Conditions are described for the preparation of cholesterol with (17)O and (18)O labels from i-cholesteryl methyl ether using minimal amounts of isotopically enriched water. Optimum yields employed trifluoromethanesulfonic acid as catalyst in 1,4-dioxane at room temperature with 5 equivalents of water. An isotopic enrichment >90% of that of the water used for the reaction could be attained. Tetrafluoroboric acid could also be used as catalyst, at the expense of a lower overall reaction yield. Byproducts from the reaction included dicholesteryl ether, methyl cholesteryl ether, compounds formed by ether hydrolysis, and olefins arising from elimination reactions. Reactions in tetrahydrofuran yielded significant amounts of cholesteryl ethers formed by reaction with alcohols arising from hydrolysis of the solvent.
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http://dx.doi.org/10.1016/j.chemphyslip.2015.12.003 | DOI Listing |
Isotopes Environ Health Stud
August 2024
WasserCluster Lunz Biologische Station GmbH, Lunz am See, Austria.
Understanding the critical thresholds of dissolved oxygen (O) that trigger adaptive physiological responses in aquatic organisms is long hampered by a lack of robust, non-lethal or non-invasive methodologies. The isotope fractionation of triple O isotopes (O/O/O) during respiration is linked to the amount of oxygen utilised, offering a potential avenue for new insights. Our experimental research involved measuring the oxygen isotope fractionation of dissolved O in closed-system aquatic respirometry experiments with wild sticklebacks ().
View Article and Find Full Text PDFJ Am Chem Soc
March 2024
Department of Materials Science and Engineering, National University of Singapore, 117575 Singapore, Singapore.
Wet-chemical oxidation of graphite in a mixture of sulfuric acid with a strong oxidizer, such as potassium permanganate, leads to the formation of graphene oxide with hydroxyl and epoxide groups as the major functional groups. Nevertheless, the reaction mechanism remains unclear and the source of oxygen is a subject of debate. It could theoretically originate from the oxidizer, water, or sulfuric acid.
View Article and Find Full Text PDFAnal Chem
January 2024
Faculty of Information Science and Engineering, Ocean University of China, Qingdao 266100, China.
Combined in situ analysis of oceanic CO concentrations and diverse C and O isotope characteristics can offer a unique perspective with multiple isotopic tracing dimensions for identifying marine biogeochemical processes. Applying this strategy in marine environments is urgently required, yet it faces inherent challenges in terms of existing analytical methods and instruments, e.g.
View Article and Find Full Text PDFSci Rep
November 2023
Department of Water, Atmosphere and Environment, Institute of Soil Physics and Rural Water Management, University of Natural Resources and Life Sciences, Vienna, Muthgasse 18, 1190, Vienna, Austria.
Recently, δO and its excess (Δ'O) have become increasingly significant "triple-oxygen-isotope" indicators of distinctive hydrological processes in hydrology and climatology. This situation mirrors the research regarding δO and δH in the 1960s towards a solid theoretical base and a surge in application examples and field studies worldwide. Currently, systematic global measurements for δO in precipitation are still lacking.
View Article and Find Full Text PDFSci Rep
November 2023
Department of Geography, Royal Holloway University of London, Egham, TW20 0EX, UK.
During the Roman domain of the Iberian Peninsula (from 201 BCE to 460 CE) water management infrastructures were built to satisfy high water demand. However, whether the Roman activities affected the hydrological balance of Iberian wetlands remains unclear. Here, we investigate the paleo-hydrology of Lake Zóñar (southern Iberia) by using the stable isotopes (O, O, O, H and H) of its gypsum (CaSO·2HO) sediments and reconstruct the isotopic composition of the lake water during Roman times.
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