Adrian Tuck

Jan 7, 2025 | mdpi.com | Adrian Tuck

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May 31, 2024 | mdpi.com | Adrian Tuck |A. F

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Apr 9, 2024 | mdpi.com | Adrian Tuck |A. F

All articles published by MDPI are made immediately available worldwide under an open access license. No specialpermission is required to reuse all or part of the article published by MDPI, including figures and tables. Forarticles published under an open access Creative Common CC BY license, any part of the article may be reused withoutpermission provided that the original article is clearly cited. For more information, please refer tohttps://www.mdpi.com/openaccess.

Oct 13, 2023 | mdpi.com | Adrian Tuck |A. F

9. Chemical and Radiative Consequences 9.1. Isotope DistributionsIsotope distributions across atmospheric molecules have been used to interpret atmospheric processes [26,52], especially the 16O, 17O, 18O in O2, O3, H2O, SO2, and N2O. Carbon isotopes 12C, 13C, and 14C have also been used, along with 14N, 15N and 32S, 33S, 34S. Water has also been studied with H and D isotopes. It is the distribution of O isotopes across O2 and O3 [53] that will primarily concern us here.

Sep 29, 2023 | mdpi.com | Adrian Tuck |A. F

1. IntroductionReference [1] reconsidered work from the 1960s, which showed that there was a germicidal effect of open air upon airborne microbes and viruses, attributed to photochemical effects driven by solar radiation. The photochemical agents are now not thought to be in direct reaction with OH and HO2, the primary tropospheric oxidisers, nor the formation of Criegee intermediates from the addition of ozone to the double bonds in biopolymers.