Investigating the effects of herbaceous root systems on the soil detachment process at the species level.

Sci Total Environ

State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, Institute of Soil and Water Conservation, Northwest A&F University, Yangling, Shaanxi 712100, PR China; University of Chinese Academy of Sciences, Beijing 100049, China.

Published: February 2023

AI Article Synopsis

  • The study investigates how different plant species, specifically Bothriochloa ischcemum (fibrous roots) and Artemisia vestita (tap roots), influence soil detachment rates under overland flow conditions on the Loess Plateau.
  • It was observed that as plant density increased, the soil detachment rates decreased significantly, with Bothriochloa ischcemum proving to be more effective in reducing soil erosion compared to Artemisia vestita.
  • The research establishes a mathematical relationship where soil detachment rate can be estimated using overland flow velocity, soil bulk density, and root length density, indicating the complex interactions between vegetation, soil, and hydrological factors.

Article Abstract

Plant root growth significantly affect soil detachment process, whereas the mechanism of how roots affect the soil detachment process by overland flow at species level is not fully understood. This study was conducted to investigate the soil detachment rate responds to plant-induce soil properties and root traits at species level. Two typical herbaceous plants, Bothriochloa ischcemum (Linn.). Keng (BI; fibrous root system) and Artemisia vestita Wall. ex Bess (AG; tap root system), from the Loess Plateau were studies for one year under six planted densities of 5 plants m, 10 plants m, 15 plants m, 20 plants m, 25 plants m, and 30 plants m. In total, 24 steel tanks were planted, and two plots were used as bare soil controls. Their soil detachment rates were tested under a constant overland flow (1.5 l s) on a 26.2 % slope. The results showed that soil detachment rate under the six planted densities ranged from 0.034 kg m s to 0.112 kg m s1 for BI and was ranged from 0.053 kg m s to 0.132 kg m s for AG, which all greatly reduced soil detachment rate and were 68.17 % to 92.33 % and 69.20 % to 87.27 % less than that of the control. In general, BI was more effective in reducing soil detachment rate than AG, achieving a mean soil detachment rate that was 23.75 % lower. With increasing plant density, soil detachment rate decreased as a power function. The overland flow hydraulic characteristics, soil properties and root traits influenced by plant density were positively or negatively correlated with soil detachment rate. Specifically, soil detachment rate decreased with velocity, bulk density, root length density, and increased with shear stress and Darcy-Weisbach friction factor as power or exponential functions. On this basis, the soil detachment rate (Dr) can be satisfactorily estimated by overland flow velocity (v), soil bulk density (BD) and root length density (RLD) as a power function (Dr = 63.03v × BD × RLDR = 0.65; NSE = 0.60; p < 0.01).

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Source
http://dx.doi.org/10.1016/j.scitotenv.2022.160196DOI Listing

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