735 resultados para Vertex Coloring
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The aim of this study was to assess the influence of the quantity of coloring agent on the bleaching efficiency of gels containing 35% H2O2. Sixty human third molars were sectioned mesiodistally, darkened in a coffee solution and sectioned in the occlusal-cervical direction, resulting in mesial (not bleached) and distal halves (bleached). They were distributed into three groups: Whiteness HP, Total Bleach, and Whiteform Perox Red Gel; and subdivided into four sub-groups: no coloring agent, manufacturer's standard, double the standard, and triple the standard. The gels were activated with light-ermitting diode/laser appliances. The images were analyzed with the Adobe Photoshop program (deltaEL*a*b*). The variation was submitted to the ANOVA test (two factors: type of gel and quantity of coloring agent) and Tukey test. Differences were observed for the quantity of coloring agent. The mean (+/-SD) was determined for each quantity of coloring used: no coloring agent -6.85 (+/-2.26)a, manufacturer's standard -794 (+/-2.55)ab, double the standard -8.65 (+/-2.47)b, triple the standard -9.05 (+/-2.72)b. In conclusion, the standard quantity of coloring agent did not provide significantly more intense bleaching than when it was completely absent. The use of double and triple the amount provided greater bleaching than that observed for the gel without coloring agent. No significant differences were observed between the tested gels.
Untersuchungen am Drei-Eichbosonen-Vertex der elektroschwachen Wechselwirkung mit dem ALEPH-Detektor
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In der vorliegenden Arbeit werden vom ALEPH-Detektor am Speicherring LEP des CERN in Genf genommene Datenmengen aus den Jahren 1997 bis 1999 analysiert und sowohl Kopplungsparameter am Drei-Eichbosonen-Vertex derW-Boson-Paarproduktion, als auch die Anteile longitudinal beziehungsweise transversal polarisierter W-Bosonen, bei Schwerpunktsenergien von 183 GeV bis 202 GeV bestimmt. Betrachtet wird der rein leptonische Zerfallskanal, in dembeide W-Bosonen in ein Elektron-Neutrino- oder ein Myon-Neutrino-Paar zerfallen, der einen geringen Wirkungsquerschnitt aufweist, aber eine klareDetektorsignatur. Die aufgezeichneten Ereignisse werden selektiert und dabei eine Reinheit von durchschnittlich 72% erreicht. Der Hauptuntergrund besteht aus W-Boson-Paaren, bei denen zumindest ein W-Boson in ein Tauon-Neutrino-Paarzerfällt. Dieser Kanal zeigt ein sehr signalähnliches Verhalten. Die selektierten Ereignisse werden kinematisch rekonstruiert, um die Winkelverteilungen der Zerfallsprodukte der W-Bosonen zu extrahieren. Aus den Polarwinkelverteilungen der geladenen Zerfallsprodukte der W-Bosonen werden die Anteile longitudinal beziehungsweise transversal polarisierterW-Bosonen durch Anpassung der theoretischen Vorhersage an die selektierten Daten bestimmt. Dabei wird gefunden, daß f? = (71,6 ? 6,4_{stat.} ? 3,7_{syst.}) % der produzierten W-Bosonen transversal polarisiert sind, in Übereinstimmung mit der Vorhersage des Standardmodells (75,1%). Dieser Wert ist ein erster Hinweis auf die Kopplungsparameter am Drei-Eichbosonen-Vertex. Die CP-erhaltenden allgemeinen Kopplungsparameter $g_{rm Z}^1$, $kappa_gamma$ und $lambda_gamma$ werden bestimmt zu: $g_{rm Z}^1 = {{1,19^{+0,13}_{-0,16}}_{stat.}} {^{+0,09}_{-0,09}}_{syst.}$,$kappa_gamma = {{1,06^{+0,27}_{-0,09}}_{stat.}} {^{+0,08}_{-0,08}}_{syst.}$,$lambda_gamma = {{0,16^{+0,11}_{-0,13}}_{stat.}} {^{+0,08}_{-0,08}}_{syst.}$. Das Standardmodell sagt $g_{rm Z}^1 = 1$, $kappa_gamma = 1$ und $lambda_gamma = 0$ voraus. Mit diesen Kopplungsparametern lassen sich das magnetischeDipolmoment und das elektrische Quadrupolmoment der W-Bosonen bestimmen zu: $mu_{rm W} = frac{e}{2m_{rm W}} cdot (2,22^{+0,31}_{-0,19})$,$q_{rm W} = - frac{e}{m_{rm W}^2} cdot (0,90^{+0,32}_{-0,18})$. Die Messung der Kopplungsparameter stellt einen wichtigen Test des minimalen Standardmodells dar. In einem Jahr wird es möglich sein, diesen Test mit allen Daten aus der Phase II des Betriebs von LEP durchzuführen und die Genauigkeit durch Kombination mit anderen LEP-Experimenten zu erhöhen.
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Nella tesi vengono presentate alcune relazioni fra gruppi quantici e modelli reticolari. In particolare si associa un modello vertex a una rappresentazione di un'algebra inviluppante quantizzata affine e si mostra che, specializzando il parametro quantistico ad una radice dell'unità, si manifestano speciali simmetrie.
