Bedoukian   RussellIPM   RussellIPM   Piezoelectric Micro-Sprayer


Home
Animal Taxa
Plant Taxa
Semiochemicals
Floral Compounds
Semiochemical Detail
Semiochemicals & Taxa
Synthesis
Control
Invasive spp.
References

Abstract

Guide

Alphascents
Pherobio
InsectScience
E-Econex
Counterpart-Semiochemicals
Print
Email to a Friend
Kindly Donate for The Pherobase

« Previous AbstractHalocarbons produced by natural oxidation processes during degradation of organic matter    Next AbstractFormation of volatile iodinated alkanes in soil: results from laboratory studies »

Environ Sci Technol


Title:Natural formation of vinyl chloride in the terrestrial environment
Author(s):Keppler F; Borchers R; Pracht J; Rheinberger S; Scholer HF;
Address:"Institute of Environmental Geochemistry, Heidelberg University, Germany. fkeppler@ix.urz.uni-heidelberg.de"
Journal Title:Environ Sci Technol
Year:2002
Volume:36
Issue:11
Page Number:2479 - 2483
DOI: 10.1021/es015611l
ISSN/ISBN:0013-936X (Print) 0013-936X (Linking)
Abstract:"Vinyl chloride is a highly reactive and toxic substance which is widely used in industry. It is the parent compound of poly(vinyl chloride) (PVC), one of the most important industrial polymers. Until now, it was thought that vinyl chloride found in the environment is exclusively man-made or results from the degradation of other anthropogenic substances, such as trichloroethylene and tetrachloroethylene. Here, we demonstrate that vinyl chloride also has natural sources. Soil air and ambient air from a rural area in Northern Germany were investigated for volatile chlorinated halocarbons. The concentrations of vinyl chloride in the soil air were significantly enhanced as compared to ambient air, indicating a natural formation of this compound in the soil. A series of laboratory experiments using different soils and model compounds was conducted, which clearly proved that vinyl chloride could be produced during soil processes. We propose that this highly reactive compound can be formed during the oxidative degradation of organic matter in soil, for example, in a reaction between humic substances, chloride ions and an oxidant (ferric ions or hydroxyl radicals). The redox-sensitive aromatic compounds in soil such as catechols and o-quinones can be degraded to CO2, accompanied by the release of vinyl chloride and other volatile chlorinated compounds. This process could have started in the Late Silurian to Early Devonian, 400 million years ago, when the first soils on earth evolved"
Keywords:"Carbon Dioxide Carcinogens/*chemistry Humic Substances/chemistry *Models, Theoretical Organic Chemicals Oxidation-Reduction Soil Pollutants/*analysis Vinyl Chloride/*chemistry Volatilization;"
Notes:"MedlineKeppler, Frank Borchers, Reinhard Pracht, Jens Rheinberger, Stefan Scholer, Heinz F eng Research Support, Non-U.S. Gov't 2002/06/22 Environ Sci Technol. 2002 Jun 1; 36(11):2479-83. doi: 10.1021/es015611l"

 
Back to top
 
Citation: El-Sayed AM 2024. The Pherobase: Database of Pheromones and Semiochemicals. <http://www.pherobase.com>.
© 2003-2024 The Pherobase - Extensive Database of Pheromones and Semiochemicals. Ashraf M. El-Sayed.
Page created on 27-12-2024