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

温度的本质和地温分布规律
引用本文:李子丰,王鹏,李雪娇,李润启.温度的本质和地温分布规律[J].中国西部科技,2010,9(14):1-2.
作者姓名:李子丰  王鹏  李雪娇  李润启
作者单位:燕山大学石油工程研究所,河北,秦皇岛,066004
摘    要:传统观点认为温度是分子的热运动的剧烈程度。这一理论不能给予恒定的地温梯度以合理的解释。提出物质的温度由分子热运动和微粒子热运动共同组成。地球内微粒子的密度分布与重力场的分布密切相关,地球内的温度分布是重力场的函数。地球内部的微粒子密度比地表微粒子密度大,地球内部的温度比地表温度高。既完善了分子热运动说,又找到了地温梯度保持恒定的原因。

关 键 词:温度  测量  地温梯度  分子热运动

The Nature of Temperature and Geothermal Distribution
LI Zi-feng,WANG Peng,LI Xue-jiao,LI Run-qi.The Nature of Temperature and Geothermal Distribution[J].Science and Technology of West China,2010,9(14):1-2.
Authors:LI Zi-feng  WANG Peng  LI Xue-jiao  LI Run-qi
Institution:(Petroleum Engineering Institute of Yanshan University, Oinhuangdao,Hebei 066004)
Abstract:The traditional view is that temperature is the intensity of thermal motion of a great number of molecules.However,it can not interpret the existence of geothermal gradient and keeping a constant.This paper advances that temperature is sum of the intensity of thermal motion of a great number of molecules and microparticles.The density of microparticles in the earth is related with gravitational field,the temperature distribution in the earth is function of gravitational field.The density of microparticles in the earth is larger than that on the surface;the temperature in the earth is higher than that on the surface.This paper not only improves the thermal vibration theory,but also interprets the existence of geothermal gradient and keeping a constant.
Keywords:Temperature  Measure  Geothermal gradient  Thermal motion of molecules
本文献已被 CNKI 维普 万方数据 等数据库收录!
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