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Journal of Desert Research ›› 2023, Vol. 43 ›› Issue (4): 220-230.DOI: 10.7522/j.issn.1000-694X.2023.00007

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Spatio-temporal differentiation and driving factors of windbreak and sand fixation services in wind erosion area of the northern Loess Plateau

Jinfeng Wang1(), Xiaoling Liu1, Qing Li2(), Rende Wang2, Sheng Wang1   

  1. 1.School of Geographical Science,Shanxi Normal University,Taiyuan 030000,China
    2.Institute of Geographical Sciences / Hebei Engineering Research Center for Geographic Information Application,Hebei Academy of Sciences,Shijiazhuang 050011,China
  • Received:2022-12-02 Revised:2023-02-11 Online:2023-07-20 Published:2023-08-14
  • Contact: Qing Li

Abstract:

The wind erosion area in the northern Loess Plateau is the typical area of soil wind erosion in the Yellow River Basin. Evaluating windbreak and sand fixation services is of great significance for the construction of ecological security barrier in the Yellow River Basin. Based on the wind erosion model in the benefit evaluation of the Beijing-Tianjin sandstorm source control project, the amount of sand fixation in wind erosion area of the northern Loess Plateau was estimated, windbreak and sand fixation services were quantitatively evaluated from 2000 to 2020, and the driving mechanism was analyzed in combination with land use, vegetation coverage and climate change. The results showed that: (1) From 2000 to 2020, the annual average amount of sand fixation in wind erosion area of the northern Loess Plateau was 5.52×108 t, and presented a decreasing trend, with the average change rate of -0.12 t·hm-2·a-1. However, the retention rate of windbreak and sand fixation services increased at a rate of 0.50%·a-1, showing an upward trend. The windbreak and sand fixation services of vegetation in study areas were enhanced. In terms of spatial distribution, windbreak and sand fixation services of vegetation were enhanced in northern Yulin, eastern Ningxia, Qingyang, the central and southern parts of Mu Us Sandy Land and Dalad Banner in the northern sandy land. (2) Grassland is the main land use type on controlling soil wind erosion and playing the role of windbreak and sand fixation. Desertification reversal and conversion of farmland to grassland significantly improved windbreak and sand fixation services, while grassland degradation will significantly weaken sand fixation services. (3) Wind speed is the main driving factor for the change of windbreak and sand fixation services in wind erosion area of the northern Loess Plateau. Vegetation restoration plays an important role in windbreak and sand fixation for the key regions, such as Kobq Desert and Mu Us Sandy Land. This study will provide reference for the construction of aeolian sand control project in the Loess Plateau.

Key words: windbreak and sand fixation, retention rate of windbreak and sand fixation services, wind erosion model, the Loess Plateau

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