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Effect of Particle Size Distribution to Remove Contaminants in Groundwater at Dengkil, Selangor

机译:粒度分布在雪兰莪邓克尔地下水中去除地下水中的污染物的影响

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Particle size distribution (PSD) below ground may influence the groundwater flow rate. Due to that, this study focuses on laboratory scale using local alluvial soil to remove contaminants from river water using different of soil PSD samples. In horizontal permeability modelling shows permeability was influenced by the coefficient of uniformity (Cu) of sand. However, the permeability changes was differ between well and poorly graded sand. Well graded sands Cu between 4 to 5 the permeability changes are only between 7.8 – 7.9×10~(-4)m/s. Whereas poorly graded sands Cu are between 2.5 to 4 the permeability change between 6.9 – 9.0× 10~(-4) m/s. Whereas poorly graded sand was shows as consistent media than well graded to remove contaminants and the permeability rate is higher than well graded sand. Poorly graded (Sand B and C) removes turbidity and iron up to 50%. Because of that poorly graded soil is preferable for RBF application.
机译:地面以下的粒度分布(PSD)可能影响地下水流速。因此,本研究侧重于使用局部发生土壤的实验室规模,从而使用不同的土壤PSD样品从河水中除去污染物。在水平渗透性建模中,显示出渗透性受沙子均匀性系数(Cu)的影响。然而,良好且较差的沙子之间的渗透性变化有所不同。良好的碎砂铜4至5之间的渗透性变化仅在7.8-7.9×10〜(-4)m / s之间。虽然较差的砂岩Cu介于2.5至4之间,但渗透率变化在6.9-9.0×10〜( - 4)m / s之间。虽然较差的沙子被显示为一致的培养基,但渐变以除去污染物,并且渗透率高于良好的分级砂。分级差(砂B和C)去除浊度和熨斗高达50%。因为RBF申请优选较差的土壤。

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