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 AbstractElucidation of the calcineurin-Crz1 stress response transcriptional network in the human fungal pathogen Cryptococcus neoformans    Next AbstractAttraction responses of the American cockroach to synthetic periplanone-B »

Air Qual Atmos Health


Title:Mass reconstruction methods for PM(2.5): a review
Author(s):Chow JC; Lowenthal DH; Chen LW; Wang X; Watson JG;
Address:"Division of Atmospheric Sciences, Desert Research Institute, Reno, NV 89512 USA ; The State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi'an, Shaanxi 710075 China ; Graduate Faculty, University of Nevada, Reno, NV 89503 USA. Division of Atmospheric Sciences, Desert Research Institute, Reno, NV 89512 USA ; Graduate Faculty, University of Nevada, Reno, NV 89503 USA. Division of Atmospheric Sciences, Desert Research Institute, Reno, NV 89512 USA ; Department of Environmental and Occupational Health, University of Nevada, Las Vegas, NV 89154 USA"
Journal Title:Air Qual Atmos Health
Year:2015
Volume:20150507
Issue:3
Page Number:243 - 263
DOI: 10.1007/s11869-015-0338-3
ISSN/ISBN:1873-9318 (Print) 1873-9326 (Electronic) 1873-9318 (Linking)
Abstract:"Major components of suspended particulate matter (PM) are inorganic ions, organic matter (OM), elemental carbon (EC), geological minerals, salt, non-mineral elements, and water. Since oxygen (O) and hydrogen (H) are not directly measured in chemical speciation networks, more than ten weighting equations have been applied to account for their presence, thereby approximating gravimetric mass. Assumptions for these weights are not the same under all circumstances. OM is estimated from an organic carbon (OC) multiplier (f) that ranges from 1.4 to 1.8 in most studies, but f can be larger for highly polar compounds from biomass burning and secondary organic aerosols. The mineral content of fugitive dust is estimated from elemental markers, while the water-soluble content is accounted for as inorganic ions or salt. Part of the discrepancy between measured and reconstructed PM mass is due to the measurement process, including: (1) organic vapors adsorbed on quartz-fiber filters; (2) evaporation of volatile ammonium nitrate and OM between the weighed Teflon-membrane filter and the nylon-membrane and/or quartz-fiber filters on which ions and carbon are measured; and (3) liquid water retained on soluble constituents during filter weighing. The widely used IMPROVE equations were developed to characterize particle light extinction in U.S. national parks, and variants of this approach have been tested in a large variety of environments. Important factors for improving agreement between measured and reconstructed PM mass are the f multiplier for converting OC to OM and accounting for OC sampling artifacts"
Keywords:Chemical speciation Mass closure Organic matter Pm2.5 Sampling artifact;
Notes:"PubMed-not-MEDLINEChow, Judith C Lowenthal, Douglas H Chen, L-W Antony Wang, Xiaoliang Watson, John G eng Netherlands 2015/06/09 Air Qual Atmos Health. 2015; 8(3):243-263. doi: 10.1007/s11869-015-0338-3. Epub 2015 May 7"

 
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 05-12-2024