Piezoerescence—the growth of Dauphiné twinning in quartz under stress
Piezoerescence—the growth of Dauphiné twinning in quartz under stress
复制标题
压电现象——应力作用下石英中多芬孪晶的生长
DOI:
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发表时间:
1951
期刊:
影响因子:
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通讯作者:
W. Wooster
中科院分区:
文献类型:
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作者:
L. A. Thomas;W. Wooster
It has been found that Dauphiné twinning can be created, modified or, in some instances, eliminated, by the subjection of α-quartz specimens to stress produced by mechanical or thermal means. The experimental observations can be explained in terms of a reversible phenomenon, the growth of one crystallographic orientation out of another under the influence of stress, for which the term piezocrescence is proposed. Plates and bars of quartz have been held at about 400° C while they were twisted or bent by external means or while they were kept in a state of strain by means of a lengthwise temperature gradient. In general, the resulting twin boundaries, as shown by acid etching, approximate to an ‘ideal’ twin pattern which is characteristic of the crystallographic orientation of the specimen and the type of stress applied. A theory of piezocrescence is proposed which depends on the principle that, at any part of a quartz specimen undergoing treatment, the crystallographic orientation developed is that which stores the maximum elastic energy. This leads to the formulation of a twin elastic function which is proportional to the difference between the elastic energies at constant stress of the two parts of the twin. Thus, if under a given system of stresses the elastic energy per unit volume in the twinned orientation is greater than in the parent orientation, then the twinned orientation is taken up by the crystal; otherwise the parent orientation remains unchanged. A knowledge of the principal stresses in a given specimen and the appropriate twin elastic function enable the ‘ideal’ twin pattern at each part of the crystal to be predicted. In the majority of the experiments there is agreement between the predicted and experimentally observed twin patterns, and the essential features of the maximum elastic energy theory would seem to be justified. The detailed testing of the theory has been handicapped by the difficulty of evaluating the principal stresses at any point within the crystal from the externally applied stress for an anisotropic body such as quartz, and also by the absence of any quantitative measure of piezocrescence other than the occurrence or absence of a twinned region. A further difficulty arises from the presence in some of the specimens of structural anomalies which hinder piezocrescence, and in this respect the study of the phenomenon is partly a study of crystal perfection.