Identification of In-Sewer Sources of Organic Solids Contributing to Combined Sewer Overflows
| Autor: | M. Ahyerre, G. Chebbo |
|---|---|
| Rok vydání: | 2002 |
| Předmět: |
Pollution
Paris Chemical Phenomena Rain media_common.quotation_subject Stormwater Waste Disposal Fluid Deposition (geology) Environmental Chemistry Organic matter Organic Chemicals Particle Size Water pollution Waste Management and Disposal Water Science and Technology media_common chemistry.chemical_classification Sewage Chemistry Physical Environmental engineering Sediment General Medicine chemistry Erosion Environmental science Combined sewer Environmental Monitoring |
| Zdroj: | Environmental Technology. 23:1063-1073 |
| ISSN: | 1479-487X 0959-3330 |
| DOI: | 10.1080/09593332308618353 |
| Popis: | Previous research has shown that combined sewer systems are the main source of particle and organic pollution during rainfall events contributing to combined sewer overflow. The aim of this article is to identify in an urban catchment area called "Le Marais", in the center of Paris, the types of sediments that are eroded and contribute to the pollution of combined sewer overflow. Three sediment types are considered: granular material found in the inverts of pipes, organic biofilms and organic sediment at the water bed interface, identified as an immobile layer in the "Le Marais" catchment area. The method used consist, firstly, of sampling and assessing the organic pollutant loads and metallic loads of the particles in each type of sediment. Then, the mass of each type of sediment is assessed. The mass and the characteristics of each type of sediment is finally compared to the mass and characteristics of the particles eroded in the catchment area, estimated by mass balances, in order to find the source of eroded particles. The only identified type of deposit that can contribute to combined sewer overflows is the organic layer. Indeed, the solids of this layer have mean and metallic loads that are of the same order of magnitude as the eroded particles. Moreover, the mass of the organic layer considered over different time scales is of the same order of magnitude as the eroded masses during rainfall events and an erosion experiment showed that the organic layer is actually eroded. |
| Databáze: | OpenAIRE |
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