Measurement of the Polarization of W Bosons with Large Transverse Momenta in W plus jets Events at the LHC

Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)

Bose-Einstein correlations in W-pair decays

Bose-Einstein correlations are studied in semileptonic (WW → qq̄lv) and fully hadronic (WW → qq̄qq̄) W-pair decays with the ALEPH detector at LEP at centre-of-mass energies of 172, 183 and 189 GeV. They are compared with those made at the Z peak after correction for the different flavour compositions. A Monte Carlo model of Bose-Einstein correlations based on the JETSET hadronization scheme was tuned to the Z data and reproduces the correlations in the WW → qq̄lv events. The same Monte Carlo reproduces the correlations in the WW → qq̄qq̄ channel assuming independent fragmentation of the two W's. A variant of this model with Bose-Einstein correlations between decay products of different W's is disfavoured. (C) 2000 Published by Elsevier Science B.V.

The cohomological invariant E'(G,W) and some properties

Let G be a group, W a nonempty G-set and M a Z2G-module. Consider the restriction map resG W : H1(G,M) → Pi wi∈E H1(Gwi,M), [f] → (resGG wi [f])i∈I , where E = {wi, i ∈ I} is a set of orbit representatives in W and Gwi = {g ∈ G | gwi = wi} is the G-stabilizer subgroup (or isotropy subgroup) of wi, for each wi ∈ E. In this work we analyze some results presented in Andrade et al [5] about splittings and duality of groups, using the point of view of Dicks and Dunwoody [10] and the invariant E'(G,W) := 1+dimkerresG W, defined when Gwi is a subgroup of infinite index in G for all wi in E, andM = Z2 (where dim = dimZ2). We observe that the theory of splittings of groups (amalgamated free product and HNN-groups) is inserted in the combinatory theory of groups which has many applications in graph theory (see, for example, Serre [12] and Dicks and Dunwoody [10]).

Na 1 Nachlass Max Horkheimer, 11 - Korrespondenzen u.a. mit Edward M. David (p. I 6, 1-183)

1 Brief von Fritz Dannenbaum an Max Horkheimer, 26.11.1935; 2 Briefe zwischen F. Darnbacher und Max Horkheimer, 24.01.1936, 22.01.1936; 3 Briefe zwischen dem Dartmouth College Hanover N.H. und Max Horkheimer, 1939-1941. 06.05.1939; 14 Briefe zwischen Edward M. David und Max Horkheimer, 1941-1942; 1 Brief von der Day Cornell University, Ithaca N.Y. an Max Horkheimer, 24.02.1939; 2 Briefe zwischen Margaret Deaner und Max Horkheimer, 01.04.1935, 04.04.1935; 1 Brief von Max Horkheimer an Hanna Deinhard, 05.01.1949; 1 Brief von Deiters an Max Horkheimer, 26.11.1935; 2 Briefe zwischen Laura Demick und Max Horkheimer, 22.12.1941, 29.12.1941; 2 Briefe zwischen Grace Dertz und Max Horkheimer, 18.10.1934, 11.10.1934; 1 Brief von Max Horkheimer an Dekan, 20.06.1940; 1 Brief von Max Dessoir an Max Horkheimer, 29.08.1937; 1 Brief von Max Horkheimer an Deutschland / deutsches Reich Minister für Wissenschaft, Kunst und Volksbildung, Berli, 21.04.1933; 4 Briefe zwischen John Dewey und Max Horkheimer, 1940-1941, 20.02.1941; 1 Brief von Max Horkheimer an Walter Strauss, 20.02.1941; 3 Briefe zwischen Frederic Dewhurst und Max Horkheimer, 1939, 08.02.1939; 5 Briefe zwischen dem Soziograph Jul Diederich und Max Horkheimer, 1934-1938; 1 Brief von Max Horkheimer an Hugo Sinzheimer, 20.10.1934; 15 Briefe zwischen William Dieterle, Charlotte Dieterle und Max Horkheimer, 1940-1944; 1 Brief von der Dillmann-Oberschule Stuttgart an Max Horkheimer, 13.12.1949; 1 Brief vonMax Horkheimer an W. R. Dittmar, 10.02.1938; 2 Briefe zwischen Sofie Doernberg, Paul Doernberg und Margot von Mendelssohn, 1942, 06.04.1942; 4 Briefe zwischen Willy Dörter und Max Horkheimer, 1936-1937, 20.02.1936; 1 Brief von Georg Glaser anMax Horkheimer; 3 Briefe zwischen Hans Venedey und Max Horkheimer, 22.01.1938, 1938; 28 Briefe sowie Zeitungsausschnitte zwischen Juliette Favez und Max Horkheimer, 1934-1938; 1 Brief von Juliette Favez ann karl Dörter, 02.10.1934; 2 Briefe von Max Horkheimer an Hans Klaus Brill, Januar 1938; 3 Briefe zwischen Karl Dörter und Max Horkheimer, 1934-1937, 12.10.1934; 4 Briefe zwischen Andrés Sternheim und Max Horkheimer, 1937, 16.06.1937; 1 Brief von Else Klee an Max Horkheimer, 13.06.1935;

