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 Abstract"Assessment of a regulatory model's performance relative to large spatial heterogeneity in observed ozone in Houston, Texas"    Next AbstractEffect of the continuous addition of ozone on biomass clogging control in a biofilter treating ethyl acetate vapors »

Environ Chem


Title:Houston's rapid ozone increases: preconditions and geographic origins
Author(s):Couzo E; Jeffries HE; Vizuete W;
Address:"University of North Carolina, Gillings School of Global Public Health, Chapel Hill, NC 27599, USA"
Journal Title:Environ Chem
Year:2013
Volume:10
Issue:3
Page Number:260 - 268
DOI: 10.1071/EN13040
ISSN/ISBN:1448-2517 (Print) 1448-2517 (Linking)
Abstract:"Many of Houston's highest 8-h ozone (O(3)) peaks are characterised by increases in concentrations of at least 40 ppb in 1 h, or 60 ppb in 2 h. These rapid increases are called non-typical O(3) changes (NTOCs). In 2004, the Texas Commission on Environmental Quality (TCEQ) developed a novel emissions control strategy aimed at eliminating NTOCs. The strategy limited routine and short-term emissions of ethene, propene, 1,3-butadiene and butene isomers, collectively called highly reactive volatile organic compounds (HRVOCs), which are released from petrochemical facilities. HRVOCs have been associated with NTOCs through field campaigns and modelling studies. This study analysed wind measurements and O(3), formaldehyde (HCHO) and sulfur dioxide (SO(2)) concentrations from 2000 to 2011 at 25 ground monitors in Houston. NTOCs almost always occurred when monitors were downwind of petrochemical facilities. Rapid O(3) increases were associated with low wind speeds; 75 % of NTOCs occurred when the 3-h average wind speed preceding the event was less than 6.5 km h(-1). Statistically significant differences in HCHO concentrations were seen between days with and without NTOCs. Early afternoon HCHO concentrations were greater on NTOC days. In the morning before an observed NTOC event, however, there were no significant differences in HCHO concentrations between days with and without NTOCs. Hourly SO(2) concentrations also increased rapidly, exhibiting behaviour similar to NTOCs. Oftentimes, the SO(2) increases preceded a NTOC. These findings show that, despite the apparent success of targeted HRVOC emission controls, further restrictions may be needed to eliminate the remaining O(3) events"
Keywords:
Notes:"PubMed-not-MEDLINECouzo, Evan Jeffries, Harvey E Vizuete, William eng T32 ES007018/ES/NIEHS NIH HHS/ Australia 2013/09/10 Environ Chem. 2013 Jun 28; 10(3):260-268. doi: 10.1071/EN13040"

 
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