A detailed structural characterization of quartz on heating through the α-β phase transition

A detailed structural characterization of quartz on heating through the α-β phase transition
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DOI:
10.1180/002646101750377524
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发表时间:
2001-08-01
影响因子:
2.7
通讯作者:
Dove, MT
Dove, MT
中科院分区:
地球科学4区
文献类型:
--
作者:
Tucker, MG;Keen, DA;Dove, MT

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总中子散射测量。用改进的反蒙特卡罗模拟方法来解释长程晶序,用来描述石英结构随温度变化的行为。报告了两个关键的观察结果。第一。在长程和短程结构关联中都观察到了与位移α-β相变相关的对称性变化。其次,结构的一些方面。例如Si-O键长和热致动力学无序,后者位于相变的显著下方,对相变相对不敏感。这些结果被用来修正β相无序的x域模型和相变的经典软模图像过于简单化。相反,有人认为,结构行为最好的描述是它对低频、高振幅振动模式的响应能力。这一观点得到了额外的单晶弥散中子散射测量的支持。
Total neutron scattering measurements. analysed using a modification of the reverse Monte Carlo modelling method to account for long-range crystallographic order, have been used to describe the temperature-dependent behaviour of the structure of quartz. Two key observations are reported. First. the symmetry change associated with the displacive alpha-beta phase transition is observed in both the long-range and short-range structural correlations. Secondly, some aspects of the structure. such as the Si-O bond length and the thermally-induced dynamic disorder, the latter of which sets in significantly below the transition, are relatively insensitive to the phase transition. These results are used to shorn that the x-domain model of the beta -phase disorder is inappropriate and that the classical soft-mode picture of the phase transition is too simplistic. Instead, it is argued that the structural behaviour is best described in terms of its ability to respond to low-frequency, high-amplitude vibrational modes. This view is supported by additional single-crystal diffuse neutron scattering measurements.