Modelling soil detachment by overland flow for the soil in the Tibet Plateau of China

The overland flow erosion is common and became more serious because of the climate warming inducing more runoff in the Tibet Plateau. The purposes of this study were to evaluate the effects of flow rate, slope gradient, shear stress, stream power, unit stream power and unit energy of water-carrying...

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Detalles Bibliográficos
Autores principales: Li, Mingyi, Hai, Xiao, Hong, Huan, Shao, Yanyan, Peng, Doudou, Xu, Wennian, Yang, Yueshu, Zheng, Yan, Xia, Zhenyao
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2019
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6542811/
https://www.ncbi.nlm.nih.gov/pubmed/31147592
http://dx.doi.org/10.1038/s41598-019-44586-5

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6542811/
https://www.ncbi.nlm.nih.gov/pubmed/31147592
http://dx.doi.org/10.1038/s41598-019-44586-5

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