Bias caused by water adsorption in hourly PM measurements
Beta-attenuation monitors are used worldwide to monitor PM mass concentration with high temporal resolution. Hourly PM<sub>10</sub> and PM<sub>2. 5</sub> dry mass concentrations are publicly available with the tacit assumption that water is effectively removed prior to the...
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doaj-34412c1ad1944180a43df2526f7640772020-11-25T00:45:53ZengCopernicus PublicationsAtmospheric Measurement Techniques1867-13811867-85482017-07-01102477248410.5194/amt-10-2477-2017Bias caused by water adsorption in hourly PM measurementsG. Kiss0K. Imre1Á. Molnár2A. Gelencsér3A. Gelencsér4MTA-PE Air Chemistry Research Group, University of Pannonia, Egyetem 10, 8200 Veszprém, HungaryMTA-PE Air Chemistry Research Group, University of Pannonia, Egyetem 10, 8200 Veszprém, HungaryMTA-PE Air Chemistry Research Group, University of Pannonia, Egyetem 10, 8200 Veszprém, HungaryMTA-PE Air Chemistry Research Group, University of Pannonia, Egyetem 10, 8200 Veszprém, HungaryDepartment of Earth and Environmental Sciences, University of Pannonia, Egyetem 10, 8200 Veszprém, HungaryBeta-attenuation monitors are used worldwide to monitor PM mass concentration with high temporal resolution. Hourly PM<sub>10</sub> and PM<sub>2. 5</sub> dry mass concentrations are publicly available with the tacit assumption that water is effectively removed prior to the measurement. However, as both the filter material of the monitor and the aerosol particles are capable of retaining a significant amount of water even at low relative humidities, the basic assumption may not be valid, resulting in significant bias in reported PM<sub>10</sub> and PM<sub>2. 5</sub> concentrations. Here we show that in PM<sub>10</sub> measurement, particle-free air can produce apparent hourly average PM concentrations in the range of −13–+21 µg m<sup>−3</sup> under conditions of fluctuating relative humidity. Positive and negative apparent readings are observed with increasing and decreasing relative humidities, respectively. Similar phenomena have been observed when the instrument filter was previously loaded with atmospheric aerosol. As a result the potential measurement biases in hourly readings arising from the interaction with water may be in the range of −53… + 69 %.https://www.atmos-meas-tech.net/10/2477/2017/amt-10-2477-2017.pdf |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
G. Kiss K. Imre Á. Molnár A. Gelencsér A. Gelencsér |
spellingShingle |
G. Kiss K. Imre Á. Molnár A. Gelencsér A. Gelencsér Bias caused by water adsorption in hourly PM measurements Atmospheric Measurement Techniques |
author_facet |
G. Kiss K. Imre Á. Molnár A. Gelencsér A. Gelencsér |
author_sort |
G. Kiss |
title |
Bias caused by water adsorption in hourly PM measurements |
title_short |
Bias caused by water adsorption in hourly PM measurements |
title_full |
Bias caused by water adsorption in hourly PM measurements |
title_fullStr |
Bias caused by water adsorption in hourly PM measurements |
title_full_unstemmed |
Bias caused by water adsorption in hourly PM measurements |
title_sort |
bias caused by water adsorption in hourly pm measurements |
publisher |
Copernicus Publications |
series |
Atmospheric Measurement Techniques |
issn |
1867-1381 1867-8548 |
publishDate |
2017-07-01 |
description |
Beta-attenuation monitors are used worldwide to monitor PM mass
concentration with high temporal resolution. Hourly PM<sub>10</sub> and PM<sub>2. 5</sub> dry mass
concentrations are publicly available with the tacit assumption that water
is effectively removed prior to the measurement. However, as both the filter
material of the monitor and the aerosol particles are capable of retaining
a significant amount of water even at low relative humidities, the basic
assumption may not be valid, resulting in significant bias in reported PM<sub>10</sub>
and PM<sub>2. 5</sub> concentrations. Here we show that in PM<sub>10</sub>
measurement,
particle-free air can produce apparent hourly average PM concentrations in
the range of −13–+21 µg m<sup>−3</sup> under conditions of
fluctuating relative humidity. Positive and negative apparent readings are
observed with increasing and decreasing relative humidities, respectively.
Similar phenomena have been observed when the instrument filter was
previously loaded with atmospheric aerosol. As a result the potential
measurement biases in hourly readings arising from the interaction with
water may be in the range of −53… + 69 %. |
url |
https://www.atmos-meas-tech.net/10/2477/2017/amt-10-2477-2017.pdf |
work_keys_str_mv |
AT gkiss biascausedbywateradsorptioninhourlypmmeasurements AT kimre biascausedbywateradsorptioninhourlypmmeasurements AT amolnar biascausedbywateradsorptioninhourlypmmeasurements AT agelencser biascausedbywateradsorptioninhourlypmmeasurements AT agelencser biascausedbywateradsorptioninhourlypmmeasurements |
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