The Campi Flegrei caldera (Italy) has been the site of intense seismic activity over the past decades. This area is densely populated and includes important towns such as Napoli with historical sites and supporting many industries. For the proper use and management of the region, the evaluation of the dynamic properties of near-surface rocks is necessary.
The volcanological pattern has been reconstructed from the lithostratigraphies of several drillings. The most interesting and widespread pyroclastic products are the pozzolana deposit (soil) and the Neapolitan Yellow Tuff (rock). Both pozzolana and tuff products are covered by recent eluvial and coastal sandy deposits and younger volcanic products (<12 000 years). The characteristic ranges of the shear wave velocity (Vs) of the Campi Flegrei–Neapolitan soils and tuffs are defined and the primary influencing factors are evaluated. For the sandy deposits, the results show that eluvial and lacustral products have lower shear wave velocities than coastal products. For the volcanic products younger than 12 000 years b.p. the influence of vertical pressure is emphasized. As regards the pozzolana deposit (soil) and the Neapolitan Yellow Tuff (rock), a major influencing factor is shown by the textural characteristics and the different hardening degrees as a consequence of the diagenetic processes. The scattering of the Vs velocities for the same formation is so wide that only the variability ranges can be individuated. These results suggest a need to carry out detailed Vs measurements or, at least, to make a parametric study of the effect of the Vs ranges on seismic response analysis in order to give safe building codes. 相似文献
针对台风数值预报中由于采用对称模型而导致预报误差的现实,通过引入非对称分布的台风最大风速、最大风速半径等因子,在得到台风报告中7级风和10级风的半径的基础上,利用最佳权系数方案来得到非对称的台风外围风速分布因子,从而对Chan and Williams 1987年提出的切向风廓线方案进行改造,进而得到了台风海面非对称风场的计算式。检验表明,该方法能够描述台风海面风场的非对称分布,具有较好的应用前景。 相似文献