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81.
Éric Chaumillon Hervé Gillet Nicolas Weber Michel Tesson 《Comptes Rendus Geoscience》2002,334(2):119-126
The evolution and the internal architecture of an estuary type sand ridge has been studied with a set of bathymetric data recorded during the last two centuries and with a dense grid of recent very high resolution seismic profiles. Bathymetric data of the so-called, Longe de Boyard sand ridge, displays sand losts due to wave and tide erosion. Internal geometry, through seismic profile analysis, indicates two main phases of deposition recording both, a recent high energy environment and an older low energy one, respectively. Such an evolution is believed to record changes in sedimentation processes mainly related to the end of the Holocene transgression (8 000–5 000 yr BP). To cite this article: É. Chaumillon et al., C. R. Geoscience 334 (2002) 119–126. 相似文献
82.
Thibaut Lery CÉline Combet Gareth Murphy Luke O. C. Drury 《Astrophysics and Space Science》2005,298(1-2):375-378
As network performance has outpaced computational power and storage capacity, a new paradigm has evolved to enable the sharing
of geographically distributed resources. This paradigm is known as Grid computing and aims to offer access to distributed
resource irrespective of their physical location. Many national, European and international projects have been launched during
the last years trying to explore the Grid and to change the way we are doing our everyday work. In Ireland, we have started
the CosmoGrid project that is a collaborative project aimed to provide high performance super-computing environments. This
will help to address complex problems such as magnetohydrodynamic outflows and jets in order to model and numerically simulate
them. Indeed, the numerical modeling of plasma jets requires massive computations, due to the wide range of spatial-temporal
scales involved. We present here the first jet simulations and their corresponding models that could help to understand results
from laboratory experiments. 相似文献
83.
Efficiency of carrier-phase integer ambiguity resolution for precise GPS positioning in noisy environments 总被引:1,自引:0,他引:1
Precise GPS positioning relies on tracking the carrier-phase. The fractional part of carrier-phase can be measured directly
using a standard phase-locked loop, but the integer part is ambiguous and the ambiguity must be resolved based on sequential
carrier-phase measurements to ensure the required positioning precision. In the presence of large phase-measurement noise,
as can be expected in a jamming environment for example, the amount of data required to resolve the integer ambiguity can
be large, which requires a long time for any generic integer parameter estimation algorithm to converge. A key question of
interest in significant applications of GPS where fast and accurate positioning is desired is then how the convergence time
depends on the noise amplitude. Here we address this question by investigating integer least-sqaures estimation algorithms.
Our theoretical derivation and numerical experiments indicate that the convergence time increases linearly with the noise
variance, suggesting a less stringent requirement for the convergence time than intuitively expected, even in a jamming environment
where the phase noise amplitude is large. This finding can be useful for practical design of GPS-based systems in a jamming
environment, for which the ambiguity resolution time for precise positioning may be critical. 相似文献
84.
Émilie Gaudry Philippe Sainctavit Farid Juillot Federica Bondioli Philippe Ohresser Isabelle Letard 《Physics and Chemistry of Minerals》2006,32(10):710-720
The best known cause for colors in insulating minerals is due to transition metal ions as impurities. As an example, Cr3+ is responsible for the red color of ruby (α-Al2O3:Cr3+) and the green color of eskolaite (α-Cr2O3). Using X-ray absorption measurements, we connect the colors of the Cr
x
Al2−x
O3 series with the structural and electronic local environment around Cr. UV–VIS electronic parameters, such as the crystal field and the Racah parameter B, are related to those deduced from the analysis of the isotropic and XMCD spectra at the Cr L2,3-edges in Cr0.07Al1.93O3 and eskolaite. The Cr–O bond lengths are extracted by EXAFS at the Cr K-edge in the whole Cr
x
Al2−x
O3 (0.07≤x< 2) solid solution series. The variation of the mean Cr–O distance between Cr0.07Al1.93O3 and α-Cr2O3 is evaluated to be 0.015 Å (≈1%). The variation of the crystal field in the Cr
x
Al2−x
O3 series is discussed in relation with the variation of the averaged Cr–O distances. 相似文献
85.
86.
Bálint Érdi 《Celestial Mechanics and Dynamical Astronomy》1977,15(3):367-383
The planar motion of a Trojan asteroid is considered within the framework of the elliptic restricted three-body problem. The solution is derived asymptotically to second order taking the square root of the Jupiter-Sun mass ratio and the orbital eccentricity of Jupiter as first order quantities. The results are given in explicit form for the coordinates as functions of the true anomaly of Jupiter including both short and long periodic terms resulting from the orbital accentricity of Jupiter. 相似文献
87.
É. Érgma 《Astrophysics》1971,7(4):363-365
88.
Bálint Érdi 《Celestial Mechanics and Dynamical Astronomy》1978,18(2):141-161
The problem is considered within the framework of the elliptic restricted three-body problem. The asymptotic solution is derived by a three-variable expansion procedure. The variables of the expansion represent three time-scales of the asteroids: the revolution around the Sun, the libration around the triangular Lagrangian pointsL
4,L
5, and the motion of the perihelion. The solution is obtained completely in the first order and partly in the second order. The results are given in explicit form for the coordinates as functions of the true anomaly of Jupiter. As an example for the perturbations of the orbital elements the main perturbations of the eccentricity, the perihelion longitude and the longitude of the ascending node are given. Conditions for the libration of the perihelion are also discussed. 相似文献
89.
90.