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 AbstractRetrofitting existing chemical scrubbers to biotrickling filters for H2S emission control    Next AbstractQueen succession in the Indian paper wasp Ropalidia marginata: On the trail of the potential queen »

Environ Geochem Health


Title:Principal biogeochemical factors affecting the speciation and transport of mercury through the terrestrial environment
Author(s):Gabriel MC; Williamson DG;
Address:"Department of Civil and Environmental Engineering, The University of Alabama, 260 MIB 7th Avenue and Campus Drive, Tuscaloosa, AL 35487-0205, USA"
Journal Title:Environ Geochem Health
Year:2004
Volume:26
Issue:4
Page Number:421 - 434
DOI: 10.1007/s10653-004-1308-0
ISSN/ISBN:0269-4042 (Print) 0269-4042 (Linking)
Abstract:"It is increasingly becoming known that mercury transport and speciation in the terrestrial environment play major roles in methyl-mercury bioaccumulation potential in surface water. This review discusses the principal biogeochemical reactions affecting the transport and speciation of mercury in the terrestrial watershed. The issues presented are mercury-ligand formation, mercury adsorption/desorption, and elemental mercury reduction and volatilization. In terrestrial environments, OH-, Cl- and S- ions have the largest influence on ligand formation. Under oxidized surface soil conditions Hg(OH)2, HgCl2, HgOH+, HgS, and Hg0 are the predominant inorganic mercury forms. In reduced environments, common mercury forms are HgSH+, HgOHSH, and HgClSH. Many of these mercury forms are further bound to organic and inorganic ligands. Mercury adsorption to mineral and organic surfaces is mainly dictated by two factors: pH and dissolved ions. An increase in Cl- concentration and a decrease in pH can, together or separately, decrease mercury adsorption. Clay and organic soils have the highest capability of adsorbing mercury. Important parameters that increase abiotic inorganic mercury reduction are availability of electron donors, low redox potential, and sunlight intensity. Primary factors that increase volatilization are soil permeability and temperature. A decrease in mercury adsorption and an increase in soil moisture will also increase volatilization. The effect of climate on biogeochemical reactions in the terrestrial watershed indicates mercury speciation and transport to receiving water will vary on a regional basis"
Keywords:Adsorption Biological Availability Geological Phenomena Geology Humans Mercury/*chemistry/*metabolism Methylmercury Compounds/*chemistry/*metabolism Organic Chemicals Soil Pollutants/*metabolism Solubility Volatilization Water Pollutants/*metabolism;
Notes:"MedlineGabriel, Mark C Williamson, Derek G eng Review Netherlands 2005/02/19 Environ Geochem Health. 2004 Dec; 26(4):421-34. doi: 10.1007/s10653-004-1308-0"

 
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 23-11-2024