943 resultados para Choruses, Sacred (Mixed voices, 4 parts) with piano.


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Issued in 4 parts (nos. 1, 5, 6, and 23 of the society's Publications, forming vols. II and III, no. 1) Each part has special t.-p., contents, and index. General title in v. 1 (vol.II of the series)

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Forewords by Natalie Curtis Burlin.

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"A reprint of Dr. Currie's second edition." cf. J. Gibson. The bibliography of Robert Burns.

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Tristesse des Choses -- Le Colibri -- Les roses d'Ispahan -- Je n'en ai jamais aimé qu'une -- Ici bas.

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Ceased publication with v.88, no.4, Feb. 1961. Vols.18-40, 1885-1907, also called "new series," v.1-22; v.41-57, 1908-24, called "new issue"; v.58-88, 1925-61, called "quarterly issue." Title varies: v.1-79, 1868-1951, Transactions and proceedings. Vol.41-44, 1908-11, issued in 2 separate parts with separate titles and pagings: "Transactions" and "Proceedings." Issued 1868-1933 by the society under its earlier name: New Zealand Institute. Includes proceedings of member institutes of the society and of the society's science congress. Superseded by 4 subseries: Botany, Geology, Zoology, and General. Indexes: v.1-8, 1868-75. 1v.; v.1-17, 1868-84. 1v.; v.1-40, 1868-1907. 1v.

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Mode of access: Internet.

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Sonata, F minor, opus 4, violin and piano; [For] violoncello and piano: Variations concertantes, D major, opus 17; Sonata no.1, B flat major, opus 45; Sonata no.2, D major, opus 58; Songs without words, D major, opus 109.

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Mode of access: Internet.

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Op. 9.

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Beginning with 2d ser. a general t.-p. is pub. for each decade

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Arrangement for violins 1-2 with piano accompaniment.

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Eleven sediment samples taken downcore and representing the past 26 kyr of deposition at MANOP site C (0°57.2°N, 138°57.3°W) were analyzed for lipid biomarker composition. Biomarkers of both terrestrial and marine sources of organic carbon were identified. In general, concentration profiles for these biomarkers and for total organic carbon (TOC) displayed three common stratigraphic features in the time series: (1) a maximum within the surface sediment mixed layer (<=4 ka); (2) a broad minimum extending throughout the interglacial deposit; and (3) a deep, pronounced maximum within the glacial deposit. Using the biomarker records, a simple binary mixing model is described that assesses the proportion of terrestrial to marine TOC in these sediments. Best estimates from this model suggest that ~20% of the TOC is land-derived, introduced by long-range eolian transport, and the remainder is derived from marine productivity. The direct correlation between the records for terrestrial and marine TOC with depth in this core fits an interpretation that primary productivity at site C has been controlled by wind-driven upwelling at least over the last glacial/interglacial cycle. The biomarker records place the greatest wind strength and highest primary productivity within the time frame of 18 to 22 kyr B.P. Diagenetic effects limit our ability to ascertain directly from the biomarker records the absolute magnitude that different types of primary productivity have changed at this ocean location over the past 26 kyr.

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Tetrazolo[1,5-a] pyridines/ 2-azidopyridines 1 undergo photochemical nitrogen elimination and ring expansion to 1,3-diazacyclohepta-1,2,4,6-tetraenes 3, which react with alcohols to afford 2-alkoxy-1H-1,3-diazepines 4 (5), with secondary amines to 2-dialkylamino-5H-1,3-diazepines 16, sometimes via isolable 2-dialkylamino-1H-1,3-diazepines 15, and with water to 1,3-diazepin-2-ones 19. The latter are also obtained by elimination of isobutene or propene from 2-tert-butoxy- or 2-isopropoxy-1H-1,3-diazepines 4 or 5. 1,3-Diazepin-2-one 22B and 1,3-diazepin-4-one 24 were obtained from hydrolysis of the corresponding 4-chlorodiazepines. Diazepinones 19 undergo photochemical ring closure to diazabicycloheptenones 25 in high yields. The 2-alkoxy-1H-1,3-diazepines 4 and 5 interconvert by rapid proton exchange between positions N1 and N3. The free energies of activation for the proton exchange were measured by the Forsen - Hoffman method as DeltaGdouble dagger(298) = 16.2 +/- 0.6 kcal mol(-1) as an average for 4a - c in CD2Cl2, acetone-d(6), and methanol-d(4), and 14.1 +/- 0.6 kcal mol(-1) for 4c in acetone/D2O. The structures of 2-methoxy-5,6-bis( trifluoromethyl)-1H-1,3-diazepine 4k, 1,2-dihydro-4-diethylamino-5H-1,3-diazepin-2-one 22bB, and diazabicycloheptanone 26 were determined by X-ray crystallography. The former represents the first reported X-ray crystal structure of any monocyclic N-unsubstituted 1H-azepine.