The heterogeneous decomposition of ozone
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Federico Karagulian; Michel J. Rossi
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Article
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2006
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John Wiley and Sons
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English
⚖ 263 KB
## Abstract The rate of uptake of ozone on various mineral dust surrogates, expressed as uptake coefficient γ, has been studied employing a Knudsen flow reactor. Experiments were performed at __T__ = 298 ± 2 K on substrates of kaolinite, CaCO~3~, natural limestone, Saharan dust, and Arizona test du