Pregled bibliografske jedinice broj: 811462
Magnetic tracing of coal slag and ash in a river basin
Magnetic tracing of coal slag and ash in a river basin // Geophysical Research Abstracts, Vol. 18 / EGU (ur.).
Beč: European Geosciences Union (EGU), 2016. str. 8475-8475 (poster, međunarodna recenzija, sažetak, znanstveni)
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Naslov
Magnetic tracing of coal slag and ash in a river basin
Autori
Appel, Erwin ; Frančišković-Bilinski, Stanislav ; Zhang, Qi ; Rösler, Wolfgang ; Zhao, Qian
Vrsta, podvrsta i kategorija rada
Sažeci sa skupova, sažetak, znanstveni
Izvornik
Geophysical Research Abstracts, Vol. 18
/ EGU - Beč : European Geosciences Union (EGU), 2016, 8475-8475
Skup
EGU 2016 - European Geosciences Union General Assembly 2016
Mjesto i datum
Beč, Austrija, 17.04.2016. - 22.04.2016
Vrsta sudjelovanja
Poster
Vrsta recenzije
Međunarodna recenzija
Ključne riječi
Mrežnica River (Croatia); aquatic transport of pollutants; magnetic ash and slag; magnetic tracing in a river system
Sažetak
Atmospheric distribution of pollutants by magnetic means has been extensively studied, but only little is known about pollution-related magnetic signatures for aquatic transport. The case of a textile factory in Croatia that released heavy-metal polluted and highly magnetic ash and slag material from coal burning into Mrežnica River for 110 years (1884-1994) represents an ideal target for studying principles of magnetic tracing through a river system. Samples from the riverside close to the factory show high concentrations of magnetite (mass-specific susceptibility 1-4 x105 m3kg1) with low frequency dependence (fd% <3%). However, quantitative detection of slag and ash transport in the downstream direction through the riverbed is hindered by extremely variable magnetic properties of the river sediments, presumably due to hydrodynamic sorting. Surface mapping of on riverbanks 3 km downstream of the factory reveals clear evidence for substantial distribution of slag and ash materials in the river basin due to flooding ; the affected area reaches to >100 m from the riverside. The spatial pattern of shallow vertical sections of (surface to 0.5 m depth) shows different layers of coal burning residues which may even allow discriminating different flooding events (historical flooding). In order to assess the possible influence of fly ash from the factory, we studied vertical soil profiles at locations which cannot be reached by floods. These (red) soils, formed on limestones, are strongly magnetic ( >106 m3kg1). Despite this strong natural magnetic signals, the depth dependence of fd% and characteristic chemical properties (sulfur content, Ni/Cu ratio) as well as the dependence of the vertical distribution with distance to the point source indicate a contribution of fly ash to soil contamination near the factory (within about one kilometer). The presently available results indicate that with a strong magnetic point source as in the case of the studied textile factory, magnetic tracing can contribute important information on the transport and mass balance of sediments in a river basin.
Izvorni jezik
Engleski
Znanstvena područja
Geologija
POVEZANOST RADA
Projekti:
098-0982934-2720 - Međudjelovanja oblika tragova metala u vodenom okolišu (Pižeta, Ivanka, MZOS ) ( CroRIS)
Ustanove:
Institut "Ruđer Bošković", Zagreb