219,593 research outputs found
Strange attractors in periodically-kicked degenerate Hopf bifurcations
We prove that spiral sinks (stable foci of vector fields) can be transformed
into strange attractors exhibiting sustained, observable chaos if subjected to
periodic pulsatile forcing. We show that this phenomenon occurs in the context
of periodically-kicked degenerate supercritical Hopf bifurcations. The results
and their proofs make use of a new multi-parameter version of the theory of
rank one maps developed by Wang and Young.Comment: 16 page
A General Signal of a Phase Transition from Single-Particle Momentum Distributions
A two-particle space correlation function is derived from the single-particle
momentum distribution of the emission source. A signal of a first order phase
transition is obtained from this correlation function if density fluctuations
are large.Comment: 5 pages, 2 Postscript figure
Confronting feedback simulations with observations of hot gas in elliptical galaxies
Elliptical galaxies comprise primarily old stars, which collectively generate
a long-lasting feedback via stellar mass-loss and Type Ia SNe. This feedback
can be traced by X-ray-emitting hot gas in and around such galaxies, in which
little cool gas is typically present. However, the X-ray-inferred mass, energy,
and metal abundance of the hot gas are often found to be far less than what are
expected from the feedback, particularly in so-called low L_X/L_B ellipticals.
This "missing" stellar feedback is presumably lost in galaxy-wide outflows,
which can play an essential role in galaxy evolution (e.g., explaining the
observed color bi-modality of galaxies). We are developing a model that can be
used to properly interpret the X-ray data and to extract key information about
the dynamics of the feedback and its interplay with galactic environment.Comment: To be published in Highlights of Astronomy, Vol 15, XXVIIth IAU
General Assembly, JD
Tectonic interpretation of the connectivity of a multiscale fracture system in limestone
This paper studies the statistics and tectonism of a multiscale natural fracture system in limestone. The fracture network exhibits a self‐similar characteristic with a correlation between its power law length exponent a and fractal dimension D, i.e., a ≈ D + 1. Contradicting the scale‐invariant connectivity of idealized self‐similar systems, the percolation state of trace patterns mapped at different scales and localities of the study area varies significantly, from well to poorly connected. A tectonic interpretation based on a polyphase fracture network evolution history is proposed to explain this discrepancy. We present data to suggest that the driving force for fracture formation may be dissipated at the end of a tectonic event when the system becomes connected. However, the “effective” connectivity can successively be reduced by cementation of early fractures and reestablished by subsequent cracking, rendering a variable “apparent” connectivity that can be significantly above the percolation threshold.ISSN:0094-8276ISSN:1944-800
Determination of anisotropic dipole moments in self-assembled quantum dots using Rabi oscillations
By investigating the polarization-dependent Rabi oscillations using
photoluminescence spectroscopy, we determined the respective transition dipole
moments of the two excited excitonic states |Ex> and |Ey> of a single
self-assembled quantum dot that are nondegenerate due to shape anisotropy. We
find that the ratio of the two dipole moments is close to the physical
elongation ratio of the quantum dot.Comment: 11 pages, 2 figures, MS Word generated PDF fil
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