Abstract

Bond-length distributions have been examined for 55 configurations of alkali-metal ions and 29 configurations of alkaline-earth-metal ions bonded to oxygen, for 4859 coordination polyhedra and 38 594 bond distances (alkali metals), and for 3038 coordination polyhedra and 24 487 bond distances (alkaline-earth metals). Bond lengths generally show a positively skewed Gaussian distribution that originates from the variation in Born repulsion and Coulomb attraction as a function of interatomic distance. The skewness and kurtosis of these distributions generally decrease with increasing coordination number of the central cation, a result of decreasing Born repulsion with increasing coordination number. We confirm the following minimum coordination numbers: ([3])Li(+), ([3])Na(+), ([4])K(+), ([4])Rb(+), ([6])Cs(+), ([3])Be(2+), ([4])Mg(2+), ([6])Ca(2+), ([6])Sr(2+) and ([6])Ba(2+), but note that some reported examples are the result of extensive dynamic and/or positional short-range disorder and are not ordered arrangements. Some distributions of bond lengths are distinctly multi-modal. This is commonly due to the occurrence of large numbers of structure refinements of a particular structure type in which a particular cation is always present, leading to an over-representation of a specific range of bond lengths. Outliers in the distributions of mean bond lengths are often associated with anomalous values of atomic displacement of the constituent cations and/or anions. For a sample of ([6])Na(+), the ratio Ueq(Na)/Ueq(bonded anions) is partially correlated with 〈([6])Na(+)-O(2-)〉 (R(2) = 0.57), suggesting that the mean bond length is correlated with vibrational/displacement characteristics of the constituent ions for a fixed coordination number. Mean bond lengths also show a weak correlation with bond-length distortion from the mean value in general, although some coordination numbers show the widest variation in mean bond length for zero distortion, e.g. Li(+) in [4]- and [6]-coordination, Na(+) in [4]- and [6]-coordination. For alkali-metal and alkaline-earth-metal ions, there is a positive correlation between cation coordination number and the grand mean incident bond-valence sum at the central cation, the values varying from 0.84 v.u. for ([5])K(+) to 1.06 v.u. for ([8])Li(+), and from 1.76 v.u. for ([7])Ba(2+) to 2.10 v.u. for ([12])Sr(2+). Bond-valence arguments suggest coordination numbers higher than [12] for K(+), Rb(+), Cs(+) and Ba(2+).

Highlights

  • Many crystal structures have been refined in the past 100 years, and a large amount of information concerning interatomic distances in the solid state is available

  • We report the bond-length distributions for 10 ions, the common alkali-metal ions (Li+, Na+, K+, Rb+ and Cs+) and alkaline-earth-metal ions (Be2+, Mg2+, Ca2+, Sr2+ and Ba2+) in all observed coordination numbers where bonded to O2À for a total of 63 081 bond lengths in 7897 polyhedra from 4258 refined crystal structures

  • Results for the alkali metals Our collection and filtering criteria resulted in a combined sample size of 38 594 bonds and 4859 coordination polyhedra

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Summary

Introduction

Many crystal structures have been refined in the past 100 years, and a large amount of information concerning interatomic distances in the solid state is available. Baur, 1971 (Si); Burns et al, 1997 (U); Hawthorne et al, 2000 (S); Schindler et al, 2000 (V); Hawthorne & Huminicki, 2002 (Be); Huminicki & Hawthorne, 2002 (P); Mills & Christy, 2013 (Te); Majzlan et al, 2014 (As)] Many of these studies have focused on subsets of the available information, both with regard to the number of ions and coordination numbers, and to the amount of data available for each example. An advantage of working with a large number of ion pairs and a large amount of data is that it allows examination of subtle differences between the shapes of various distributions (e.g. bondlength distributions, mean-bond-length distributions) for various configurations of ions, which reflect differences in their bonding behaviour. We give a preliminary examination of the alkali-metal ions and alkaline-earth-metal ions in all observed coordination numbers where bonded to O2À, and make our complete dataset available for future more detailed work. (2) A comprehensive knowledge of the observed variation in bond lengths is critically important in assessing the validity of computational results on possible atomic arrangements (e.g. Richardson, 2013) and identifying unusual stereochemical features in newly solved or refined crystal structures

Definitions
Large coordination numbers
Methods
Selection criteria
Determination of coordination polyhedra
Shape of the bond-length distributions
Sample size
The effect of outliers
Observed coordination numbers
Skewness and kurtosis as a function of coordination number
Results for the alkaline-earth metals
Range in bond length as a function of coordination number
Skewness
Kurtosis
Bond valences
10. Mean bond-length distributions
10.1. The effect of distortion
10.2. Atomic displacement
10.3. The relation between mean bond length and atomic displacement
11. Summary
Full Text
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