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Microstructural evolution during thermal annealing of ice-I-h

机译:冰-I-h热退火过程中的微观组织演变

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摘要

We studied the evolution of the microstructure of ice-I-h during static recrystallization by stepwise annealing experiments. We alternated thermal annealing and electron backscatter diffraction (EBSD) analyses on polycrystalline columnar ice pre-deformed in uniaxial compression at temperature of -7 degrees C to macroscopic strains of 3.0-5.2. Annealing experiments were carried out at -5 degrees C and -2 degrees C up to a maximum of 3.25 days, typically in 5-6 steps. EBSD crystal orientation maps obtained after each annealing step permit the description of microstructural changes. Decrease in average intragranular misorientation at the sample scale and modification of the misorientation across subgrain boundaries provide evidence for recovery from the earliest stages of annealing. This initial evolution is similar for all studied samples irrespective of their initial strain or annealing temperature. After an incubation period >= 1.5 h, recovery is accompanied by recrystallization (nucleation and grain boundary migration). Grain growth proceeds at the expense of domains with high intragranular misorientations, consuming first the most misorientated parts of primary grains. Grain growth kinetics fits the parabolic growth law with grain growth exponents in the range of 2.4-4.0. Deformation-induced tilt boundaries and kink bands may slow down grain boundary migration. They are stable features during early stages of static recrystallization, only erased by normal growth, which starts after > 24 h of annealing. (C) 2017 Elsevier Ltd. All rights reserved.
机译:我们通过逐步退火实验研究了静态再结晶过程中I-h冰的微观结构的演变。我们对在-7摄氏度温度下单轴压缩中预变形为3.0-5.2宏观应变的多晶柱状冰进行了热退火和电子背散射衍射(EBSD)分析。退火实验在-5摄氏度和-2摄氏度下进行,最多3.25天,通常以5-6个步骤进行。在每个退火步骤之后获得的EBSD晶体取向图可以描述微观结构的变化。样品尺度上平均晶粒内取向的减少和亚晶粒边界上取向的改变为从退火的最早阶段恢复提供了证据。不论其初始应变或退火温度如何,所有研究样品的初始演化均相似。孵育期> = 1.5小时后,恢复伴随着重结晶(成核和晶界迁移)。晶粒的生长以晶粒内取向错误程度高的区域为代价,首先消耗了原始晶粒取向最差的部分。晶粒生长动力学符合抛物线生长规律,晶粒生长指数在2.4-4.0范围内。变形引起的倾斜边界和扭结带可能会减慢晶粒边界的迁移。它们在静态再结晶的早期阶段是稳定的特征,只有通过正常的生长才能消除,而正常的生长在退火> 24小时后才开始。 (C)2017 Elsevier Ltd.保留所有权利。

著录项

  • 来源
    《Journal of structural geology》 |2017年第6期|31-44|共14页
  • 作者单位

    CNRS, Geosci Montpellier, Pl E Bataillon, F-34095 Montpellier 5, France|Univ Montpellier, Pl E Bataillon, F-34095 Montpellier 5, France|CSIC, Inst Andaluz Ciencias Tierra, Ave Palmeras 4, Granada 18100, Spain|Univ Granada, Ave Palmeras 4, Granada 18100, Spain;

    CNRS, Geosci Montpellier, Pl E Bataillon, F-34095 Montpellier 5, France|Univ Montpellier, Pl E Bataillon, F-34095 Montpellier 5, France;

    CNRS, Geosci Montpellier, Pl E Bataillon, F-34095 Montpellier 5, France|Univ Montpellier, Pl E Bataillon, F-34095 Montpellier 5, France;

    Univ Grenoble Alpes, CNRS, Inst Geosci Environm, 54 Rue Moliere,BP96, F-38402 St Martin Dheres, France;

    CNRS, Geosci Montpellier, Pl E Bataillon, F-34095 Montpellier 5, France|Univ Montpellier, Pl E Bataillon, F-34095 Montpellier 5, France;

    Univ Grenoble Alpes, CNRS, Inst Geosci Environm, 54 Rue Moliere,BP96, F-38402 St Martin Dheres, France;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Annealing; Hexagonal ice; EBSD; Static recrystallization; Grain boundary migration; Grain growth;

    机译:退火;六角冰;EBSD;静态重结晶;晶粒边界迁移;晶粒长大;

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