magnetoelastic transition in a quasi-one-dimensional system [16]. ...
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... Torres et al calculated various cobalt oxides, 1D-Ca 3 Co 2 O 6 , 2D-Ca 3 Co 4 O 9 and 3D-Ca 2 Co 2 O 5 for CIBs cathode applications and demonstrated the specific capacity to be 160, 165 and 192 mAh g −1 respectively. The calculated diffusion barrier was 0.9, 0.9 and 1.3 eV respectively [39]. ...
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... The broad peak centered at~25°is due to conductive carbon as mentioned above. A sharp peak at 29°is detected, which could be attributed to MnO 2 as per the literature [43][44][45]. The crystalline peak centered at~34°indexed to the (121) plane of CaMnO 3 reduces in intensity upon Ca-extraction and appears to shift to~35°, whereas other peaks also originally assigned to CaMnO 3 namely at 41.8°(220) and 60.5°(321) shift to 42°and 61.6°, respectively. ...
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