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当前位置: 首页 > 文章 > 重庆四面山不同林地土壤颗粒特征及其与土壤侵蚀的关系 水土保持学报 2011,25 (5) 219-223
Position: Home > Articles > Soil Particles Characteristics and the Relationship Between Soil Particles and Soil Erosion in Different Forestlands in Simian Mountains,Chongqing Journal of Soil and Water Conservation 2011,25 (5) 219-223

重庆四面山不同林地土壤颗粒特征及其与土壤侵蚀的关系

作  者：
吴煜禾;张洪江;程金花;王伟;吕文星;杜士才;肖莉
单  位：
重庆市森林病虫防治检疫站;重庆市林业局;北京林业大学水土保持学院
关键词：
四面山;土壤颗粒;微团聚体;分形维数;土壤侵蚀
摘  要：
通过对重庆四面山的槲栎林、川柯林、柳杉林和毛竹林4种林地土壤颗粒状况的分析,探讨不同林地土壤颗粒特征及其与土壤侵蚀之间的关系。结果表明:除柳杉林以外,其他林地土壤均属于级配良好土壤,毛竹林表层土壤颗粒的分散度较低、偏度较大,土壤颗粒分布不均衡,土壤流失程度较高。不同林地土壤的微团聚体分形维数表现为川柯林40-60cm层最小,柳杉林0-20cm层最大,微团聚体分形维数与<0.001mm粒级微团聚体含量成正比,与0.25～0.05mm粒级微团聚体含量成反比。川柯林土壤团聚状况最高(19.38%),分散率最低(32.13%);柳杉林土壤团聚状况最低(10.88%),分散率最高(74.41%)。
译  名：
Soil Particles Characteristics and the Relationship Between Soil Particles and Soil Erosion in Different Forestlands in Simian Mountains,Chongqing
作  者：
WU Yu-he1,ZHANG Hong-jiang1,CHENG Jin-hua1,WANG Wei1,LV Wen-xing1,DU Shi-cai2,XIAO Li3(1.College of Soil and Water Conservation,Beijing Forestry University,Beijing 100083;2.Chongqing Forestry Bureau, Chongqing 401147;3.Chongqing Station of Forest Diseases and Pest Control and Quarantine,Chongqing 400015)
关键词：
Simian mountains;soil particles;micro-aggregates;fractal dimension;soil erosion
摘  要：
Through analysis of soil particles situation in 4 different forestlands of Quercus aliena,Lithocarpus fangii,Cryptomeria fortunei and Phyllostachys heterocycla cv.pubescens in Simian mountains in Chongqing,the relationship between different forestland soil particles characteristics and soil erosion was discussed.The results showed that most of the forestlands soil were good gradation soil except Cryptomeria fortunei.Phyllostachys heterocycla cv.pubescens forestland.Surface soil particles dispersion was lower and soil particles skewness was larger,so the soil particles were with unbalanced distribution and the extent of soil loss was higher.The fractal dimension of soil micro-aggregates structure of the 40-60 cm layer of Lithocarpus fangii forestland soil was the smallest and the 0-20 cm layer of Cryptomeria fortunei forestland soil was the largest;The fractal dimension of soil micro-aggregates was proportional to the <0.001 mm soil micro-aggregates content and inversely proportional to the 0.25~0.05 mm soil micro-aggregates content.Lithocarpus fangii forestland soil was with the highest aggregation condition(19.38%) and the lowest rate of divergence(32.13%),and Cryptomeria fortunei forestland soil was with the lowest aggregation condition(10.88%) and the highest rate of divergence(74.41%).

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