岩石的热模型

岩石的热模型

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Contributor(s)

Initial contribute: 2018-12-04

Authorship

Affiliation:  
岳天祥编著
Email:  
yue@lreis.ac.cn
Homepage:  
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Classification(s)

Method-focused categoriesData-perspectiveRemote sensing analysis
Method-focused categoriesProcess-perspectivePhysical process calculation

Model Description

Chinese {{currentDetailLanguage}} Chinese

岩石的热模型

(1)    克兰克-尼克森公式:

式中,i代表位置;j代表时间;r为比例因子;u为岩石表面绝对温度;p为岩石密度;C为比热容;k为热传导率;x为岩石内距表面深度;t为时间。

(2)    上边界模型:

 

式中,P为热惯量;Q为地表径向地热热流通量;为太阳常数;L为云层影响因子;A为地面反照率;为辐射系数;为斯蒂芬-波尔兹曼常数;为等效空气温度;m(z)为大气透过率,是天顶角z的函数;z为由于地面坡度形成的区域天顶角;分别为太阳升起和落下的时间。

(3)    下边界模型:

式中,随岩石的不同而略有差异。

参考文献

    崔承禹,肖青,支毅乔等:岩石的热模型分析。遥感学报,199821

How to Cite

《资源环境数学模型手册》 (2018). 岩石的热模型, Model Item, OpenGMS, https://geomodeling.njnu.edu.cn/modelItem/6e0f390a-e594-4dde-9603-0d2b4b3c037a
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Last modifier : 
zhangshuo
Last modify time : 
2020-12-29
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Contributor

Initial contribute: 2018-12-04

Co-contributor(s)

Authorship

Affiliation:  
岳天祥编著
Email:  
yue@lreis.ac.cn
Homepage:  
View
Is authorship not correct? Feedback

History

Last modifier : 
zhangshuo
Last modify time : 
2020-12-29
Modify times : 
View History

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