The bonding environment of chlorine in silicate melts
The bonding environment of chlorine in silicate melts
复制标题
硅酸盐熔体中氯的结合环境
DOI:
10.1016/j.chemgeo.2022.121269
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发表时间:
2023
期刊:
影响因子:
3.9
通讯作者:
Thomas R
中科院分区:
文献类型:
--
作者:
Thomas R
The local bonding environment of chlorine in silicate melts has a profound influence over the thermodynamic properties and structure of a melt, affecting the viscosity, rheology, and volatile degassing potential. To constrain the bonding environment of Cl in natural silicate melts, we have determined Cl K-edge X-ray absorption fine structure (XAFS) spectra for 44 experimentally produced silicate glasses in both the X-ray absorption near edge structure (XANES) and extended X-ray absorption fine structure (EXAFS) regions. In the pre-edge region, the presence of a pre-edge peak indicates covalent bonding of chlorine with silicon. Addition of divalent cations suppresses this pre-edge feature, and its centroid shifts to higher energy, indicating a change to increasingly more ionic bonding. In the XANES region the main absorption edge energy, E0, and the energy of maximum intensity, EMax, are also compositionally dependent. SiO2- rich glasses have relatively low values of E0and EMaxwhile the addition of 2+ions increases both to values close to those found in the end-member chlorides CaCl2,MgCl2,and FeCl2. In two Na-rich glasses, E0and EMaxare close to corresponding energies in NaCl. It appears, therefore that bonding in the glasses is closely related to that found in the simple chlorides. This may be due to clustering which generates Casingle bondCl, Mgsingle bondCl, Fesingle bondCl and Nasingle bondCl linkages either in the melts themselves or in the glasses due to rearrangements during quenching.The EXAFS parts of the glass spectra confirm the conclusions derived from the XANES region. These show that, as expected from the XANES region, addition of Ca and Fe2+leads to R-space peaks which are closely related to those found in anhydrous CaCl2and FeCl2respectively.In order to determine if the spectra depend on pressure, temperature or chlorine fugacity of synthesis, 9 experiments were conducted using a single starting composition (Fe-free haplobasalt, An50Di28Fo22) across a range of temperatures (1300–1400 °C), pressures (5–20 kbar), chlorine fugacities (f(Cl2)) (1.38E−03to 1.66E−06), and water contents (expected 0–8 wt% H2O). The results show that there is almost no change in the spectra across the XANES and EXAFS regions, indicating either that chlorine bonding is independent of the intensive parameters of the experiment or that all melts quench to glasses with the same local structure around the Cl atoms.
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DOI:
--
发表时间:
1997
期刊:
影响因子:
--
作者:
A. Rompel;J. Andrews;R. M. Cinco;M. Wemple;G. Christou;N. A. Law;V. Pecoraro;K. Sauer;V. Yachandra;M. Klein
通讯作者:
M. Klein
DOI:
10.2138/am-2022-8450
发表时间:
2023
期刊:
Journal of Earth and Planetary Materials
影响因子:
--
作者:
Thomas R
通讯作者:
Thomas R
影响因子:
3.9
作者:
A. Baasner;B. Schmidt;S. Webb
通讯作者:
A. Baasner;B. Schmidt;S. Webb
影响因子:
3.1
作者:
J. Stebbins;L. Du
通讯作者:
L. Du
DOI:
--
发表时间:
1996
期刊:
影响因子:
--
作者:
A. Chmel;V. Svetlov
通讯作者:
V. Svetlov