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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

Biodegradation of high-molecular-weight polycyclic aromatic hydrocarbons by bacteria.

TL;DR: Interest in the biodegradation mechanisms and environmental fate of polycyclic aromatic hydrocarbons is prompted by their ubiquitous distribution and their potentially deleterious effects on human health.
Journal ArticleDOI

Bioremediation of high molecular weight polycyclic aromatic hydrocarbons: a review of the microbial degradation of benzo[a]pyrene.

TL;DR: The focuss of this review is on the high molecular weight PAH benzo[a]pyrene (BaP), which has been observed to accumulate in marine organisms and plants which could indirectly cause human exposure through food consumption.
Journal ArticleDOI

Biodegradation of polycyclic aromatic hydrocarbons

TL;DR: The intent of this review is to provide an outline of the microbial degradation of polycyclic aromatic hydrocarbons, a catabolically diverse microbial community, consisting of bacteria, fungi and algae, metabolizes aromatic compounds.
Journal ArticleDOI

Bioremediation of soil contaminated with polynuclear aromatic hydrocarbons (PAHs): A review

TL;DR: The bioremediation of contaminated soils with in-situ, on-site, and bioreactor techniques is reviewed, together with the factors affecting PAH degradation.
Journal ArticleDOI

Polynuclear aromatic hydrocarbons in the United Kingdom environment: a preliminary source inventory and budget.

TL;DR: There is good evidence to suggest that air concentrations and fluxes to the UK surface are now lower than at any time throughout this century, but the UK sigmaPAH burden is still increasing at the present time, principally through retention by soils.
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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