{"title":"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","authors":"K. Jóźwiak","doi":"10.5604/01.3001.0012.5048","DOIUrl":null,"url":null,"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 \nof 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 \nof 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.\n\n","PeriodicalId":321173,"journal":{"name":"Biuletyn Państwowego Instytutu Geologicznego","volume":"136 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2018-10-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"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\",\"authors\":\"K. Jóźwiak\",\"doi\":\"10.5604/01.3001.0012.5048\",\"DOIUrl\":null,\"url\":null,\"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 \\nof 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 \\nof 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.\\n\\n\",\"PeriodicalId\":321173,\"journal\":{\"name\":\"Biuletyn Państwowego Instytutu Geologicznego\",\"volume\":\"136 1\",\"pages\":\"0\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2018-10-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Biuletyn Państwowego Instytutu Geologicznego\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.5604/01.3001.0012.5048\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Biuletyn Państwowego Instytutu Geologicznego","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.5604/01.3001.0012.5048","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
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
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.