El teatro y el Príncipe : La representación del rey en la Henriada de W. Shakespeare

El teatro es el espacio público más significativo en lo que respecta a la construcción de representaciones en la sociedad de la modernidad. En este sentido, indagaremos sobre las representaciones del poder, particularmente sobre la legitimidad monárquica en el teatro isabelino. Nos centraremos en las obras denominadas Henriada de W. Shakespeare, un autor que se ha detenido particularmente en la figura del rey, del príncipe y de las relaciones de alta política. Indagación que tiene como fin introducirse en la problemática de la legitimidad monárquica a la luz de los sucesos ocurridos en una Europa donde la discusión sobre el poder tendrá importantes consecuencias en los desarrollos posteriores del Estado moderno

El teatro y el Príncipe : La representación del rey en la Henriada de W. Shakespeare

El teatro es el espacio público más significativo en lo que respecta a la construcción de representaciones en la sociedad de la modernidad. En este sentido, indagaremos sobre las representaciones del poder, particularmente sobre la legitimidad monárquica en el teatro isabelino. Nos centraremos en las obras denominadas Henriada de W. Shakespeare, un autor que se ha detenido particularmente en la figura del rey, del príncipe y de las relaciones de alta política. Indagación que tiene como fin introducirse en la problemática de la legitimidad monárquica a la luz de los sucesos ocurridos en una Europa donde la discusión sobre el poder tendrá importantes consecuencias en los desarrollos posteriores del Estado moderno

Calcareous nannofossil stratigraphy, nannofossil events and carbon isotopic ratios of ODP Leg 183 sites

Cores from Sites 1135, 1136, and 1138 of Ocean Drilling Program Leg 183 to the Kerguelen Plateau (KP) provide the most complete Paleocene and Eocene sections yet recovered from the southern Indian Ocean. These nannofossil-foraminifer oozes and chalks provide an opportunity to study southern high-latitude biostratigraphic and paleoceanographic events, which is the primary subject of this paper. In addition, a stable isotope profile was established across the Cretaceous/Tertiary (K/T) boundary at Site 1138. An apparently complete K/T boundary was recovered at Site 1138 in terms of assemblage succession, isotopic signature, and reworking of older (Cretaceous) nannofossil taxa. There is a significant color change, a negative carbon isotope shift, and nannofossil turnover. The placement of the boundary based on these criteria, however, is not in agreement with the available shipboard paleomagnetic stratigraphy. We await shore-based paleomagnetic study to confirm or deny those preliminary results. The Paleocene nannofossil assemblage is, in general, characteristic of the high latitudes with abundant Chiasmolithus, Prinsius, and Toweius. Placed in context with other Southern Ocean sites, the biogeography of Hornibrookina indicates the presence of some type of water mass boundary over the KP during the earliest Paleocene. This boundary disappeared by the late Paleocene, however, when there was an influx of warm-water discoasters, sphenoliths, and fasciculiths. This not only indicates that during much of the late Paleocene water temperatures were relatively equable, but preliminary floral and stable isotope analyses also indicate that a relatively complete record of the late Paleocene Thermal Maximum event was recovered at Site 1135. It was only at the beginning of the middle Eocene that water temperatures began to decline and the nannofossil assemblage became dominated by cool-water species while discoaster and sphenolith abundances and diversity were dramatically reduced. One new taxonomic combination is proposed, Heliolithus robustus Arney, Ladner, and Wise.

El teatro y el Príncipe : La representación del rey en la Henriada de W. Shakespeare

El teatro es el espacio público más significativo en lo que respecta a la construcción de representaciones en la sociedad de la modernidad. En este sentido, indagaremos sobre las representaciones del poder, particularmente sobre la legitimidad monárquica en el teatro isabelino. Nos centraremos en las obras denominadas Henriada de W. Shakespeare, un autor que se ha detenido particularmente en la figura del rey, del príncipe y de las relaciones de alta política. Indagación que tiene como fin introducirse en la problemática de la legitimidad monárquica a la luz de los sucesos ocurridos en una Europa donde la discusión sobre el poder tendrá importantes consecuencias en los desarrollos posteriores del Estado moderno

Silicoflagellate abundance in ODP Holes 183-1138A and 183-1140A

The biostratigraphic distribution and abundance of lower Oligocene and Miocene to Pleistocene silicoflagellates are documented from Ocean Drilling Program Leg 183 Holes 1138A and 1140A, on the Kerguelen Plateau. The Distephanus speculum speculum forma pseudofibula plexus is found in the upper Miocene in Hole 1138A, but other important biostratigraphic markers are not available. Diversity and abundance of silicoflagellates vary considerably in Hole 1138A, with silicoflagellates more abundant in the Pliocene and Pleistocene and some intervals of the Miocene barren of silicoflagellates or containing only limited numbers of specimens. The silicoflagellates of Hole 1140A include a new skeletal morphology, described here as Distephanus speculum speculum forma cylindrus. Silicoflagellates were generally abundant throughout the lower and middle Miocene in Hole 1140A.

