776 research outputs found
Quantum Mechanics with Trajectories: Quantum Trajectories and Adaptive Grids
Although the foundations of the hydrodynamical formulation of quantum
mechanics were laid over 50 years ago, it has only been within the past few
years that viable computational implementations have been developed. One
approach to solving the hydrodynamic equations uses quantum trajectories as the
computational tool. The trajectory equations of motion are described and
methods for implementation are discussed, including fitting of the fields to
gaussian clusters.Comment: Prepared for CiSE, Computing in Science and Engineering IEEE/AIP
special issue on computational chemistr
Hydrodynamic View of Wave-Packet Interference: Quantum Caves
Wave-packet interference is investigated within the complex quantum
Hamilton-Jacobi formalism using a hydrodynamic description. Quantum
interference leads to the formation of the topological structure of quantum
caves in space-time Argand plots. These caves consist of the vortical and
stagnation tubes originating from the isosurfaces of the amplitude of the wave
function and its first derivative. Complex quantum trajectories display
counterclockwise helical wrapping around the stagnation tubes and hyperbolic
deflection near the vortical tubes. The string of alternating stagnation and
vortical tubes is sufficient to generate divergent trajectories. Moreover, the
average wrapping time for trajectories and the rotational rate of the nodal
line in the complex plane can be used to define the lifetime for interference
features.Comment: 4 pages, 3 figures (major revisions with respect to the previous
version have been carried out
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Scattered-wave-packet formalism with applications to barrier scattering and quantum transistors
The scattered wave formalism developed for a quantum subsystem interacting with reservoirs through open boundaries is applied to one- or two-dimensional barrier scattering and quantum transistors. The total wave function is divided into incident and scattered components. Markovian outgoing wave boundary conditions are imposed on the scattered or total wave function by either the ratio or polynomial methods. For barrier scattering problems, accurate time-dependent transmission probabilities are obtained through the integration of the modified time-dependent Schrodinger equations for the scattered wave function. For quantum transistors, the time-dependent transport is studied for a quantum wave packet propagating through the conduction channel of a field effect transistor. This study shows that the scattered wave formalism significantly reduces computational effort relative to other open boundary methods and demonstrates wide applications to quantum dynamical processes.Robert Welch Foundation F-0362Chemical Engineerin
Growth Response of Kenhy Fescue to Nitrogen Fertilizer
Kenhy fescue is a new, improved variety of tall fescue which has recently been released by the University of Kentucky Agricultural Experiment Station and the U.S.D.A. Agricultural Research Service (see University of Kentucky publication AGR-60, Kenhy A New Tall Fescue Variety ). Seed of this variety should become available to farmers in limited quantities in the summer 1977. The purpose of this report is to provide information on how this newly developed fescue variety produces as affected by time and rate of nitrogen application
Quantum interference within the complex quantum Hamilton-Jacobi formalism
Quantum interference is investigated within the complex quantum
Hamilton-Jacobi formalism. As shown in a previous work [Phys. Rev. Lett. 102,
250401 (2009)], complex quantum trajectories display helical wrapping around
stagnation tubes and hyperbolic deflection near vortical tubes, these
structures being prominent features of quantum caves in space-time Argand
plots. Here, we further analyze the divergence and vorticity of the quantum
momentum function along streamlines near poles, showing the intricacy of the
complex dynamics. Nevertheless, despite this behavior, we show that the
appearance of the well-known interference features (on the real axis) can be
easily understood in terms of the rotation of the nodal line in the complex
plane. This offers a unified description of interference as well as an elegant
and practical method to compute the lifetime for interference features, defined
in terms of the average wrapping time, i.e., considering such features as a
resonant process.Comment: revised version, 13 pages, 11 figures, 1 tabl
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Surface temperature and salinity observations at Pacific Northwest shore stations : for 1963 and 1964
During 1963 and 1964 the Department of Oceanography, Oregon
State University, continued its program of shore sampling, of ocean
temperatures and salinities along the coast of the Pacific Northwest.
Observations for 1960, 1961, and 1962 are contained in three Data
Reports: No. 6 (Kujala and Wyatt, 1961), No. 8 (Oliphant, Wyatt,
and Kujala, 1962), and No. 11 (Still, Wyatt, and Kujala, 1963). The
data in this report were collected at twelve stations in 1963 and at
five stations in 1964. The locations of these stations are shown in
Figure 1. Table I lists the station names, locations, and year( s) for
which data are being reported. The names of the observers at each
station are also listed in Table I. The assistance of these observers
is greatly appreciated. Without them this program could not continue
successfully
Morphological and genetic analyses in the Melanoplus packardii group (Orthoptera: Acrididae)
Melanoplus packardii Scudder was described in 1897. Three additional closely-related species were later described and their status as species has been questioned on numerous occasions. We examined morphology from specimens collected in Nebraska which fit descriptions of three of the four forms and specimens that appeared to be hybrids. We found distinct morphological characters suggesting species status for M. foedus and M. packardii, but not for M. foedus fluviatilis. Examination of aedeagi of these three forms suggests that M. foedus and M. packardii are each distinct, but that the aedeagi of M. f. fluviatilis and M. f. foedus cannot be distinguished. Molecular analyses of the three groups did not produce clear separations and suggest gene exchange between these three forms may be ongoing. Together, these data suggest that M. foedus and M. packardii should be recognized as sibling species, but M. foedus fluviatilis is best considered a form of M. foedus, typically found in low lying areas
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