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 AbstractDual herbivore attack and herbivore density affect metabolic profiles of Brassica nigra leaves    Next AbstractEvaluation of the separation characteristics of application-specific (volatile organic compounds) open-tubular columns for gas chromatography »

J Environ Monit


Title:Models for the adsorption of organic compounds at gas-water interfaces
Author(s):Poole CF;
Address:"Department of Chemistry, Wayne State University, Detroit, MI 48202, USA. cfp@chem.wayne.edu"
Journal Title:J Environ Monit
Year:2005
Volume:20050422
Issue:6
Page Number:577 - 580
DOI: 10.1039/b501776a
ISSN/ISBN:1464-0325 (Print) 1464-0325 (Linking)
Abstract:"The solvation parameter model is used to characterize interactions responsible for adsorption at the gas-water interface for bulk water at 15 and 25 degrees C, snow at -6.8 degrees C, mineral-supported water films (alumina, calcium carbonate and quartz) at 15 degrees C, and dry soil at 15 degrees C. The mineral-supported water films and dry soil adsorption data are modeled at different relative humidities in the range 40-99%. The models produce satisfactory results with standard errors of the estimate of 0.12 to 0.17 for regression of the model predicted adsorption equilibrium constants against the experimental values (range for equilibrium constants -2 to -7 log units). The water surface is polar with a significant capacity for dipole-type and hydrogen-bonding interactions. In addition, it is strongly electron lone pair repulsive. Dispersion interactions favor adsorption at the water surface. Mineral-supported water films at relative humidities greater than 40% demonstrate adsorption properties similar to bulk water. The adsorption characteristics, however, depend on the relative humidity and the nature of the support. In the case of dry soil the adsorption properties at different relative humidities cannot simply be explained by adsorption of a water film covering the soil surface and the changes in adsorption characteristics with relative humidity are more complex than the mineral-supported water films"
Keywords:"Adsorption Gases/*chemistry Humidity Mathematics Minerals/chemistry *Models, Chemical Organic Chemicals/*chemistry Volatilization Water/*chemistry;"
Notes:"MedlinePoole, Colin F eng England 2005/06/03 J Environ Monit. 2005 Jun; 7(6):577-80. doi: 10.1039/b501776a. Epub 2005 Apr 22"

 
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 05-11-2024