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991.
This article describes the patterns of distribution of sorbed gaseous hydrocarbons in dispersed rocks of oil and gas areas
to determine the possibility of using them as indicators of water pollution. Sorbed gaseous hydrocarbons have a number of
geochemical properties that contribute to their influence on technological conditions and long-term preservations of the changes
that occur in their composition in man-made conditions. 相似文献
992.
V. V. Emel’yanenko 《Solar System Research》2010,44(4):281-289
One of the main particular features of the structure of the Kuiper Belt is that it contains clusters of objects of small orbital
eccentricity and inclination (“cold population”). In order to solve the problem of the origin of the objects, we considered
the process of the gravitational interaction of a comparatively small-mass planet with a planetesimal disk. We found that
one particular property of the process is that the planet changes its direction of migration. The interaction with the planet
results in the transportation of a considerable portion of planetesimals from the inner zone out to the Kuiper Belt. After
such a transition of the objects, the planet returns to the inner regions of the planetesimal disk. Numerical simulations
show that the reversible migration of a planet of a mass similar to that of the Earth can explain the main properties of the
Kuiper Belt’s cold population orbit distribution. 相似文献
993.
The structure of the AGN object 1803+784 has been investigated at a wavelength of 7 mm with a limiting angular resolution
reaching 20 μas. The ejector nozzle surrounded by a ring structure, an accretion disk, has been identified. The nozzle size
is ∼0.1 pc, the diameter of the ring structure is ∼1.4 pc, and its width is ∼0.25 pc. The reaction of the plasma flow produces
a multimode precession responsible for the conical helical structure of the jet with a variable step and a curved axis. The
viewing angle of the flow ejection is ∼40°. The central part of the ejected flow moving along the axis accelerates to a relativistic
velocity. The apparent velocity reaches 12 s at a distance of ∼1 mas or ∼6 pc from the ejector. The outer part of the flow
moves along a helix around a high-velocity component whose step is a factor of 4 smaller, because the longitudinal velocity
is relatively low. The plasma is ejected almost toward the observer, as confirmed by its high brightness temperature T
b ≈ 8 × 1013 K and highly beamed emission. The polarized emission from the nozzle is axisymmetric. The orientation of the polarization
of the flow along the whole length is aligned with the direction of its motion, suggesting the excitation of a ring magnetic
field around it and self-focusing. 相似文献
994.
995.
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998.
A. E. Vol’vach L. N. Vol’vach A. M. Kut’kin M. G. Larionov M. F. Aller H. D. Aller 《Astronomy Reports》2010,54(1):28-37
Long-term, multi-frequency monitoring of the radio fluxes of the four BL Lac objects 3C 120, OJ 287, 1308+326, and BL Lac
is considered. Harmonic components of the flux variability on scales from one year to decades are determined. The observational
data used were obtained at the Radio Astronomy Laboratory of the Crimean Astrophysical Observatory (Ukraine) and the University
of Michigan Radio Astronomy Observatory (USA). These data are used to construct kinematic models for active galactic nuclei
using values for the orbital and precessional periods of binary systems consisting of supermassive black holes. The derived
speeds of the companions in their orbits lie in the narrow range 3000–4000 km/s. The orbital radii for the binary supermassive
black holes also lie in a narrow range, 1017–1018 cm, providing evidence that observed prominent examples of active galactic nuclei are fairly close binary systems. The parameters
of the mediumin which the components of the binary systems are moving are estimated, as well as the rates at which the systems
are losing orbital angular momentum and their lifetimes to coalescence. 相似文献
999.
N. P. Laverov N. S. Bortnikov L. S. Borodin L. Z. Bykhovsky D. V. Grichuk V. I. Kazansky V. I. Kovalenko M. I. Kuz’min I. V. Migachev B. I. Omel’yanenko V. Yu. Prokof’ev I. D. Ryabchikov Yu. G. Safonov A. I. Khanchuk V. N. Kholodov V. V. Yarmolyuk I. V. Murav’eva 《Geology of Ore Deposits》2010,52(5):337-338
1000.