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Tree water uptake on suction distribution in unsaturated tropical residual soil slope

机译:非饱和热带残土边坡树木吸水对吸力分布的影响。

摘要

This study provides an investigation of active root tree zone located at the toe of a slope. This section and its vicinity generated matric suction due to tree wateruduptake on tropical residual soil slope. The research employed several approaches i.e field monitoring, laboratory experimental and numerical modelling. A fieldudmonitoring was carried out to collect matric suction data at the slope with two conditions; in absence of a tree and with a tree located at the toe of a slope. Theudunsaturated shear strength behaviour of soil under different stress level is investigated, using uncomplicated testing procedure subject to actual matric suction encountered during field monitoring. The numerical simulation modelling was applied based on the laboratory results to obtain the most appropriate condition to replicate the tree water uptake within the soil slope. A decrease in matric suction occured after a long duration of intense rainfall. This condition was function as an initial condition before the water uptake driven by active root tree generated to the maximum matric suction (low moisture content). The pattern of matric suction profiles revealed that majority of matric suction changes was greater at the proximity of tree trunk below 4 in and at a shallow depth of 0.5 m. Transpiration on single mature tree has significantly altered the matric suction or moisture variationuddistribution on an unsaturated soil slope. This study also illustrated the nonlinear relationship between the apparent shear strength and suction influencing the stability of the slope. The assessment of slope stability due to the influence of a tree induced suction was provided in this research. The factor of safety against slope failure has improved up to 63 % on slope with tree at toe compared to a slope without tree. Lastly, the numerical simulation modelling of matric suction induced by a tree has been verified through comparison to actual field monitoring results recorded during the dry period. Generally, an acceptable aggrement between simulation and field monitoring results has been achieved. This research delivers a strong belief that a preserved mature tree can improve soil properties in slopes designs.
机译:这项研究提供了对位于坡脚趾处的活动根树区域的调查。该断面及其附近区域由于热带残留土壤边坡上的树木水吸收而产生基质吸力。该研究采用了几种方法,即现场监测,实验室实验和数值建模。进行现场监测以收集两种情况下斜坡上的基质吸力数据。没有树木并且树木位于斜坡的脚趾处。使用简单的测试程序,根据现场监测过程中遇到的实际基质吸力,研究了在不同应力水平下土壤的不饱和抗剪强度行为。根据实验室结果,采用了数值模拟模型,以获得最合适的条件来复制土壤坡度内树木的水分吸收。长时间的强降雨后,基质吸力降低。该条件作为初始条件发挥作用,然后由主动根树驱动的吸水量产生最大的基质吸力(低水分含量)。基质吸力剖面图显示,在4英寸以下的树干附近和0.5 m的浅层深度处,大多数基质吸力变化较大。单个成熟树上的蒸腾作用显着改变了非饱和土壤坡面的基质吸力或水分变化 ud分布。这项研究还说明了表观抗剪强度与吸力之间的非线性关系,从而影响了边坡的稳定性。这项研究提供了对因树木引起的吸力影响而引起的边坡稳定性的评估。与没有树木的斜坡相比,有树木的脚趾的斜坡的安全系数提高了63%。最后,通过与干旱期间记录的实际现场监测结果进行比较,验证了树木引起的基质吸力的数值模拟模型。通常,已经获得了模拟和现场监视结果之间的可接受的增加。这项研究坚信,保存成熟的树木可以改善边坡设计中的土壤特性。

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  • 作者

    Mohd Fakhrurrazi Ishak;

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  • 年度 2014
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