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Incommensurately modulated crystal structure of flamite - natural analogue of αH′-Ca2SiO4
被引:5
作者:
Rashchenko, Sergey, V
[1
,2
]
Seryotkin, Yurii, V
[1
,2
]
Sokol, Ella, V
[1
]
Kokh, Svetlana N.
[1
]
机构:
[1] Soboley Inst Geol & Mineral SB RAS, 3 Koptyuga Ave, Novosibirsk 630090, Russia
[2] Noyosibirsk State Univ, 1 Pirogova St, Novosibirsk 630090, Russia
来源:
基金:
俄罗斯科学基金会;
关键词:
flamite;
calcium orthosilicate;
aperiodic structure;
incommensurate modulation;
combustion metamorphism;
SOLID-SOLUTION;
DICALCIUM;
TEMPERATURE;
ROCKS;
PHASE;
NA;
D O I:
10.1107/S2052520619013623
中图分类号:
O6 [化学];
学科分类号:
0703 ;
摘要:
Crystal structures of unquenchable high-temperature polymorphs of Ca2SiO4, important in cement chemistry, have eluded single-crystal X-ray analysis. However, the problem may be addressed by studying chemically stabilized Ca2SiO4 polymorphs at ambient temperature. Here an incommensurately modulated crystal structure of flamite [Pnma(0 beta 0)00s, q = 0.2728 (2)b*, a = 6.8588 (2) angstrom, b = 5.4301 (2) angstrom, c = 9.4052 (3) angstrom] is described. It is a mineral analogue of orthorhombic alpha(H)'-Ca2SiO4 (stable between 1160 and 1425 degrees C), naturally stabilized by substitution with phosphorus. The incommensurate modulation results from wave-like displacement of cation sites accompanied by tilting of (Si,P)O-4 tetrahedra and variation of the Na/(Ca + Na + K) ratio along the modulation period. The studied sample from Hatrurim Basin (Negev Desert, Israel) with composition (Ca1.75K0.12Na0.12)(1.99)(Si0.74P0.26)(1.00)O-4 also demonstrates pseudomerohedral cyclic twinning around the a axis, which results from pseudohexagonal topology of the crystal structure and complicates the indexing of X-ray diffraction data.
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页码:1137 / 1143
页数:7
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