Impacts of frozen layer and rock fragment on sediment transport capacity on frozen‐stony slopes-Reference-Cited by-同舟云学术

Impacts of frozen layer and rock fragment on sediment transport capacity on frozen‐stony slopes

Published:2022-06 Issue:6 Volume:36 Page:
ISSN:0885-6087
Container-title:Hydrological Processes
language:en
Short-container-title:Hydrological Processes

Author:

Ban Yunyun¹²^ORCID,Lei Tingwu²^ORCID

Affiliation:

1. Key Laboratory of Water Cycle and Related Land Surface Processes, Institute of Geographic Sciences and Natural Resources Research Chinese Academy of Sciences Beijing People's Republic of China

2. College of Water Resources and Civil Engineering China Agricultural University Beijing People's Republic of China

Funder

National Natural Science Foundation of China

Publisher

Wiley

Subject

Water Science and Technology

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1002/hyp.14627

Reference39 articles.

1. Soil Erosion Control and Moisture Conservation of Arid Lands with Stone Cover

2. Stone cover and rain intensity - Effects on infiltration, erosion and water splash

3. Effect of stone content on water flow velocity over Loess slope: non-frozen soil

4. Meltwater erosion process of frozen soil as affected by thawed depth under concentrated flow in high altitude and cold regions

5. Birhan H.(2000).Soil and runoff losses by snowmelt on hillslopes. In 2nd National snow congress Publication No. 73 (pp. 41–50). February 21–25. Erzurum Turkey: Directorate of Rural Works Research Institute (in Turkish).

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