论文标题
大数据存在理论,用于与应力扩散的速率粘弹性流体的三维不稳定流动
Large data existence theory for three-dimensional unsteady flows of rate-type viscoelastic fluids with stress diffusion
论文作者
论文摘要
我们证明,对于任意较大的时间间隔和数据,在三个维度上管理粘弹性流体不稳定流动的系统存在薄弱的解决方案。流体是由速度$ v $的不可压缩的Navier-Stokes方程描述的,再加上Oldroyd-B和Giesekus型号的扩散变体,用于张量$ \ Mathbb {B} $。 By a proper choice of the constitutive relations for the Helmholtz free energy (which, however, is non-standard in the current literature, despite the fact that this choice is well motivated from the point of view of physics) and for the energy dissipation, we are able to prove that $\mathbb{B}$ enjoys the same regularity as $v$ in the classical three-dimensional Navier-Stokes equations.这使我们能够处理$ \ mathbb {b} $的任何客观导数,从而为扩散的约翰逊 - 塞加尔曼模型的类别获得了存在结果。此外,使用合适的近似方案,我们能够证明$ \ mathbb {b} $如果初始基准是一个积极的确定矩阵(从点上意义上讲),则仍然是积极的。我们还展示了如何以自然方式从基本平衡方程和热力学原理中得出的模型。
We prove that there exists a weak solution to a system governing an unsteady flow of a viscoelastic fluid in three dimensions, for arbitrarily large time interval and data. The fluid is described by the incompressible Navier-Stokes equations for the velocity $v$, coupled with a diffusive variant of a combination of the Oldroyd-B and the Giesekus models for a tensor $\mathbb{B}$. By a proper choice of the constitutive relations for the Helmholtz free energy (which, however, is non-standard in the current literature, despite the fact that this choice is well motivated from the point of view of physics) and for the energy dissipation, we are able to prove that $\mathbb{B}$ enjoys the same regularity as $v$ in the classical three-dimensional Navier-Stokes equations. This enables us to handle any kind of objective derivative of $\mathbb{B}$, thus obtaining existence results for the class of diffusive Johnson-Segalman models as well. Moreover, using a suitable approximation scheme, we are able to show that $\mathbb{B}$ remains positive definite if the initial datum was a positive definite matrix (in a pointwise sense). We also show how the model we are considering can be derived from basic balance equations and thermodynamical principles in a natural way.