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Effect of roots on the soil detachment process in grassland and shrubland

Bibliographic Data

ID21647752
AuthorsJianye Ma (0000-0002-9098-0588, State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, Institute of Soil and Water Conservation Northwest Agriculture and Forestry University Yangling PR China), Bo Ma (0000-0002-7475-250X, State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, Institute of Soil and Water Conservation Northwest Agriculture and Forestry University Yangling PR China, corresponding author), Zhanbin Li (0000-0003-3389-5069, State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, Institute of Soil and Water Conservation Northwest Agriculture and Forestry University Yangling PR China), Chenguang Wang (0000-0002-3953-5008, State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, Institute of Soil and Water Conservation Northwest Agriculture and Forestry University Yangling PR China), Zeyu Zhang (0000-0002-3628-141X, State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, Institute of Soil and Water Conservation Northwest Agriculture and Forestry University Yangling PR China), Li Gui (0000-0003-2076-7658, Institute of Soil and Water Conservation), Gui Li (State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, Institute of Soil and Water Conservation Northwest Agriculture and Forestry University Yangling PR China)
Year2023
Volume34
Issue10
Pages3017-3032
Publication date2023-06-01
Peer ReviewedYes
Open AccessYes
TypeARTICLE
VenueLand Degradation and Development (JOURNAL)
Journal identifiersISSN: 1085-3278 • E-ISSN: 1099-145X
PublisherWiley (PUBLISHER • GB)
DOI10.1002/ldr.4664
OpenAlexW4323045336
LanguageEN
References cited50

Plant roots play an important role in reducing soil detachment and increasing soil erosion resistance. Current studies have mainly focused on the quantification of the soil detachment rate (SDR). However, few studies have been conducted to explore the variation in the SDR and root effects during the soil detachment process. In this study, undisturbed soil samples were collected from four shrublands (with the main species Caragana korshinskii , C. korshinskii mixed with Agropyron cristatum , C. korshinskii mixed with Bothriochloa ischaemum , and C. korshinskii mixed with Artemisia gmelinii ) and three grasslands (with the main species B. ischaemum , B. ischaemum mixed with A. cristatum , and B. ischaemum mixed with A. gmelinii ) on the Loess Plateau, China. The samples were subjected to flow scouring through hydraulic flume experiments under six different shear stresses. The duration of this experiment was 6 min, and the SDR of each minute was estimated. The results showed that the SDR of shrubland was higher than that of grassland in each detachment process. The dominant factors affecting SDR gradually changed from the root–soil composite properties to the hydrodynamic parameters in this process. The effect of roots on the SDR was stronger than that of soil properties in the root–soil composite. In the early detachment stage, the 0–2 mm fine roots had the strongest effect on the SDR, while it was affected by the combined effect of fine roots and coarse roots in the later stage. When the fibrous roots were mixed with the tap roots, the fibrous roots had a significant negative effect on the SDR and mainly affected the early detachment stage. However, the tap roots had a weak effect in all stages. With the detachment process, the soil erosion resistance first increased and then stabilized, and the variations were mainly concentrated from 0 to 3 min. The roots mainly affected the SDR and soil erosion resistance by influencing rill erodibility parameters

Agronomy · Biology · Ecosystem · Grassland · Shrubland · Environmental Science · Plant responses to water stress · Soil erosion and sediment transport · Tree Root and Stability Studies · Ecology · Soil Science

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