论文标题
耦合的Boussinesq方程和Ostrovsky型模型的定期解决方案无零质量矛盾
Periodic solutions of coupled Boussinesq equations and Ostrovsky-type models free from zero-mass contradiction
论文作者
论文摘要
耦合的Boussinesq方程描述了双层层中长弱非斜线纵向应变波(例如,柔软的粘合剂)。从数学角度来看,当层中的线性长波速度显着不同时,就会出现一个特别困难的情况(高对比度)。单向模型的传统推导导致四个未耦合的奥斯特罗夫斯基方程,对于每一层的右和左传播波。但是,模型强加了``零质量约束'',即初始条件必须具有零均值,从而限制了该描述的适用性。在这里,我们使用渐近的多尺度扩展涉及两对快速特征变量和两个慢速变量,绕过了这种高对比度情况下的矛盾。通过构造,在本范围内出现的Ostrovsky方程在零平均值的初始条件下可以解决,而原始系统的初始条件可能具有非零的平均值。仔细检查溶液的渐近有效性。我们将模型应用于由孤立波初始条件产生的反向传播波的描述,或者由cNoidal波浪初始条件产生的联合传播波,以及所得的波相互作用,并与双层层中波的行为形成鲜明对比(在层中线性长波速度接近(低构造构件)。得出了菌株耦合的Boussinesq方程的一个局部(经典)和两个非本地(广义)保护定律,并用于控制数值模拟的准确性。
Coupled Boussinesq equations describe long weakly-nonlinear longitudinal strain waves in a bi-layer with a soft bonding between the layers (e.g. a soft adhesive). From the mathematical viewpoint, a particularly difficult case appears when the linear long-wave speeds in the layers are significantly different (high-contrast case). The traditional derivation of the uni-directional models leads to four uncoupled Ostrovsky equations, for the right- and left-propagating waves in each layer. However, the models impose a ``zero-mass constraint'' i.e. the initial conditions should necessarily have zero mean, restricting the applicability of that description. Here, we bypass the contradiction in this high-contrast case by constructing the solution for the deviation from the evolving mean value, using asymptotic multiple-scale expansions involving two pairs of fast characteristic variables and two slow-time variables. By construction, the Ostrovsky equations emerging within the scope of this derivation are solved for initial conditions with zero mean while initial conditions for the original system may have non-zero mean values. Asymptotic validity of the solution is carefully examined numerically. We apply the models to the description of counter-propagating waves generated by solitary wave initial conditions, or co-propagating waves generated by cnoidal wave initial conditions, as well as the resulting wave interactions, and contrast with the behaviour of the waves in bi-layers when the linear long-wave speeds in the layers are close (low-contrast case). One local (classical) and two non-local (generalised) conservation laws of the coupled Boussinesq equations for strains are derived, and these are used to control the accuracy of the numerical simulations.