Erosion-reducing effects of plant roots during concentrated flow under contrasting textured soils

被引:43
|
作者
Hao, Hao-xin [1 ,2 ]
Qin, Jia-hui [1 ]
Sun, Zhao-xiang [1 ]
Guo, Zhong-lu [1 ]
Wang, Jun-guang [1 ]
机构
[1] Huazhong Agr Univ, Key Lab Arable Land Conservat Middle & Lower Reac, Minist Agr & Rural Affairs, Wuhan 430070, Peoples R China
[2] Changjiang Water Resources Protect Inst, Wuhan 430051, Peoples R China
基金
中国国家自然科学基金;
关键词
Concentrated flow; Grass root; Trait variability; Soil texture; Rill erodibility; WATER EROSION; INTRASPECIFIC VARIABILITY; ARCHITECTURAL ANALYSIS; DETACHMENT CAPACITY; TYPICAL GRASSLANDS; FUNCTIONAL TRAITS; SIZE DISTRIBUTION; OVERLAND-FLOW; RESISTANCE; SIMULATION;
D O I
10.1016/j.catena.2021.105378
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
The effects of plant roots on water erosion are likely to vary according to the range of root traits and soil textures. However, little is known about the erosion-reducing potential of roots under different soil textures due to the lack of sufficient texture variations which come from a comparable system. In this study, we systematically investigate how root functional traits respond to soil sand contents and their combined effects on rill erosion. Seeding of Cynodon dactylon (L.) Pers. were grown in a greenhouse under varied proportions of sand mass (ranging from 14% to 83%) by mixing silty clay soil (Ultisols derived from quaternary red clay) and engineering sand. After six months growing, the root-soil composites were subjected to concentrated flow in a hydraulic flume to obtain soil detachment capacity (D-c), then roots were separated to measure their morphology and architecture traits. The results showed that sand content significantly affected root morphology traits (e.g., RD and RLD) (p < 0.01). In contrast, root architecture traits (e.g., mot fractal dimension, topological index and radius frequency distribution function) showed no significant changes with soil texture (p > 0.05). Generally, root strongly promoted soil cohesion and they mitigated rill erodibility in a coordinated way. Rill erodibility was mostly determined by soil texture even in soils with dense roots, and the erosion-reducing effects of roots were less efficient in heavy-textured soils. Moreover, no significant correlations were found between critical flow shear stress (tau(c)) and root traits, and soil with a loam texture displayed the lowest tau(c). Those relationships are likely to exist elsewhere, but its strength and direction could be changed according to the mot trait variability and the varied root-soil feedbacks. The results of this study would be quite relevant for soil erosion modeling and imply the bare sandy soils are more urgent to be recovered during engineering constructions. Moreover, the inclusion of plant with dense fibrous roots could be the optimal species mixtures to stable sandy slopes.
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页数:9
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