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J'erôme P'etri 《Astrophysics and Space Science》2006,302(1-4):117-139
This is the second of a series of papers aimed to look for an explanation on the generation of high frequency quasi-periodic
oscillations (QPOs) in accretion disks around neutron star, black hole, and white dwarf binaries. The model is inspired by
the general idea of a resonance mechanism in the accretion disk oscillations as was already pointed out by Abramowicz and
Klu’zniak (2001). In a first paper (P'etri, 2005a, paper I), we showed that a rotating misaligned magnetic field of a neutron
star gives rise to some resonances close to the inner edge of the accretion disk. In this second paper, we suggest that this
process does also exist for an asymmetry in the gravitational potential of the compact object. We prove that the same physics
applies, at least in the linear stage of the response to the disturbance in the system. This kind of asymmetry is well suited
for neutron stars or white dwarfs possessing an inhomogeneous interior allowing for a deviation from a perfectly spherically
symmetric gravitational field. After a discussion on the magnitude of this deformation applied to neutron stars, we show by
a linear analysis that the disk initially in a cylindrically symmetric stationary state is subject to {three kinds of resonances:
a corotation resonance, a Lindblad resonance due to a driven force and a parametric resonance}. In a second part, we focus
on the linear response of a thin accretion disk in the 2D limit. {Waves are launched at the aforementioned resonance positions
and propagate in some permitted regions inside the disk, according to the dispersion relation obtained by a WKB analysis}.
In a last part, these results are confirmed and extended via non linear hydrodynamical numerical simulations performed with
a pseudo-spectral code solving Euler's equations in a 2D cylindrical coordinate frame. {We found that for a weak potential
perturbation, the Lindblad resonance is the only effective mechanism producing a significant density fluctuation}. In a last
step, we replaced the Newtonian potential by the so called logarithmically modified pseudo-Newtonian potential in order to
take into account some general-relativistic effects like the innermost stable circular orbit (ISCO). The latter potential
is better suited to describe the close vicinity of a neutron star or a black hole. However, from a qualitative point of view,
the resonance conditions remain the same. The highest kHz QPOs are then interpreted as the orbital frequency of the disk at
locations where the response to the resonances are maximal. It is also found that strong gravity is not required to excite
the resonances. 相似文献
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A new algorithm of order five is presented for the solution of the initial value problem where the system of ordinary differential equations is of second order and does not contain the first derivative. 相似文献
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Dan Gill 《Mathematical Geology》1993,25(4):471-482
The ability of association analysis to discriminate sedimentary facies was tested on Purdy's modal analyses of modern sediments of the Great Bahama Bank. Purdy's data set has served in the past as a standard reference for evaluating various multivariate classification algorithms. In order to adapt Purdy's data to association analysis, the percent abundance of the 12 constituents was converted to binary form by dichotomizing each variable on its mean value. The results obtained by association analysis are virtually identical to those obtained by Purdy and other authors. The same four main sedimentary facies were discriminated; 86% of the samples were identically classified (97% when misclassified borderline cases are counted as matches); the total partition variance of the classification is only negligibly greater (4%); and the grouping of the variables yielded the same four groups. The rank order of the three division-attributes responsible for the sample classification is fines, oolites, and corals. Association analysis has been employed by other authors to differentiate meaningful facies groups in studies of ancient reef carbonates, modern reef sediments, and heavy minerals in stream sediments. In all these studies, the results were found to be compatible with those obtained by using the continuous quantitative measurements, indicating that qualitative binary data may often be sufficient for the purpose of facies discrimination in many branches of geology and that association analysis is an effective method for this purpose. 相似文献