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A priori error estimates for semidiscrete finite element approximations to equations of motion arising in oldroyd fluids of order one

机译:半离散有限元逼近运动方程的先验误差估计

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In this paper, a semidiscrete finite element Galerkin method for the equations of motion arising in the 2D Oldroyd model of viscoelastic fluids of order one with the forcing term independent of time or in L~∞ in time, is analyzed. A step-by-step proof of the estimate in the Dirichlet norm for the velocity term which is uniform in time is derived for the nonsmooth initial data. Further, new regularity results are obtained which reflect the behavior of solutions as t → 0 and t → ∞. Optimal L~∞(L~2) error estimates for the velocity which is of order O(t~(-1/2)h~2) and for the pressure term which is of order O(t~(-1/2)h) are proved for the spatial discretization using conforming elements, when the initial data is divergence free and in H_0~1. Moreover, compared to the results available in the literature even for the Navier-Stokes equations, the singular behavior of the pressure estimate as t → 0, is improved by an order 1/2, from t~(-1) to t~(-1/2), when conforming elements are used. Finally, under the uniqueness condition, error estimates are shown to be uniform in time.
机译:本文针对一阶粘弹性流体的二维Oldroyd模型中所产生的运动方程,采用半离散有限元Galerkin方法,其强迫项与时间无关或在时间上与L〜∞无关。对于不光滑的初始数据,得出了狄利克雷范数中速度项的估计的逐步证明,该估计在时间上是均匀的。此外,获得了新的规律性结果,这些结果反映了解决方案的行为,即t→0和t→∞。速度为O(t〜(-1/2)h〜2)和压力项为O(t〜(-1/2)的最优L〜∞(L〜2)误差估计)h)证明了当初始数据无散度且在H_0〜1时使用一致元进行空间离散化。此外,与文献中甚至是Navier-Stokes方程的结果相比,压力估计值从t〜(-1)到t〜(t)从0〜(-1)改善了1/2级。 -1/2),使用一致的元素时。最后,在唯一性条件下,误差估计在时间上是一致的。

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