首页 | 本学科首页   官方微博 | 高级检索  
     检索      

瑞利数对热对流的影响——在地幔柱中的应用
引用本文:王青平,白武明,王洪亮.瑞利数对热对流的影响——在地幔柱中的应用[J].地球物理学报,2011,54(6):1566-1574.
作者姓名:王青平  白武明  王洪亮
作者单位:1. 中国科学院地质与地球物理研究所,北京 100029; 2. 中国科学院研究生院,北京 100049
摘    要:本文分别在直角坐标系和柱坐标系下,研究瑞利数从104逐渐增大到107对热对流的影响,数值计算结果表明:瑞利数越大,地幔柱越窄,地幔柱上升速度也越快;源自上地幔的地幔柱半径的范围为9到210 km.根据峨眉山内带的半径推算出地幔的黏性系数约为3.8×1021Pa·s,地幔柱平均流动速度为2.5 cm/a.

关 键 词:瑞利数  热对流  热边界层  地幔柱半径  峨眉山
收稿时间:2010-12-10

The influence of Rayleigh number on thermal convection -application to mantle plume
WANG Qing-Ping,BAI Wu-Ming,WANG Hong-Liang.The influence of Rayleigh number on thermal convection -application to mantle plume[J].Chinese Journal of Geophysics,2011,54(6):1566-1574.
Authors:WANG Qing-Ping  BAI Wu-Ming  WANG Hong-Liang
Institution:1. Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China; 2. Graduate University, Chinese Academy of Sciences, Beijing 100049, China
Abstract:In this paper, we simulate increasing Rayleigh number from 104 to 107 to observe its influence on thermal convection in Cartesian and cylindrical coordinate respectively. The numerical examples prove that the range of radius of mantle plume is from 90 to 210 kilometer and the larger the Rayleigh number, the narrower and faster the mantle plume. Our results suggest that the viscosity of mantle is about 3.8×1021Pa·s and the speed of mantle plume is about 2.5 cm/a, according to the radius of Inner Zone of Emeishan mantle plume.
Keywords:Rayleigh number  Thermal convection  Thermal boundary layer  Radius of mantle plume  Emeishan
本文献已被 万方数据 等数据库收录!
点击此处可从《地球物理学报》浏览原始摘要信息
点击此处可从《地球物理学报》下载免费的PDF全文
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号