Diatom biostratigraphy and datum events of ODP Hole 183-1140A

Ocean Drilling Program (ODP) Leg 183 Site 1140 provided a lower Oligocene to middle Miocene record of diatom assemblages from the northern Kerguelen Plateau. Samples were examined to improve the resolution of shipboard diatom biostratigraphy. The material is complementary to that recovered during ODP Legs 119 and 120, and the diatom zonation of Harwood and Maruyama could be readily applied. A standard succession of biostratigraphic zones from the middle Miocene and lower Oligocene was delineated, although some zones were unrecognizable because of poor core recovery. The detailed diatom biostratigraphy presented here agrees well with shipboard calcareous nannofossil biostratigraphy. Sediment accumulation rates based on diatom bioevents average 1.26 cm/k.y.

Nannofossil and stable isotope record across the Paleocene/Eocene Thermal Maximum in ODP Hole 183-1135A

The Paleocene/Eocene Thermal Maximum (PETM, ca. 55 Ma) is an abrupt, profound perturbation of climate and the carbon cycle associated with a massive injection of isotopically light carbon into the ocean-atmosphere system. As such, it provides an analogue for understanding the interplay between phytoplankton and climate under modern anthropogenic global-warming conditions. However, the accompanying enhanced dissolution poses uncertainty on the reconstruction of the affected ecology and productivity. We present a high-resolution record of bulk isotopes and nannofossil absolute abundance from Ocean Drilling Program (ODP) Site 1135 on the Kerguelen Plateau, Southern Indian Ocean to quantitatively constrain for the first time the influence of dissolution on paleoecological reconstruction. Our bulk-carbonate isotope record closely resembles that of the classic PETM site at ODP Site 690 on the opposite side of the Antarctic continent, and its correlation with those from ODP Sites 690, 1262 and 1263 records allows recognition of 14 precessional cycles upsection from the onset of the carbon isotopic excursion (CIE). This, together with a full range of common Discoasteraraneus and an abundance crossover between Fasciculithus and Zygrhablithusbijugatus, indicates the presence of the PETM at Site 1135, a poorly known record with calcareous fossils throughout the interval. The strong correlation between the absolute abundances of Chiasmolithus and coccolith assemblages reveals a dominant paleoecological signal in the poorly preserved fossil assemblages, while the influence of dissolution is only strong during the CIE. This suggests that r-selected taxa can preserve faithful ecological information even in the severely-altered assemblages studied here, and therefore provide a strong case for the application of nannofossils to paleoecological studies in better-preserved PETM sections. The inferred nannoplankton productivity drops abruptly at the CIE onset, but rapidly increases after the CIE peak, both of which may be driven by nutrient availability related to ocean stratification and vertical mixing due to changed sea-surface temperatures.

Diatom biostratigraphy, Argon ages and chronology of ODP Hole 183-1138A

A thick Neogene section was recovered in the upper ~300 m of Ocean Drilling Program Hole 1138A, drilled on the Central Kerguelen Plateau in the Indian sector of the Southern Ocean. Sediment lithologies consist primarily of mixed carbonate and biosiliceous clays and oozes, with several thin (1-3 cm) tephra horizons. The tephras are glass rich, well sorted, and dominantly trachytic to rhyolitic in composition. Volcaniclastic material in these horizons is interpreted to have originated from Heard Island, 180 km northwest of Site 1138, and was likely emplaced through both primary ash fall and turbiditic, submarine flows. A Neogene age-depth model for Hole 1138A is constructed primarily from 36 diatom biostratigraphic datums. Nannofossil and planktonic foraminifer biostratigraphy provides supporting age information. Additionally, four high-precision 40Ar-39Ar ages are derived from ash and tephra horizons, and these radiometric ages are in close agreement with the biostratigraphic ages. The integrated age-depth model reveals a reasonably complete lower Miocene to upper Pleistocene section in Hole 1138A, with the exception of a ~1-m.y. hiatus at the Miocene/Pliocene boundary. Another possible hiatus is also identified at the Oligocene/Miocene boundary. High Neogene sedimentation rates and the presence of both calcareous and siliceous microfossils, combined with datable tephra horizons, establish Site 1138 as a suitable target for future drilling legs with paleoceanographic objectives. This report also proposes two new diatom species, Fragilariopsis heardensis and Azpeitia harwoodii, from Pliocene strata of Hole 1138A.