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 AbstractIdentification of volatile metabolites in human saliva from patients with oral squamous cell carcinoma via zeolite-based thin-film microextraction coupled with GC-MS    Next AbstractAdsorption of selected volatile organic vapors on multiwall carbon nanotubes »

Environ Toxicol Chem


Title:Distinctive sorption mechanisms of soil organic matter and mineral components as elucidated by organic vapor uptake kinetics
Author(s):Shih YH; Wu SC;
Address:"Department of Soil and Environmental Sciences, Center of Nanoscience and Nanotechnology, National Chung Hsing University, Taichung 402, Taiwan, Republic of China. yhs@nchu.edu.tw"
Journal Title:Environ Toxicol Chem
Year:2005
Volume:24
Issue:11
Page Number:2827 - 2832
DOI: 10.1897/05-186r.1
ISSN/ISBN:0730-7268 (Print) 0730-7268 (Linking)
Abstract:"Sorption kinetics and capacities of volatile organic compounds (VOCs) affect the remediation and fate of these pollutants in soils. The soil organic-mineral compositional heterogeneity complicates the transport and fate of VOCs in soils. The sorption kinetics of toluene vapor with two common soil components, kaolinite and humic acid, shows two distinct sorption patterns. Results with kaolinite are characteristic of surface adsorption, whereas results with humic acid are characteristic of solvation and partition effects. On soils, the kinetics of toluene vapor sorption show a two-stage sorption phenomenon. The first stage is reflective of surface adsorption (1-4 h to completion) and the second stage of much slower partitioning into soil organic matter, which was preceded by a lag phase (approximately 4 h) and took as long as 15 h for completion. The relative contributions of these two stages to soil uptake are quantifiable by two independent parameters, the soil organic fraction and the surface area. A better understanding of the effect of soil compositional heterogeneity on sorption kinetics and capacities facilitates our understanding of the prediction for the fate of organic contaminants in the environment"
Keywords:Kinetics Minerals/*chemistry Organic Chemicals/*chemistry Soil/*analysis Volatilization;
Notes:"MedlineShih, Yang-Hsin Wu, Shian-Chee eng Research Support, Non-U.S. Gov't 2006/01/10 Environ Toxicol Chem. 2005 Nov; 24(11):2827-32. doi: 10.1897/05-186r.1"

 
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 29-12-2024