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This paper presents results from the "INUIT-JFJ/CLACE 2013" field campaign at the high alpine research station Jungfraujoch in January/February 2013. The chemical composition of ice particle residuals (IPR) in a size diameter range of 200–900 nm was measured in orographic, convective and non-convective clouds with a single particle mass spectrometer (ALABAMA) under ambient conditions characterized by temperatures between −28 and −4 °C and wind speed from 0.1 to 21 km h−1. Additionally, background aerosol particles in cloud free air were investigated. The IPR were sampled from mixed-phase clouds with two inlets which selectively extract small ice crystals in-cloud, namely the Counterflow Virtual Impactor (Ice-CVI) and the Ice Selective Inlet (ISI). The IPR as well as the aerosol particles were classified into seven different particle types: (1) black carbon, (2) organic carbon, (3) black carbon internally mixed with organic carbon, (4) minerals, (5) one particle group (termed "BioMinSal") that may contain biological particles, minerals, or salts, (6) industrial metals, and (7) lead containing particles. For any sampled particle population it was determined by means of single particle mass spectrometer how many of the analyzed particles belonged to each of these categories. Accordingly, between 20 and 30% of the IPR and roughly 42% of the background particles contained organic carbon. The measured fractions of minerals in the IPR composition varied from 6 to 33%, while the values for the "BioMinSal" group were between 15 and 29%. Four percent to 31% of the IPR contained organic carbon mixed with black carbon. Both inlets delivered similar results of the chemical composition and of the particle size distribution, although lead was found only in the IPR sampled by the Ice-CVI. The results show that the ice particle residual composition varies substantially between different cloud events, which indicates the influence of different meteorological conditions, such as origin of the air masses, temperature and wind speed.
In the upcoming years, the internet of things (IoT)will enrich daily life. The combination of artificial intelligence(AI) and highly interoperable systems will bring context-sensitive multi-domain services to reality. This paper describesa concept for an AI-based smart living platform with open-HAB, a smart home middleware, and Web of Things (WoT) askey components of our approach. The platform concept con-siders different stakeholders, i.e. the housing industry, serviceproviders, and tenants. These activities are part of the Fore-Sight project, an AI-driven, context-sensitive smart living plat-form.
Clinical data on antifungal combination therapy are limited, in particular in the pediatric setting. We analyzed real-life data collected in two major pediatric cancer centers over a period of 4 years. Patients were identified in an observational study on children with acute leukemia and lymphoma or undergoing hematopoietic cell transplantation. Out of 438 patients, 19 patients received 21 episodes of antifungal combination therapy. Therapy was mostly started for sepsis (n = 5) or clinical deterioration with pulmonary infiltrates (n = 10), and less often for periorbital swelling with suspected mold infection (n = 2), clinical deterioration and new skin lesions, secondary antifungal prophylaxis, a persistently elevated galactomannan index, or as pre-emptive treatment (n = 1 each). Diagnostics revealed proven, probable, and possible invasive fungal disease in two, seven and four episodes, respectively. Most regimens included caspofungin (n = 19), and treatment was initiated as first line therapy in 10 episodes. The median duration was 13 days (4–46 days). Nine of the 13 patients with proven, probable, or possible invasive fungal disease survived, which was comparable to patients receiving antifungal monotherapy. Our analysis demonstrates that combination therapy has mainly been prescribed in selected immunocompromised patients with clinical deterioration due to suspected invasive fungal disease or those with sepsis, and is well tolerated. Future studies need to better characterize clinical settings in which patients may benefit from antifungal combination therapy.
B lymphocytes are key players in humoral immunity, expressing diverse surface immunoglobulin receptors directed against specific antigenic epitopes. The development and profile of distinct subpopulations have gained awareness in the setting of primary immunodeficiency disorders, primary or secondary autoimmunity and as therapeutic targets of specific antibodies in various diseases. The major B cell subpopulations in peripheral blood include naïve (CD19+ or CD20+IgD+CD27−), non-switched memory (CD19+ or CD20+IgD+CD27+) and switched memory B cells (CD19+ or CD20+IgD−CD27+). Furthermore, less common B cell subpopulations have also been described as having a role in the suppressive capacity of B cells to maintain self-tolerance. Data on reference values for B cell subpopulations are limited and only available for older age groups, neglecting the continuous process of human B cell development in children and adolescents. This study was designed to establish an exponential regression model to produce continuous reference values for main B cell subpopulations to reflect the dynamic maturation of the human immune system in healthy children.
