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 AbstractSteric accessibility of the N-terminus improves the titer and quality of recombinant proteins secreted from Komagataella phaffii    Next Abstract"Olfactory-based discrimination learning in the moth, Manduca sexta" »

Environ Sci Technol


Title:Simulating the influence of snow on the fate of organic compounds
Author(s):Daly GL; Wania F;
Address:"Department of Physical and Environmental Sciences and Department of Chemistry, University of Toronto at Scarborough, 1265 Military Trail, Toronto, Ontario, Canada MIC 1A4"
Journal Title:Environ Sci Technol
Year:2004
Volume:38
Issue:15
Page Number:4176 - 4186
DOI: 10.1021/es035105r
ISSN/ISBN:0013-936X (Print) 0013-936X (Linking)
Abstract:"Snow scavenging, a seasonal snowpack, and a dynamic water balance are incorporated in a non-steady-state generic multimedia fate model in order to investigate the effect of snow on the magnitude and temporal variability of organic contaminant concentrations in various environmental media. Efficient scavenging of large nonpolar organic vapors and particle-bound organic chemicals by snow can lead to reduced wintertime air concentrations and incorporation in the snowpack. The snow cover functions as a temporary storage reservoir that releases contaminants accumulating over the winter during a short melt period, resulting in temporarily elevated concentrations in air, water, and soil. The intensity of these peaks increases with the length of the snow accumulation period. Organic chemicals of sufficient volatility (log KOA < 9; e.g., light polychlorinated biphenyls) can volatilize from the snowpack, resulting in springtime concentration maxima in the atmosphere. The behavior of fairly water-soluble chemicals during snowmelt depends on their relative affinity for the newly formed liquid water phase and the rapidly diminishing ice surface-quantitatively expressed by their interface-water partition coefficient (KIW). Chemicals with a preference for the dissolved phase (low KIW; e.g., pentachlorophenol) can become enriched in the first meltwater fractions and experience a temporary concentration peak in lakes and rivers. Organic chemicals that are neither volatile enough to evaporate from the snowpack nor sufficiently water soluble to dissolve in the meltwater (e.g., polybrominated diphenyl ethers) sorb to the particles in the snowpack. These particles may be sufficiently contaminated to constitute the major input route to the terrestrial environment upon release during snowmelt. Because wintertime deposition to the snowpack may be higher than to a non-snow covered surface, this can result in higher soil concentrations of persistent organic contaminants in the long term. The potential ecotoxicological significance of peak exposures demands a better understanding of the role of snow in the fate of organic contaminants"
Keywords:"Environmental Monitoring Environmental Pollutants/analysis Fresh Water/analysis/chemistry Models, Theoretical Octanols/chemistry Organic Chemicals/analysis/*chemistry Seasons *Snow Volatilization Water Movements;"
Notes:"MedlineDaly, Gillian L Wania, Frank eng Research Support, Non-U.S. Gov't 2004/09/09 Environ Sci Technol. 2004 Aug 1; 38(15):4176-86. doi: 10.1021/es035105r"

 
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 26-12-2024