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Chapter 1 is used to introduce the basic tools and mechanics used within this thesis. Some historical uses and background are touched upon as well. The majority of the definitions are contained within this chapter as well. In Chapter 2 we consider the question whether one can decompose λ copies of monochromatic Kv into copies of Kk such that each copy of the Kk contains at most one edge from each Kv. This is called a proper edge coloring (Hurd, Sarvate, [29]). The majority of the content in this section is a wide variety of examples to explain the constructions used in Chapters 3 and 4. In Chapters 3 and 4 we investigate how to properly color BIBD(v, k, λ) for k = 4, and 5. Not only will there be direct constructions of relatively small BIBDs, we also prove some generalized constructions used within. In Chapter 5 we talk about an alternate solution to Chapters 3 and 4. A purely graph theoretical solution using matchings, augmenting paths, and theorems about the edgechromatic number is used to develop a theorem that than covers all possible cases. We also discuss how this method performed compared to the methods in Chapters 3 and 4. In Chapter 6, we switch topics to Latin rectangles that have the same number of symbols and an equivalent sized matrix to Latin squares. Suppose ab = n2. We define an equitable Latin rectangle as an a × b matrix on a set of n symbols where each symbol appears either [b/n] or [b/n] times in each row of the matrix and either [a/n] or [a/n] times in each column of the matrix. Two equitable Latin rectangles are orthogonal in the usual way. Denote a set of ka × b mutually orthogonal equitable Latin rectangles as a k–MOELR(a, b; n). We show that there exists a k–MOELR(a, b; n) for all a, b, n where k is at least 3 with some exceptions.
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A dedicated reconstruction algorithm to find decay vertices in the ATLAS muon spectrometer is presented. The algorithm searches the region just upstream of or inside the muon spectrometer volume for multi-particle vertices that originate from the decay of particles with long decay paths. The performance of the algorithm is evaluated using both a sample of simulated Higgs boson events, in which the Higgs boson decays to long-lived neutral particles that in turn decay to b final states, and pp collision data at √s = 7 TeV collected with the ATLAS detector at the LHC during 2011.
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A search for the direct production of charginos and neutralinos in final states with three electrons or muons and missing transverse momentum is presented. The analysis is based on 4.7 fb(-1) of root s = 7 TeV proton-proton collision data delivered by the Large Hadron Collider and recorded with the ATLAS detector. Observations are consistent with Standard Model expectations in three signal regions that are either depleted or enriched in Z-boson decays. Upper limits at 95% confidence level are set in R-parity conserving phenomenological minimal supersymmetric models and in simplified models, significantly extending previous results.
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Many extensions of the Standard Model posit the existence of heavy particles with long lifetimes. In this Letter, results are presented of a search for events containing one or more such particles, which decay at a significant distance from their production point, using a final state containing charged hadrons and an associated muon. This analysis uses a data sample of proton-proton collisions at root s = 7 TeV corresponding to an integrated luminosity of 4.4 fb(-1) collected in 2011 by the ATLAS detector operating at the Large Hadron Collider. Results are interpreted in the context of R-parity violating supersymmetric scenarios. No events in the signal region are observed and limits are set on the production cross section for pair production of supersymmetric particles, multiplied by the square of the branching fraction for a neutralino to decay to charged hadrons and a muon, based on the scenario where both of the produced supersymmetric particles give rise to neutralinos that decay in this way. However, since the search strategy is based on triggering on and reconstructing the decay products of individual long-lived particles, irrespective of the rest of the event, these limits can easily be reinterpreted in scenarios with different numbers of long-lived particles per event. The limits are presented as a function of neutralino lifetime, and for a range of squark and neutralino masses.
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A series of long-chain (C37, C38, C39), primarily di and tri-unsaturated methyl and ethyl ketones, first identified in sediments from Walvis Ridge off West Africa and from Black Sea (de Leeuw et al., 1979), has been found in marine sediments throughout the world (Brassell et al., 1986 doi:10.1038/320129a0). The marine coccolithophorid Emiliania huxleyi and members of the class Prymnesiophyceae are now the recognized sources of these compounds (Volkman et al., 1979; Marlowe, et al., 1984). Experiments with laboratory cultures of algae showed the degree of unsaturation in the ketone seris biosynthesized depends on growth temperature (Brassell et al., 1986; Marlowe, 1984), a physiological respons observed for classical membrane lipids (vanDeenen et al., 1972). Brassell and co-workers (Brassell et al., 198; Brassell et al., 1986b) thus proposed that systematic fluctuations in the unsaturation of these alkenones noted down-core in sediments from the Kane Gap region of the north-east tropical Atlantic Ocean and correlated with glacial-interglacial cycles provide an organic geochemical measure of past sea-surface water temperatures. Using laboratory cultures of E. huxleyi, we have calibrated changes in the unsaturation pattern of the long-chain ketone series versus growth temperature. The calibration curve is linear and accurtely predicts unsuturation patterns observed in natural particulate materials collected from oceanic waters of known temperature. We present evidence supporting the proposed paleotemperature hypothesis (Brassell et al., 1986, Brassel et al., 1986b) and suggesting absolute 'sea-surface temperatures' for a given oceanic location can be estimated from an analysis of long-chain ketone compositions preserved in glacial and interglacial horizons of deep-sea sediment cores.
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In this paper we propose four approximation algorithms (metaheuristic based), for the Minimum Vertex Floodlight Set problem. Urrutia et al. [9] solved the combinatorial problem, although it is strongly believed that the algorithmic problem is NP-hard. We conclude that, on average, the minimum number of vertex floodlights needed to illuminate a orthogonal polygon with n vertices is n/4,29.
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Presents children in grade 1 through 3 with information about environmental dangers and ecology.
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"References" at end of each chapter.
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Mode of access: Internet.