Arid Zone Research ›› 2024, Vol. 41 ›› Issue (11): 1875-1886.doi: 10.13866/j.azr.2024.11.08

• Plant Ecology • Previous Articles     Next Articles

Effects of Caragana microphylla on vegetation and soil in the restoration of desertified grasslands

ZHU Tiantian1(), HAI Lu2, CAO Wenxu1, LI Xu1, LI Qinghe1()   

  1. 1. Key Laboratory of Tree Breeding and Cultivation of National Forestry and Grassland Administration, State Key Laboratory of Efficient Production of Forest Resources, Research Institute of Forestry, Chinese Academy of Forestry,Beijing 100091, China
    2. Experimental Center of Desert Forestry, Chinese Academy of Forestry, Dengkou 015200, Inner Mongolia, China
  • Received:2024-05-17 Revised:2024-07-31 Online:2024-11-15 Published:2024-11-29
  • Contact: LI Qinghe

Abstract:

Caragana microphylla, a shrub species commonly used to promote vegetation recovery in grasslands affected by desertification, plays a significant role in the ecological restoration and sustainable development of sandy lands. Understanding its impact on understory vegetation and soil physicochemical characteristics during different stages of desertified grassland recovery is crucial. This study focuses on C. microphylla shrublands in three typical stages of desertified grassland vegetation recovery in the Hulun Buir sandy land: semi-fixed, fixed, and sandy grasslands. This study used ANOVA, Pearson’s correlation analysis, and redundancy analysis methods to explore the changes in understory plant communities and soil physicochemical characteristics in C. microphylla shrublands during different stages of desertified grassland vegetation recovery and their interrelationships. The results indicate that, as the degree of vegetation recovery in desertified grasslands increases, the species richness of the understory vegetation, Shannon-Wiener index, community height, and biomass also increase. The community height and biomass within the shrublands are higher than outside, with species richness within the shrublands being higher than outside during the semi-fixed and fixed sandland stages. In the 0-10 cm and 10-20 cm soil layers, SWC displays an increasing trend, peaking in the sandy grassland stage (1.2%), and is higher within the shrublands than outside. The SWC at 10-20 cm is higher at 0-10 cm. In both layers, clay and silt content gradually increases with the degree of vegetation recovery in the sandy land and is higher within the shrublands than outside, while the opposite is true for sand content. In both soil layers, SOC gradually increases with the degree of vegetation recovery, peaking in the sandy grassland stage (4.12 g·kg-1) and is higher within the shrublands than outside. TN increases from the semi-fixed to the fixed sand land stage, with higher levels within the shrublands than outside at all stages. Soil pH within the shrublands decreases as the degree of vegetation recovery increases. No significant change in TP is observed. Additionally, soil physicochemical characteristics account for 59.6% and 46.9% of the vegetation changes in both soil layers within and outside the shrublands, respectively, with the main influencing factors being soil particle size, TN, SWC, and SOC. This study demonstrates that during vegetation recovery in desertified grasslands, C. microphylla shrublands promote vegetation growth and development by improving the soil physicochemical characteristics under the shrublands, including soil particle size, SWC, SOC, and TN.

Key words: desertified grassland vegetation recovery, Caragana microphylla, vegetation characteristics, soil physicochemical characteristics, Hulun Buir