680 research outputs found

    Inlet conditions for large eddy simulation of gas-turbine swirl injectors

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    Copyright © 2008 American Institute of Aeronautics and AstronauticsIn this paper, we present a novel technique for generating swirl inlets for large eddy simulation. The velocity a short distance downstream of the inlet to the main domain is sampled and the flow velocity data are reintroduced back into the domain inlet, creating an inlet section integrated into the main domain in which turbulence can develop. Additionally, variable artificial body forces and velocity corrections are imposed in this inlet section, with feedback control to force the flow toward desired swirl, mean, and turbulent profiles. The method was applied to flow in an axisymmetric sudden expansion, with and without swirl at the inlet, and compared against experimental and literature large eddy simulation data and against similar results in the literature. The method generates excellent results for this case and is elegant and straightforward to implement

    Measurement of the 187Re({\alpha},n)190Ir reaction cross section at sub-Coulomb energies using the Cologne Clover Counting Setup

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    Uncertainties in adopted models of particle+nucleus optical-model potentials directly influence the accuracy in the theoretical predictions of reaction rates as they are needed for reaction-network calculations in, for instance, {\gamma}-process nucleosynthesis. The improvement of the {\alpha}+nucleus optical-model potential is hampered by the lack of experimental data at astrophysically relevant energies especially for heavier nuclei. Measuring the Re187({\alpha},n)Ir190 reaction cross section at sub-Coulomb energies extends the scarce experimental data available in this mass region and helps understanding the energy dependence of the imaginary part of the {\alpha}+nucleus optical-model potential at low energies. Applying the activation method, after the irradiation of natural rhenium targets with {\alpha}-particle energies of 12.4 to 14.1 MeV, the reaction yield and thus the reaction cross section were determined via {\gamma}-ray spectroscopy by using the Cologne Clover Counting Setup and the method of {\gamma}{\gamma} coincidences. Cross-section values at five energies close to the astrophysically relevant energy region were measured. Statistical model calculations revealed discrepancies between the experimental values and predictions based on widely used {\alpha}+nucleus optical-model potentials. However, an excellent reproduction of the measured cross-section values could be achieved from calculations based on the so-called Sauerwein-Rauscher {\alpha}+nucleus optical-model potential. The results obtained indicate that the energy dependence of the imaginary part of the {\alpha}+nucleus optical-model potential can be described by an exponential decrease. Successful reproductions of measured cross sections at low energies for {\alpha}-induced reactions in the mass range 141{\leq}A{\leq}187 confirm the global character of the Sauerwein-Rauscher potential

    Instabilitäten von Infiltrationsfronten verursacht durch langzeitige Bewässerung mit behandelten Abwässern

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    Die Bewässerung von Agrarflächen mit behandelten Abwässern (TWW) ist eine weitverbreitete Praxis in ariden und semi-ariden Gebieten. In Israel liegt auf dieser Wasserressource ein besonderer Fokus, da Abwässer ganzjährig verfügbar sind, Frischwasserressourcen schonen und einen wichtigen Beitrag zur Wiederverwendung von Nährstoffen leisten. Vorangegangene Studien haben gezeigt, dass organische Stoffe die Benetzbarkeit von Mineraloberflächen beeinträchtigen und die Bodenstruktur verändern können. Auf Grund der erhöhten Restmenge an organischen Bestandteilen im TWW kann eine langzeitige Bewässerung im Boden zu Veränderungen der Struktur, Hydrophobizität, präferentiellen Fließwegen und dem Auswaschen von Pflanzenschutzmitteln und Nährstoffen führen. In dieser Studie wurden (i) eine neue Methode zur Quantifizierung von Wassergehaltsänderungen in ungestörten Bodenproben via Radiographie entwickelt und (ii) Instabilitäten von Infiltrationsfronten in Böden, die seit über zwanzig Jahren mit TWW bewässert wurden, detektiert. Wir untersuchten ungestörte Bodenproben von zwei Obstplantagen in Israel mit langzeitiger TWW-Bewässerung, wobei an einem Standort zusätzlich ein Teil mit Frischwasser bewässert wird. Die Proben umfassen zwei unterschiedliche Bodentexturen und zwei unterschiedliche Bewässerungsverfahren: Frischwasser und TWW. Des Weiteren wurden saisonale Abhängigkeiten (Trocken-/ Regenzeit) mit in die Studie eingeschlossen um die Persistenz der Effekte zu erfassen. Ungestörte, zylindrische Bodenproben wurden aus dem Oberboden (0-20 cm) genommen und Bewässerungsversuche innerhalb eines Röntgensystems durchgeführt. Durch Bildanalyse konnten die Ausbreitung der Infiltrationsfronten und räumliche Wassergehaltsänderungen als Funktion der Zeit erfasst werden. Die Versuche wurden mit unterschiedlichen Anfangswassergehalten wiederholt. In dieser Studie konnte gezeigt werden, dass die Stabilität der Infiltrationsfronten in diesen Böden von der Wasserqualität und dem initialen Wassergehalt abgängig sind. Darüber hinaus konnte dargelegt werden, dass langzeitige TWW-Bewässerung zu einer persistenten Veränderung der Benetzbarkeit führen kann, unabhängig von der Saison. Diese Studie liefert einen experimentellen Nachweis über die Notwendigkeit von optimiertem Bewässerungsmanagement um präferentielles Wasserfließen zu vermeiden

