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 AbstractVolatiles of Grape Inoculated with Microorganisms: Modulation of Grapevine Moth Oviposition and Field Attraction    Next Abstract"Volatile organic compounds (VOCs) in air from Nisyros Island (Dodecanese Archipelago, Greece): Natural versus anthropogenic sources" »

Int J Mol Sci


Title:Origin and distribution of thiophenes and furans in gas discharges from active volcanoes and geothermal systems
Author(s):Tassi F; Montegrossi G; Capecchiacci F; Vaselli O;
Address:"Department of Earth Sciences, University of Florence, Italy. franco.tassi@unifi.it"
Journal Title:Int J Mol Sci
Year:2010
Volume:20100331
Issue:4
Page Number:1434 - 1457
DOI: 10.3390/ijms11041434
ISSN/ISBN:1422-0067 (Electronic) 1422-0067 (Linking)
Abstract:"The composition of non-methane organic volatile compounds (VOCs) determined in 139 thermal gas discharges from 18 different geothermal and volcanic systems in Italy and Latin America, consists of C(2)-C(20) species pertaining to the alkanes, alkenes, aromatics and O-, S- and N-bearing classes of compounds. Thiophenes and mono-aromatics, especially the methylated species, are strongly enriched in fluids emissions related to hydrothermal systems. Addition of hydrogen sulphide to dienes and electrophilic methylation involving halogenated radicals may be invoked for the formation of these species. On the contrary, the formation of furans, with the only exception of C(4)H(8)O, seems to be favoured at oxidizing conditions and relatively high temperatures, although mechanisms similar to those hypothesized for the production of thiophenes can be suggested. Such thermodynamic features are typical of fluid reservoirs feeding high-temperature thermal discharges of volcanoes characterised by strong degassing activity, which are likely affected by conspicuous contribution from a magmatic source. The composition of heteroaromatics in fluids naturally discharged from active volcanoes and geothermal areas can then be considered largely dependent on the interplay between hydrothermal vs. magmatic contributions. This implies that they can be used as useful geochemical tools to be successfully applied in both volcanic monitoring and geothermal prospection"
Keywords:"Carbon Dioxide/analysis Chromatography, Gas Furans/*chemistry Gases/*chemistry Hydrogen Sulfide/analysis Thiophenes/*chemistry Volatile Organic Compounds/analysis/chemistry Volcanic Eruptions/*analysis furans geothermal fluids heteroaromatics thiophenes v;"
Notes:"MedlineTassi, Franco Montegrossi, Giordano Capecchiacci, Francesco Vaselli, Orlando eng Research Support, Non-U.S. Gov't Switzerland 2010/05/19 Int J Mol Sci. 2010 Mar 31; 11(4):1434-57. doi: 10.3390/ijms11041434"

 
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 17-11-2024