耕作的数值模型

耕作的数值模型

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contributed at 2018-12-04

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Affiliation:  
岳天祥编著
Email:  
yue@lreis.ac.cn
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Application-focused categoriesNatural-perspectiveLand regions

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耕作的数值模型

土壤水热运动方程――Philip方程:

式中,为比水容量;Ψ为土壤水的基质势;t为时间;为与温度梯度有关的水汽扩散率;T为土壤温度;K为非饱和土壤导水率;z为向上为正的高度坐标;为土壤热容量;λ为导热率;为液态水密度;L为水的汽化潜热;为水汽在基质势梯度下的当量导水率。

参考文献

杨邦杰:耕作的数值模型及其应用。生态学报,199616(6)

How to Cite

《资源环境数学模型手册》 (2018). 耕作的数值模型, Model Item, OpenGMS, https://geomodeling.njnu.edu.cn/modelItem/af841e19-9ffd-4321-9abe-001af1f6050b
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Last modifier : 
zhengzhong
Last modify time : 
2020-10-27
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Contributor

contributed at 2018-12-04

Authorship

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

History

Last modifier : 
zhengzhong
Last modify time : 
2020-10-27
Modify times : 
View History

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