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土壤-含水层处理过程中有机物的归宿:现场去除的可持续性

Fate of organics during soil-aquifer treatment: sustainability of removals in the field.

作者信息

Quanrud David M, Hafer Jennifer, Karpiscak Martin M, Zhang Jianmin, Lansey Kevin E, Arnold Robert G

机构信息

Department of Civil Engineering and Engineering Mechanics, The University of Arizona, Tucson, AZ 85721, USA.

出版信息

Water Res. 2003 Aug;37(14):3401-11. doi: 10.1016/S0043-1354(02)00489-X.

Abstract

A 5-year program of study was conducted at the Sweetwater Recharge Facilities (SRF) to assess the performance of surface spreading operations for organics attenuation during field-scale soil-aquifer treatment (SAT) of municipal wastewater. Studies were conducted utilizing both mature (approximately 10 yr old) and new infiltration basins. Removals of dissolved organic carbon (DOC) were robust, averaging >90 percent during percolation through the local 37-m vadose zone. The hydrophilic (most polar) fraction of DOC was preferentially removed during SAT; removals were attributed primarily to biodegradation. Reductions in trihalomethane formation potential (THMFP) averaged 91 percent across the vadose zone profile. The reactivity (specific THMFP) of post-SAT organic residuals with chlorine decreased slightly from pre-SAT levels (60 vs. 72 microg THM per mg DOC, respectively). Variations in the duration of wetting/drying periods did not significantly impact organic removal efficiencies.

摘要

在斯威特沃特回灌设施(SRF)开展了一项为期5年的研究项目,以评估城市污水进行现场规模土壤-含水层处理(SAT)期间,地表漫流操作对有机物衰减的性能。研究使用了成熟(约10年历史)和新建的渗滤池。溶解有机碳(DOC)的去除效果显著,在通过当地37米厚的包气带渗流过程中,平均去除率>90%。SAT过程中,DOC的亲水性(极性最强)部分被优先去除;去除主要归因于生物降解。整个包气带剖面中,三卤甲烷生成势(THMFP)的降低平均为91%。SAT后有机残余物与氯的反应性(特定THMFP)比SAT前水平略有下降(分别为每毫克DOC 60微克与72微克三卤甲烷)。湿润/干燥周期持续时间的变化对有机物去除效率没有显著影响。

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