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Book ChapterDOI

Fate of polynuclear aromatic compounds (PNAs) in soil-plant systems

TLDR
A polycyclic aromatic hydrocarbons (PAH) as discussed by the authors consist of three or more fused benzene rings in linear, angular, or cluster arrangements, which can be substituted by a variety of substituents.
Abstract
Polycyclic aromatic hydrocarbons (PAH) consist of three or more fused benzene rings in linear, angular, or cluster arrangements. Substitution of carbon in the benzene ring with nitrogen, sulfur, oxygen, or other elements creates heterocyclic aromatic compounds (Blumer 1976). Excluding diphenyl types there are some 70 possible isomers of 4-6 fused rings. Additionally these isomers may be substituted by a variety of substituents (Erskine and Whitehead 1975). The aromatic hydrocarbons and heterocycles, unsubstituted and substituted, are referred to alternatively as polynuclear aromatics (PNAs), polycyclic aromatic compounds (PCAs), and polycyclic organic matter (POM) (NAS 1972, U.S. EPA 1975 b).

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Citations
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Journal ArticleDOI

Synthesis of zirconia-immobilized copper chelates for catalytic decomposition of hydrogen peroxide and the oxidation of polycyclic aromatic hydrocarbons.

TL;DR: The most effective DTPMPA-based catalysts G-32 and G-35 caused almost complete decomposition of 15 ppm anthracene and benzo[a]pyrene during a five day catalytic cycle at 30 degrees C.
Journal ArticleDOI

Aliphatic and polycyclic aromatic hydrocarbons in surface seawater of the GULF of Trieste (northern ADRIATIC).

TL;DR: According to the presented results and compared to results from different areas worldwide, the seawater in the Gulf of Trieste can still be considered slightly to moderately polluted with PAHs.
Journal ArticleDOI

Adsorption and Desorption Kinetics of Pyrene onto a Great Lakes Sediment

TL;DR: In this article, the authors examined the kinetics of pyrene adsorption onto, and desorption from, a Great Lake sediment using two separate mathematical models: batch pore surface diffusion model and radial diffusion model.
Journal ArticleDOI

Benzo(a)pyrene degradation pathway in Bacillus subtilis BMT4i (MTCC 9447)

TL;DR: The identified metabolites indicated that BMT4i initially oxidized BaP with monooxygenases and dioxygenases at C-11,12 or and C-7,8 andC-9,10 positions, suggesting operation of multiple pathways for BaP degradation in B. subtilis.
Journal ArticleDOI

Mutagenicity of algal metabolites of benzo(a)pyrene for Salmonella typhimurium.

TL;DR: The metabolism and growth effects of benzo(a)pyrene (BaP) were studied using a freshwater green alga and the observed mutagenic response can be attributed in part to the presence of unmetabolized BaP or to BaP diols.
References
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Journal ArticleDOI

Sorption of hydrophobic pollutants on natural sediments

TL;DR: In this article, the authors investigated the sorption of hydrophobic compounds (aromatic hydrocarbons and chlorinated polycyclic aromatic compounds) spanning a concentration range in water solubility from 500 parts per trillion (ppt) to 1800 parts per million (ppm) on local pond and river sediments.
Journal ArticleDOI

Sorption of polynuclear aromatic hydrocarbons by sediments and soils

TL;DR: A highly significant negative correlation was observed between log substrate and log water solubility for these compounds and the equilibrium Freundlich constants and linear partition coefficients for each compound were highly correlated with the organic carbon content of the soils/sediments tested.
Journal ArticleDOI

Polycyclic aromatic hydrocarbons in the environment: homologous series in soils and recent marine sediments☆

TL;DR: In this article, it is suggested that polycyclic aromatic hydrocarbons are formed in natural fires, are dispersed and mixed by air transport and eventually deposited into surface sediments.
Journal ArticleDOI

Polycyclic Aromatic Compounds in Nature

Max Blumer
- 01 Mar 1976 - 
TL;DR: The great uniformity of composition and the nature of alkyl substituents suggest that most of the PAHs in the soil and in the sea-bed have been derived over eons from the fall-out of soot from forest and prairie fires, while the aromatic hydrocarbons of crude oil have been formed over millions of years from organic matter in sediments at 100 to 150 C.
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