Transport mechanism of eroded sediment particles under freeze-thaw and runoff conditions-Reference-Cited by-同舟云学术

Transport mechanism of eroded sediment particles under freeze-thaw and runoff conditions

Published:2022-05 Issue:5 Volume:14 Page:490-501
ISSN:1674-6767
Container-title:Journal of Arid Land
language:en
Short-container-title:J. Arid Land

Author:

Wang Tian,Li Peng,Hou Jingming,Tong Yu,Li Jing,Wang Feng,Li Zhanbin

Publisher

Springer Science and Business Media LLC

Subject

Management, Monitoring, Policy and Law,Earth-Surface Processes,Water Science and Technology

Link

https://link.springer.com/content/pdf/10.1007/s40333-022-0016-x.pdf

Reference41 articles.

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3. Blott S J, Pye K. 2001. GRADISTAT: a grain size distribution and statistics package for the analysis of unconsolidated sediments. Earth Surface Processes and Landforms, 26(11): 495–503.

4. Blott S J, Pyem K. 2006. Particle size distribution analysis of sand-sized particles by laser diffraction: an experimental investigation of instrument sensitivity and the effects of particle shape. Sedimentology, 53(3): 495–503.

5. Chaplot V, Le Bissonnais Y. 2003. Runoff features for interrill erosion at different rainfall intensities, slope lengths, and gradients in an agricultural loessial hillslope. Soil Science Society of America Journal, 67(3): 495–503.

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