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Acta Prataculturae Sinica ›› 2024, Vol. 33 ›› Issue (6): 17-28.DOI: 10.11686/cyxb2023243

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Effects of different grazing times on soil particle composition and fractal dimension in the desert steppe

Hai-xin JIANG1,2,3(), Yao ZHOU1,2,3,4, Ke HU5, Zhan-sheng DING5, Hong-bin MA1,2,3,4()   

  1. 1.Key Laboratory for Model Innovation in Forage Production Efficiency,Ministry of Agriculture and Rural Affairs,P. R. China,Ningxia University,Yinchuan 750021,China
    2.Ningxia Grassland and Animal Husbandry Engineering Technology Research Center,Ningxia University,Yinchuan 750021,China
    3.College of Forestry and Prataculture,Ningxia University,Yinchuan 750021,China
    4.Breeding Base for State Key Laboratory of Land Degradation and Ecological Restoration of Northwest China,Ningxia University,Yinchuan 750021,China
    5.Ningxia Wuzhong City Litong District Forestry and Grassland Administration,Wuzhong 751100,China
  • Received:2023-07-13 Revised:2023-09-11 Online:2024-06-20 Published:2024-03-20
  • Contact: Hong-bin MA

Abstract:

Studying the impact of the timing of grazing on soil particle composition and fractal dimension in grasslands is crucial for understanding how grazing disturbances affect soil quality and the ecological conditions of grasslands. The overall aim of this research, therefore, was to provide a theoretical foundation for determining the most suitable timing of grazing in grassland ecosystems. This study was conducted on the desert steppe of Ningxia, and five grazing treatments were implemented: forbidden grazing (FY), traditional time rotational grazing (FG), delayed start rotational grazing (YG), early end rotational grazing (TG), and delayed start and early end rotational grazing (YT). We collected soil samples from all of these treatments. Then, we determined how different grazing timing influenced changes in soil particle composition and fractal dimension on the desert steppe and identified the factors driving these changes. The results clearly demonstrate that across all treatments, the primary components of soil texture in desert steppe were silt, very fine sand, and fine sand particles. We observed significant variations in soil particle composition among treatments within the 0-40 cm soil depth range (P<0.05). The soil particle fractal dimension ranged from 2.11 to 2.75, with a gradual increase with increasing soil depth. Notably, YG had the highest silt content and fractal dimension. The silt content and fractal dimension FY of 0-10 cm soil layer were the lowest, and the FG treatment was the lowest in the other soil layers. The soil fractal dimension was significantly positively correlated with silt content (P<0.01), and significantly negatively correlated with very fine sand and fine sand contents (P<0.01, P<0.05). The soil particle fractal dimension was positively correlated with organic carbon content and total porosity, and negatively correlated with bulk density, available potassium content, and capillary porosity. In conclusion, our results suggest that the fractal dimension can effectively serve as an indicator of changes in soil texture on the desert steppe. Delayed grazing practices positively influence soil particle composition and fractal dimension, ultimately improving soil quality. These findings offer valuable insights for determining the optimal timing of grazing on the desert steppe.

Key words: particle composition, fractal dimension, grazing time, desert steppe