Historic records of organic compounds from a high Alpine glacier: influences of biomass burning, anthropogenic emissions, and dust transport

Historic records of α-dicarbonyls (glyoxal, methylglyoxal), carboxylic acids (C6–C12 dicarboxylic acids, pinic acid, p-hydroxybenzoic acid, phthalic acid, 4-methylphthalic acid), and ions (oxalate, formate, calcium) were determined with annual resolution in an ice core from Grenzgletscher in the southern Swiss Alps, covering the time period from 1942 to 1993. Chemical analysis of the organic compounds was conducted using ultra-high-performance liquid chromatography (UHPLC) coupled to electrospray ionization high-resolution mass spectrometry (ESI-HRMS) for dicarbonyls and long-chain carboxylic acids and ion chromatography for short-chain carboxylates. Long-term records of the carboxylic acids and dicarbonyls, as well as their source apportionment, are reported for western Europe. This is the first study comprising long-term trends of dicarbonyls and long-chain dicarboxylic acids (C6–C12) in Alpine precipitation. Source assignment of the organic species present in the ice core was performed using principal component analysis. Our results suggest biomass burning, anthropogenic emissions, and transport of mineral dust to be the main parameters influencing the concentration of organic compounds. Ice core records of several highly correlated compounds (e.g., p-hydroxybenzoic acid, pinic acid, pimelic, and suberic acids) can be related to the forest fire history in southern Switzerland. P-hydroxybenzoic acid was found to be the best organic fire tracer in the study area, revealing the highest correlation with the burned area from fires. Historical records of methylglyoxal, phthalic acid, and dicarboxylic acids adipic acid, sebacic acid, and dodecanedioic acid are comparable with that of anthropogenic emissions of volatile organic compounds (VOCs). The small organic acids, oxalic acid and formic acid, are both highly correlated with calcium, suggesting their records to be affected by changing mineral dust transport to the drilling site.

Gas/particle partitioning of carbonyls in the photooxidation of isoprene and 1,3,5-trimethylbenzene

A new denuder-filter sampling technique has been used to investigate the gas/particle partitioning behaviour of the carbonyl products from the photooxidation of isoprene and 1,3,5-trimethylbenzene. A series of experiments was performed in two atmospheric simulation chambers at atmospheric pressure and ambient temperature in the presence of NOx and at a relative humidity of approximately 50%. The denuder and filter were both coated with the derivatizing agent O-(2,3,4,5,6-pentafluorobenzyl)-hydroxylamine (PFBHA) to enable the efficient collection of gas- and particle-phase carbonyls respectively. The tubes and filters were extracted and carbonyls identified as their oxime derivatives by GC-MS. The carbonyl products identified in the experiments accounted for around 5% and 10% of the mass of secondary organic aerosol formed from the photooxidation of isoprene and 1,3,5-trimethylbenzene respectively. Experimental gas/particle partitioning coefficients were determined for a wide range of carbonyl products formed from the photooxidation of isoprene and 1,3,5-trimethylbenzene and compared with the theoretical values based on standard absorptive partitioning theory. Photooxidation products with a single carbonyl moiety were not observed in the particle phase, but dicarbonyls, and in particular, glyoxal and methylglyoxal, exhibited gas/particle partitioning coefficients several orders of magnitude higher than expected theoretically. These findings support the importance of heterogeneous and particle-phase chemical reactions for SOA formation and growth during the atmospheric degradation of anthropogenic and biogenic hydrocarbons.

Formation de centres quaternaires entièrement carbonés et dérivations d’ions iminiums encombrés

Le projet présenté au cours de cette thèse porte sur la formation de centres quaternaires entièrement carbonés. Plusieurs axes d’approche ont été établis, et seront présentés par chapitre : le premier fait état de l’utilisation d’une réaction de Vilsmeier-Haack, le second rapporte la fabrication de nouveaux catalyseurs pour la réaction de condensation de Claisen et le dernier utilise la réaction de Vilsmeier-Haack pour la formation d’acides [béta]-aminés non-racémiques. Lors du premier chapitre, le sujet abordé sera l’utilisation de la réaction de Vilsmeier-Haack pour la formation de composés 1,3-dicarbonylés contenant un centre quaternaire entièrement carboné. D’abord nous verrons comment, théoriquement, la chiralité du centre quaternaire peut être contrôlée par l’utilisation d’amines chirales. Puis nous suivrons le développement d’une méthode d’hydrolyse spécifique à l’obtention de composés 1,3-dicarbonylés avec ses forces et ses limites. La deuxième partie de cette thèse portera sur le développement de nouveaux catalyseurs pour la réaction de condensation de Claisen. Plusieurs avenues seront exposées. Dans un premier temps, nous verrons la rationalisation validant chacune des idées d’avenues envisagées, puis nous aborderons les méthodes de synthèses essayées pour les catalyseurs imaginés dans chacune de ces avenues. Le dernier chapitre portera sur la formation de dérivés d’acides [béta]-aminés non-racémiques via l’utilisation d’une réaction de Vilsmeier-Haack. Dans un premier temps, différentes méthodes de réduction applicables à cette réaction seront présentées, et ensuite, le concept d’un nouveau groupe protecteur spécifique aux ions iminiums sera démontré.