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塔拉  陈阜超  郭良迁  陈聚忠  薄万举 《大地测量与地球动力学》2013,33(4):1-3

????1951??????????????????1999-2007???GPS???????????????????α???????о???????????????岻????ε????α???????????α?????8.0??????????????????????????????8.0?????????????α?????????????α???????????????????????????????????????骲???????????й????λ?????????????????????????????????????γ????????????????????????????????????  相似文献   

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塔拉  陈阜超  韩月萍 《大地测量与地球动力学》2013,33(5):11-15

????1998-2006??????????????????????????????????????о??????????????????????????????????????????39.3°N??磬?????????????????С???????????????????1998-2002???в????????????????????????2002-2004??????????????????????2004-2006??????????  相似文献   

云南地区地壳垂直运动与地震的关系     

郭良迁  塔拉  陈阜超  周海涛  陈聚忠  薄万举 《大地测量与地球动力学》2013,33(1):1-5

利用云南地区1951—2011年的水准复测资料,计算获得了1951—1980年、1980—1994年、1994—2011年、1951—2011年的垂直形变速率图和各个阶段的形变增量场,结合该区的地震活动,研究了垂直形变与地震的关系。结果表明：7级以上地震主要发生在上升区,与区域性上升有关;地震多数发生在垂直形变速率增量场的正值区。  相似文献   

中国大陆应变应力场研究     

郭良迁  周海涛  杜雪松  塔拉 《华南地震》2012,32(1):1-10

根据1999～2009年网络工程GPS观测资料计算得到的应变率参数,研究了中国大陆地壳的应变应力场及其地壳现今的水平活动特征。结果表明,中国大陆地壳西部青藏亚板块的压应力主方向围绕藏南和阿萨姆构造结向北、东、南依次辐射撒开。新疆亚板块自西向东由近SN向变为NE向。中国大陆东部地壳的压应力主方向自北向南由NEE变为近EW向,再变为SEE向。中国大陆主压应力作用强度西部显著大于东部。中国大陆地壳西部强于东部,南部强于北部,现今西部地壳以挤压、走滑为主,东部地壳既有挤压、走滑,也有拉张。  相似文献   

Scale-based statistical analysis of sediment fluxes   总被引：1，自引：1，他引：0  

Jenny Campagnol  Alessio Radice  Francesco Ballio 《Acta Geophysica》2012,60(6):1744-1777

The flux of sediments over a line perpendicular to the main flow direction was measured during experiments of weak one-dimensional bed load. The standard definition of solid discharge through a boundary is a straightforward issue, yet the dependence of resulting values on the spatial and temporal scales used as a support for measurement is not. In this work, first- and second-order statistics of sediment transport rates were analyzed as scale-dependent quantities. The spatial scales used were significantly larger than the particle size, while the temporal scales covered a two-orders-of-magnitude range enabling the physical time scales of the single particles to be appreciated. In addition, the relationship between sediment fluxes, process intermittency and particle interarrival times was investigated. Proper knowledge of the scale-dependence of statistical properties of sediment transport fluxes may allow for adequate design of measuring campaigns (both in the laboratory and field) and for sound interpretation of data from multiple sources.  相似文献   

A Quantitative Assessment of DInSAR Measurements of Interseismic Deformation: The Southern San Andreas Fault Case Study     

Mariarosaria Manzo  Yuri Fialko  Francesco Casu  Antonio Pepe  Riccardo Lanari 《Pure and Applied Geophysics》2012,169(8):1463-1482

We investigate the capabilities and limitations of the Differential Interferometric Synthetic Aperture Radar (DInSAR) techniques, in particular of the Small BAseline Subset (SBAS) approach, to measure surface deformation in active seismogenetic areas. The DInSAR analysis of low-amplitude, long-wavelength deformation, such as that due to interseismic strain accumulation, is limited by intrinsic trade-offs between deformation signals and orbital uncertainties of SAR platforms in their contributions to the interferometric phases, the latter being typically well approximated by phase ramps. Such trade-offs can be substantially reduced by employing auxiliary measurements of the long-wavelength velocity field. We use continuous Global Positioning System (GPS) measurements from a properly distributed set of stations to perform a pre-filtering operation of the available DInSAR interferograms. In particular, the GPS measurements are used to estimate the secular velocity signal, approximated by a spatial ramp within the azimuth-range radar imaging plane; the phase ramps derived from the GPS data are then subtracted from the available set of DInSAR interferograms. This pre-filtering step allows us to compensate for the major component of the long-wavelength range change that, within the SBAS procedure, might be wrongly interpreted and filtered out as orbital phase ramps. With this correction, the final results are obtained by simply adding the pre-filtered long-wavelength deformation signal to the SBAS retrieved time series. The proposed approach has been applied to a set of ERS-1/2 SAR data acquired during the 1992–2006 time interval over a 200?×?200?km area around the Coachella Valley section of the San Andreas Fault in Southern California, USA. We present results of the comparison between the SBAS and the Line Of Sight (LOS)—projected GPS time series of the USGC/PBO network, as well as the mean LOS velocity fields derived using SBAS, GPS and stacking techniques. Our analysis demonstrates the effectiveness of the presented approach and provides a quantitative assessment of the accuracy of DInSAR measurements of interseismic deformation in a tectonically active area.  相似文献   

