欢迎访问《应用生态学报》官方网站,今天是 分享到:

应用生态学报 ›› 2011, Vol. 22 ›› Issue (02): 418-424.

• 研究报告 • 上一篇    下一篇

长江上游不同植物篱系统的土壤物理性质

黎建强,张洪江,程金花,王幸,吕文星   

  1. 北京林业大学水土保持学院, 北京 100083
  • 出版日期:2011-02-18 发布日期:2011-02-18

Soil physical properties of different hedgerow systems in upper reaches of Yangtze River.

LI Jian-qiang, ZHANG Hong-jiang, CHENG Jin-hua, WANG Xing, LÜ|Wen-xing   

  1. College of Soil and Water Conservation, Beijing Forestry University, Beijing 100083, China
  • Online:2011-02-18 Published:2011-02-18

摘要: 在长江上游现有植物篱调查的基础上,对3种不同植物篱(乔木类、灌木类和草本类)不同位置的土壤物理性质进行了分析.结果表明:与植物篱带间相比,研究区3种不同类型植物篱带内土壤物理性质均得到了显著改善和提高;乔木类、草本类和灌木类植物篱带内土壤孔隙度、含水量、饱和导水率、水稳性团聚体含量、抗蚀指数、抗冲指数和土壤粘粒含量平均值分别提高了18.8%、30.1%、12.9%、139.3%、108.3%、95.9%和25.5% ,土壤容重和土壤沙粒含量分别平均减小17.3%和9.6%;3种不同植物篱带内的土壤物理性质存在差异性,乔木类植物篱带内土壤抗冲性指数最大,灌木类植物篱带内土壤孔隙度、含水量、饱和导水率、抗蚀指数、水稳性团聚体含量、土壤粘粒含量高于乔木类和草本类,其土壤容重则低于乔木类和草本类;植物篱对植物篱-坡耕地系统内不同位置土壤物理性质影响程度的差异导致了土壤物理性质各指标在植物篱带内、带上、带下和带间坡耕地也存在一定的变异性,乔木类植物篱土壤水分含量、抗蚀指数、饱和导水率和土壤粘粒含量的变异系数大于灌木类和草本类植物篱,灌木类植物篱土壤容重、孔隙度、水稳性团聚体含量和抗冲指数的变异系数高于乔木类和草本类植物篱.

关键词: 土壤物理性质, 植物篱, 水平变异, 长江上游

Abstract: Based on the investigation of present hedgerows in the upper reaches of Yangtze River, this paper analyzed the soil physical properties at different positions of three kinds of hedgerows (arbor, shrub, and grass). Comparing with those between the hedgerows, the soil physical properties within the hedgerows improved significantly. The average values of soil porosity, moisture content, saturated conductivity, water stable aggregates content, anti-erodibility index, anti-scouribility index, and clay content within the arbor, grass, and shrub hedgerows increased by 18.8%, 30.1%, 12.9%, 139.3%, 108.3%, 95.9%, and 25.5%, and the soil bulk density and sand content averagely decreased by 17.3% and 9.6%, respectively. The soil properties within the three hedgerows differed significantly. The soil anti-scouribility index within arbor hedgerow was the highest; the soil porosity, moisture content, saturated conductivity, anti-scouribility index, water-stable aggregates content, and clay content within the shrub hedgerow were higher than those within the tree and grass hedgerows; while the soil bulk density within the shrub hedgerows was lower than that within the tree and grass hedgerows. Because of the differences in the affecting degree of hedgerow on the soil physical properties at different positions of the three hedgerow systems, the related parameters presented definite horizontal variation at steep lands within, before, and behind the hedgerows, and between the hedgerows. The coefficient of variation (CV) of soil moisture content, anti-erodibility index, saturated conductivity, and clay content of arbor hedgerows was bigger than that of shrub and grass hedgerows, while the CV of soil bulk density, porosity, water-stable aggregates content, and anti-scouribility index of shrub hedgerow was bigger than that of arbor and grass hedgerows.

Key words: soil physical property, hedgerow, horizontal variance, upper reaches of Yangtze River