1,714 research outputs found
Drie nieuwe Ponto-Kaspische inwijkelingen dringen door tot in kanalen in de provincie Antwerpen: De zoetwaterpolychaet <i>Hypania invalida</i> (Grube, 1860) en, voor het eerst in België, de platworm <i>Dendrocoelum romanodanubiale</i> (Codreanu, 1949) en de Donaupissebed <i>Jaera istri</i> Veuille, 1979
Since 2000 three Ponto-Caspian invaders have been found in canals in the province of Antwerp (N.E.-Belgium): the freshwater polychaete Hypania invalida (Grube, 1860), the triclad Dendrocoelum romanodanubiale (Codreanu, 1949) and the freshwater isopod Jaera istri Veuille, 1979. Staff members of the 'Vlaamse Milieumaatschappij (Flemish Environmental Agency) collected these species on artificial substrates (nets filled with broken bricks). H. invalida had been discovered before in Belgium in the river Meuse in 2000 (Vanden Bossche et.al., 2001). D. romanodanubiale and J. istri were never recorded before in Belgium. Before its discovery in the Belgian Meuse in August-September 2000, H.invalida had already been found in May 2000 in the Albert Canal at Genk in the province of Limbourg. Between 2001 and 2003, the polychaete was sampled at several stations of the Albert Canal and its adjacent canals in the provinces of Antwerp and Limbourg. Here, it often is accompanied by D. romanodanubiale and J. istri. In 2003 the polychaet had also been encountered in the Sea canal Brussels - Scheldt in the province of Antwerp. The discontinuous distribution indicates that navigation plays an important role in the dispersal of the species. Other Ponto-Caspian species such as Dikerogammarus villosus (Sovinskij, 1894) are either already present in the canals or soon to be expected there. Some of these species will probably also invade the Scheldt basin
Direct magneto-optical compression of an effusive atomic beam for high-resolution focused ion beam application
An atomic rubidium beam formed in a 70 mm long two-dimensional
magneto-optical trap (2D MOT), directly loaded from a collimated Knudsen
source, is analyzed using laser-induced fluorescence. The longitudinal velocity
distribution, the transverse temperature and the flux of the atomic beam are
reported. The equivalent transverse reduced brightness of an ion beam with
similar properties as the atomic beam is calculated because the beam is
developed to be photoionized and applied in a focused ion beam. In a single
two-dimensional magneto-optical trapping step an equivalent transverse reduced
brightness of A/(m sr eV) was
achieved with a beam flux equivalent to nA. The
temperature of the beam is further reduced with an optical molasses after the
2D MOT. This increased the equivalent brightness to A/(m sr eV). For currents below 10 pA, for which disorder-induced
heating can be suppressed, this number is also a good estimate of the ion beam
brightness that can be expected. Such an ion beam brightness would be a six
times improvement over the liquid metal ion source and could improve the
resolution in focused ion beam nanofabrication.Comment: 10 pages, 8 figures, 1 tabl
Separation of Time Scales in a Quantum Newton’s Cradle
We provide detailed modeling of the Bragg pulse used in quantum Newton’s-cradle-like settings or in Bragg spectroscopy experiments for strongly repulsive bosons in one dimension. We reconstruct the postpulse time evolution and study the time-dependent local density profile and momentum distribution by a combination of exact techniques. We further provide a variety of results for finite interaction strengths using a time-dependent Hartree-Fock analysis and bosonization-refermionization techniques. Our results display a clear separation of time scales between rapid and trap-insensitive relaxation immediately after the pulse, followed by slow in-trap periodic behavior
The arthroscopic treatment of displaced tibial spine fractures in children and adolescents using Meniscus Arrows®
This article summarises the results of a newly developed technique that utilises Meniscus Arrows(A (R)) for the arthroscopic fixation of displaced tibial spine fractures in children and adolescents. Twelve tibial spine fractures in the knees of eleven children between 6 and 15 years old, with an average age of 12 years, were arthroscopically fixed with Meniscus Arrows(A (R)), after a reduction of their fractures. This was followed by 5 weeks immobilisation in a plaster of Paris. Postoperative follow-up included radiographs, Lachmann tests on all of the children's knees and KT-1000 tests of eight out of twelve of the children's knees. The postoperative follow-up time ranged from 3 to 10 years, with patients being seen for an average of 4 years. All of the fractures consolidated uneventfully, and all of the patients returned unrestricted to their previous activity level. The Lachmann tests revealed no, or a non-functional, laxity in any of the patients' knees. The KT-1000 tests showed a difference between the operated side, and non-operated side, of between 3 mm in the first knee operated on and an average of 1 mm in the remaining knees. The arthroscopic fixation of tibial spine fractures using Meniscus Arrows(A (R)) showed that this minimally invasive procedure resulted in the uneventful consolidation of all twelve of the fractures, with excellent results, and without the need for a second, hardware removal, operation. Level of Evidence: Level IV
