Kammermusik Nr. 1 : mit Finale 1921 : für zwölf Solo-Instrumente : Opus 24, Nr. 1 /

Mode of access: Internet.

補注黃帝內經素問 24巻. 靈樞 12巻. 素問遺篇 1巻

Mode of access: Internet.

Organizational maintenance repair parts and special tools list for recorder-reproducer sets, sound, AN/TNH-24(V)1, (NSN 5835-01-017-0958), AN/TNH-24(V)2, (NSN 5835-01-018-4197), AN/TNH-24(V)3, (NSN 5835-01-021-9681), and AN/TNH-24(V)4, (NSN 5835-01-021-9680).

Includes index.

Patrimoine – vol.24 n.1, automne 2016

En 2003, L’Université de Montréal fondait la société du Patrimoine afin de regrouper, honorer et remercier les donateurs qui ont prévu un don planifié ainsi que les représentants des successions des donateurs qui ont fait un legs dans le passé. La société regroupe plus de 150 individus et successions. Pour toute demande de reproduction de contenu se trouvant dans cette publication, communiquer avec le Bureau du développement et des relations avec les diplômés de l’UdeM.

Patrimoine – vol.24 n.1, automne 2016

En 2003, L’Université de Montréal fondait la société du Patrimoine afin de regrouper, honorer et remercier les donateurs qui ont prévu un don planifié ainsi que les représentants des successions des donateurs qui ont fait un legs dans le passé. La société regroupe plus de 150 individus et successions. Pour toute demande de reproduction de contenu se trouvant dans cette publication, communiquer avec le Bureau du développement et des relations avec les diplômés de l’UdeM.

(Appendix 1-4) Geochemistry, desorption methods, TOC, TC, and mineral content of different settings

Sorption of volatile hydrocarbon gases (VHCs) to marine sediments is a recognized phenomenon that has been investigated in the context of petroleum exploration. However, little is known about the biogeochemistry of sorbed methane and higher VHCs in environments that are not influenced by thermogenic processes. This study evaluated two different extraction protocols for sorbed VHCs, used high pressure equipment to investigate the sorption of methane to pure clay mineral phases, and conducted a geochemical and mineralogical survey of sediment samples from different oceanographic settings and geochemical regimes that are not significantly influenced by thermogenic gas. Extraction of sediments under alkaline conditions yielded higher concentrations of sorbed methane than the established protocol for acidic extraction. Application of alkaline extraction in the environmental survey revealed the presence of substantial amounts of sorbed methane in 374 out of 411 samples (91%). Particularly high amounts, up to 2.1 mmol kg**-1 dry sediment, were recovered from methanogenic sediments. Carbon isotopic compositions of sorbed methane suggested substantial contributions from biogenic sources, both in sulfate-depleted and sulfate-reducing sediments. Carbon isotopic relationships between sorbed and dissolved methane indicate a coupling of the two pools. While our sorption experiments and extraction conditions point to an important role for clay minerals as sorbents, mineralogical analyses of marine sediments suggest that variations in mineral composition are not controlling variations in quantities of sorbed methane. We conclude that the distribution of sorbed methane in sediments is strongly influenced by in situ production.

Ban yue 半月 (The Half Moon Journal) Vol 1 No 24

A bimonthly literary magazine edited by Zhou Shoujuan 周瘦鵑, featuring fiction, topical articles, and entertainment features, published from September 1921 through November 1925.

Solution structure of methionine-oxidized amyloid beta-peptide (1-40). Does oxidation affect conformational switching?

The solution structure of A beta(1-40)Met(O), the methionine-oxidized form of amyloid beta-peptide A beta(1-40), has been investigated by CD and NMR spectroscopy. Oxidation of Met35 may have implications in the aetiology of Alzheimer's disease. Circular dichroism experiments showed that whereas A beta(1-40) and A beta(1-40)Met(O) both adopt essentially random coil structures in water (pH 4) at micromolar concentrations, the former aggregates within several days while the latter is stable for at least 7 days under these conditions. This remarkable difference led us to determine the solution structure of A beta(1-40)Met(O) using H-1 NMR spectroscopy. In a water-SDS micelle medium needed to solubilize both peptides at the millimolar concentrations required to measure NMR spectra, chemical shift and NOE data for A beta(1-40)Met(O) strongly suggest the presence of a helical region between residues 16 and 24. This is supported by slow H-D exchange of amide protons in this region and by structure calculations using simulated annealing with the program XPLOR. The remainder of the structure is relatively disordered. Our previously reported NMR data for A beta(1-40) in the same solvent shows that helices are present over residues 15-24 (helix 1) and 28-36 (helix 2), Oxidation of Met35 thus causes a local and selective disruption of helix 2. In addition to this helix-coil rearrangement in aqueous micelles, the CD data show that oxidation inhibits a coil-to-beta-sheet transition in water. These significant structural rearrangements in the C-terminal region of A beta may be important clues to the chemistry and biology of A beta(1-40) and A beta(1-42).