摘要
文章在分析地球表层动态特征的基础上 ,依据熵原理提出耗散运动的概念 ,并揭示地球表层耗散运动的形成机制 ;分析地球表层耗散运动形成的内、外环境及无穷自由度背景 。
By analyzing the dynamic features of the earth surface, this paper puts forward the concept of dissipation movement according to the principle of entropy flow. Then it explains the formation mechanism, the internal and external circumstances and the background of infinite degree of freedom of the dissipation movement on the earth surface. Finally it concludes that the dissipation movement on the earth surface is the origin of evolution.
出处
《哈尔滨工业大学学报(社会科学版)》
2000年第1期34-36,共3页
Journal of Harbin Institute of Technology(Social Sciences Edition)
关键词
地球表层
耗散运动
熵流
earth surface, dissipation movement, entropy flow