Comment on “Evolution model of the earth's limited expanding” from comparative planetology

被引:0
作者
SHI YaolinGraduate School
机构
基金
中国国家自然科学基金;
关键词
from comparative planetology; Evolution model of the earth’s limited expanding;
D O I
暂无
中图分类号
P185 [行星、卫星、彗星、流星、陨星];
学科分类号
070401 ;
摘要
In the article "Evolution Model of the Earth’s Limited Expanding" published in Volume 45 Number (4) of Chinese Science Bulletin[1], the author suggests that the earth expands according to a law R(t) = R0+A(1 -exp(β(t-ts))) (remark: this formula was mistakenly printed as R(t) = R0 + Aexp(β(t-ts)) in the and formula (12) of the text of ref. [1]). According to ref. [1], the earth was formed 4.6 billion years ago. After 0.3 billion years from its birth (ts), it started expansion from an initial radius R0 of 4651 km, and may reach a final maximum radius of R0+A = 6511 km. In the 4.6 billion years history, the radius of the earch has increased by 1720 km, or the density decreased from 14200 km/m3 (2.57 times the present density) to 5520 kg/m3 within the latest 4.3 billion years.
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页码:1495 / 1496
页数:2
相关论文
共 3 条
[1]   The evolution model of the earth's limited expanding [J].
Chen, ZG .
CHINESE SCIENCE BULLETIN, 2000, 45 (04) :304-313
[2]   类地行星半径与转动惯量系数相关关系及其地球动力学意义 [J].
陈志耕 ;
万明华 .
ChineseJournalofAstronomyandAstrophysics, 1985, (04) :315-324
[3]  
Modelling plume-related uplift, gravity and melting on Venus[J] . Francis Nimmo,Dan McKenzie.Earth and Planetary Science Letters . 1996 (1)