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曝气和混合在修复盐分层河流中的有效性。

Effectiveness of aeration and mixing in the remediation of a saline stratified river.

作者信息

Lamping Jens, Worrall Fred, Morgan Huw, Taylor Sam

机构信息

Department of Geological Sciences, University of Durham, Science Laboratories, South Road, Durham, DH1 3LE, UK.

出版信息

Environ Sci Technol. 2005 Sep 15;39(18):7269-78. doi: 10.1021/es040471b.

Abstract

This study examines the use of an aeration scheme to remediate low oxygen conditions in a saline stratified system. The Tawe estuary was impounded in 1992 and quickly developed saline stratification during the summer months which led to an anoxic hypolimnon. In 1998 trials began in which a suite of aerators was applied to remediate the water quality; the trial was later extended to a full aeration scheme. This study examines pre-aeration conditions in order to delineate conditions under which poor water quality would develop, and would therefore be the conditions when aeration would be necessary. Furthermore, the study compared identical periods within the impoundment during which the following conditions existed: no aeration; and aeration with first 44, then 88, aerators. The study shows that (i) destratification occurred naturally under flows of >10 m3/s, and no low dissolved oxygen conditions were observed at higher flows; (ii) the presence of all levels of aeration had a statistically significant effect upon dissolved oxygen (DO) levels; the effect of increasing the number of aerators was approximately linear; (iii) the average effect of aeration was an increase of up to 3 mg/L DO in the deepest water; (iv) the frequency of low DO conditions decreased from 19% to 3% with the operation of aerators; and (v) aeration is most effective during periods of no tidal incursion and further from the saline water source. This study is the first to demonstrate the effectiveness of aeration in a saline stratified system.

摘要

本研究考察了一种曝气方案在修复盐性分层系统中低氧状况方面的应用。陶伊河河口于1992年被蓄水,在夏季迅速形成了盐性分层,导致下层滞水层缺氧。1998年开始进行试验,应用了一套曝气装置来改善水质;该试验后来扩展为全面的曝气方案。本研究考察了曝气前的状况,以确定可能导致水质恶化的条件,而这些条件就是需要进行曝气的情况。此外,该研究比较了蓄水期间相同时间段内存在的以下条件:无曝气;以及分别使用44个和88个曝气器进行曝气的情况。研究表明:(i)当流量大于10立方米/秒时会自然发生分层消除,在较高流量下未观察到低溶解氧状况;(ii)各级曝气对溶解氧(DO)水平均有统计学上的显著影响;增加曝气器数量的影响大致呈线性;(iii)曝气的平均效果是使最深层水体中的溶解氧增加高达3毫克/升;(iv)随着曝气器的运行,低溶解氧状况的发生频率从19%降至3%;(v)在无潮汐入侵且远离咸水源头的时期,曝气最为有效。本研究首次证明了曝气在盐性分层系统中的有效性。

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