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Chinese Journal of Applied Ecology ›› 2016, Vol. 27 ›› Issue (3): 705-715.doi: 10.13287/j.1001-9332.201603.013

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Spatial heterogeneity and influencing factors of soil phosphorus concentration in a mid-subtropical Choerospondias axillaris deciduous broad-leaved forest, China

HU Rui-bin1, FANG Xi1,2,3*, XIANG Wen-hua1,2,3, JIANG Fang1, LEI Pi-feng1,2,3, ZHAO Li-juan1,2, ZHU Wen-juan1, DENG Xiang-wen1,2,3   

  1. 1College of Life Science and Technology, Central South University of Forestry and Technology, Changsha 410004, China;
    2National Engineering Laboratory for Applied Forest Ecological Technology in Southern China, Changsha 410004, China;
    3Huitong National Field Station for Scientific Observation and Research of Chinese Fir Plantation Ecosystem in Hunan Province, Huitong 438107, China
  • Received:2015-08-24 Online:2016-03-18 Published:2016-03-18
  • Contact: * E-mail: fangxizhang@sina.com
  • Supported by:
    This work was supported by the Program of State Forestry Special Fund for Public Welfare Industry of China (201304317), the International Cooperation Project of Ministry of Science and Technology of China (2013DFA32190), and the Research Fund for the Doctoral Program of Higher Education of

Abstract: In order to investigate spatial variations in soil phosphorus (P) concentration and the influencing factors, one permanent plot of 1 hm2 was established and stand structure was surveyed in Choerospondias axillaries deciduous broadleaved forest in Dashanchong Forest Park in Changsha County, Hunan Province, China. Soil samples were collected with equidistant grid point sampling method and soil P concentration and its spatial variation were analyzed by using geo-statistics and geographical information system (GIS) techniques. The results showed that the variations of total P and available P concentrations in humus layer and in the soil profile at depth of 0-10, 10-20 and 20-30 cm were moderate and the available P showed higher variability in a specific soil layer compared with total P. Concentrations of total P and available P in soil decreased, while the variations increased with the increase in soil depth. The total P and available P showed high spatial autocorrelation, primarily resulted from the structural factors. The spatial heterogeneity of available P was stronger than that of total P, and the spatial autocorrelation ranges of total P and available P varied from 92.80 to 168.90 m and from 79.43 to 106.20 m in different soil layers, respectively. At the same soil depth, fractal dimensions of total P were higher than that of available P, with more complex spatial pattern, while available P showed stronger spatial correlation with stronger spatial structure. In humus layer and soil depths of 0-10, 10-20 and 20-30 cm, the spatial variation pattern of total P and available P concentrations showed an apparent belt-shaped and spot massive gradient change. The high value appeared at low elevation and valley position, and the low value appeared in the high elevation and ridge area. The total P and available P concentrations showed significantly negative correlation with elevation and litter, but the relationship with convexity, species, numbers and soil pH was not significant. The total P and available P exhibited significant positive correlations with soil organic carbon (SOC), total nitrogen concentration, indicating the leaching characteristics of soil P. Its spatial variability was affected by many interactive factors.