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This paper reports on Monte Carlo simulation results for future measurements of the moduli of time-like proton electromagnetic form factors, |GE | and |GM|, using the ¯pp → μ+μ− reaction at PANDA (FAIR). The electromagnetic form factors are fundamental quantities parameterizing the electric and magnetic structure of hadrons. This work estimates the statistical and total accuracy with which the form factors can be measured at PANDA, using an analysis of simulated data within the PandaRoot software framework. The most crucial background channel is ¯pp → π+π−,due to the very similar behavior of muons and pions in the detector. The suppression factors are evaluated for this and all other relevant background channels at different values of antiproton beam momentum. The signal/background separation is based on a multivariate analysis, using the Boosted Decision Trees method. An expected background subtraction is included in this study, based on realistic angular distribuations of the background contribution. Systematic uncertainties are considered and the relative total uncertainties of the form factor measurements are presented.
The Transition Radiation Detector (TRD) was designed and built to enhance the capabilities of the ALICE detector at the Large Hadron Collider (LHC). While aimed at providing electron identification and triggering, the TRD also contributes significantly to the track reconstruction and calibration in the central barrel of ALICE. In this paper the design, construction, operation, and performance of this detector are discussed. A pion rejection factor of up to 410 is achieved at a momentum of 1 GeV/c in p-Pb collisions and the resolution at high transverse momentum improves by about 40% when including the TRD information in track reconstruction. The triggering capability is demonstrated both for jet, light nuclei, and electron selection.
The Transition Radiation Detector (TRD) was designed and built to enhance the capabilities of the ALICE detector at the Large Hadron Collider (LHC). While aimed at providing electron identification and triggering, the TRD also contributes significantly to the track reconstruction and calibration in the central barrel of ALICE. In this paper the design, construction, operation, and performance of this detector are discussed. A pion rejection factor of up to 410 is achieved at a momentum of 1 GeV/c in p-Pb collisions and the resolution at high transverse momentum improves by about 40% when including the TRD information in track reconstruction. The triggering capability is demonstrated both for jet, light nuclei, and electron selection.
The Transition Radiation Detector (TRD) was designed and built to enhance the capabilities of the ALICE detector at the Large Hadron Collider (LHC). While aimed at providing electron identification and triggering, the TRD also contributes significantly to the track reconstruction and calibration in the central barrel of ALICE. In this paper the design, construction, operation, and performance of this detector are discussed. A pion rejection factor of up to 410 is achieved at a momentum of 1 GeV/c in p–Pb collisions and the resolution at high transverse momentum improves by about 40% when including the TRD information in track reconstruction. The triggering capability is demonstrated both for jet, light nuclei, and electron selection.
Ein intaktes Arbeitsgedächtnis ermöglicht es, Informationen, z.B. visuellen oder auditorischen Ursprungs temporär zu speichern, zu manipulieren und weiterzuverarbeiten. Es bildet die Grundlage zum Lernen, zum Begreifen und zum Verstehen von Sprache und somit die Grundlage zum tagtäglichen Funktionieren.
Beeinträchtigungen des Arbeitsgedächtnisses sind mit schlechten (Arbeits-) Leistungen, eingeschränkter zwischenmenschlicher Kommunikation, niedrigerem gesellschaftlichem Funktionsniveau und Arbeitslosigkeit vergesellschaftet und somit folgenschwer.
Psychiatrische Erkrankungen aus dem schizophrenen Spektrum, die unipolare Depression oder das Aufmerksamkeitsdefizit-Hyperaktivitätssyndrom (ADHS) gehen gehäuft mit kognitiven Beeinträchtigungen einher. Auch die bipolare affektive Störung zählt zu den psychiatrischen Erkrankungen, die mit kognitiver Beeinträchtigung assoziiert ist.
Das Ziel der Studie war es, darzustellen, dass kognitive Einschränkungen von Patienten, die an einer bipolaren affektiven Störung leiden, unter den exekutiven Funktionen insbesondere das Arbeitsgedächtnis betreffen und diese auch in euthymer Stimmungslage zu erfassen sind.
