994 resultados para 333.8


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O presente estudo teve por finalidade avaliar o efeito de um estimulante vegetal, Agrostemin, no desenvolvimento de plantas de soja (Glycine max (L.) Merrill cv. IAC-8), através de alguns parâmetros que compõem a análise de crescimento. O experimento foi conduzido em casa de vegetação. Foram estudados seis tratamentos, correspondentes às seguintes dosagens, épocas e formas de aplicação: testemunha (T1); 0,125g de Agrostemin/100g sementes (T2); 0,125g de Agrostemin/l00g sementes e pulverização foliar à 333 ppm (T3); 0,125g de Agrostemin/100g sementes e pulverização foliar à 500 ppm (T4); pulverização foliar à 333 ppm (T5) e pulverização foliar à 500 ppm (T6). Realizaram-se três épocas de coleta, à intervalos de 14 dias. O experimento foi em delineamento inteiramente casualizado. Os parâmetros estudados foram: razão de área foliar (RAF), taxa assimilatória líquida (TAL) e taxa de crescimento relativo (TCR). Dentre os resultados obtidos, concluiu-se que à medida que aumentou-se a concentração, diminuiram-se os parâmetros estudados, no intervalo 71-85.

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A search for pair production of third-generation scalar leptoquarks and supersymmetric top quark partners, top squarks, in final states involving tau leptons and bottom quarks is presented. The search uses events from a data sample of proton-proton collisions corresponding to an integrated luminosity of 19.7 fb(-1), collected with the CMS detector at the LHC with root s = 8 TeV. The number of observed events is found to be in agreement with the expected standard model background. Third-generation scalar leptoquarks with masses below 740 GeV are excluded at 95% confidence level, assuming a 100% branching fraction for the leptoquark decay to a tau lepton and a bottom quark. In addition, this mass limit applies directly to top squarks decaying via an R-parity violating coupling. lambda(') (333). The search also considers a similar signature from top squarks undergoing a chargino-mediated decay involving the Rparity violating coupling. lambda(')(3jk). Each top squark decays to a tau lepton, a bottom quark, and two light quarks. Top squarks in this model with masses below 580 GeV are excluded at 95% confidence level. The constraint on the leptoquark mass is the most stringent to date, and this is the first search for top squarks decaying via. lambda(')(3jk). (C) 2014 The Authors. Published by Elsevier B. V.

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16 Briefe zwischen Ruth Nanda Anshen und Max Horkheimer, 1938-1941; 5 Briefe zwischen Peter Appel und Max Horkheimer, 1937; 1 Drucksache der Arbeitsgemeinschaft Sozialistischer Ärzte in Hessen, Juli 1949; 1 Brief der Arbeitsgemeinschaft für Soziale Betriebsgestaltung in Heidelberg an Max Horkheimer, 18.10.1949; 2 Briefe zwischen Lois Archer und Max Horkheimer, 24.07.1947, 04.08.1947; 2 Briefe zwischen Camille Arnaud und Max Horkheimer, 03.03.1946, 22.03.1946; 39 Briefe zwischen Raymond Aron und Max Horkheimer, 1935-1938; 2 Briefe zwischen Ruth Arrau und Max Horkheimer, 28.06.1949, 10.10.1949; 3 Briefe zwischen S. Aufhauser und Max Horkheimer, 1939-1941, 16.04.1941; 8 Briefe zwischen der Zeitschrift 'Aufbau' und Max Horkheimer, 1944-1944; 3 Briefe zwischen der Automobile Club of New York und Max Horkheimer, 1937, 10.08.1937;

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Reaktion auf eine "Strafpredigt", "Bis zum letzten Tropfen Blut", Bundesschießen, Rede an die Schützen aus Schwaben, Toast auf Frankfurt, Herbert von Bismarck, Hedwig Wilhelmi

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The mechanical behavior of the plate boundary fault zone is of paramount importance in subduction zones, because it controls megathrust earthquake nucleation and propagation as well as the structural style of the forearc. In the Nankai area along the NanTroSEIZE (Kumano) drilling transect offshore SW Japan, a heterogeneous sedimentary sequence overlying the oceanic crust enters the subduction zone. In order to predict how variations in lithology, and thus mechanical properties, affect the formation and evolution of the plate boundary fault, we conducted laboratory tests measuring the shear strengths of sediments approaching the trench covering each major lithological sedimentary unit. We observe that shear strength increases nonlinearly with depth, such that the (apparent) coefficient of friction decreases. In combination with a critical taper analysis, the results imply that the plate boundary position is located on the main frontal thrust. Further landward, the plate boundary is expected to step down into progressively lower stratigraphic units, assisted by moderately elevated pore pressures. As seismogenic depths are approached, the décollement may further step down to lower volcaniclastic or pelagic strata but this requires specific overpressure conditions. High-taper angle and elevated strengths in the toe region may be local features restricted to the Kumano transect.

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