4.6 Article

Effects of shrub-grass patterns on soil detachment and hydraulic parameters of slope in the Pisha sandstone area of Inner Mongolia, China

Journal

JOURNAL OF FORESTRY RESEARCH
Volume 33, Issue 2, Pages 519-528

Publisher

NORTHEAST FORESTRY UNIV
DOI: 10.1007/s11676-021-01319-7

Keywords

Vegetation pattern; Soil detachment rate; Hydraulic parameters; Soil erosion; Caragana korshinskii

Categories

Funding

  1. National Natural Science Foundation of China [41701327, 31870708, 51879155, 51579157, 51779156]
  2. National Key Research and Development Program of China [2016YFC0500504]
  3. Inner Mongolia Natural Science Foundation [2017BS0405]

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Plant root systems play a crucial role in reducing erosion on slopes. Different vegetation patterns exhibit varying soil detachment rates, with shrubbery on the lower parts of slopes proving to be the most effective in combating erosion.
The characteristics of soil holding capacity for different shrub-grass patterns are important to research the mechanisms regulating vegetation on slopes. The objective of this study was to describe the characteristics and mechanisms of soil erosion and hydraulic parameters under different vegetation patterns in the Pisha sandstone area of Inner Mongolia on lands of 8 degrees slope gradient. We carried out field scouring experiments on five different shrub-grass patterns as treatments, viz no shrubs (GL), shrubs on the upper part of the slope (SU), middle part of the slope (SM) and lower part of the slope (SL). We designated bare slope (BL) as the control. We employed three different water flow rates (15, 20, 30 L center dot min(-1)). Our results showed that the contribution of plant root systems to slope sediment reduction ranged from 64 to 84%. The root systems proved to be the main contributing factor to reduction of erosion by vegetation. The relationship between soil detachment rate, stream flow power, and flow unit stream power under different scouring discharge rates showed that soil detachment declined in rank order as: BL > GL > SU > SM > SL. The SL pattern had the lowest soil detachment rate (0.098 g center dot m(-2)center dot s(-1)), flow stream power (2.371 W center dot m(-2)), flow unit stream power (0.165 m center dot s(-1)) and flow shear stress (16.986 Pa), and proved to be the best erosion combating pattern. The results of decision coefficient and path analysis showed that stream power was the most important hydraulic parameter for describing soil detachment rate. The combination of stream power and shear stress, namely Dr = 0.1 omega - 0.03 tau - 0.56 (R-2 = 0.924), most accurately simulated the soil detachment characteristics on slopes. Our study suggests that the risk of soil erosion can be reduced by planting shrub-grass mixes on these slopes. Under the conditions of limited water resources and economy, the benefit of sediment reduction can be maximized by planting shrubbery on the lower parts of slopes.

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