1000 resultados para 619 - Veterinària


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This work presents a brief historical about the use of ionizing radiations in Veterinary Medicine, instructing the physical beginnings and techniques wrapped in the realization of the proceedings of radiotherapy in animals, illustrating some treated cases, highlighting the difficulties and pointing to the perspectives and importance of the acting of the medical physics in this kind of therapeutic still little used in the national scenery.

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Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)

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Supervisão da revisão do livro.

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Friedrich Stoltze II

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"Einleitung in die Philosophie", Wintersemester 1932/33, eigenhändige Notizen, 1 Heft, 12 Blatt, davon 5 leer, und 8 zusätzliche Blätter; Zwei Aufsätze vor 1933 (enthält: "Über Kants Philosophie", Typoskript mit eigenhändigen Korrekturen, 8 Blatt. Mit 1 Blatt von Theodor W. Adorno an Max Horkheimer, 29.04.1954 (GS 11, S. 202-208; "Nicolai Hartmann", ca 1931, Typoskript mit eigenhändigen Korrekturen, 6 Blatt (GS 2, S. 172-176)); "Zur Emanzipation der Philosophie von der Wissenschaft" (GS 10, S. 334-419). Über Empiriokritizismus (Mach), Neukantianismus (Cohen), Phänomenologie (Husserlm Scheler), Lebensphilosophie (Bergson), nach 1927 - vor 1933; a) Typoskript mit eigenhändigen Korrekturen, gebunden, 114 Blatt, b) Typoskript mit handschriftlichen Korrekturen, 109 Blatt; Über Erkenntnistheorie und Gestalttheorie (GS 11, S. 22-69), Manuskript, in 2 Heften (Heft 1, 96 Blatt; Heft 2, 32 Blatt);

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Pigmy Basin sediments cored in Hole 619 of Deep Sea Drilling Project Leg 96 are silty clays composed, on the average, of < 1% sand, 37% silt, 48% clay, and 14% carbonate minerals. Except for minor grain dissolution in some silt grains, there is no distinctive variation with depth in either composition or texture of the sand- and silt-sized minerals. This suggests a constant source of sediment supply and little diagenetic alteration of these size fractions. Clay minerals are dominated by smectite or, more precisely, montmorillonite. On the average, the clay-sized fraction consists of 48% smectite and mixed layer minerals, 30% illite, and 23% total kaolinite and chlorite. There appears to be a slight decrease in smectite and concomitant increases in other clay minerals with depth. These changes are further substantiated by the variations of ammonium acetate exchangeable K+, Mg2+, and Na+ in bulk samples. Thus, incipient diagenesis of Pigmy Basin sediments is evidenced in the mineralogical and associated chemical characteristics of the clay fractions.

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A preliminary palynological survey of 118 samples from the Mississippi Fan (Sites 615, 616, and 620) and from 2 intraslope basins (Sites 619 and 618) shows pollen in all samples. Reworked pollen is generally abundant, forming over 50% of the sum of pollen and reworked pollen. Concentration of nonreworked pollen is usually low (on the order of tens to hundreds of pollen grains per cubic centimeter wet sediment). Conifers, primarily Pinus, Picea, and Tsuga, dominate Pleistocene marine pollen spectra; significant percentages of Quercus are present in Holocene sediments and in sediments deposited during oxygen-isotope Stage 5.

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