Following the LAMOST Spectroscopic Survey and the Xuyi’s Photometric Survey of the Galactic Anti-center, we plan to carry out a time-domain survey of the Galactic Anti-center (TDS-GAC) to study variable stars by using the Nanshan 1-meter telescope. Before the beginning of TDS-GAC, a precursive sky survey (PSS) has been executed. The goal of the PSS is to optimize the observation strategy of TDS-GAC and to detect some strong transient events, as well as to find some short time-scale variable stars of different types. By observing a discontinuous sky area of \(15.03~\mbox{deg}^{2}\) with the standard Johnson-Cousin-Bessel \(V\) filter, 48 variable stars are found and the time series are analyzed. Based on the behaviors of the light curves, 28 eclipsing binary stars, 10 RR Lyraes, 3 periodic pulsating variables of other types have been classified. The rest 7 variables stay unclassified with deficient data. In addition, the observation strategy of TD-GAC is described, and the pipeline of data reduction is tested. 相似文献
Imaging Atmospheric Cherenkov Telescopes have revealed more than 100 TeV sources along the galactic plane, around 45% of them remain unidentified. However, radio observations revealed that dense molecular clumps are associated with 67% of 18 unidentified TeV sources. In this paper, we propose that an electron–positron magnetospheric accelerator emits detectable TeV gamma-rays when a rapidly rotating black hole enters a gaseous cloud. Since the general-relativistic effect plays an essential role in this magnetospheric lepton accelerator scenario, the emissions take place in the direct vicinity of the event horizon, resulting in a point-like gamma-ray image. We demonstrate that their gamma-ray spectra have two peaks around 0.1 GeV and 0.1 TeV and that the accelerators become most luminous when the mass accretion rate becomes about 0.01% of the Eddington accretion rate. We compare the results with alternative scenarios such as the cosmic-ray hadron scenario, which predicts an extended morphology of the gamma-ray image with a single power-law photon spectrum from GeV to 100 TeV. 相似文献
The acquisition of paleostress data has always been a key and difficult problem in the field of tectonics and crustal dynamics. Previous findings show that the distribution of dykes and the alignment of volcano vents can indicate the direction of major principal stresses during the volcanic eruption period. The extension direction of underground dyke is generally parallel to the linear arrangement direction of vent and both of them give the direction of maximum horizontal principal stress in this period. This law has similar mechanical principle to hydraulic fracturing. Vent alignment survey method is a kind of geostress inversion method based on volcanic linear mode. In this paper theoretical basis of vent alignment survey method and the linear model of volcanic array are introduced. Based on the panchromatic high-resolution remote sensing image and digital elevation model(DEM)data in the Tengchong area, combining the geological exploration data about lithologic distribution of igneous rocks and the past research results of volcanic activities in the area, the research divides the volcanoes in this area, according to the age of volcanic eruption, into Holocene, late Pleistocene, early Pleistocene and Pliocene. Nakamura model was established based on the morphological characteristics and spatial distribution of the crater, and volcanic eruption period to evaluate the linear degree of the volcano in different age, and to carry out inversion of the paleostress field of the four volcanic eruption periods in Tengchong area. The reliability of the inversion results is evaluated according to Paulsen's data reliability assessment system. The data from inverting the paleostress of each show that maximum horizontal principal stress directions in the early Pleistocene period and late Pleistocene period are 39° and 37° respectively and reliability grades of inverted paleostress results in the two eras all belong to grade B; Inverted paleostress results in Holocene and Pliocene are not reliable because of the poor linearity of volcanic arrangement. The geostress direction determined by the vent alignment survey method is fairly consistent with the current geostress field obtained by the focal mechanism solution and the anelastic strain recovery(ASR method)and matches the tectonic history of Tengchong area since Neogene. The research findings demonstrate that the vent alignment survey method is an effective paleostress inversion method. The application of this method in the paleostress inversion of the Tengchong volcanic area is of important reference significance for the study of paleostress field in other volcanic areas in China. 相似文献
Acta Geotechnica - The paper examines three-dimensional (3D) analyses of the load bearing capacity of square and strip footings on a spatially variable cohesive–frictional (c–φ)... 相似文献
Light rain or moderate rain is the most common meteorological event in the rainy season in the loess area of China, so the probability of landslide hazards induced by the coupling effect of earthquakes and rainfall under the condition of light rain or moderate rain is relatively higher than that under heavy rain. To study the dynamic response characteristics and instability mechanism of loess slopes by the coupling effect of earthquakes and rainfall under the conditions of moderate rain and light rain, a low-angle slope model test of a large-scale shaking table after 10 mm of rainfall was carried out. By gradually increasing the dynamic loading, the evolution of the macroscopic deformation and the instability failure mode of the slope model are observed; the temporal and spatial trends of the amplification effect, acceleration spectrum, pore pressure and soil pressure are analyzed; and the failure mechanism of the slope is determined. The results showed that the amplification effect increased along the slope surface upward, and a strong amplification effect appeared at the front of the top of the slope. Because of the stronger dynamic stress action on the upper part of the slope, the immersed soil in the upper part of the slope experienced seismic subsidence deformation, the saturation in the seismic subsidence soil increased, and the water content temporarily increased locally. With the further increase in the loading intensity, a large number of tension cracks were generated in the seismic subsidence area, and water infiltrated down along the cracks and the wetting range expanded under dynamic action. The range of seismic subsidence and cracks further extended to the deep part of the slope. Under the reciprocating action of the subsequent ground motion, the swing amplitude of the soil mass in the seismic subsidence area, which is divided by a large number of cracks in the upper part of the slope, increased further, resulting in the further reduction in the residual strength of the seismic subsidence soil mass located at the crack tip due to the pull and shear action. Finally, under the combined action of gravity and dynamic force, the upper soil mass in the seismic subsidence area dragged the lower soil mass in the seismic subsidence area downward because the sliding force is greater than the residual strength of the soil mass, which induced a seismic subsidence-type loess landslide. Under the coupling effect of earthquakes and rainfall, the instability mode and mechanism of this landslide are significantly different from those of liquefaction-type landslides.