High-temperature (440 °C) chlorination of C with SbCl promotes Stone-Wales transformations and loss of the C fragment, which results in a non-classical CCl partially hydrolyzed to CCl(OH) and CCl(OH). X-ray diffraction reveals an unprecedented C cage with three heptagons and 15 pentagons arranged in fused pairs and triples. The shortest possible transformation pathways include one C loss step and four Stone-Wales transformation steps.
Download full-text PDF |
Source |
---|---|
http://dx.doi.org/10.1039/d2cc01719a | DOI Listing |
J Phys Chem A
June 2015
‡Department of Civil and Environmental Engineering, Korea Advanced Institute of Science and Technology (KAIST), 291 Daehak-ro, Yuseong-gu, Daejeon 305-701, Korea.
Chlorinated organics are the principal and most frequently found contaminants in soil and groundwater, generating significant environmental problems. Over the past several decades, Fe-containing minerals naturally occurring in aquatic and terrestrial environments have been used as natural electron donors, which can effectively dechlorinate a variety of chlorinated organics. However, a full understanding of the reaction mechanism of the dechlorination pathway cannot be obtained by experimental investigations alone, due to the immeasurability of chemical species formed over a short reaction time.
View Article and Find Full Text PDFEnter search terms and have AI summaries delivered each week - change queries or unsubscribe any time!