Isotope fractionation associated with the direct photolysis of 4-chloroaniline

Marco Ratti, Silvio Canonica, Kristopher McNeill, Paul R. Erickson, Jakov Bolotin, Thomas B. Hofstetter

Research output: Contribution to journalArticlepeer-review

13 Scopus citations

Abstract

Compound-specific isotope analysis is a useful approach to track transformations of many organic soil and water pollutants. Applications of CSIA to characterize photochemical processes, however, have hardly been explored. In this work, we systematically studied C and N isotope fractionation associated with the direct photolysis of 4-Cl-Aniline used as a model compound for organic micropollutants that are known to degrade via photochemical processes. Laboratory experiments were carried out at an irradiation wavelength of 254 nm over the pH range 2.0 to 9.0 as well as in the presence of Cs+ as a quencher of excited singlet 4-Cl-Aniline at pH 7.0 and 9.0. We observed considerable variation of C and N isotope enrichment factors, C and N, between -1.2 ± 0.2‰ to -2.7 ± 0.2‰ for C and -0.6 ± 0.2‰ to -9.1 ± 1.6‰ for N, respectively, which could not be explained by the speciation of 4-Cl-Aniline alone. In the presence of 1 M Cs+, we found a marked increase of apparent 13C-kinetic isotope effects (13C-AKIE) and decrease of 4-Cl-Aniline fluorescence lifetimes. Our data suggest that variations of C and N isotope fractionation originate from heterolytic dechlorination of excited triplet and singlet states of 4-Cl-Aniline. Linear correlations of 13C-AKIE vs 15N-AKIE were distinctly different for these two reaction pathways and may be explored further for the identification of photolytic aromatic dechlorination reactions.

Original languageEnglish (US)
Pages (from-to)4263-4273
Number of pages11
JournalEnvironmental Science and Technology
Volume49
Issue number7
DOIs
StatePublished - Apr 7 2015

Fingerprint

Dive into the research topics of 'Isotope fractionation associated with the direct photolysis of 4-chloroaniline'. Together they form a unique fingerprint.

Cite this