Issue 7, 2004

Automated measurement and calibration of reactive volatile halogenated organic compounds in the atmosphere

Abstract

The automated calibration and analysis of very low mixing ratios of the reactive volatile organic halocarbons CH3I, CHCl3, C2H5I, 2-C3H7I, CH2Br2, CH2ClI, CHBr2Cl, 1-C3H7I, CH2BrI, CHBr3 and CH2I2 for long term atmospheric field measurements are described. Analytes were pre-concentrated from 3 l of air onto an adsorbent trap cooled to −10 °C using Peltier plates, and rapidly transferred to a gas chromatograph (GC) by resistive heating. A two stage Carboxen 1016/Carbotrap C adsorbent trap allowed good analyte recovery and rapid desorption without the need for post-desorption cryofocussing. Halocarbons were detected using a mass spectrometer (MS) in selective ion mode. Detection limits were between 0.02 and 0.12 pptv (parts per trillion by volume) for approximately hourly samples of CHCl3, CH3I, C2H5I, 1-C3H7I, 2-C3H7I, CH2ClI, CH2Br2, CHBr2Cl, CH2BrI, CHBr3 and CH2I2 with a precision of 3–8%. A novel calibration system was constructed which utilised fixed volume (50 µl) injections of the output of thermostatted permeation tubes into a stream of nitrogen gas in order to dilute parts per million by volume (ppmv) mixing ratios into pptv. The calibration was completely automated, allowing multi-point calibrations during routine operation. The overall accuracy of the measurements is estimated to be ±15%. The instrument was used continuously for automated atmospheric measurements during a 4-month research cruise from Germany to Antarctica, and a 6 week field campaign at Mace Head, Ireland. The results for CHCl3 during the latter campaign were within 13% of measurements made by a GC-MS operating continuously at the site within the long term Advanced Global Atmospherics Gases Experiment.

Article information

Article type
Paper
Submitted
08 Mar 2004
Accepted
05 May 2004
First published
08 Jun 2004

Analyst, 2004,129, 634-638

Automated measurement and calibration of reactive volatile halogenated organic compounds in the atmosphere

D. J. Wevill and L. J. Carpenter, Analyst, 2004, 129, 634 DOI: 10.1039/B403550J

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