首页> 中文期刊> 《绵阳师范学院学报 》 >四川盆地紫色土小流域土壤的可蚀性

四川盆地紫色土小流域土壤的可蚀性

             

摘要

In order to reveal the impacts of different patterns of land use and vegetation types on the purple soil erodibility,investigated and monitored the soil properties of surface soil(0-20cm) in forestry land,garden-plot and cultivated land of 3 typical agro-watersheds in purple soil region,and the values of soil erodibility K were calculated by using the EPIC model.Results show that the order of the K is SP4SP7SP5SP2SP6SP3SP1.the K value is lowly correlated with the total phosphorus,while others are significant,and even extremely significant.The correlation of K values and impact-factors is TOCSANSIL=CLA TNTP.Thus,the principal countermeasures to improve soil anti-erodibility for the purple soil are to improve the organic matter,reduce the quantity of chemical fertilizer,promote soil-aggregate formation,and increase aggregate ratio.%为揭示不同土地利用方式和植被类型对紫色土壤可蚀性的影响,调查和测试了紫色土丘陵区3个典型小流域内林地、园地和旱耕地的表层土壤(0-20 cm)的理化性质,并利用EPIC公式计算了土壤可蚀性K值,结果表明:样地表层土壤(0-20 cm)可蚀性K值大小顺序依次是:SP4〉SP7〉SP5〉SP2〉SP6〉SP3〉SP1;除全磷与K值相关性较小外,K值与其他影响因子达到了显著(极显著)相关;K值与各影响因子之间的相关程度:有机碳〉砂粒〉粉粒=黏粒〉全氮〉全磷。因此,提高有机碳含量,降低化肥的使用量,促进土壤团聚体形成,增加团聚度,是增加紫色土抗蚀性能的重要途径。

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