Effect of relative humidity on hydrogen peroxide production in water droplets

Mist is generated by ultrasonic cavitation of water (Fisher Biograde, pH 5.5–6.5) at room temperature (20–25 °C) in open air with nearly constant temperature (22–25 °C) but varying relative humidity (RH; 24–52%) over the course of many months. Water droplets in the mist are initially about 7 μm in d...

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Main Authors: Maria T. Dulay, Carlos Alberto Huerta-Aguilar, Christian F. Chamberlayne, Richard N. Zare, Adriaan Davidse, Sinisa Vukovic
Format: Article
Language:English
Published: Cambridge University Press 2021-01-01
Series:QRB Discovery
Subjects:
Online Access:https://www.cambridge.org/core/product/identifier/S2633289221000065/type/journal_article
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author Maria T. Dulay
Carlos Alberto Huerta-Aguilar
Christian F. Chamberlayne
Richard N. Zare
Adriaan Davidse
Sinisa Vukovic
author_facet Maria T. Dulay
Carlos Alberto Huerta-Aguilar
Christian F. Chamberlayne
Richard N. Zare
Adriaan Davidse
Sinisa Vukovic
author_sort Maria T. Dulay
collection DOAJ
description Mist is generated by ultrasonic cavitation of water (Fisher Biograde, pH 5.5–6.5) at room temperature (20–25 °C) in open air with nearly constant temperature (22–25 °C) but varying relative humidity (RH; 24–52%) over the course of many months. Water droplets in the mist are initially about 7 μm in diameter at about 50% RH. They are collected, and the concentration of hydrogen peroxide (H2O2) is measured using commercial peroxide test strips and by bromothymol blue oxidation. The quantification method is based on the Fenton chemistry of dye degradation to determine the oxidation capacity of water samples that have been treated by ultrasonication. It is found that the hydrogen peroxide concentration varies nearly linearly with RH over the range studied, reaching a low of 2 parts per million (ppm) at 24% RH and a high of 6 ppm at 52% RH. Some possible public health implications concerning the transmission of respiratory viral infections are suggested for this threefold change in H2O2 concentration with RH.
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spelling doaj.art-e8039f4e8b574be389fb3bf43bda7f7c2023-03-09T12:43:33ZengCambridge University PressQRB Discovery2633-28922021-01-01210.1017/qrd.2021.6Effect of relative humidity on hydrogen peroxide production in water dropletsMaria T. Dulay0https://orcid.org/0000-0002-4678-3480Carlos Alberto Huerta-Aguilar1https://orcid.org/0000-0001-9274-5330Christian F. Chamberlayne2https://orcid.org/0000-0001-8589-5074Richard N. Zare3https://orcid.org/0000-0001-5266-4253Adriaan Davidse4https://orcid.org/0000-0001-7335-0333Sinisa Vukovic5https://orcid.org/0000-0002-7682-0705Department of Chemistry, Stanford University, Stanford, CA 94305, USADepartment of Chemistry, Stanford University, Stanford, CA 94305, USADepartment of Chemistry, Stanford University, Stanford, CA 94305, USADepartment of Chemistry, Stanford University, Stanford, CA 94305, USAPO Box 93167 Headon PO Burlington, ON L7M 4A3, CanadaMineRP, 333 Bay Street, Toronto, ON M5H 2T6, CanadaMist is generated by ultrasonic cavitation of water (Fisher Biograde, pH 5.5–6.5) at room temperature (20–25 °C) in open air with nearly constant temperature (22–25 °C) but varying relative humidity (RH; 24–52%) over the course of many months. Water droplets in the mist are initially about 7 μm in diameter at about 50% RH. They are collected, and the concentration of hydrogen peroxide (H2O2) is measured using commercial peroxide test strips and by bromothymol blue oxidation. The quantification method is based on the Fenton chemistry of dye degradation to determine the oxidation capacity of water samples that have been treated by ultrasonication. It is found that the hydrogen peroxide concentration varies nearly linearly with RH over the range studied, reaching a low of 2 parts per million (ppm) at 24% RH and a high of 6 ppm at 52% RH. Some possible public health implications concerning the transmission of respiratory viral infections are suggested for this threefold change in H2O2 concentration with RH.https://www.cambridge.org/core/product/identifier/S2633289221000065/type/journal_articleH2O2 quantificationhydrogen peroxidemicrodroplet chemistryreactive oxygen speciesrelative humidityrespiratory viral infections
spellingShingle Maria T. Dulay
Carlos Alberto Huerta-Aguilar
Christian F. Chamberlayne
Richard N. Zare
Adriaan Davidse
Sinisa Vukovic
Effect of relative humidity on hydrogen peroxide production in water droplets
QRB Discovery
H2O2 quantification
hydrogen peroxide
microdroplet chemistry
reactive oxygen species
relative humidity
respiratory viral infections
title Effect of relative humidity on hydrogen peroxide production in water droplets
title_full Effect of relative humidity on hydrogen peroxide production in water droplets
title_fullStr Effect of relative humidity on hydrogen peroxide production in water droplets
title_full_unstemmed Effect of relative humidity on hydrogen peroxide production in water droplets
title_short Effect of relative humidity on hydrogen peroxide production in water droplets
title_sort effect of relative humidity on hydrogen peroxide production in water droplets
topic H2O2 quantification
hydrogen peroxide
microdroplet chemistry
reactive oxygen species
relative humidity
respiratory viral infections
url https://www.cambridge.org/core/product/identifier/S2633289221000065/type/journal_article
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AT richardnzare effectofrelativehumidityonhydrogenperoxideproductioninwaterdroplets
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