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    盆地型喀斯特流域土壤侵蚀模数的沉积量测量法

    Calculation of the soil erosion modulus of basin with the measurement method of sedimentation in Karst area

    • 摘要: 为研究盆地型喀斯特石漠化地区的土壤侵蚀模数,运用沉积量测量法计算乌蒙山脉的麻窝山岩溶盆地中沉积区内土壤的沉积量,推算出流域内的土壤侵蚀模数,从而反演其石漠化进程,并探讨人类活动对喀斯特石漠化地区土壤侵蚀模数的影响。结果表明:麻窝山岩溶盆地流域的土壤侵蚀模数较高,为2900.55t/(km2.a),能客观地反映喀斯特石漠化山区土壤的侵蚀状况;沉积量测量法计算的土壤侵蚀模数比较接近现实,且其计算方法简单,数据可靠,容易操作,因此,该方法可作为无资料数据和测站时盆地型喀斯特流域计算土壤侵蚀模数的首选模型。

       

      Abstract: For studying the soil erosion modulus in the Karst rocky desertification areas,the measurement method of the sedimentation at the deposition zone of basin is used to calculate the soil erosion modulus and to speculate on the rocky desertification process of the Mawoshan of Wumeng range in the Karst area.The environmental effects on the soil erosion modulus,caused by human being's activities in Karst rocky desertification areas are discussed simultaneously.The research results indicate that the soil erosion modulus in the Mawoshan is very high,up to 2 900.55 t/(km2·a),which can reflect the position of the soil erosion objectively in the karst rocky desertification areas.Considering nothing but total quantity changes in the process of calculating the soil erosion modulus,the measurement method of the sedimentation at the deposition zone should be choiced firstly for the soil erosion calculation in the Karst rocky desertification areas where there is no observation data and survey station.

       

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