Hierzu wurde mittels einer Aufgabe zur Farbveränderung vier verschiedener Kreise, die um ein zentral platziertes, schwarzes Kreuz angeordnet waren, das visuelle Arbeitsgedächtnis anhand der Merkfähigkeit der Patienten, deren euthyme Stimmungslage mit den Ratingskalen MADRS und YMRS bestätigt wurde, im Vergleich zu einer Gruppe gesunder Kontrollprobanden, die mit der Patientengruppe in den Faktoren Alter, Geschlechterverteilung, prämorbide Intelligenz, Schulbildung und Händigkeit vergleichbar war, überprüft.
Anhand der erzielten Ergebnisse wurde die Arbeitsgedächtniskapazität K nach Pashler bestimmt. Es ergab sich eine bei mittlerer Effektstärke signifikant geringere Arbeitsgedächtniskapazität in der Gruppe der remittierten Patienten mit bipolarer affektiver Störung im Vergleich zur Kontrollgruppe gesunder Probanden.
Ein Einfluss der zum Zeitpunkt der Testung in der Patientengruppe angewandten Psychopharmaka auf die Arbeitsgedächtniskapazität konnte ausgeschlossen werden, sodass die ermittelten Defizite nicht als eine Form von Medikamentennebenwirkungen erklärt werden konnten. Interessanterweise betrug die mediane Erkrankungsdauer in der Patientengruppe drei Jahre, sodass davon auszugehen ist, dass die Ausprägung von Defiziten des Arbeitsgedächtnisses keinen langen Krankheitsverlauf bedingt, sondern bereits zu Beginn der Erkrankung vorhanden sein könnte.
Somit konnte die Studie darlegen, dass kognitive Defizite, insbesondere Störungen des Arbeitsgedächtnisses mit daraus resultierender signifikant erniedrigter Arbeitsgedächtniskapazität, bei Patienten mit bipolarer affektiver Störung in euthymer Stimmungslage bereits zu einem frühen Zeitpunkt des Krankheitsverlaufs bestehen, die eine Folge der Erkrankung selbst sind und keine Nebenwirkung von psychopharmazeutischer Medikation darstellen. Den Grund für das Auftreten kognitiver Defizite bei Patienten mit bipolarer affektiver Störung liefert diese Studie nicht, sie impliziert dennoch, dass das Verständnis und die Berücksichtigung kognitiver Störungen bei der bipolaren affektiven Störung zukünftig ein wichtiges Therapieziel darstellen sollte um das funktionelle Outcome von Patienten, die an dieser Störung leiden, entscheidend zu verbessern und somit eine Teilnahme am tagtäglichen Funktionieren weiterhin ermöglicht wird.
In die Zukunft blickend sollten unsere Ergebnisse mithilfe weiterer Untersuchungen validiert werden, insbesondere in Bezug auf genetische Komponenten, die die Arbeitsgedächtniskapazität regulieren. Es sollten Faktoren identifiziert werden, die eine reduzierte Arbeitsgedächtniskapazität bei Patienten mit bipolarer affektiver Störung bedingen. Die vorliegende Studie beantwortet nämlich nicht die Frage, wie genetische Faktoren und Umweltfaktoren die Arbeitsgedächtniskapazität auf kognitiver und neurophysiologischer Ebene beeinflussen könnten.
Angesichts der erwähnten Relevanz eines intakten Arbeitsgedächtnisses für die Funktionsfähigkeit der Patienten sollten zukünftige Studien prüfen, ob prokognitive Interventionen wie die kognitive Remediation oder sogar medikamentöse Therapieoptionen diese Defizite verbessern könnten.