Bone metabolism appears to influence insulin secretion and sensitivity, and insulin promotes bone formation in animals, but similar evidence in humans is limited. The objectives of this study are to explore if bone turnover markers were associated with insulin secretion and sensitivity and to determine if bone turnover markers predict changes in insulin secretion and sensitivity. The study population encompassed 576 non-diabetic adult men with normal glucose tolerance (NGT; n = 503) or impaired glucose regulation (IGR; n = 73). Baseline markers of bone resorption (CTX) and formation (P1NP) were determined in the fasting state and after a 2-h hyperinsulinaemic, euglycaemic clamp. An intravenous glucose tolerance test (IVGTT) and a 2-h oral glucose tolerance test (OGTT) were performed at baseline, and the OGTT was repeated after 3 years. There were no differences in bone turnover marker levels between NGT and IGR. CTX and P1NP levels decreased by 8.0% (p < 0.001) and 1.9% (p < 0.01) between baseline and steady-state during the clamp. Fasting plasma glucose was inversely associated with CTX and P1NP both before and after adjustment for recruitment centre, age, BMI, smoking and physical activity. However, baseline bone turnover markers were neither associated with insulin sensitivity (assessed using hyperinsulinaemic euglycaemic clamp and OGTT) nor with insulin secretion capacity (based on IVGTT and OGTT) at baseline or at follow-up. Although inverse associations between fasting glucose and markers of bone turnover were identified, this study cannot support an association between insulin secretion and sensitivity in healthy, non-diabetic men.
In the present work, three different techniques are used to separate ice-nucleating particles (INP) and ice particle residuals (IPR) from non-ice-active particles: the Ice Selective Inlet (ISI) and the Ice Counterflow Virtual Impactor (Ice-CVI), which sample ice particles from mixed phase clouds and allow for the analysis of the residuals, as well as the combination of the Fast Ice Nucleus Chamber (FINCH) and the Ice Nuclei Pumped Virtual Impactor (IN-PCVI), which provides ice-activating conditions to aerosol particles and extracts the activated ones for analysis. The collected particles were analyzed by scanning electron microscopy and energy-dispersive X-ray microanalysis to determine their size, chemical composition and mixing state. Samples were taken during January/February 2013 at the High Alpine Research Station Jungfraujoch. All INP/IPR-separating techniques had considerable abundances (median 20–70%) of contamination artifacts (ISI: Si-O spheres, probably calibration aerosol; Ice-CVI: Al-O particles; FINCH + IN-PCVI: steel particles). Also, potential measurement artifacts (soluble material) occurred (median abundance < 20%). After removal of the contamination particles, silicates and Ca-rich particles, carbonaceous material and metal oxides were the major INP/IPR particle types separated by all three techniques. Minor types include soot and Pb-bearing particles. Sea-salt and sulfates were identified by all three methods as INP/IPR. Lead was identified in less than 10% of the INP/IPR. It was mainly present as an internal mixture with other particle types, but also external lead-rich particles were found. Most samples showed a maximum of the INP/IPR size distribution at 400 nm geometric diameter. In a few cases, a second super-micron maximum was identified. Soot/carbonaceous material and metal oxides were present mainly in the submicron range. ISI and FINCH yielded silicates and Ca-rich particles mainly with diameters above 1 μm, while the Ice-CVI also sampled many submicron particles. Probably owing to the different meteorological conditions, the INP/IPR composition was highly variable on a sample to sample basis. Thus, some part of the discrepancies between the different techniques may result from the (unavoidable) non-parallel sampling. The observed differences of the particles group abundances as well as the mixing state of INP/IPR point to the need of further studies to better understand the influence of the separating techniques on the INP/IPR chemical composition.
