Probing the Freezing Chemistry of Singly Levitated Aqueous Trifluoroacetic Acid Droplets in a Cryogenically Cooled Simulation Chamber Relevant to Earth’s Upper Troposphere
Koushik Mondal, Souvick Biswas, Nils Wrangell Melbourne, Rui Sun, Ralf I. Kaiser
{"title":"Probing the Freezing Chemistry of Singly Levitated Aqueous Trifluoroacetic Acid Droplets in a Cryogenically Cooled Simulation Chamber Relevant to Earth’s Upper Troposphere","authors":"Koushik Mondal, Souvick Biswas, Nils Wrangell Melbourne, Rui Sun, Ralf I. Kaiser","doi":"10.1039/d5sc01698c","DOIUrl":null,"url":null,"abstract":"Trifluoroacetic acid (CF<small><sub>3</sub></small>COOH, TFA), the primary upper terrestrial atmosphere degradation product of several fluorinated hydrocarbons primarily used as refrigerants, poses a significant environmental challenge due to its growing atmospheric accumulation and extremely low reactivity. This combined experimental and theoretical study of TFA-doped water droplets, conducted inside a cryogenically cooled ultrasonic levitator simulation chamber utilizing time-dependent Raman spectroscopy and optical visualization techniques, addresses the dynamic chemical changes during the freezing event for the first time. The low-temperature experimental approach mimics TFA's interactions within water droplets in the upper troposphere and arctic regions, particularly at subzero temperatures. Key findings reveal structural transformation towards the formation of undissociated neutral TFA in hexagonal ice environments compared to the anionic form, providing fundamental insight into the role of TFA in ice nucleation. Furthermore, state-of-the-art electronic structure calculations provide insights into the stability of this undissociated TFA within the hexagonal ice-encapsulated environment, wherein structural distortions of the regular hexagonal ice crystal and secondary F—H interactions mostly between anionic TFA forms and the ice lattice are evidenced at the molecular level. This research untangles the chemical insight to the TFA on ice nucleation leading to cloud glaciation, hence providing a plausible reason behind its presence in remote arctic regions through long-range transport.","PeriodicalId":9909,"journal":{"name":"Chemical Science","volume":"7 1","pages":""},"PeriodicalIF":7.6000,"publicationDate":"2025-05-10","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Chemical Science","FirstCategoryId":"92","ListUrlMain":"https://doi.org/10.1039/d5sc01698c","RegionNum":1,"RegionCategory":"化学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"CHEMISTRY, MULTIDISCIPLINARY","Score":null,"Total":0}
引用次数: 0
Abstract
Trifluoroacetic acid (CF3COOH, TFA), the primary upper terrestrial atmosphere degradation product of several fluorinated hydrocarbons primarily used as refrigerants, poses a significant environmental challenge due to its growing atmospheric accumulation and extremely low reactivity. This combined experimental and theoretical study of TFA-doped water droplets, conducted inside a cryogenically cooled ultrasonic levitator simulation chamber utilizing time-dependent Raman spectroscopy and optical visualization techniques, addresses the dynamic chemical changes during the freezing event for the first time. The low-temperature experimental approach mimics TFA's interactions within water droplets in the upper troposphere and arctic regions, particularly at subzero temperatures. Key findings reveal structural transformation towards the formation of undissociated neutral TFA in hexagonal ice environments compared to the anionic form, providing fundamental insight into the role of TFA in ice nucleation. Furthermore, state-of-the-art electronic structure calculations provide insights into the stability of this undissociated TFA within the hexagonal ice-encapsulated environment, wherein structural distortions of the regular hexagonal ice crystal and secondary F—H interactions mostly between anionic TFA forms and the ice lattice are evidenced at the molecular level. This research untangles the chemical insight to the TFA on ice nucleation leading to cloud glaciation, hence providing a plausible reason behind its presence in remote arctic regions through long-range transport.
期刊介绍:
Chemical Science is a journal that encompasses various disciplines within the chemical sciences. Its scope includes publishing ground-breaking research with significant implications for its respective field, as well as appealing to a wider audience in related areas. To be considered for publication, articles must showcase innovative and original advances in their field of study and be presented in a manner that is understandable to scientists from diverse backgrounds. However, the journal generally does not publish highly specialized research.