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Dislocation recovery experiment of hydrous olivine as a function of water content and crystallographic orientation

Dislocation recovery experiment of hydrous olivine as a function of water content and crystallographic orientation
水合橄榄石的位错恢复实验作为含水量和晶体取向的函数
批准号:
229061489
负责人:
Professor Dr. Tomoo Katsura
金额:
$0.0万
依托单位国家:
德国
项目类别:
Research Grants
财政年份:
2012
资助国家:
德国
项目状态:
已结题
起止时间:
2011-12-31 至 2022-12-31

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中文摘要
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英文摘要
Deformation experiments suggested that dislocation mobility should be enhanced by water incorporation, and the water-content dependence of dislocation mobility in the [100](010) (Type-A), [100](001) (Type-E) and [001](100) (Type-C)slips should be higher in this order. The overall water-content exponent of dislocation mobility should be 1.2. In order to examine these results, the applicant conducted dislocation recovery experiment in the preceding project and obtained the following results. (1) In spite of at least four reported fabric types (Type A, B, C and E), there are only two kinds of dislocations. Dislocations for Type A and E fabrics are edge dislocations with a [100] Burgers vector (a-dislocations), whereas those for Type B and C fabrics are screw dislocations with a [001] Burgers vector (c-dislocations).(2) The activation energies and volumes of annihilation-rate constants of a- and c-dislocations are identical, and are also comparable with those of the Si diffusions. These facts suggest that motions of these two dislocations are diffusion-controlled. (3) The water-content exponents of annihilation-rate constants of a- and c-dislocations are 0.2±0.4 and -0.5±0.2, respectively. Namely, their water content dependences are zero with in uncertainty and negative, respectively.Although these striking results were thus obtained, there are insufficient Points.(1) Uncertainties of the annihilation-rate constants of a-dislocations by the [100](010) slip are very large.(2) Data points of the annihilation-rate constants of c-dislocations by the [001](010) slip are too few.(3) It is not clear whether dislocations accounting for Type-E fabric are really absent under any condition.(4) It is not clear whether c-dislocations responsible for Type-B and Type-C fabrics are identical or not. For these reasons, the following experiments will be conducted in this project.(1) Data points of water-content dependence of annihilation-rate constants of a-dislocations will be reinvestigated by means of more precise techniques.(2) More data points will be produced for water-content dependence of annihilation-rate constants of c-dislocations.(3) Olivine single crystals will be sheared in the [100] direction on the (001) plane under various pressure, temperature, strain-rate and water-content conditions to examine their dislocation textures.(4) Pressure and temperature dependence of c-dislocations by the [001](100) slip and water-content dependence of those by the [001](010) slip will be obtained.
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Temperature dependence of [100](010) and [001](010) dislocation mobility in natural olivine
天然橄榄石中[100](010)和[001](010)位错迁移率的温度依赖性
DOI: 10.1016/j.epsl.2016.02.029
发表时间: 2016
期刊: Earth and Planetary Science Letters
影响因子: 5.3
作者: [S. Blaha, Z. Pintér, R. Farla, T. Kawazoe, N. Miyajima, K. Michibayashi, T. Katsura]
通讯作者: T. Katsura
Evaluation of the aspect ratio of ferropericlase under lower-mantle conditions
Determining the water dissociation constant from the relationship between water solubility in ringwoodite and oxygen fugacity
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