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Wyszukujesz frazę "Janeczek, M." wg kryterium: Autor


Wyświetlanie 1-2 z 2
Tytuł:
Composition and source of polycyclic aromatic compounds in deposited dust from selected sites around the Upper Silesia, Poland
Autorzy:
Marynowski, L.
Pięta, M.
Janeczek, J.
Powiązania:
https://bibliotekanauki.pl/articles/2058768.pdf
Data publikacji:
2004
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
deposited dust
polycyclic aromatic hydrocarbons
oxygen derivatives of PAH
phenyl-polyaromatic hydrocarbons
polyphenyls
Opis:
About 300 polycyclic aromatic compounds were identified using the GC-MSmethod in deposited dust collected in sites located outside the industrial belt of the Upper Silesia agglomeration. Concentrations of selected polycyclic aromatic hydrocarbons (PAH) range from 6.8 mg/g dust for anthracene to 142 mg/g dust for fluoranthene. Concentrations of highly carcinogenic PAH e.g. benzo(a)pyrene, benzofluoranthenes and benzo(a)anthracene range from 49 to 145.5 mg/g of dust. Significant concentrations (up to 35 mg/g of dust) of carcinogenic C22H14 PAHs (m/z 278) and C24H14 PAHs (m/z 302) were determined in all samples. Aromatic ketones and quinones as well as aromatic nitrogen and sulphur compounds with concentrations ranging from 2 to 45 mg/g of dust, were found in the polar NSO fraction. Molecular composition of hydrocarbons in the deposited dust is characteristic of the terrestrial organicmatter, as suggested by the presence of long chain n-alkanes with odd carbon skeleton predominance. However, relatively high concentrations of steranes and distribution of homohopanes different from terrestrial organic matter suggest that part of extractable organic mattermay be from diesel engine exhausts and/or paved road dust. The origin of the organic compounds adsorbed on the deposited dust is related to not complete coal combustion and possibly to other sources, such as automobile exhaust. The occurrence of phenyl-polyaromatic hydrocarbons and polyphenyls such as terphenyls, phenylnaphthalenes and their methyl derivatives, phenylphenanthrenes, phenylfluoranthenes and/or phenylpyrenes results from the free radical phenylation of aromatics during organic matter combustion.
Źródło:
Geological Quarterly; 2004, 48, 2; 169--180
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Mineralogy and organic geochemistry of phyllite from the Dewon-Pokrzywna deposit, the Opava Mountains (SW Poland)
Autorzy:
Sawicka, N.
Janeczek, J.
Fabiańska, M.
Bahranowski, K.
Krzykawski, T.
Matuszewska, A.
Powiązania:
https://bibliotekanauki.pl/articles/2060078.pdf
Data publikacji:
2018
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
phyllite
chlorite
organic matter
Dewon Quarry
Polska
Opis:
Phyllites from the Dewon-Pokrzywna deposit in the Opava Mts., SW Poland, were investigated by XRD (Rietveld method), XRF, EPMA, SEM, and ATR-FTIR from the perspective of their potential usage as a buffer and/or backfill material in a geological repository of radioactive waste. Organic matter dispersed in the phyllite matrix was analysed by GC-MS. Fine-grained Mg-Fe-muscovite (13 to 29 wt.%), Fe-ripidolite (10 to 25 wt.%), detrital quartz (20 to 46 wt.%), and albite (7 to 28 wt.%) ± microcline, illite or illite/smectite, and kaolinite are major minerals in phyllite samples. The chlorite/muscovite ratio ranges from 0.65 to 1.1. Mg-annite inherited from the precursor rock is a minor constituent. Detrital ilmenite is a dominant accessory mineral. Ancylite-(Ce) occurs in quartz-calcite-ripidolite veins. Two types of phyllite have been distinguished based on the proportion of phyllosilicates to silt fraction: argillaceous (47 to 55 wt.% phyllosilicates) and silt-rich (28 wt.% phyllosilicates). Argillaceous phyllite shows elevated content of alumina and moderate concentration of silica. It is highly enriched in Fe compared to phyllites from other localities worldwide. The BET specific surface area of argillaceous phyllite ranges from 1.73 to 3.64 m2/g. Whole-rock chemical composition, mineral assemblages, chlorite geothermometry, and the occurrence of aliphatic hydrocarbons suggest that argillaceous phyllite originated from a pelagic pelite protolith under low-temperature (260-370°C) greenschist to subgreenschist facies conditions. Persistent biomarkers are indicative of bacterial degradation of planktonic organic matter suspended in a high water column. Enrichment in Fe-rich chlorite and Mg,Fe-muscovite, low volume of interconnected pores with dominant mesopores suggest that argillaceous phyllite from the Dewon-Pokrzywna deposit is a potential candidate for a buffer and/or backfill material.
Źródło:
Geological Quarterly; 2018, 62, 4; 817--828
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
    Wyświetlanie 1-2 z 2

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