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Effects of ryegrass canopy and roots on the distribution characteristics of eroded sediment particles during heavy rainfall events on steep loess‐cinnamon slopes in Zhangjiakou, China

Bibliographic Data

ID21649752
AuthorsXiaona Liu (0000-0001-8934-056X, Key Laboratory of Soil and Water Conservation and Desertification Combating, State Forestry Administration Beijing Forestry University Beijing 100083 PR China), Xinxiao Yu (0000-0003-1260-5712, Key Laboratory of Soil and Water Conservation and Desertification Combating, State Forestry Administration Beijing Forestry University Beijing 100083 PR China, corresponding author), Dengxing Fan (Key Laboratory of Soil and Water Conservation and Desertification Combating, State Forestry Administration Beijing Forestry University Beijing 100083 PR China), Guodong Jia (0000-0002-8360-0460, Key Laboratory of Soil and Water Conservation and Desertification Combating, State Forestry Administration Beijing Forestry University Beijing 100083 PR China)
Year2021
Volume32
Issue4
Pages1643-1655
Publication date2021-02-28
Peer ReviewedYes
Open AccessYes
TypeARTICLE
VenueLand Degradation and Development (JOURNAL)
Journal identifiersISSN: 1085-3278 • E-ISSN: 1099-145X
PublisherWiley (PUBLISHER • GB)
DOI10.1002/ldr.3769
OpenAlexW3087541377
LanguageEN
Citations received1
References cited45

To evaluate the effects of ryegrass ( Lolium perenne ) canopy and roots on eroded sediment particle distribution characteristics, simulated rainfall tests were implemented on grass caopy, roots, and bare slopes. The grass coverage density were 0, 20, 40, and 60%. The results showed that ryegrass canopies mainly contributed to runoff reduction and ryegrass roots primarily contributed to erosion reduction. With increasing rainfall duration, smaller particles (clay and fine silt particles) increased and larger particles (coarse silt and sand particles) decreased in the eroded sediment on the grass slope while the opposite trend was observed for the roots and bare slopes. Moreover, the clay and sand particles were eroded as aggregates and most silt particles were transported in the form of primary particles. Compared to the original soil, larger particles in the eroded sediment mainly occurred on the grass slopes because smaller particles were intercepted by the grass canopies, while smaller particles primarily occurred in the eroded sediment of the root slopes because grass roots inhibited soil erosion. These results illustrate that grass cover can prevent the loss of small particles in the topsoil and avoid soil coarsening, which provides guidance for the comprehensive control of soil erosion

Agronomy · Biology · Canopy · Erosion · Geomorphology · Geotechnical engineering · Loess · Lolium perenne · Poaceae · Sediment · Silt · Soil water · Surface runoff · Topsoil · Aeolian processes and effects · Environmental Science · Hydrology and Sediment Transport Processes · Soil erosion and sediment transport · Ecology · Geology · Soil Science

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Unique citing works1
Citations per year0.33
Citation span2023 - 2023 (1)
Citation velocityhistorical
Highly citedNo

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