2019
DOI: 10.1002/crat.201900037
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Empirical Electronic Polarizabilities: Deviations from the Additivity Rule. II. Structures Exhibiting Ion Conductivity

Abstract: Ion conductivity in minerals and compounds is associated with continuous migration paths and leads to negative total electronic polarizability deviations [ = (α obs −α calc )/α obs )] up to 13%. Such deviations can be related to continuous migration paths determined in an earlier Voronoi-Dirichlet Partition (VDP) analysis of fast-ion conductors, that is, compounds such as LiB 3 O 5 with 1D conductivity, Li 4 SiO 4 with 2D conductivity, and Li 2 SO 4 with 3D conductivity. Using the Voronoi-Dirichlet (VD) method… Show more

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Cited by 6 publications
(8 citation statements)
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“…Garnet refractive index ( n ) at 589 nm was calculated by methods developed by Shannon and coworkers: 72–74,93 n2badbreak=4παT()bold-italicc4π3αT+Vmgoodbreak+1$$\begin{equation}{{\bm{n}}}^2 = \frac{{4\pi {{\bm{\alpha }}}_{\bm{T}}}}{{\left( {{\bm{c}} - \frac{{4\pi }}{3}} \right){{\bm{\alpha }}}_{\bm{T}} + {V}_m}} + 1\end{equation}$$ Vmbadbreak=a3/normalZ.$$\begin{equation}{{\rm{V}}}_{\rm{m}} = {{\bm{a}}}^3/{\rm{Z}}.\end{equation}$$ V m is the molecular volume in Å 3 . Z is the number of formula units per unit cell, which for garnets is 8. α T , the total polarizability (Å 3 ), is: αTbadbreak=normali=1Nmibold-italicαei.$$\begin{equation}{{\bm{\alpha }}}_T = \sum\nolimits_{{\rm{i }} = {\rm{ }}1}^{\rm{N}} {{m}_i{{\bm{\alpha }}}_{ei}} .\end{equation}$$…”
Section: Methodsmentioning
confidence: 99%
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“…Garnet refractive index ( n ) at 589 nm was calculated by methods developed by Shannon and coworkers: 72–74,93 n2badbreak=4παT()bold-italicc4π3αT+Vmgoodbreak+1$$\begin{equation}{{\bm{n}}}^2 = \frac{{4\pi {{\bm{\alpha }}}_{\bm{T}}}}{{\left( {{\bm{c}} - \frac{{4\pi }}{3}} \right){{\bm{\alpha }}}_{\bm{T}} + {V}_m}} + 1\end{equation}$$ Vmbadbreak=a3/normalZ.$$\begin{equation}{{\rm{V}}}_{\rm{m}} = {{\bm{a}}}^3/{\rm{Z}}.\end{equation}$$ V m is the molecular volume in Å 3 . Z is the number of formula units per unit cell, which for garnets is 8. α T , the total polarizability (Å 3 ), is: αTbadbreak=normali=1Nmibold-italicαei.$$\begin{equation}{{\bm{\alpha }}}_T = \sum\nolimits_{{\rm{i }} = {\rm{ }}1}^{\rm{N}} {{m}_i{{\bm{\alpha }}}_{ei}} .\end{equation}$$…”
Section: Methodsmentioning
confidence: 99%
“…A complete list of α ei used for calculations is in Table 1. Detailed discussion of α ei for most cations is available in the literature 72–74,93 …”
Section: Methodsmentioning
confidence: 99%
See 1 more Smart Citation
“…The calculated mean values of <α AE > for 54 common minerals and 650 minerals and synthetic compounds differ by less than 3% from the observed values. Using dynamic polarizabilities, we observed systematic deviations in: (1) M 2+ SO 4 •nH 2 O, blödite (Na 2 M 2+ (SO 4 ) 2 •4H 2 O), and kieserite-related minerals (Gagné et al 2018), (2) fast-ion conductors (Shannon et al, 2019), (3) crystal structures containing corner-shared octahedra such as MTiO 3 (M = Ca, Sr, Ba), KNbO 3 , KTaO 3 , Ba .25 Sr .75 Nb 2 O 6 and KTiOPO 4 , and (4) crystal structures containing edge-shared Fe 3+ , Mn 3+ , Ti 4+ , Mo 6+ , and W 6+ octahedra such as MnWO 4 (hübnerite) (Shannon and Fischer, 2016).…”
Section: Generalmentioning
confidence: 99%
“…In virtue of strong interactions of heterointerface between NMNO and NSO and the invoking of the built-in electric field in heterointerface, this novel heterostructure NMNO/NSO achieves a synergy function in enhancing structural stability and boosting Na + diffusion and charge transfer kinetics, resulting in a significant enhancement in cycling stability and rate capability. NSO is a potential Na + 2D conductor along the (010) plane according to previously calculated [31] and shows a stable structure. It can be easily in situ grown during NMNO synthesis to form a novel heterostructure NMNO/NSO.…”
Section: Introductionmentioning
confidence: 99%