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西南喀斯特区不同土地利用梯田优先流定量分析

A Quantitative Analysis of Preferential Flow in Different Land Use Terraces in the Southwest Karst Region

  • 摘要: 为探明不同土地利用类型条件下优先流入渗的定量特征,以西南喀斯特地区梯田的园地、耕地和林地为研究对象,通过表置式环式入渗仪和亮蓝进行染色入渗试验,对梯田上不同土地利用类型的优先流和基质流进行了定量划分,并对其入渗速率和累积入渗量进行了对比研究。结果表明:(1)基质流是该地区梯田土壤入渗的主要部分。(2)在整个入渗过程中,园地和耕地的优先流渗透率都大于林地,达到稳定入渗时,耕地和园地的优先流入渗率分别是林地的1.87和1.80倍,累积入渗量是林地的1.2和1.3倍。(3)从染色渗透深度来看,耕地的优先流运动深度可达32.1 cm,明显大于园地(25.5 cm)和林地(15.7 cm),即与林地相比,园地和耕地具有更好的孔隙发育,优先流现象更明显。(4)不同土地利用方式的土壤质地显著影响优先流入渗率和入渗量的大小。研究结果可深化对西南喀斯特梯田入渗过程的认识,并对防控西南喀斯特地区水土流失具有一定指导意义。

     

    Abstract: In order to investigate the quantitative characteristics of priority infiltration under different land use types, this paper takes garden land, cultivated land and forest land of terraced fields in the southwest karst region as research objects, and carries out staining infiltration tests by means of a table-mounted ring infiltrator and bright blue to quantitatively classify the priority flow and matrix flow of different land use types on terraced fields, and conducts a comparative study on their infiltration rates and cumulative infiltration amounts. The results show that:(1) matrix flow is the main part of soil infiltration in the terraces in this area.(2) During the whole infiltration process, the infiltration rates of priority flow in both garden land and cultivated land are greater than those in forest land, and when stable infiltration is reached, the infiltration rates of priority flow in cultivated land and garden land are 1.87 and 1.80 times higher than those in forest land, respectively, and the cumulative infiltration number is 1.2 or 1.3 times higher than those in forest land.(3) In terms of staining infiltration depth, the preferential flow movement depth of arable land can reach 32.1 cm, which is significantly greater than that of garden land(25.5 cm) and forest land(15.7 cm), that is, compared with forest land, garden land and arable land have better pore development and the preferential flow phenomenon is more obvious.(4) The soil texture of different land uses significantly affects the priority inflow rate and the magnitude of infiltration.

     

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