During January/February 2013, at the High Alpine Research Station Jungfraujoch a measurement campaign was carried out, which was centered on atmospheric ice-nucleating particles (INP) and ice particle residuals (IPR). Three different techniques for separation of INP and IPR from the non-ice-active particles are compared. The Ice Selective Inlet (ISI) and the Ice Counterflow Virtual Impactor (Ice-CVI) sample ice particles from mixed phase clouds and allow for the analysis of the residuals. The combination of the Fast Ice Nucleus Chamber (FINCH) and the Ice Nuclei Pumped Counterflow Virtual Impactor (IN-PCVI) provides ice-activating conditions to aerosol particles and extracts the activated INP for analysis.Collected particles were analyzed by scanning electron microscopy and energy-dispersive X-ray microanalysis to determine size, chemical composition and mixing state. All INP/IPR-separating techniques had considerable abundances (median 20 – 70 %) of instrumental contamination artifacts (ISI: Si-O spheres, probably calibration aerosol; Ice-CVI: Al-O particles; FINCH+IN-PCVI: steel particles). Also, potential sampling artifacts (e.g., pure soluble material) occurred with a median abundance of < 20 %. While these could be explained as IPR by ice break-up, for INP their IN-ability pathway is less clear. After removal of the contamination artifacts, silicates and Ca-rich particles, carbonaceous material and metal oxides were the major INP/IPR particle types separated by all three techniques. Soot was a minor contributor. Lead was detected in less than 10 % of the particles, of which the majority were internal mixtures with other particle types. Sea-salt and sulfates were identified by all three methods as INP/IPR. Most samples showed a maximum of the INP/IPR size distribution at 400 nm geometric diameter. In a few cases, a second super-micron maximum was identified. Soot/carbonaceous material and metal oxides were present mainly in the submicron range. ISI and FINCH yielded silicates and Ca-rich particles mainly with diameters above 1 μm, while the Ice-CVI also separated many submicron IPR. As strictly parallel sampling could not be performed, a part of the discrepancies between the different techniques may result from variations in meteorological conditions and subsequent INP/IPR composition. The observed differences in the particle group abundances as well as in the mixing state of INP/IPR express the need for further studies to better understand the influence of the separating techniques on the INP/IPR chemical
composition.
Die Universität Frankfurt will Stiftungsuniversität mit einem hohen Maß an Autonomie werden. Die Vortragsreihe „Die Universität der Zukunft“ begleitet diesen Prozess des Wandels. Profilierte Hochschulpioniere, Hochschulreformer und Stifter geben Auskunft über ihre Visionen einer Universität der Zukunft und über die Projekte, an denen sie arbeiten. Thomas Oppermann und Dr. Konrad Schily machten im Sommersemester 2007 den Auftakt. Im Wintersemester wurde die Vortragsreihe von Dr. Arend Oetker eröffnet, Prof. Matthias Kleiner folgte und Prof. Andreas Pinkwart schloss sie am 28. November ab. Die Johann Wolfgang Goethe-Universität steht mit der geplanten Umwandlung in eine Stiftungsuniversität mit weitgehender Autonomie vor den größten Veränderungen der letzten 50 Jahre. Solche grundlegenden Veränderungsprozesse bieten Gelegenheit, auch einen Blick auf andere Reform-Modelle zu werfen mit dem Ziel, die eigene Urteilsfähigkeit zu stärken. Die neue, hochkarätig besetzte Vortragsreihe „Die Universität der Zukunft“ sollte den Prozess der Veränderung der Universität Frankfurt in diesem und im kommenden Jahr inhaltlich begleiten. Zu Wort kamen Frauen und Männer, die als politische Pioniere Hochschulen den Weg der Veränderung geebnet, als Geldgeber ermöglicht oder gar eine neue Hochschule gegründet und mit aufgebaut haben. Was hat sie bewegt, diese Schritte zu unternehmen? Wo sahen und sehen sie die Chancen? Mit welchen Widerständen waren sie konfrontiert? Darüber werden sie Auskunft geben und sich auch den Fragen des Publikums stellen. Den Auftakt machten im Sommersemester zwei Männer, die in Deutschland viel bewegt haben: Der ehemalige niedersächsische Wissenschaftsminister Thomas Oppermann gilt als „Vater“ der deutschen Stiftungsuniversität. Während seiner Amtszeit in Hannover hat er die Landesuniversitäten einem grundlegenden Veränderungsprozess unterzogen: Sie wurden Stiftungshochschule mit einem höheren Maß an Autonomie als davor. Wie sehen die Erfahrungen mit diesem Modell