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

Author:

Ban Yunyun1,Lei Tingwu12ORCID,Chen Chao1,Yin Zhe3,Qian Dengfeng4

Affiliation:

1. College of Water Resources and Civil Engineering; China Agricultural University; Beijing P. R. China

2. State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau; Institute of Soil and Water Conservation, Chinese Academy of Sciences and Ministry of Water Resources; Yangling Shanxi Province P. R. China

3. China Institute of Water Resources and Hydropower Research; Beijing P. R. China

4. College of Resource and Environment; Xizang Agriculture and Animal Husbandry College; Linzhi Tibet Autonomous Region P. R. China

Funder

National Natural Science Foundation of China

Publisher

Wiley

Subject

Earth and Planetary Sciences (miscellaneous),Earth-Surface Processes,Geography, Planning and Development

Reference45 articles.

1. Comparison of rill flow velocity over frozen and thawed slopes with electrolyte tracer method;Ban;Journal of Hydrology,2016a

2. Study on the facilities and procedures for meltwater erosion of thawed soil;Ban;International Soil and Water Conservation Research,2016b

3. Comparative study of erosion processes of thawed and non-frozen soil by concentrated meltwater flow;Ban;Catena,2016c

4. US Army Cold Regions Research Engineering Laboratory Special Report 90-91;Benoit,1990

5. Soil erodibility and processes of water erosion on hillslope;Bryan;Geomorphology,2000

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