Influence of thawed soil depth on rainfall erosion of frozen bare meadow soil in the Qinghai

Influence of thawed soil depth on rainfall erosion of frozen bare meadow soil in the Qinghai–Tibet Plateau

Published:2021-05-24 Issue:10 Volume:46 Page:1953-1963
ISSN:0197-9337
Container-title:Earth Surface Processes and Landforms
language:en
Short-container-title:Earth Surf. Process. Landforms

Author:

Gao Xiaofeng¹^ORCID,Shi Xiaonan¹²^ORCID,Lei Tingwu¹³^ORCID

Affiliation:

1. College of Water Resources and Civil Engineering China Agricultural University Beijing 100083 China

2. Key Laboratory of Tibetan Environment Changes and Land Surface Processes, Institute of Tibetan Plateau Research Chinese Academy of Sciences Beijing 100101 China

3. State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, Institute of Soil and Water Conservation Chinese Academy of Science and Ministry of Water Resources Yangling 712100 China

Funder

National Natural Science Foundation of China

Publisher

Wiley

Subject

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

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1002/esp.5138

Reference62 articles.

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

2. Comparative study of erosion processes of thawed and non-frozen soil by concentrated meltwater flow

3. Soil erodibility and processes of water erosion on hillslope

4. Using quartz grain size and shape analysis to distinguish between aeolian and fluvial deposits in the Dallol Bosso of Niger (West Africa)

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