对殖民地咖啡区不同类型的树荫的土壤上的饱和液压传导分析

Desy Annisa, Sugeng Prijono
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引用次数: 0

摘要

咖啡树是苏伯曼京魏坛地区小农广泛种植的人工林作物之一。咖啡农经常遇到的问题是气候导致的咖啡产量下降。气候变化的不利影响可以通过种植遮荫植物来缓解。土壤的饱和水力导电性被定义为水在多孔介质中处于饱和状态的运动。通过测量水导率,可以确定土壤的导水能力,看到水在土壤中的运动。在深度为0 ~ 20 cm的咖啡树中,sengon遮荫的饱和水导率在31.02 cm h -1时达到最大值。在20 ~ 40 cm深度,咖啡树的饱和水导率最高,为56.67 cm h -1,属于快类。咖啡田遮荫和土壤深度的差异会影响饱和导电性的值。土壤的几种物理性质与土壤的饱和水力导电性之间存在一定的关系。土壤的物理性质影响土壤的饱和导水率。
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ANALISIS KONDUKTIVITAS HIDROLIK JENUH TANAH PADA BERBAGAI JENIS NAUNGAN DI LAHAN KOPI RAKYAT KECAMATAN SUMBERMANJING WETAN
Coffee plants are one of the plantation crops that are widely cultivated by smallholders in Sumbermanjing Wetan District. The problem that is often experienced by coffee farmers is the decline in coffee production due to climate. The adverse effect of climate change can be overcome through mitigation by implementing shade plants. The saturated hydraulic conductivity of the soil is defined as the movement of water in a porous medium in a saturated state. By measuring hydraulic conductivity, it can determine the ability of the soil to conduct water and see the movement of water in the soil. The highest value of saturated hydraulic conductivity at a depth of 0-20 cm was found in coffee plants with sengon shade at 31.02 cm hour-1. The highest value of saturated hydraulic conductivity at a depth of 20-40 cm was found in coffee plants with the shade of Dadap plants, which was 56.67 cm hour-1, included in the fast category. Differences in shade and soil depth in coffee fields affect the value of the saturated hydraulic conductivity. There is a relationship between several physical properties of the soil and the saturated hydraulic conductivity of the soil. The physical properties of the soil affect the saturated hydraulic conductivity of the soil.
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