3,284 research outputs found

    The Dimension Six Triple Gluon Operator in Higgs+Jet Observables

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    Recently a lot of progress has been made towards a full classification of new physics effects in Higgs observables by means of effective dimension six operators. Specifically, Higgs production in association with a high transverse momentum jet has been suggested as a way to discriminate between operators that modify the Higgs-top coupling and operators that induce an effective Higgs-gluon coupling---a distinction that is hard to achieve with signal strength measurements alone. With this article we would like to draw attention to another source of new physics in Higgs+jet observables: the triple gluon operator O3gO_{3g} (consisting of three factors of the gluon field strength tensor). We compute the distortions of kinematic distributions in Higgs+jet production at a 14 TeV LHC due to O3gO_{3g} and compare them with the distortions due to dimension six operators involving the Higgs doublet. We find that the transverse momentum, the jet rapidity and the difference between the Higgs and jet rapidity are well suited to distinguish between the contributions from O3gO_{3g} and those from other operators, and that the size of the distortions are similar if the Wilson coefficients are of the same order as the expected bounds from other observables. We conclude that a full analysis of new physics in Higgs+jet observables must take the contributions from O3gO_{3g} into account.Comment: To appear as a Rapid Communication in Physical Review

    Aftershocks and Preearthquake Seismicity

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    Although primary surface faulting was mapped for nearly 30 km, aftershocks extended in a complex pattern more than 100 km along the trend of the Imperial fault. A first-motion focal mechanism for the main shock is consistent with right-lateral motion on a vertical fault striking N. 42° W., in agreement with the strike of the Imperial fault within the limits of resolution. There is evidence that conjugate faulting on a buried complementary northeast-trending structure occurred at the north limit of displacement on the Imperial fault near Brawley, Calif. This faulting was apparently initiated at the time of a magnitude 5.8 aftershock 8 hours after the main shock. A line of epicenters extending along the trend of the San Andreas fault nearly 100 km into the eastern Imperial Valley was noted during the aftershock sequence, in an area recognized as notably aseismic during the preceding 5 years. The main shock was preceded by a 3-month period of significantly reduced seismicity affecting the central Imperial Valley. Although three small events near the incipient epicenter during this interval may be deemed foreshocks, no distinct foreshocks immediately before the main shock were observed

    Happiness as stable extraversion : internal consistency reliability and construct validity of the Oxford Happiness Questionnaire among undergraduate students

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    The Oxford Happiness Questionnaire (OHQ) was developed by Hills and Argyle (2002) to provide a more accessible equivalent measure of the Oxford Happiness Inventory (OHI). The aim of the present study was to examine the internal consistency reliability, and construct validity of this new instrument alongside the Eysenckian dimensional model of personality. The Oxford Happiness Questionnaire was completed by a sample of 131 undergraduate students together with the abbreviated form of the Revised Eysenck Personality Questionnaire. The data demonstrated good internal consistency reliability (alpha = .92) and good construct validity in terms of positive association with extraversion (r = .38 p < .001) and negative association with neuroticism (r = −.57 p < .001). The kind of happiness measured by the OHQ is clearly associated with stable extraversion

    Executive function in first-episode schizophrenia

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    BACKGROUND: We tested the hypothesis that schizophrenia is primarily a frontostriatal disorder by examining executive function in first-episode patients. Previous studies have shown either equal decrements in many cognitive domains or specific deficits in memory. Such studies have grouped test results or have used few executive measures, thus, possibly losing information. We, therefore, measured a range of executive ability with tests known to be sensitive to frontal lobe function. METHODS: Thirty first-episode schizophrenic patients and 30 normal volunteers, matched for age and NART IQ, were tested on computerized test of planning, spatial working memory and attentional set shifting from the Cambridge Automated Neuropsychological Test Battery. Computerized and traditional tests of memory were also administered for comparison. RESULTS: Patients were worse on all tests but the profile was non-uniform. A componential analysis indicated that the patients were characterized by a poor ability to think ahead and organize responses but an intact ability to switch attention and inhibit prepotent responses. Patients also demonstrated poor memory, especially for free recall of a story and associate learning of unrelated word pairs. CONCLUSIONS: In contradistinction to previous studies, schizophrenic patients do have profound executive impairments at the beginning of the illness. However, these concern planning and strategy use rather than attentional set shifting, which is generally unimpaired. Previous findings in more chronic patients, of severe attentional set shifting impairment, suggest that executive cognitive deficits are progressive during the course of schizophrenia. The finding of severe mnemonic impairment at first episode suggests that cognitive deficits are not restricted to one cognitive domain

    Seismicity of Southern California: Earthquakes of ML 3.0 and Greater, 1975 through 1983

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    The time period since the last published California Institute of Technology (CIT) earthquake catalog (Hileman 1974; Friedman 1976) has seen many changes in data analysis and reporting procedures at the Seismological Laboratory. CIT merged its operation with the U.S. Geological Survey (USGS) during this period. Digital recording (Johnson 1979) was introduced in 1977 and computer systems improved several times since. The seismic network itself expanded from 125 stations in 1975 to more than 200 in early 1983 (Figure 1). The result is an agglomeration of data that way take a superhuman effort to sort through. Much use can be made, however, of a timely earthquake catalog which is restricted to the larger earthquakes. We therefore present as complete and reliable a list of events of ML 3.0 and greater as possible, comprising 3,650 individual earthquakes

    Characterization of Prepreg Tack for Composite Manufacturing by Automated Fiber Placement

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    Automated fiber placement (AFP) has become the industry standard for large-scale production of carbon fiber reinforced plastics (CFRP) to improve rate and reduce defects associated with manual layup. Still, defects generated during AFP processes require manual, painstaking inspection by technicians and rework of the part when substantial defects are found. Prepreg (carbon fiber infused with uncured epoxy resin) tack is one of the primary factors that influences the generation of defects that arise during auto-mated fiber placement (AFP). Tack, as it relates to AFP processes and defect formation, can be understood as a combination of two stages, cohesion and decohesion. During the cohesion phase, two pieces of prepreg are brought into contact under elevated temperature and pressure. Compaction of the resin within the contact area will result in a degree of intimate contact, I, between the mating prepreg surfaces. Defect formation, as a result of decohesion between prepreg surfaces, occurs after the cohesion phase and arises due to stress from events such as fiber placement over an existing defect, on a contoured path, etc. (Figure 1). Tack strength resists the displacement of prepreg on a surface due to stresses developed during deposition

    The 3 December 1988 Pasadena, California earthquake: Evidence for strike-slip motion on the Raymond fault

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    The Pasadena earthquake (M_L = 4.9) occurred on 3 December 1988, at a depth of 16 km. The hypocenters of the earthquake and its aftershocks define a east-northeast striking, steeply northwest-dipping surface that projects up to the active surficial trace of the Raymond fault. One of the nodal planes of the focal mechanism of the earthquake parallels the Raymond fault with left-lateral strike-slip movement on that plane, and is consistent with geomorphic and paleoseismic evidence that the Raymond fault is dominantly a left-lateral strike-slip fault. The existence of a component of sinistral slip along the Raymond fault had been suspected prior to the earthquake, but the northward dip of the fault and the prominent scarp along the western portion of its trace had led most workers to conclude that slip along the fault was dominantly reverse
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