43,577 research outputs found
Charmless Hadronic B Decays at BABAR
We present preliminary results of several searches for rare charmless
hadronic decays of the B meson using data collected by the BABAR detector at
the Stanford Linear Accelerator Center's PEP-II storage ring. We search for the
decays h^+h^-, h^+h^-h^+, h^+h^-pi^0, X^0h^+, and X^0 K_S^0, where h = pi or K,
and X^0 = eta^prime or omega. In a sample of 8.8 million B-anti-B decays we
measure the branching fractions: BF(B^0 --> pi^+pi^-) =
(9.3^{+2.6}_{-2.3}^{+1.2}_{-1.4}) x 10^{-6}, BF(B^0 --> K^+pi^-) =
(12.5^{+3.0}_{-2.6}^{+1.3}_{-1.7}) x 10^{-6}, BF(B^0 --> rho^-pi^+) = (49 +/-
13^{+6}_{-5}) x 10^{-6}. We calculate upper limits for the modes without a significant signal.Comment: 6 pages, 2 postscript figues, submitted to Proceedings of DPF200
St Thomas Fishermen's Association: protecting St. Thomas & St. John natural heritage and culture through participatory management
Rules for the Cortical Map of Ocular Dominance and Orientation Columns
Three computational rules are sufficient to generate model cortical maps that simulate the interrelated structure of cortical ocular dominance and orientation columns: a noise input, a spatial band pass filter, and competitive normalization across all feature dimensions. The data of Blasdel from optical imaging experiments reveal cortical map fractures, singularities, and linear zones that are fit by the model. In particular, singularities in orientation preference tend to occur in the centers of ocular dominance columns, and orientation contours tend to intersect ocular dominance columns at right angles. The model embodies a universal computational substrate that all models of cortical map development and adult function need to realize in some form.Air Force Office of Scientific Research (F49620-92-J- 0499, F49620-92-J-0334); Office of Naval Research (N00014-92-J-4015, N00014-91-J-4100); National Science Foundation (IRI-90-24877); British Petroleum (BP 89A-1204
Quantum corrected Langevin dynamics for adsorbates on metal surfaces interacting with hot electrons
We investigate the importance of including quantized initial conditions in
Langevin dynamics for adsorbates interacting with a thermal reservoir of
electrons. For quadratic potentials the time evolution is exactly described by
a classical Langevin equation and it is shown how to rigorously obtain quantum
mechanical probabilities from the classical phase space distributions resulting
from the dynamics. At short time scales, classical and quasiclassical initial
conditions lead to wrong results and only correctly quantized initial
conditions give a close agreement with an inherently quantum mechanical master
equation approach. With CO on Cu(100) as an example, we demonstrate the effect
for a system with ab initio frictional tensor and potential energy surfaces and
show that quantizing the initial conditions can have a large impact on both the
desorption probability and the distribution of molecular vibrational states
Tripartite and bipartite entanglement in continuous-variable tripartite systems
We examine one asymmetric adnd two fully symmetric Gaussian
continuous-variable systems in terms of their tripartite and bipartite
entanglement properties. We treat pure states and are able to find analytic
solutions using the undepleted pump approximation for the Hamiltonian models,
and standard beamsplitter relations for a model that mixes the outputs of
optical parametric oscillators. Our two symmetric systems exhibit perfect
tripartite correlations, but only in the unphysical limit of infinite
squeezing. For more realistic squeezing parameters, all three systems exhibit
both tripartite and bipartite entanglement. We conclude that none of the
outputs are completely analogous to either GHZ or W states, but there are
parameter regions where they produce T states introduced by Adesso \etal The
qualitative differences in the output states for different interaction
parameters indicate that continuous-variable tripartite quantum information
systems offer a versatility not found in bipartite systems.Comment: 18 pages, 6 figures. arXiv admin note: text overlap with
arXiv:1510.0182
Ice shapes and the resulting drag increase for a NACA 0012 airfoil
Experimental measurements of the ice shapes and resulting drag increases were measured in the NASA-Lewis Icing Research Tunnel. The measurements were made over a large range of conditions (e.g., airspeed and temperature, drop size and liquid water content of the cloud, and the angle of attack of the airfoil). The measured drag increase did not agree with the existing correlation. Additional results were given which are helpful in understanding the ice structure and the way it forms, and in improving the ice accretion modeling theories. There are data on the ice surface roughness, on the effect of the ice shape on the local droplet catch, and on the relative importance of various parts of the ice shape on the drag increase. Experimental repeatability is also discussed
Study of ice accretion on icing wind tunnel components
In a closed loop icing wind tunnel the icing cloud is simulated by introducing tiny water droplets through an array of nozzles upstream of the test section. This cloud will form ice on all tunnel components (e.g., turning vanes, inlet guide vanes, fan blades, and the heat exchanger) as the cloud flows around the tunnel. These components must have the capacity to handle their icing loads without causing significant tunnel performance degradation during the course of an evening's run. To aid in the design of these components for the proposed Altitude Wind Tunnel (AWT) at NASA Lewis Research Center the existing Icing Research Tunnel (IRT) is used to measure icing characteristics of the IRT's components. The results from the IRT are scaled to the AWT to account for the AWT's larger components and higher velocities. The results show that from 90 to 45 percent of the total spray cloud froze out on the heat exchanger. Furthermore, the first set of turning vanes downstream of the test section, the FOD screen and the fan blades show significant ice formation. The scaling shows that the same results would occur in the AWT
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