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 AbstractLong-term evaluation of the controlled pressure method for assessment of the vapor intrusion pathway    Next AbstractElectrophilic Methylation of Decaborane(14): Selective Synthesis of Tetramethylated and Heptamethylated Decaboranes and Their Conjugated Bases »

Environ Sci Technol


Title:Creation of a Sub-slab Soil Gas Cloud by an Indoor Air Source and Its Dissipation Following Source Removal
Author(s):Holton C; Guo Y; Luo H; Dahlen P; Gorder K; Dettenmaier E; Johnson PC;
Address:"School of Sustainable Engineering and the Built Environment, Ira A. Fulton Schools of Engineering , Arizona State University , Tempe , Arizona 85287 , United States. Chevron Energy Technology Company , 1200 Smith Street , Houston , Texas 77002 , United States. Hill Air Force Base , 7290 Weiner Street , Building 383, Hill Air Force Base , Utah 84056 , United States. Department of Civil and Environmental Engineering , Colorado School of Mines , Golden , Colorado 80401 , United States"
Journal Title:Environ Sci Technol
Year:2018
Volume:20180829
Issue:18
Page Number:10637 - 10646
DOI: 10.1021/acs.est.8b01188
ISSN/ISBN:1520-5851 (Electronic) 0013-936X (Linking)
Abstract:"It is accepted that indoor sources of volatile organic compounds can confound vapor intrusion (VI) pathway assessment. When they are discovered during pre-sampling inspection, indoor sources are removed and air sampling is delayed, with the assumption that a few hours to a few days are sufficient for indoor source impacts to dissipate. This assumption was tested through the controlled release of SF(6) and its monitoring in indoor air and soil gas at a study house over 2 years. Results show that indoor sources generate subsurface soil gas clouds as a result of fluctuating direction in the exchange between soil gas and indoor air and that it may take days to weeks under natural conditions for a soil gas cloud beneath a building to dissipate following indoor source removal. The data also reveal temporal variability in indoor air and soil gas concentrations, long-term seasonal patterns, and dissipation of soil gas clouds over days to weeks following source removal. Preliminary modeling results for similar conditions are consistent field observations. If representative of other sites, these results suggest that a typical 1-3 day waiting period following indoor source removal may not be sufficient to avoid confounding data and erroneous conclusions regarding VI occurrence"
Keywords:"*Air Pollutants *Air Pollution, Indoor Gases Soil *Volatile Organic Compounds;"
Notes:"MedlineHolton, Chase Guo, Yuanming Luo, Hong Dahlen, Paul Gorder, Kyle Dettenmaier, Erik Johnson, Paul C eng Research Support, U.S. Gov't, Non-P.H.S. 2018/08/19 Environ Sci Technol. 2018 Sep 18; 52(18):10637-10646. doi: 10.1021/acs.est.8b01188. Epub 2018 Aug 29"

 
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 19-12-2024