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Saturated Hydraulic Conductivity in a Tropical Alfisol in South-West Nigeria

机译:尼日利亚西南部热带铝镁溶胶中的饱和水力传导率

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This study presents the results of a comprehensive laboratory investigation program on the spatial variability of saturated hydraulic conductivity within a 44.3 ha twin-forested watershed at the International Institute for Tropical Agriculture (IITA) Ibadan in south-west Nigeria. The saturated conductivity was excessively rapid. In pre-clearing 2001, the mean saturated hydraulic conductivity ranged from 178 cm h 1 for 15-20 cm depth to 336 cm h 1 for 0-5 cm depth.The standard deviation was often equal to or even more than the average. In addition to high values, the variability in saturated conductivity was also very high amongst the 14 sub-watersheds. The high variability in hydraulic conductivity was due to the effects of pre-clearing vegetation, influence of roots and stumps, activity of soil fauna (earthworm and termites) and the size distribution and percent of gravel and coarse fraction present. Empirical relationships have been developed between the hydraulic parameters and the properties of fines particles.
机译:这项研究介绍了尼日利亚西南部国际热带农业研究所(IITA)伊巴丹44.3公顷双林流域内饱和水力传导率空间变异性的综合实验室调查计划的结果。饱和电导率过快。在2001年的清理前,平均饱和导水率范围从15-20 cm深度的178 cm h 1到0-5 cm深度的336 cm h 1。标准偏差通常等于或大于平均值。除了较高的值外,在14个子流域中,饱和电导率的变化也非常大。导水率的高度变化是由于预先清除了植被,根和树桩的影响,土壤动物(ear和白蚁)的活动以及存在的砾石和粗碎物的百分比以及百分比的影响。在水力参数和细颗粒的性质之间已经建立了经验关系。

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