Vertical distribution character of soil inorganic phosphorus in mountain meadow system of WuGong Mountain
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Abstract
The spatial distribution of soil inorganic phosphorus and the correlation between soil inorganic phosphorus and soil available phosphorus along the different altitudes (the altitude range from 1 600~1 900 m) and different soil depths were analyzed in mountain meadow system of Wugong Mountain. The soil inorganic phosphorus (P) content ranged in 175.48~524.06 mg·kg-1, significantly increased (P0.05) with the increase of altitude and decreased gradually with the increase of soil depth. There was a vertical distribution law and surface gathering character. The range of variation in water-soluble P, Al-P, Fe-P, O-P, Ca-P was 0.423~4.781, 16.27~90.72, 54.13~344.34, 19.66~90.32, 15.12~76.21 mg·kg-1, respectively. There were also vertical distribution and surface gathering character in each proportions of inorganic phosphorus. The percentage of Fe-P was the highest which followed by Al-P, O-P, Ca-P and water soluble P. There was a significantly positive correlations between soil available P and Al-P which suggest that Al-P was the potential resource for available P in this area. This research revealed the spatial distribution of soil inorganic P and the correlation between available P and soil inorganic P, determinate the resource of soil P which provided a guidance for vegetation restoration in mountain meadow ecosystem.
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