康仁科

个人信息Personal Information

教授

博士生导师

硕士生导师

任职 : 国际磨粒技术学会(International Committee of Abrasive Technology, ICAT)委员,中国机械工程学会极端制造分会副主任、生产工程分会常务委员、微纳米制造技术分会常务委员,中国机械工程学会生产工程分会磨粒加工技术专业委员会副主任、切削加工专业委员会常委委员、精密工程与微纳技术专业委员会常委委员,中国机械工程学会特种加工分会超声加工技术委员会副主任,中国机械工程学会摩擦学分会微纳制造摩擦学专业委员会常务委员,中国机械工业金属切削刀具协会切削先进制造技术研究会常务理事、对外学术交流工作委员会副主任、切削先进制造技术研究会自动化加工技术与系统委员会副主任。

性别:男

毕业院校:西北工业大学

学位:博士

所在单位:机械工程学院

学科:机械制造及其自动化. 机械电子工程. 航空宇航制造工程

办公地点:机械工程学院7191

电子邮箱:kangrk@dlut.edu.cn

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Subsurface Damage in Scratch Testing of Potassium Dihydrogen Phosphate Crystal

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论文类型:期刊论文

发表时间:2009-02-01

发表刊物:CHINESE JOURNAL OF MECHANICAL ENGINEERING

收录刊物:CSCD、SCIE、EI、Scopus

卷号:22

期号:1

页面范围:15-20

ISSN号:1000-9345

关键字:potassium dihydrogen phosphate (KDP) crystal; scratch; subsurface damage

摘要:Potassium dihydrogen phosphate (KDP) is an important. electro-optic crystal, often used for frequency conversion and Pockels cells in large aperture laser systems. To investigate the influence of anisotropy to the depth of subsurface damage and the profiles of cracks in subsurface of KDP crystal, an experimental study was made to obtain the form of subsurface damage produced by scratches on KDP crystal in [100], [120] and [1101 crystal directions oil (001) crystal plane. The results indicated that there were great differences between depth and crack shape in different directions. For many slip planes in KDP, the plastic deformation and cracks generated under pressure in the subsurface were complex. Fluctuations of subsurface damage depth at transition point were attributed to the deformation of the surface which consumed more energy when the surface deformation changed from the mixed region of brittle and plastic to the complete brittle region along the scratch. Also, the process of subsurface damage from shallow to deep, from dislocation to big crack in KDP crystal with the increase of radial force and etch pit oil different crystal plane were obtained. Because crystallographic orientation and processing orientation was different, etching pits on (100) crystal plane were quadrilateral while on (110) plane and (120) plane were trapezoidal and triangular, respectively.