To study the rolling motion of a ship in the presence of water on its deck,a linear-plus-quadratic damping term was incorporated into its equation of motion.Ship model tests indicates that the key dynamics of the phys...To study the rolling motion of a ship in the presence of water on its deck,a linear-plus-quadratic damping term was incorporated into its equation of motion.Ship model tests indicates that the key dynamics of the physical system are preserved in the ship rolling equation with the linear-plus-quadratic type damping term.To take into account the presence of randomness in the excitation and the response,a new method was developed and a Melnikov criterion was obtained to provide an upper bound on the domain of the potential chaotic rolling motion(erratic rocking).Additionally,the Melnikov criterion proposed in this study was verified by the utilization of phase plane diagrams and Poincare maps.Furthermore,this research has made the initial endeavor to systematically modify the system parameters in the rolling equation of motion for ship stability analysis.展开更多
冰川漂砾的形成年代通常难以直接测定,并且漂砾形成以后是否被再次搬运或者移动过,更是无法知道。本文研究发现,通过测试砾石不同部位的宇生同位素,不仅可以测定砾石形成的时代,而且可以确定砾石再次被搬运或者被翻转的年代,从而恢复砾...冰川漂砾的形成年代通常难以直接测定,并且漂砾形成以后是否被再次搬运或者移动过,更是无法知道。本文研究发现,通过测试砾石不同部位的宇生同位素,不仅可以测定砾石形成的时代,而且可以确定砾石再次被搬运或者被翻转的年代,从而恢复砾石运动的历史。本文以石英中生成的宇生同位素^(10)Be,对青藏高原东南部海子山的冰川漂砾进行了探讨,结果表明该砾石形成于倒数第二次冰期(186～128 ka BP之间),在末次冰期中再次被冰川搬运,使之反转。该方法不局限于^(10)Be和冰川漂砾,也适用于其他陆面岩石中生成的宇生同位素以及其他成因的石块或者砾石。因此为探讨冰川作用、泥石流活动、重力崩塌等过程提供了一种重要的方法和技术途径。展开更多
文摘To study the rolling motion of a ship in the presence of water on its deck,a linear-plus-quadratic damping term was incorporated into its equation of motion.Ship model tests indicates that the key dynamics of the physical system are preserved in the ship rolling equation with the linear-plus-quadratic type damping term.To take into account the presence of randomness in the excitation and the response,a new method was developed and a Melnikov criterion was obtained to provide an upper bound on the domain of the potential chaotic rolling motion(erratic rocking).Additionally,the Melnikov criterion proposed in this study was verified by the utilization of phase plane diagrams and Poincare maps.Furthermore,this research has made the initial endeavor to systematically modify the system parameters in the rolling equation of motion for ship stability analysis.
文摘冰川漂砾的形成年代通常难以直接测定,并且漂砾形成以后是否被再次搬运或者移动过,更是无法知道。本文研究发现,通过测试砾石不同部位的宇生同位素,不仅可以测定砾石形成的时代,而且可以确定砾石再次被搬运或者被翻转的年代,从而恢复砾石运动的历史。本文以石英中生成的宇生同位素^(10)Be,对青藏高原东南部海子山的冰川漂砾进行了探讨,结果表明该砾石形成于倒数第二次冰期(186～128 ka BP之间),在末次冰期中再次被冰川搬运,使之反转。该方法不局限于^(10)Be和冰川漂砾,也适用于其他陆面岩石中生成的宇生同位素以及其他成因的石块或者砾石。因此为探讨冰川作用、泥石流活动、重力崩塌等过程提供了一种重要的方法和技术途径。