Huygens probe entry dynamic model and accelerometer data analysis     

Giacomo Colombatti  Alessio Aboudan  Francesca Ferri  Francesco Angrilli 《Planetary and Space Science》2008,56(5):601-612

During the first phase of Huygens arrival into Titan's atmosphere the probe is subjected to gravitational and aerodynamic forces in aerodynamic hypersonic regime. Atmospheric drag exerts a strong deceleration on the capsule measured by Huygens atmospheric structure instrument (HASI) servo accelerometer. A 6 DOF (Degree of Freedom) model of the Huygens probe entry dynamics has been developed and used for data analysis. The accelerometer data are analysed and the model allows the retrieval of dynamics information of Huygens probe from 1545 km altitude down to end of the entry phase. Probe's initial conditions (velocity and position) were refined to match the measured deceleration profile resulting in a different altitude at interface epoch with respect to those of the Cassini Navigation Team. Velocity and position of probe at interface epoch are compatible with those used by Descent Trajectory Working Group (DTWG).Measurements acquired before atmosphere detection are used to estimate probe's angular rate, bound attitude and characterise the angle of attack profile which results to be lower than 4^° during the whole entry. Probe's spin calculated (6.98 RPM) is slightly different with respect to DTWG of 7.28 RPM but considering a 2% error in the Inertia matrix these results are inside the 1-σ error band.  相似文献   

Compact massive objects in Virgo galaxies: the black hole population     

Marta Volonteri  Francesco Haardt  Kayhan Gültekin 《Monthly notices of the Royal Astronomical Society》2008,384(4):1387-1392

We investigate the distribution of massive black holes (MBHs) in the Virgo cluster. Observations suggest that active galactic nuclei activity is widespread in massive galaxies ( M _*≳ 10¹⁰ M_⊙), while at lower galaxy masses star clusters are more abundant, which might imply a limited presence of central black holes in these galaxy-mass regimes. We explore if this possible threshold in MBH hosting is linked to nature , nurture or a mixture of both. The nature scenario arises naturally in hierarchical cosmologies, as MBH formation mechanisms typically are efficient in biased systems, which would later evolve into massive galaxies. Nurture , in the guise of MBH ejections following MBH mergers, provides an additional mechanism that is more effective for low mass, satellite galaxies. The combination of inefficient formation, and lower retention of MBHs, leads to the natural explanation of the distribution of compact massive objects in Virgo galaxies. If MBHs arrive to the correlation with the host mass and velocity dispersion during merger-triggered accretion episodes, sustained tidal stripping of the host galaxies creates a population of MBHs which lie above the expected scaling between the holes and their host mass, suggesting a possible environmental dependence.  相似文献   

A model to simulate recharge processes of karst massifs   总被引：1，自引：0，他引：1       下载免费PDF全文

Francesco Fiorillo  Mauro Pagnozzi  Gerardo Ventafridda 《水文研究》2015,29(10):2301-2314

The recharge processes have been evaluated for two karst massifs of southern Italy, the Mt Terminio and Mt Cervialto, characterized by wide endorheic areas. The annual mean recharge has been estimated by Geographic Information System (GIS) tools, from regression of annual mean values of different ground‐elevated rain gauges and thermometers. The recharge has been distinguished for endorheic areas and the other areas of spring catchment, and the ratio between the output spring and input rainfall has been also estimated (recharge coefficient). The annual recharge has been used to calibrate a daily scale model, which allows to estimate the amount of effective rainfall, which is retained as soil moisture; the amount reaching the water table (recharge s.s.); and the amount of rainfall, which develops the runoff and leaves the catchment. All these amounts vary through the hydrological year, in function of soil moisture deficit and daily rainfall intensity. The model allows estimating the recharge conditions through the hydrological year, and it is a useful tool for water management. Copyright © 2014 John Wiley & Sons, Ltd.  相似文献   

Dismissing return periods!   总被引：5，自引：3，他引：2  

Francesco Serinaldi 《Stochastic Environmental Research and Risk Assessment (SERRA)》2015,29(4):1179-1189

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