im Rückblick mehrerer Jahre Praxis heute aus? Der Arzt und Gründer der Privaten Universität Witten/Herdecke, Dr. Konrad Schily, hat sich als deutscher Hochschulpionier einen Namen gemacht: Witten/Herdecke, 1982 gegründet, ist die erste private Volluniversität in Deutschland. Mit ihrem ambitionierten und bis heute einzigartigen Bildungskonzept hat die kleine Universität an der Ruhr deutsche Bildungsgeschichte geschrieben, war aber auch oft von Finanznöten geplagt. Bedeutet „privat“ eine zu starke Abhängigkeit von Geldgebern aus der Wirtschaft. Oder hat die Universität ihren Freiheitskurs über die Jahre erfolgreich verteidigen können? Im Wintersemester 2007/08 wurde die Reihe fortgesetzt. Dann standen auf dem Programm Dr. Arend Oetker (23.10.), Präsident des Stifterverbandes und Unternehmer, Prof. Matthias Kleiner (13.11.), Präsident der Deutschen Forschungsgemeinschaft (DFG) sowie der nordrhein-westfälische Minister für Innovation, Wissenschaft, Forschung und Technologie, Prof. Andreas Pinkwart (28.11.). Dr. Arend Oetker ist einer der herausragenden Mäzene und Unternehmer unseres Landes. Als Präsident des Stifterverbandes für die deutsche Wissenschaft in Essen sitzt er mit über 350 Einzelstiftungen und einem Gesamtvermögen von 1,4 Mrd. Euro dem wichtigsten Fördernetzwerk privater Stiftungen in Deutschland vor. Damit ist er in der BRD der bedeutendste Experte im Bereich der privaten Förderung von Wissenschaft. Daneben trägt er Verantwortung für die "Dr. Arend Oetker Holding", zu der rund 5.500 Mitarbeiter gehören und die sich mit Rohstoffhandel ebenso beschäftigt wie mit Schifffahrt. Sein Vortrag wird u.a. Auskunft darüber geben, wie man Stiftungs-Potenziale für universitäre Zwecke besser nutzen kann. Prof. Matthias Kleiner ist seit Januar 2007 DFG-Präsident. Bei seinem Vortrag im Universitätsklinikum wird er berichten über die Arbeit der wichtigsten und größten Förderorganisation für die Forschung in Deutschland. Ihre Kernaufgabe besteht in der Finanzierung von Forschungsvorhaben von Wissenschaftlerinnen und Wissenschaftlern in Universitäten und Forschungsinstituten und in der Auswahl der besten Projekte im Wettbewerb. Prof. Andreas Pinkwart ist seit 2005 Minister für Innovation, Wissenschaft, Forschung und Technologie sowie stellvertretender Ministerpräsident in Nordrhein-Westfalen. Das Hochschulfreiheitsgesetz gilt als eines der wichtigsten Reform-Projekte in der deutschen Bildungspolitik. Ermöglicht es doch allen Landes-Hochschulen ein Ausmaß an Freiheit und Selbstverantwortung, das bisher nicht denkbar war. Pinkwarts Vortrag reflektiert die Erfahrungen, die er und sein Haus in der Phase der Umsetzung mit den Hochschulen gemacht haben.
We have sampled atmospheric ice nuclei (IN) and aerosol in Germany and in Israel during spring 2010. IN were analyzed by the static vapor diffusion chamber FRIDGE, as well as by electron microscopy. During the Eyjafjallajökull volcanic eruption of April 2010 we have measured the highest ice nucleus number concentrations (>600 l−1) in our record of 2 yr of daily IN measurements in central Germany. Even in Israel, located about 5000 km away from Iceland, IN were as high as otherwise only during desert dust storms. The fraction of aerosol activated as ice nuclei at −18 °C and 119% rhice and the corresponding area density of ice-active sites per aerosol surface were considerably higher than what we observed during an intense outbreak of Saharan dust over Europe in May 2008.
Pure volcanic ash accounts for at least 53–68% of the 239 individual ice nucleating particles that we collected in aerosol samples from the event and analyzed by electron microscopy. Volcanic ash samples that had been collected close to the eruption site were aerosolized in the laboratory and measured by FRIDGE. Our analysis confirms the relatively poor ice nucleating efficiency (at −18 °C and 119% ice-saturation) of such "fresh" volcanic ash, as it had recently been found by other workers. We find that both the fraction of the aerosol that is active as ice nuclei as well as the density of ice-active sites on the aerosol surface are three orders of magnitude larger in the samples collected from ambient air during the volcanic peaks than in the aerosolized samples from the ash collected close to the eruption site. From this we conclude that the ice-nucleating properties of volcanic ash may be altered substantially by aging and processing during long-range transport in the atmosphere, and that global volcanism deserves further attention as a potential source of atmospheric ice nuclei.