An unheated permeation device for calibrating atmospheric VOC measurements

The development of an unpowered permeation device for continuous calibration of in-situ instruments measuring atmospheric volatile organic compounds (VOCs) is described. Being lightweight and compact, and containing only negligible amounts of chemicals, the device is especially suited for field use...

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Main Authors: J. Brito, A. Zahn
Format: Article
Language:English
Published: Copernicus Publications 2011-10-01
Series:Atmospheric Measurement Techniques
Online Access:http://www.atmos-meas-tech.net/4/2143/2011/amt-4-2143-2011.pdf
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spelling doaj-2a83d9dff9a04c779cc505f98dc5ca282020-11-25T00:04:10ZengCopernicus PublicationsAtmospheric Measurement Techniques1867-13811867-85482011-10-014102143215210.5194/amt-4-2143-2011An unheated permeation device for calibrating atmospheric VOC measurementsJ. BritoA. ZahnThe development of an unpowered permeation device for continuous calibration of in-situ instruments measuring atmospheric volatile organic compounds (VOCs) is described. Being lightweight and compact, and containing only negligible amounts of chemicals, the device is especially suited for field use such as on board aircraft. Its speciality is to maintain the permeation process in thermal equilibrium, so that the instantaneous permeation rate can be ascribed to a simple temperature measurement. This equilibrium state is maintained by a combination of three features: (i) a thin PTFE membrane as permeation medium which guarantees short stabilization times, (ii) a water bath as heat buffer, and (iii) a vacuum-panel based insulation, in which features (ii) and (iii) minimize temperature drifts to ~30 mK h<sup>−1</sup> per Kelvin temperature difference to the environment. The respective uncertainty of the permeation rate due to thermal non-equilibrium is kept below 1%. An extensive theory part details the major permeation processes of gases through porous polymers, being Fick's diffusion, Knudsen flow, and viscous flow. Both the measured stabilization time and the measured temperature dependence of the permeation rate independently indicate that the permeation can be described by a viscous flow model, where diffusion of the gas molecules in large pores (having a diameter of >0.05 μm) dominates.http://www.atmos-meas-tech.net/4/2143/2011/amt-4-2143-2011.pdf
collection DOAJ
language English
format Article
sources DOAJ
author J. Brito
A. Zahn
spellingShingle J. Brito
A. Zahn
An unheated permeation device for calibrating atmospheric VOC measurements
Atmospheric Measurement Techniques
author_facet J. Brito
A. Zahn
author_sort J. Brito
title An unheated permeation device for calibrating atmospheric VOC measurements
title_short An unheated permeation device for calibrating atmospheric VOC measurements
title_full An unheated permeation device for calibrating atmospheric VOC measurements
title_fullStr An unheated permeation device for calibrating atmospheric VOC measurements
title_full_unstemmed An unheated permeation device for calibrating atmospheric VOC measurements
title_sort unheated permeation device for calibrating atmospheric voc measurements
publisher Copernicus Publications
series Atmospheric Measurement Techniques
issn 1867-1381
1867-8548
publishDate 2011-10-01
description The development of an unpowered permeation device for continuous calibration of in-situ instruments measuring atmospheric volatile organic compounds (VOCs) is described. Being lightweight and compact, and containing only negligible amounts of chemicals, the device is especially suited for field use such as on board aircraft. Its speciality is to maintain the permeation process in thermal equilibrium, so that the instantaneous permeation rate can be ascribed to a simple temperature measurement. This equilibrium state is maintained by a combination of three features: (i) a thin PTFE membrane as permeation medium which guarantees short stabilization times, (ii) a water bath as heat buffer, and (iii) a vacuum-panel based insulation, in which features (ii) and (iii) minimize temperature drifts to ~30 mK h<sup>−1</sup> per Kelvin temperature difference to the environment. The respective uncertainty of the permeation rate due to thermal non-equilibrium is kept below 1%. An extensive theory part details the major permeation processes of gases through porous polymers, being Fick's diffusion, Knudsen flow, and viscous flow. Both the measured stabilization time and the measured temperature dependence of the permeation rate independently indicate that the permeation can be described by a viscous flow model, where diffusion of the gas molecules in large pores (having a diameter of >0.05 μm) dominates.
url http://www.atmos-meas-tech.net/4/2143/2011/amt-4-2143-2011.pdf
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