Li Jian-Qiang, Zhang Hong-Jiang, Cheng Jin-Hua, Wang Xing, Lü Wen-Xing
College of Soil and Water Conservation, Beijing Forestry University, Beijing 100083, China.
Ying Yong Sheng Tai Xue Bao. 2011 Feb;22(2):418-24.
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.
基于对长江上游现有绿篱的调查,本文分析了三种绿篱(乔木、灌木和草本)不同位置的土壤物理性质。与绿篱间的土壤相比,绿篱内的土壤物理性质有显著改善。乔木、草本和灌木绿篱内土壤孔隙度、含水量、饱和导水率、水稳性团聚体含量、抗侵蚀指数、抗冲刷指数和黏粒含量的平均值分别增加了18.8%、30.1%、12.9%、139.3%、108.3%、95.9%和25.5%,土壤容重和砂粒含量平均分别降低了17.3%和9.6%。三种绿篱内的土壤性质差异显著。乔木绿篱内的土壤抗冲刷指数最高;灌木绿篱内的土壤孔隙度、含水量、饱和导水率、抗冲刷指数、水稳性团聚体含量和黏粒含量均高于乔木和草本绿篱;而灌木绿篱内的土壤容重低于乔木和草本绿篱。由于三种绿篱系统不同位置绿篱对土壤物理性质的影响程度存在差异,绿篱内、前、后的陡坡以及绿篱间相关参数呈现出一定的水平变化。乔木绿篱土壤含水量、抗侵蚀指数、饱和导水率和黏粒含量的变异系数(CV)大于灌木和草本绿篱,而灌木绿篱土壤容重、孔隙度、水稳性团聚体含量和抗冲刷指数的CV大于乔木和草本绿篱。