Cumulant theory of the unitary Bose gas: Prethermal and Efimovian dynamics
We study the quench of a degenerate ultracold Bose gas to the unitary regime,
where interactions are as strong as allowed by quantum mechanics. We lay the
foundations of a cumulant theory able to capture simultaneously the three-body
Efimov effect and ergodic evolution. After an initial period of rapid quantum
depletion, a universal prethermal stage is established characterized by a
kinetic temperature and an emergent Bogoliubov dispersion law while the
microscopic degrees of freedom remain far-from-equilibrium. Integrability is
then broken by higher-order interaction terms in the many-body Hamiltonian,
leading to a momentum-dependent departure from power law to decaying
exponential behavior of the occupation numbers at large momentum. We find also
signatures of the Efimov effect in the many-body dynamics and make a precise
identification between the observed beating phenomenon and the binding energy
of an Efimov trimer. Throughout the work, our predictions for a uniform gas are
quantitatively compared with experimental results for quenched unitary Bose
gases in uniform potentials.Comment: 34 pages, 12 figure
Cytophagic histiocytic panniculitis: is it a macrophage activation syndrome in situ?
International audiencepas de résum
Sculpting oscillators with light within a nonlinear quantum fluid
Seeing macroscopic quantum states directly remains an elusive goal. Particles
with boson symmetry can condense into such quantum fluids producing rich
physical phenomena as well as proven potential for interferometric devices
[1-10]. However direct imaging of such quantum states is only fleetingly
possible in high-vacuum ultracold atomic condensates, and not in
superconductors. Recent condensation of solid state polariton quasiparticles,
built from mixing semiconductor excitons with microcavity photons, offers
monolithic devices capable of supporting room temperature quantum states
[11-14] that exhibit superfluid behaviour [15,16]. Here we use microcavities on
a semiconductor chip supporting two-dimensional polariton condensates to
directly visualise the formation of a spontaneously oscillating quantum fluid.
This system is created on the fly by injecting polaritons at two or more
spatially-separated pump spots. Although oscillating at tuneable THz-scale
frequencies, a simple optical microscope can be used to directly image their
stable archetypal quantum oscillator wavefunctions in real space. The
self-repulsion of polaritons provides a solid state quasiparticle that is so
nonlinear as to modify its own potential. Interference in time and space
reveals the condensate wavepackets arise from non-equilibrium solitons. Control
of such polariton condensate wavepackets demonstrates great potential for
integrated semiconductor-based condensate devices.Comment: accepted in Nature Physic
Knowledge deficit and fear of COVID-19 among higher education students during the first wave of the pandemic and implications for public health: a multi-country cross-sectional survey
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[Arctic] Greenland ice sheet [in “State of the Climate in 2012”]
Melting at the surface of the Greenland Ice Sheet set new records for extent and melt index (i.e., the number of days on which melting occurred multiplied by the area where melting was detected) for the period 1979–2012, according to passive microwave observations (e.g., Tedesco 2007, 2009; Mote and Anderson 1995). Melt extent reached ~97% of the ice sheet surface during a rare, ice-sheet-wide event on 11–12 July (Fig. 5.13a; Nghiem et al. 2012). This was almost four times greater than the average melt extent for 1981–2010. The 2012 standardized melting index (SMI, defined as the melting index minus its average and divided by its standard deviation) was +2.4, almost twice the previous record of about +1.3 set in 2010
A tipping point in refreezing accelerates mass loss of Greenland’s glaciers and ice caps
Melting of the Greenland ice sheet (GrIS) and its peripheral glaciers and ice caps (GICs) contributes about 43% to contemporary sea level rise. While patterns of GrIS mass loss are well studied, the spatial and temporal evolution of GICs mass loss and the acting processes have remained unclear. Here we use a novel, 1 km surface mass balance product, evaluated against in situ and remote sensing data, to identify 1997 (±5 years) as a tipping point for GICs mass balance. That year marks the onset of a rapid deterioration in the capacity of the GICs firn to refreeze meltwater. Consequently, GICs runoff increases 65% faster than meltwater production, tripling the post-1997 mass loss to 36±16 Gt−1, or ∼14% of the Greenland total. In sharp contrast, the extensive inland firn of the GrIS retains most of its refreezing capacity for now, buffering 22% of the increased meltwater production. This underlines the very different response of the GICs and GrIS to atmospheric warming
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