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Transport and solubility of Hetero-disperse dry deposition particulate matter subject to urban source area rainfall–runoff processes

机译:受城市源区降雨径流过程影响的杂散干沉降颗粒物的迁移和溶解度

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With respect to hydrologic processes, the impervious pavement interface significantly alters relationships between rainfall and runoff. Commensurate with alteration of hydrologic processes the pavement also facilitates transport and solubility of dry deposition particulate matter (PM) in runoff. This study examines dry depositional flux rates, granulometric modification by runoff transport, as well as generation of total dissolved solids (TDS), alkalinity and conductivity in source area runoff resulting from PM solubility. PM is collected from a paved source area transportation corridor (I-10) in Baton Rouge, Louisiana encompassing 17 dry deposition and 8 runoff events. The mass-based granulometric particle size distribution (PSD) is measured and modeled through a cumulative gamma function, while PM surface area distributions across the PSD follow a log-normal distribution. Dry deposition flux rates are modeled as separate first-order exponential functions of previous dry hours (PDH) for PM and suspended, settleable and sediment fractions. When trans-located from dry deposition into runoff, PSDs are modified, with a d50m decreasing from 331 to 14 lm after transport and 60 min of settling. Solubility experiments as a function of pH, contact time and particle size using source area rainfall generate constitutive models to reproduce pH, alkalinity, TDS and alkalinity for historical events. Equilibrium pH, alkalinity and TDS are strongly influenced by particle size and contact times. The constitutive leaching models are combined with measured PSDs from a series of rainfall–runoff events to demonstrate that the model results replicate alkalinity and TDS in runoff from the subject watershed. Results illustrate the granulometry of dry deposition PM, modification of PSDs along the drainage pathway, and the role of PM solubility for generation of TDS, alkalinity and conductivity in urban source area rainfall–runoff.
机译:关于水文过程,不透水的人行界面显着改变了降雨与径流之间的关系。与水文过程的变化相对应,路面还有助于径流中干沉降颗粒物(PM)的运输和溶解性。这项研究检查了干沉降通量率,通过径流传输进行的粒度修改以及源于PM溶解度的源区径流中总溶解固体(TDS)的生成,碱度和电导率。颗粒物是从路易斯安那州巴吞鲁日的一条铺装的源区运输走廊(I-10)收集的,涵盖了17次干沉降和8次径流事件。通过累积伽马函数对基于质量的粒度分布(PSD)进行测量和建模,而整个PSD的PM表面积分布遵循对数正态分布。干沉降通量速率被建模为PM和悬浮,可沉降和沉积物部分的先前干时(PDH)的单独一阶指数函数。当从干沉降转移到径流时,对PSD进行了修改,运输和沉降60分钟后d50m从331 lm减小到14 lm。利用源区降雨,溶解度实验随pH,接触时间和粒径的变化而生成本构模型,以再现历史事件的pH,碱度,TDS和碱度。平衡pH,碱度和TDS受到粒径和接触时间的强烈影响。本构性淋洗模型与一系列降雨-径流事件的测得的PSDs结合在一起,证明了该模型的结果可复制目标流域径流中的碱度和TDS。结果说明了干沉降颗粒物的粒度,沿排水路径的PSD修饰以及颗粒物溶解度对TDS生成,碱度和电导率在城市源区降雨径流中的作用。

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