Welcome to Chinese Journal of Applied Ecology! Today is Share:

Chinese Journal of Applied Ecology

• Articles • Previous Articles     Next Articles

Soil microelements under different vegetation restoration patterns in yellow soil slope region of mid-subtropics.

QI Liang-hua1;ZHANG Xu-dong2; PENG Zhen-hua1,2;FAN Shao-hui1; ZHOU Jin-xing2   

  1. 1International Center for Bamboo and Rattan, Beijing 100102, China;2Research Institute of Forestry, Chinese Academy of Forestry, Beijing 100091, China
  • Received:2007-09-12 Revised:1900-01-01 Online:2008-04-20 Published:2008-04-20

Abstract: With the Nüerzhai watershed in Wuling Mountain as a case, this paper studied the contents and availabilities of soil microelements and their relationships with soil organic matter and pH value in yellow soil slope region of midsubtropics under seven typical vegetation restoration patterns, i.e., Pinus massoniana natural forest (Ⅰ), Cunninghamia lanceolata plantation (Ⅱ), Eucommia ulmoides plantation (Ⅲ), Vernicia fordii plantation (Ⅳ), Machilus pingii secondary forest (Ⅴ), Phyllostachys edulis-C. lanceolata mixed forest (Ⅵ), and wasteland-shrub community (Ⅶ). It was found that in 0-20 cm soil layer, the contents of B and Mn, Mo and Cu, Zn, and Fe reached the peaks under Ⅶ, Ⅳ, III and Ⅵ; while in 20-40 cm soil layer, Ⅲ, Ⅳ, Ⅴand Ⅶ had the highest contents of Cu, Zn, B, and Fe and Mn, Mo, respectively. In both two soil layers under Ⅵ, the contents of B, Mo, Cu and Mn were the lowest. Mn had the biggest single element available index, while Cu had the smallest one. The biggest and smallest total available index of soil microelements was 12.28 for Ⅶ and 2.95 for Ⅵ, respectively. There existed the regularities of Mn>Zn>Fe>Mo>B>Cu for single microelement available index and Ⅶ>Ⅴ>III>Ⅳ>Ⅰ>Ⅱ>Ⅵ for comprehensive microelement available index under different vegetation patterns. A good linear relationship was observed between soil organic matter and B and Zn availabilities, and the relationship of soil organic matter with available Mn could be described by a quadratic equation. Soil pH was highly positively correlated with soil Cu and Zn contents, correlated with soil Mo and Mn contents, slightly correlated with soil B content, and slightly negatively correlated with soil Fe content.

Key words: stomatal conductivity optimization model, abscisic acid, hydraulic regulation, water-regulation strategy