金刚石单晶解理断裂的研究  

Study on fracture of diamond single crystal

作　　者：宿庆财[1] 孙广增[2] 宿超 亓永新[1] 徐振军[4] 李木森[1] 

机构地区：[1]山东大学材料科学与工程学院 [2]山东大学自然科学学报编辑部,济南250061 [3]山东省广播电视大学,济南250014 [4]济南一机床集团有限公司,济南250022

出　　处：《金刚石与磨料磨具工程》2008年第4期12-17,共6页Diamond & Abrasives Engineering

基　　金：国家自然科学基金资助(No．50772060);山东省自然科学基金资助(No．Y2007F12);山东省博士后创新项目基金资助(No．200702024)

摘　　要：本文通过实验观察和理论计算研究了金刚石单晶解理断裂现象。金刚石单晶晶面上实际的价电子密度并非简单的正比于原子密度。(110)晶面上原子分布不均匀。(110)晶面BQKJB区域内原子分布较少,原子密度低于其它晶面。(111)晶面的价电子键络分布均匀,且实际发生作用的价电子密度最大。计算和分析结果表明,金刚石单晶(111)晶面的有效价电子密度为46.212 nm^(-2),明显高于(110)晶面的38.542 nm^(-2),成为有效原子密排面。当金刚石受到外力作用时,(111)面间较弱的键相对更容易断裂,因而导致沿(111)面产生解理。这与实验观察结果相吻合。The fracture of diamond single crystal was studied through experimental observation .and calculation. It was observed that the actual valence electron density of crystal plane was not simply in direct proportion to that of atom. The distribution of atoms in the （110） plane was not uniform. There were a little atoms in BQKJB region of （110） plane, and its atom density was less than others. The valence electron bond of （ 111 ） plane was distributed uniformly, and the valence electron density acting to （ 111 ） plane was the biggest. The result of calculation and analysis indicated that the available valence electron density of （ 111 ） plane, 46.212 nm^-2, was higher than that of （110） plane which is 38. 542 nm^-2. And the （111） plane became the available atom close arrangement plane. Therefore, the cleavage of diamond maybe start from （ 111 ） plane. The conclusion is in good agreement with the result of experimental observation.

关 键 词：金刚石 解理面 有效价电子密度 固体与分子经验电子理论 

分 类 号：TQ164[化学工程—高温制品工业]