Significant reductions in stratospheric ozone occur inside the polar vortices each spring when chlorine radicals produced by heterogeneous reactions on cold particle surfaces in winter destroy ozone mainly in two catalytic cycles, the ClO dimer cycle and the ClO/BrO cycle. Chlorofluorocarbons (CFCs), which are responsible for most of the chlorine currently present in the stratosphere, have been banned by the Montreal Protocol and its amendments, and the ozone layer is predicted to recover to 1980 levels within the next few decades. During the same period, however, climate change is expected to alter the temperature, circulation patterns and chemical composition in the stratosphere, and possible geo-engineering ventures to mitigate climate change may lead to additional changes. To realistically predict the response of the ozone layer to such influences requires the correct representation of all relevant processes. The European project RECONCILE has comprehensively addressed remaining questions in the context of polar ozone depletion, with the objective to quantify the rates of some of the most relevant, yet still uncertain physical and chemical processes. To this end RECONCILE used a broad approach of laboratory experiments, two field missions in the Arctic winter 2009/10 employing the high altitude research aircraft M55-Geophysica and an extensive match ozone sonde campaign, as well as microphysical and chemical transport modelling and data assimilation. Some of the main outcomes of RECONCILE are as follows: (1) vortex meteorology: the 2009/10 Arctic winter was unusually cold at stratospheric levels during the six-week period from mid-December 2009 until the end of January 2010, with reduced transport and mixing across the polar vortex edge; polar vortex stability and how it is influenced by dynamic processes in the troposphere has led to unprecedented, synoptic-scale stratospheric regions with temperatures below the frost point; in these regions stratospheric ice clouds have been observed, extending over >106km2 during more than 3 weeks. (2) Particle microphysics: heterogeneous nucleation of nitric acid trihydrate (NAT) particles in the absence of ice has been unambiguously demonstrated; conversely, the synoptic scale ice clouds also appear to nucleate heterogeneously; a variety of possible heterogeneous nuclei has been characterised by chemical analysis of the non-volatile fraction of the background aerosol; substantial formation of solid particles and denitrification via their sedimentation has been observed and model parameterizations have been improved. (3) Chemistry: strong evidence has been found for significant chlorine activation not only on polar stratospheric clouds (PSCs) but also on cold binary aerosol; laboratory experiments and field data on the ClOOCl photolysis rate and other kinetic parameters have been shown to be consistent with an adequate degree of certainty; no evidence has been found that would support the existence of yet unknown chemical mechanisms making a significant contribution to polar ozone loss. (4) Global modelling: results from process studies have been implemented in a prognostic chemistry climate model (CCM); simulations with improved parameterisations of processes relevant for polar ozone depletion are evaluated against satellite data and other long term records using data assimilation and detrended fluctuation analysis. Finally, measurements and process studies within RECONCILE were also applied to the winter 2010/11, when special meteorological conditions led to the highest chemical ozone loss ever observed in the Arctic. In addition to quantifying the 2010/11 ozone loss and to understand its causes including possible connections to climate change, its impacts were addressed, such as changes in surface ultraviolet (UV) radiation in the densely populated northern mid-latitudes.
The international research project RECONCILE has addressed central questions regarding polar ozone depletion, with the objective to quantify some of the most relevant yet still uncertain physical and chemical processes and thereby improve prognostic modelling capabilities to realistically predict the response of the ozone layer to climate change. This overview paper outlines the scope and the general approach of RECONCILE, and it provides a summary of observations and modelling in 2010 and 2011 that have generated an in many respects unprecedented dataset to study processes in the Arctic winter stratosphere. Principally, it summarises important outcomes of RECONCILE including (i) better constraints and enhanced consistency on the set of parameters governing catalytic ozone destruction cycles, (ii) a better understanding of the role of cold binary aerosols in heterogeneous chlorine activation, (iii) an improved scheme of polar stratospheric cloud (PSC) processes that includes heterogeneous nucleation of nitric acid trihydrate (NAT) and ice on non-volatile background aerosol leading to better model parameterisations with respect to denitrification, and (iv) long transient simulations with a chemistry-climate model (CCM) updated based on the results of RECONCILE that better reproduce past ozone trends in Antarctica and are deemed to produce more reliable predictions of future ozone trends. The process studies and the global simulations conducted in RECONCILE show that in the Arctic, ozone depletion uncertainties in the chemical and microphysical processes are now clearly smaller than the sensitivity to dynamic variability.