王德真

个人信息Personal Information

教授

博士生导师

硕士生导师

任职 : 《Plasma Science and Technology》学术期刊编委

性别:男

毕业院校:大连工学院

学位:硕士

所在单位:物理学院

学科:等离子体物理

办公地点:主楼东侧楼(物理系楼)304室

联系方式:0411-84707981

电子邮箱:wangdez@dlut.edu.cn

扫描关注

论文成果

当前位置: 中文主页 >> 科学研究 >> 论文成果

Dynamic Monte-Carlo modeling of thermal desorption of H-2 from H+ irradiated graphite

点击次数:

论文类型:期刊论文

发表时间:2011-02-15

发表刊物:NUCLEAR INSTRUMENTS & METHODS IN PHYSICS RESEARCH SECTION B-BEAM INTERACTIONS WITH MATERIALS AND ATOMS

收录刊物:SCIE、EI

卷号:269

期号:4

页面范围:431-436

ISSN号:0168-583X

关键字:Thermal desorption; Fluence; Trap site; Porosity; Crystallite volume

摘要:Thermal desorption of hydrogen molecules from H+ irradiated graphite is studied using dynamic Monte Carlo simulation. The purpose of this study is to understand the experimentally observed phenomena that the thermal desorption of H-2 from the graphite exhibits sometimes single desorption peak, sometimes double peaks, and even three desorption peaks under certain circumstances. The study result reveals that the fluence of pre-implanted H+, the concentration of trap sites, porosity, and mean crystallite volume are important parameters in determining the number of desorption peaks. It is found that low implantation fluence and high concentration of trap sites easily lead to the occurrence of single desorption peak at around 1000 K, and high implantation fluence and low concentration of trap sites favor the occurrence of double desorption peaks, with a new desorption peak at around 820 K. It is also found that small porosity of graphite and large crystallite volume benefit the occurrence of single desorption peak at around 1000 K while large porosity of graphite and small crystallite volume facilitate the occurrence of double desorption peaks, respectively, at around 820 and 1000 K. In addition, experimentally observed third desorption peak at lower temperature is reproduced by simulation with assuming the graphite containing a small concentration of solute hydrogen atoms. (C) 2010 Elsevier B.V. All rights reserved.