碎石入口系统在低堆积条件下的过滤能力

A. Ranaivoson, J. Moncrief
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引用次数: 0

摘要

将过滤模型应用于砾石入口系统,以估计颗粒在收集器(砾石颗粒)上的附着和/或脱离。采用质量浓度和颗粒数两种方法来估计砾石入口的固体捆扎效率。第一种方法基于两次平均计算提供了11%到22%的捕获估计。第二种方法(颗粒计数)表明,总固体分离主要发生在粘土粒径类别中,并且在降雨事件发生的早期。分离显示出水的质量,可以解释为颗粒从以前的总固体沉积物中分离出来或未被收集器保留。根据Rajagopalan和Tien的模型,对于小于100 μm的颗粒和团聚体,碎石入口的捕获能力相对较低(<50%)。对2002年5次降雨事件进行了分析,结果表明,第一次降雨事件的截留能力为32%,对砾石“上”和“下”的样品进行了配对t检验,差异有统计学意义。根据相同的统计检验,以下降雨事件在以上和以下水样之间没有显着差异;然而,成对样品的滞留模式表明,大过滤值与进入的大固体浓度有关,而大固体浓度又与降雨爆发有关。激光衍射技术允许用颗粒计数法来估计相对于砾石介质保留或分离的颗粒数量。在细粉粒和粘土粒区,通过直接测量获得颗粒数;在粉砂粒区,通过外推测量数据(包括小颗粒和团聚体)获得大颗粒数。基于粒子计数方法,8月3日和8月21日两个降雨事件表现出重要的分离。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Filtration capacity of a gravel inlet system under low accumulation conditions
Filtration models were applied to a gravel inlet system to estimate attachment and/or detachment of particles onto collectors (gravel grain). Two methods were used to estimate total solidstrapping efficiency at the gravel inlet: mass concentration and particle count. The first method provided trapping estimate between 11% and 22% based on two averaging computations. The second method, particle count, showed that detachment of total solids occurred mostly with the clay size category and early duringrainfall events. Detachment reveals the quality of effluent and can be interpreted as particles being detached either from previous total solids deposit or not being retained by the collector. Based on a model by Rajagopalan and Tien, trapping ability of gravel inlet was expected to be relatively low (<50%) for particles and aggregates smaller than 100 μm. Five rainfall events in 2002 were analyzed and showed that the first event had a retention capacity of 32% with a significant statistical difference between pairs of samples from “above” and “below” the gravel, based on a paired t-test. The following rainfall events had not seen any significant difference based on the same statistical test between the above and below water samples; however, the pattern of retention within pairs of samples showed that large filtration values were associated with incoming large solids concentrations, which, in turn, are related to rainfall bursts. The laser diffractometer technique allowed the particle count method to estimate number of particles retained or detached with respect to the gravel media. Particle count was obtained by direct measurement in the fine silt and clay size region and by extrapolation of measured data for large size in the silt-sand region including small particles and aggregates. Two rainfall events (August 3 and 21) showed important detachment based on particle counting method.
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