Variations in Soil Physico-Chemical Properties along Slope Position Gradient in Secondary Vegetation of the Hilly Region, Guilin, Southwest China

• Published in: Sustainability 2020-01, Vol.12 (4), p.1303
• Main Authors: Liu, Runhong, Pan, Yuanfang, Bao, Han, Liang, Shichu, Jiang, Yong, Tu, Hongrun, Nong, Juanli, Huang, Wanqing
• Format: Article
• Language: English
• Subjects: Carbon; Chemical properties; Correlation analysis; Ecosystems; Investigations; Microclimate; Moisture content; Nitrogen; Organic matter; Organic soils; Phosphorus; Physicochemical properties; Potassium; Precipitation; Principal components analysis; Reconstruction; Restoration strategies; Sea level; Slope gradients; Soil chemistry; Soil erosion; Soil organic matter; Soil properties; Soil water; Sustainability; Sustainable development; Topography; Variation; Vegetation; Water content
• ISSN: 2071-1050; 2071-1050
• DOI: 10.3390/su12041303

Understanding the variation of soil physico-chemical properties along slope position gradients is essential for vegetation restoration and reconstruction, but how slope positions impact the soil physico-chemical properties in the secondary vegetation of hilly regions is poorly understood. To address these uncertainties, we examined the changes in soil physico-chemical properties and their relationships along the slope position gradient in secondary vegetation of the hilly region in Guilin, southwest China. The results showed that except for the soil water content, soil total phosphorus and soil total potassium which reached the highest value at the footslope, other soil physico-chemical properties reached the highest content in the middle slope, and most of the soil physico-chemical properties showed the lowest content in the upper slope or footslope. Moreover, Pearson’s correlation analysis revealed that there were no significant correlations between most of the soil physico-chemical properties and that the correlations between soil physico-chemical properties were not consistent across different slope positions. Additionally, the principal component analysis showed that the first 4 principal components together explained 84.32% of the total variation and might be interpreted as the change of soil total nitrogen, soil organic matter, soil available nitrogen, soil available potassium, soil water content and soil total potassium. Overall, our results strongly demonstrated that slope positions showed significant effects on most of the soil physico-chemical properties and would provide an important reference for the formulation of restoration strategies in different slope positions to facilitate vegetation restoration and reconstruction and the sustainable development of the ecological environment in the hilly region.