THE EFFECTS OF MIXING UNDERGROUND AND SURFACE WATER IN THE CONDITIONS OF WATER DISCHARGE FROM THE EXCAVATION DRAINAGE – CASE STUDY OF THE POTOK SŁUŻEWIECKI IN WARSAW

K. Jóźwiak
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Abstract

The paper presents a typical problem for agglomeration areas, i.e. the discharge of drainage water from the excavation pit to the watercourse. In case of the Potok Służewiecki, the most important problem is a significant difference in the chemical composition of surface and groundwater. An important part of the Potok Służewiecki water originates from polluted water discharged from rainwater sewage collectors. Discharged groundwater is mostly categorized as the quality class II, but significant concentrations of Fe and Mn reduce its categorization to quality class III. In order to determine the extent of changes in the chemical composition of the Potok Służewiecki water due to water mixing process, geochemical modelling in various quantitative ratios was carried out. Obtained results show lowering of the pH and almost complete transition of all Fe speciations into the Fe3+ form, regardless of the mixing ration of ground and surface water. This implies the appearance of coloured water in the Potok Służewiecki. Therefore, assuming the use of additional aeration measures, the oxygen amount needed for complete removal of iron from groundwater before its discharge to the Potok Służewiecki was calculated. Possible impact of the Potok Służewiecki on the rock matrix before and after mixing with discharge water was also presented in the article.
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地下水和地表水混合在开挖排水条件下的影响——以华沙potok sŁuŻewiecki为例
本文提出了堆积区的一个典型问题,即基坑排水向河道的排放问题。就Potok Służewiecki而言,最重要的问题是地表水和地下水化学成分的显著差异。Potok Służewiecki水的重要组成部分来自雨水污水收集器排放的污水。排放的地下水大多属于二类水质,但铁和锰的显著浓度降低了其分类为三类水质。为了确定Potok Służewiecki水体在水混合过程中化学成分变化的程度,开展了不同定量比例的地球化学模拟。所得结果表明,无论地下水和地表水的混合比例如何,pH值都降低,所有铁形态几乎完全转变为Fe3+形态。这意味着Potok中彩色水的出现Służewiecki。因此,假设使用额外的曝气措施,计算了地下水中铁在排放到Potok Służewiecki之前完全去除所需的氧气量。本文还介绍了Potok Służewiecki与排放水混合前后对岩石基质可能产生的影响。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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ZŁOTO W POTOKACH I PEGMATYCIE Z REJONU STRZELINA ROZPOZNANIE LOKALIZACJI WYROBISK PIASKÓW I ŻWIRÓW WZGLĘDEM GRANIC GZWP ORAZ CIEKÓW POWIERZCHNIOWYCH NA OBSZARZE WOJEWÓDZTWA ŚLĄSKIEGO INTERPRETACJA ZMIENNOŚCI TEMPERATURY WODY W ŹRÓDLE NA WSCHODNIM STOKU ZAMECZKÓW (TATRY ZACHODNIE) NA PODSTAWIE CIĄGŁYCH OBSERWACJI MONITORINGOWYCH I NUMERYCZNEGO MODELU TRANSPORTU CIEPŁA PARAMETRY MIGRACJI ZANIECZYSZCZEŃ W ODPADACH FLOTACYJNYCH NA PODSTAWIE TERENOWEGO EKSPERYMENTU ZNACZNIKOWEGO NA PRZYKŁADZIE OBIEKTU UNIESZKODLIWIANIA ODPADÓW WYDOBYWCZYCH „GILÓW” ZRÓŻNICOWANIE TŁA HYDROGEOCHEMICZNEGO WÓD PODZIEMNYCH EKSPLOATOWANYCH W ZLEWNI BIEBRZY
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