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首页> 外文期刊>Journal of Hydrology >Temporal changes in hydraulic conductivity of sand porous media biofilters during wastewater infiltration due to biomat formation
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Temporal changes in hydraulic conductivity of sand porous media biofilters during wastewater infiltration due to biomat formation

机译:由于生物垫的形成,污水渗入过程中砂多孔介质生物滤池的水力传导率随时间变化

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Porous media biofilters (PMBs) are commonly used to treat domestic wastewater. Biomats develop at the infiltrative surface of PMBs due to continued wastewater application and create an impedance to flow. The goal of this research is to quantify the temporal evolution of normalized biomat hydraulic conductivity (K-bm/b(bm)) and effective hydraulic conductivity (K-e). K-e is the overall hydraulic conductivity of the infiltrative zone, including biomat and unsaturated media below the biomat. Research was conducted using eight one-dimensional (1D) sand columns with gravel-free and gravel-laden infiltrative surfaces. The columns were loaded at design rates of 100-200 cm/d for 20 weeks of column operation. The K, values for these continuously loaded columns were determined from analyses of bromide-tracer tests, falling-head permeability tests, and volumetric water content measurements during biomat development. The reduction in the K-e due to biomat formation is due to two factors: reduced hydraulic conductivity of the thin biomat, and a reduced hydraulic conductivity of the subsoil due to development of a biomatinduced unsaturated flow regime. Unsaturated hydraulic conductivities of the subsoil below the biomat (K-ss) were estimated from capillary curves and water content measurements. For observed final biomat thicknesses (less than I cm), the biomat hydraulic conductivity, K-bm, is three orders of magnitude smaller than the unsaturated hydraulic conductivity (K-ss). However, the relatively large thickness of the vadose zone causes the K-ss to be an important contributor to the overall K-e value. For these columns, the final Ke values were approximately two orders of magnitude smaller than the original value. Because the exact thickness of the biomat (b(bm)) is unknown during the flow experiments, the hydraulic conductance of the biomat zone is presented using a normalized hydraulic conductivity function (K-bm/b(bm)). A similar K-bm/b(bm) is reached regardless of wastewater loading rate. An exponential relationship exists between the volume of wastewater applied to the column and both K, and K-bm/b(bm). (c) 2005 Elsevier B.V. All rights reserved.
机译:多孔介质生物滤池(PMB)通常用于处理生活废水。由于持续不断的废水应用,生物垫在PMB的渗透表面上形成,并形成了流动阻力。这项研究的目的是量化归一化生物垫水力传导率(K-bm / b(bm))和有效水力传导率(K-e)的时间演变。 K-e是渗透区的总体水力传导率,包括生物垫和生物垫下面的非饱和介质。使用八个具有无砾石和充满砾石的渗透面的一维(1D)砂柱进行了研究。色谱柱以100-200 cm / d的设计速率装载,运行20周。这些连续加载的色谱柱的K值是由生物示踪剂分析过程中的溴化物示踪剂测试,落头渗透性测试和体积水含量测量确定的。由于生物垫形成而导致的K-e降低是由两个因素引起的:薄生物垫的水力传导率降低,以及由于生物垫诱导的不饱和流态的发展而使底土的水力传导率降低。根据毛细曲线和水含量测量值估算了生物垫层下的地下土壤的不饱和水导率(K-ss)。对于观察到的最终生物垫厚度(小于1 cm),生物垫水力传导率K-bm比不饱和水力传导率(K-ss)小三个数量级。但是,渗流区的相对较大的厚度使K-ss成为总体K-e值的重要因素。对于这些柱,最终的Ke值比原始值小大约两个数量级。由于在流动实验过程中生物垫的确切厚度(b(bm))是未知的,因此使用归一化的水力传导函数(K-bm / b(bm))表示生物垫区域的水力传导率。无论废水负荷率如何,均达到相似的K-bm / b(bm)。加在色谱柱上的废水量与K和K-bm / b(bm)之间都存在指数关系。 (c)2005 Elsevier B.V.保留所有权利。

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