Abstract
The sample of cubic lazurite, collected in the Baikal region, with incommensurately 3D modulated (ITM) structure has been studied by the method of high-temperature X-ray powder diffraction. At short time of annealing in high-temperature diffraction experiment the modulation recovery proceeds during cooling down the sample to room temperature. The identity of the period of both initial and recovered modulation demonstrates that the system has a structural memory. The acquired results are interpreted through comparison of thermal behavior of lazurite, sodalite and quartz structures. It is supposed that two kinetically different and thermally activated processes proceed under heating: 1) reversible framework expansion due to Si-O-Al angle increase, and 2) equalizing of periodic local distortions via the diffusion-controlled transfer of cage ions between adjacent subcells. The second process seems to be much slower than the first one, especially at lower temperatures. With increasing temperature, both processes are activated. However, the framework expands more rapidly than the cage clusters migrate, and the periodic distortions of the framework are aligned. Under lower temperatures, the framework shrinks and again accommodates to the configuration of cage cations (clusters), which may be changed at high temperature and sufficient time or may not at lower temperature, short time, unfavorable SO2 fugacity values. In the first case the modulation disappears entirely, while in the second case it arises again. The probable reason for ITM formation is the balance of counteracting energetic terms: the elastic strain energy of structure deformation and the energy of cluster ordering providing the state of forced equilibrium. The excess free energy due to structure distortion is compensated by the increment associated with the cluster ordering process. However, no significant variations in sulphur anion speciation for different degrees of modulation retention were observed by XPS S 2p. This may be due to the ordering of Na- and Ca-containing clusters rather than the clusters with different sulphur species. ITM reversion is considered as an example of reversible forced equilibrium with completely reproducible forcing factor.
Highlights
Lazurite is a sulfur-containing aluminosilicate mineral with formula Na6Ca2[Al6Si6O24](SO4,S,Cl
The samples with incommensurable three-dimentional modulation (ITM) structure were extracted from the lazurite-bearing metasomatites at the lazurite deposit Pokhabikha of the Slyudyanka metamorphic sequence (Southern Baikal region in East Siberia)
Previous data obtained for ITM-lazurite samples, heated at different temperature, time, sulfur dioxide fugacity and quenched [4] [6]-[9] are used in this study
Summary
Lazurite is a sulfur-containing aluminosilicate mineral with formula Na6Ca2[Al6Si6O24](SO4,S,Cl). Lazurite is a sulfur-containing aluminosilicate mineral with formula Na6Ca2[Al6Si6O24](SO4,S,Cl)2 It is a member of the group of sodalite minerals and characterizes by an Al, Si-ordered tetrahedral framework of corner-linked SiO4 and AlO4 tetrahedra. The framework contains large cubo-octahedral (sodalite-type) cages, each bounded by six four-fold and eight six-fold rings of tetrahedra. The cages are packed according to the bodycenter law, so that every six-fold ring is shared by the two cages, so forming a set of channels running through the corners and center of the unit cell. The framework is permeated by intersecting channels with the diameters not larger than six-rings. The crossing channels may serve as paths for migrating cage ions. The diffraction pattern of isotropic cubic lazurite usually includes two types of reflections: basic reflections and satellites (Figure 1)
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