Brittle-to-ductile transition and slip band structure in ionic crystals

N. Narita, Y. Takahara, K. Higashida
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引用次数: 3

Abstract

Abstract The interrelation between the brittle-to-ductile transition (BDT) and slip structure has been examined using NaCl and KCl crystals. In pre-cracked crystals of NaCl and KCl having a ⟨100⟩ axis, the fracture toughness K*ic increases above 300 and 220 K, and the BDT occurs at 510 and 430 K respectively. Scale-like wavy lines are revealed ahead of a pre-crack on etched fracture faces of NaCl tested above 300 K. As the temperature increases, the step height and density of the lines are increased but the lines are more restricted near the pre-crack front. In NaCl and KCl crystals without pre-cracking, the critical resolved shear stress for {110} main slip is very low above 77 K, while that for {010} slip markedly increases as temperature decreases below 500 and 300 K respectively. In ⟨100⟩-uniaxial tests for non-pre-cracked NaCl crystals, the BDT takes place at around 380 and 480 K at strain rates of 5.5 × 10−6 and 5.5 × 10−5s−1 respectively. Above the BDT temperature, wavy slip lines are abundantly produced by the marked operation of cross-slip. A mechanism based on the crack tip shielding through the cross-slip of dislocations along a crack front is proposed to explain observed crack face morphology as well as the BDT in ionic crystals of NaCl structure.
离子晶体的脆性-延性转变和滑移带结构
摘要采用NaCl和KCl晶体研究了脆性到韧性转变(BDT)与滑移结构之间的相互关系。在⟨100⟩轴的NaCl和KCl的预裂晶体中,断裂韧性K*ic在300和220 K以上增加,BDT分别发生在510和430 K。在300 K以上NaCl腐蚀断口上,在预裂纹前面出现了鳞状波纹线。随着温度的升高,裂纹线的台阶高度和密度增加,但裂纹线在裂纹前附近受到更多的限制。在没有预裂的NaCl和KCl晶体中,{110}主滑移的临界分解剪应力在77 K以上非常低,而{010}滑移的临界分解剪应力在500和300 K以下分别随着温度的降低而显著增加。在非预裂NaCl晶体的⟨100⟩单轴测试中,BDT分别在约380和480 K下以5.5 × 10−6和5.5 × 10−5s−1的应变速率发生。在BDT温度以上,由于交叉滑动的显著作用,波状滑动线大量产生。提出了一种基于裂纹尖端通过位错沿裂纹前沿的交叉滑移屏蔽的机制来解释观察到的裂纹表面形貌以及NaCl结构离子晶体中的BDT。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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