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

基本信息

项目摘要

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.
变形实验表明,水工业应增强位错迁移率,以及在[100](010)(type-a),[100](001)(type-e)(type-e)和[001](100)(100)(type-c)(type-c)(type-c)(type-c)(type-c)中的水位依赖性依赖性应在此顺序上更高。位错迁移率的总体水含量指数应为1.2。为了检查这些结果,该应用在上述项目中进行了脱位恢复实验,并获得了以下结果。 (1)尽管至少有四种织物类型(A型,B,C和E),但只有两种位错。 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扩散。这些事实表明,这两个位错的运动是扩散控制的。 (3)A-和C-伸缩的an灭速率常数的水含量指数分别为0.2±0.4和-0.5±0.2。也就是说,它们的水含量依赖性分别为不确定性和负面。尽管获得了这些惊人的结果,但没有足够的点。(1)[100](010)滑移的不确定性不确定性的A-A-dislations的不确定性很大。很少。(3)尚不清楚在任何情况下是否真的不存在考虑类型织物的位错。(4)尚不清楚负责B型B和Type-C织物是否相同的C-脱位。由于这些原因,该项目将在此项目中进行以下实验。(1)通过更精确的技术来重新投资A范围的水含量依赖性的数据点。(2)将产生更多的数据点,以使c-DiSloctation的c-DiSlants的水位依赖性依赖于C-DISSERTIANT。 (001)平面在各种压力,温度,应变率和水含水条件下检查其脱位纹理。(4)将获得[001](100)[001](100)[001](010)对c-脱位的压力和温度依赖性。

项目成果

期刊论文数量(1)
专著数量(0)
科研奖励数量(0)
会议论文数量(0)
专利数量(0)
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:
  • 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
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Professor Dr. Tomoo Katsura其他文献

Professor Dr. Tomoo Katsura的其他文献

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{{ truncateString('Professor Dr. Tomoo Katsura', 18)}}的其他基金

Evaluation of the aspect ratio of ferropericlase under lower-mantle conditions
下地幔条件下方镁石长径比的评估
  • 批准号:
    449701262
  • 财政年份:
    2020
  • 资助金额:
    --
  • 项目类别:
    Research Grants
Determination of water partition coefficients between upper mantle minerals and melts as a function of pressure, temperature, and CO2 content using a rapid quench cell in multi-anvil experiments
在多砧实验中使用快速淬火室确定上地幔矿物和熔体之间的水分配系数作为压力、温度和 CO2 含量的函数
  • 批准号:
    402695659
  • 财政年份:
    2018
  • 资助金额:
    --
  • 项目类别:
    Research Grants
Determining the water dissociation constant from the relationship between water solubility in ringwoodite and oxygen fugacity
根据尖晶橄榄石的水溶性与氧逸度之间的关系确定水解离常数
  • 批准号:
    392411544
  • 财政年份:
    2018
  • 资助金额:
    --
  • 项目类别:
    Research Grants
Measurement of Si grain-boundary diffusion coefficients of forsterite as a function of water content: Estimation of the degree of creep enhancement with water within different regions of the upper mantle
镁橄榄石硅晶界扩散系数随含水量变化的测量:估计上地幔不同区域内水的蠕变增强程度
  • 批准号:
    247132310
  • 财政年份:
    2014
  • 资助金额:
    --
  • 项目类别:
    Research Grants
Determination of the three phase region of the post-spinel transition in (Mg,Fe)2SiO4: explanation of the extreme sharpness of the 660-km discontinuity and implication for chemical structure and dynamics of the deep mantle
(Mg,Fe)2SiO4 后尖晶石相变三相区的确定:解释 660 公里不连续性的极端锐度及其对深部地幔化学结构和动力学的影响
  • 批准号:
    257122795
  • 财政年份:
    2014
  • 资助金额:
    --
  • 项目类别:
    Research Grants
Measurement of Si self-diffusion coefficients of wadsleyite as a function of water content
硅锰矿硅自扩散系数随含水量变化的测量
  • 批准号:
    251472533
  • 财政年份:
    2014
  • 资助金额:
    --
  • 项目类别:
    Research Grants
Accurate determination of the melting relations of primitive peridotite under lower-mantle conditions up to 35 GPa using advanced multi-anvil techniques
利用先进的多砧技术准确测定高达 35 GPa 的下地幔条件下原始橄榄岩的熔化关系
  • 批准号:
    461495683
  • 财政年份:
  • 资助金额:
    --
  • 项目类别:
    Research Grants
H2O solubilities in Al-free and Al-bearing high-pressure silica polymorphs as a function of pressure and temperature: H2O storage in the lower mantle
无铝和含铝高压二氧化硅多晶型物中的水溶解度与压力和温度的函数关系:下地幔中的水储存
  • 批准号:
    518398967
  • 财政年份:
  • 资助金额:
    --
  • 项目类别:
    Research Grants

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短时间歇运动训练促进卒中后运动功能恢复及PLD2/PA/mTOR传导通路的实验研究
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