    The role of alanine and aspartate aminotransferases in C<sub>4</sub> photosynthesis

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    Schlüter U, Bräutigam A, Droz J‐M, Schwender J, Weber APM. The role of alanine and aspartate aminotransferases in C&lt;sub&gt;4&lt;/sub&gt; photosynthesis. Plant Biology. 2019;21(S1):64-76.• Alanine and aspartate are essential transfer metabolites for C4 species of the NADmalic enzyme and phosphoenolpyruvate carboxykinase subtype. To some degree both amino acids are also part of the metabolite shuttle in NADP-malic enzyme plants. In comparison with C3 species, the majority of C4 species are therefore characterised by enhanced expression and activity of alanine and aspartate aminotransferases (AT) in the photosynthetically active tissue. Both enzymes exist in multiple copies and have been found in different subcellular compartments. We tested whether different C4 species show preferential recruitment of enzymes from specific lineages and subcellular compartments. • Phylogenetic analysis of alanine and aspartate ATs from a variety of monocot and eudicot C4 species and their C3 relatives was combined with subcellular prediction tools and analysis of the subsequent transcript amounts in mature leaves. • Recruitment of aspartate AT from a specific subcellular compartment was strongly connected to the biochemical subtype. Deviation from the main model was however observed in Gynandropsis gynandra. The configuration of alanine AT generally differed in monocot and eudicot species. C4 monocots recruited an alanine AT from a specific cytosolic branch, but eudicots use alanine AT copies from a mitochondrial branch. • Generally, plants display high plasticity in the setup of the C4 pathway. Beside the common models for the different C4 subtypes, individual solutions were found for plant groups or lineages

    Operational flood management under large-scale extreme conditions, using the example of the Middle Elbe

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    In addition to precautionary or technical flood protection measures, short-term strategies of the operational management, i.e. the initiation and co-ordination of preventive measures during and/or before a flood event are crucially for the reduction of the flood damages. This applies especially for extreme flood events. These events are rare, but may cause a protection measure to be overtopped or even to fail and be destroyed. In such extreme cases, reliable decisions must be made and emergency measures need to be carried out to prevent even larger damages from occurring. &lt;br&gt;&lt;br&gt; Based on improved methods for meteorological and hydrological modelling a range of (physically based) extreme flood scenarios can be derived from historical events by modification of air temperature and humidity, shifting of weather fields and recombination of flood relevant event characteristics. By coupling the large scale models with hydraulic and geotechnical models, the whole flood-process-chain can be analysed right down to the local scale. With the developed GIS-based tools for hydraulic modelling &lt;i&gt;FlowGIS&lt;/i&gt; and the Dike-Information-System, (IS-dikes) it is possible to quantify the endangering shortly before or even during a flood event, so the decision makers can evaluate possible options for action in operational mode

    Search for a dark vector gauge boson decaying to π+π\pi^+ \pi^- using ηπ+πγ\eta \rightarrow \pi^+\pi^- \gamma decays

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    We report a search for a dark vector gauge boson UU^\prime that couples to quarks in the decay chain D+D0π+,D0KS0η,ηUγD^{*+} \to D^0 \pi^+, D^0 \to K^0_S \eta, \eta \to U^\prime \gamma, Uπ+πU^\prime \to \pi^+ \pi^-. No signal is found and we set a mass-dependent limit on the baryonic fine structure constant of 10310210^{-3} - 10^{-2} in the UU^\prime mass range of 290 to 520 MeV/c2c^2. This analysis is based on a data sample of 976 fb1^{-1} collected by the Belle experiment at the KEKB asymmetric-energy e+ee^+e^- collider.Comment: 6 pages, 4 figure

    First Observation of Doubly Cabibbo-Suppressed Decay of a Charmed Baryon: Λc+pK+π\Lambda^{+}_{c} \rightarrow p K^{+} \pi^{-}

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    We report the first observation of the decay Λc+pK+π\Lambda^{+}_{c} \rightarrow p K^{+} \pi^{-} using a 980 fb1\mathrm{fb^{-1}} data sample collected by the Belle detector at the KEKB asymmetric-energy e+ee^{+}e^{-} collider. This is the first doubly Cabibbo-suppressed decay of a charmed baryon to be observed. We measure the branching ratio of this decay with respect to its Cabibbo-favored counterpart to be B(Λc+pK+π)/B(Λc+pKπ+)=(2.35±0.27±0.21)×103\mathcal{B}(\Lambda^{+}_{c} \rightarrow p K^{+} \pi^{-})/\mathcal{B}(\Lambda^{+}_{c} \rightarrow p K^{-} \pi^{+})=(2.35\pm0.27\pm0.21)\times10^{-3}, where the uncertainties are statistical and systematic, respectively.Comment: 6 pages, 3 figure
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