翟子宁, 王克勤, 苏备, 张香群, 华锦欣, 朱晓婷. 松华坝水源区不同土地利用类型土壤可蚀性研究[J]. 西南林业大学学报, 2016, 36(5): 118-124. DOI: 10.11929/j.issn.2095-1914.2016.05.020
引用本文: 翟子宁, 王克勤, 苏备, 张香群, 华锦欣, 朱晓婷. 松华坝水源区不同土地利用类型土壤可蚀性研究[J]. 西南林业大学学报, 2016, 36(5): 118-124. DOI: 10.11929/j.issn.2095-1914.2016.05.020
Zhai Zining, Wang Keqin, Su Bei, Zhang Xiangqun, Hua Jinxin, Zhu Xiaoting. Study on Soil Erodibility of Different Land Utilization Styles in the Songhuaba Water Source Area[J]. Journal of Southwest Forestry University, 2016, 36(5): 118-124. DOI: 10.11929/j.issn.2095-1914.2016.05.020
Citation: Zhai Zining, Wang Keqin, Su Bei, Zhang Xiangqun, Hua Jinxin, Zhu Xiaoting. Study on Soil Erodibility of Different Land Utilization Styles in the Songhuaba Water Source Area[J]. Journal of Southwest Forestry University, 2016, 36(5): 118-124. DOI: 10.11929/j.issn.2095-1914.2016.05.020

松华坝水源区不同土地利用类型土壤可蚀性研究

Study on Soil Erodibility of Different Land Utilization Styles in the Songhuaba Water Source Area

  • 摘要: 为揭示松华坝水源区3种不同土地利用类型的土壤可蚀性状况,采用通用土壤流失方程计算研究区土壤可蚀性估算K值,并用EPIC公式计算研究区土壤可蚀性实测K值,探求实测K值与估算K值的相关性,利用实测K值对通用土壤流失方程进行修正。结果表明:该区域的土壤可蚀性实测K值主要分布在02866~03427;3种不同土地利用类型的土壤可蚀性实测K值大小顺序是裸地 > 坡耕地 > 灌木林地;可蚀性实测K值与粉粒呈极显著正相关,与粘粒和砂粒呈极显著负相关,与有机碳含量相关性不显著。

     

    Abstract: In order to reveal the condition of the soil erodibility in Songhuaba Water Source Area in Kumming City. Using the universal soil loss equation to calculate estimated K value of soil erdibility and EPIC model was used to calculate measured K value of soil erdibility of three different land utilization styles of songhuaba water source area. To explore the correlation between the measured K value and the estimated K value and based on the measured data to revised USLE. The measured K value of soils mainly ranged from 02866 to 03427. For measured K value of three different land utilization styles, the order was as follow: wasteland > farmland slope > shrub land. The Pearson correlation of the indicators of EPIC model showed that the correlation of soil erodibility K value with silts contents was obviously positive, but which showed obviously negative with sand contents and clay contents. Correlation of K value with organic carbon content was not significant.

     

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