4.7 Article

Plant morphology and distribution control runoff and erosion in semi-arid environments

期刊

CATENA
卷 211, 期 -, 页码 -

出版社

ELSEVIER
DOI: 10.1016/j.catena.2022.106022

关键词

Multidimensional morphology metrics; Morphology expectation; Hydrological function; Isolated plant; Vegetation community; Contributing runoff area

资金

  1. national major science and technology program for water pollution control and treatment [2017X07101001]
  2. National Natural Science Foundation of China [41930649]

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This study used multidimensional morphology metrics and expectations to analyze the effects of two plant species on runoff and sediment in the Loess Plateau of China. The results showed that the isolated Spiraea pubescens Turcz had a stronger ability to control runoff and erosion compared to Artemisia sacrorum Ledeb. At a larger scale, the Spiraea pubescens Turcz field-plots had a significantly larger canopy surface area and plant volume compared to the Artemisia sacrorum Ledeb field-plots, resulting in a more effective ability to retain runoff and trap sediment. The findings provide insights into the role of plant morphology and distribution in controlling soil erosion in water-limited ecosystems.
Understanding of the effects of vegetation patches and their distribution on soil erosion is important for ecological restoration in semi-arid environments. In this study, six multidimensional morphology metrics and expectations were applied to analyze the effects of plant morphology and distribution on runoff and sediment in two dominant plant species, Artemisia sacrorum Ledeb (AS) and Spiraea pubescens Turcz (SP), at micro-plots (60 cm x 60 cm plots) and field-plots (3 m x 10 m field-plots) in the Loess Plateau of China. The results indicated that, at micro-plot scale, the morphological heterogeneity of the two isolated shrubs (AS and SP) could be identified by spherical cap surface area of canopy and plant volume, which also lead to the isolated SP to have stronger ability to control runoff and erosion than the isolated AS. At field-plot scale, spherical cap surface area of canopy expectation (32.01 +/- 1.99 m(2)) and plant volume expectation (4.06 +/- 0.38 m(3)) of SP field-plots was significantly larger than those of the AS field-plots (15.85 +/- 2.46 m(2) and 1.10 +/- 0.21 m(3) respectively) in the potential contributing runoff area (2 m area form the field outlet). These differences result in SP field-plot to have more effective ability to retain runoff and to trap sediment than AS field-plot. The high-dimensional morphology metrics and expectations could determine the role of plant hydrological functions in controlling runoff and sediment at multiple spatial scales. This knowledge improves our understanding of the roles that plant morphology and distribution have on the runoff and erosion from different vegetated plots, and offers a new route to explaining plant morphology and distribution as controls on soil erosion in water-limited ecosystem.

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