1991
DOI: 10.1038/350675a0
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Medium-range order in the cation distribution of a calcium silicate glass

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Cited by 251 publications
(151 citation statements)
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“…The structure of the glass at a composition close to CaSiO 3 ͑with the addition of 3% Al 2 O 3 ͒ has been studied in exceptional detail using a double difference neutron isotopic substitution method. 4 Gaskell et al 4 provided evidence that the distribution of calcium atoms was not random in the glass but exhibited a well-defined Ca-Ca peak at 3.8 Å bearing many characteristics of the crystalline form. The structures of crystalline pyroxenes such as wollastonite can be considered as a close packed oxygen sublattice with Ca occupying octahedral interstices in alternate layers in a fcc model.…”
Section: Resultsmentioning
confidence: 99%
See 1 more Smart Citation
“…The structure of the glass at a composition close to CaSiO 3 ͑with the addition of 3% Al 2 O 3 ͒ has been studied in exceptional detail using a double difference neutron isotopic substitution method. 4 Gaskell et al 4 provided evidence that the distribution of calcium atoms was not random in the glass but exhibited a well-defined Ca-Ca peak at 3.8 Å bearing many characteristics of the crystalline form. The structures of crystalline pyroxenes such as wollastonite can be considered as a close packed oxygen sublattice with Ca occupying octahedral interstices in alternate layers in a fcc model.…”
Section: Resultsmentioning
confidence: 99%
“…2,3 This is despite the analysis of quenched glass structures that indicate atomic to nanometer scale structural heterogeneity must occur in the liquid state. [4][5][6][7] Silica is classified as a strong liquid with an Arrhenius viscosity-temperature relation and only subtle differences occur between the liquid and glass structures. 8,9 In contrast CaO-SiO 2 liquids can be considered fragile based on viscosity measurements 10,11 and consequently larger structural rearrangements are likely to be necessary to form a glass.…”
Section: Introductionmentioning
confidence: 99%
“…A similar argument can be made for minerals crystallizing from magmas. For example, Gaskell et al (1991) showed that a glass of composition CaSiO 3 has a local structure very similar to that of wollastonite. Assuming that the structure of the glass is somewhat similar to that of CaSiO 3 melt close to the liquidus, the initial reactant in the crystallization of wollastonite (a CaSiO 3 ''magma'') is already templated with much of the wollastonite structure, and many of the atoms in the system will obey the Reaction Principle, resulting in the crystallization of wollastonite.…”
Section: Fourth-moment Changesmentioning
confidence: 99%
“…The wave vector Q, of the FSDP corresponds to a length scale L, = 2x/Q, on the order of 2.5 r, (rl is the nearest-neighbor distance in the glass), greater than the dimensions of the nominal building blocks of the glasses [8,9]. Recently, the nature and origin of extendedrange order, corresponding to a correlation length Lo that is greater than that of the intermediaterange order and characterized by a diffraction peak in S(Q) at lower wave vector than the FSDP, was probed in alkali germanate glasses using a combination of anomalous X-ray scamkg (AXS) and neutron diffraction (ND) [ 10,113. Spectroscopic tools such as EXAFS and NMR have proved successful for investigating the cation surroundings and network structure, respectively.…”
Section: *mentioning
confidence: 99%