在浅水方程的背景下,通过稳定均匀的非牛顿流体流动评估剪切速率公式

Pub Date : 2023-08-11 DOI:10.1590/2318-0331.282320230005
Yuri Taglieri Sáo, J. B. Pereira, G. Maciel
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引用次数: 0

摘要

非牛顿流变效应,如假塑性和粘塑性,被理解为剪切应力,纳入浅水方程(SWE)中的能量斜率项。然而,非牛顿剪切应力依赖于剪切速率,其公式是底部速度剖面梯度的函数。本研究探讨了两种在SWE文献中常用的剪切速率公式:1)非参数化函数;2)基于Herschel-Bulkley流变模型的函数。通过数值-理论比较,评价了它们对非牛顿流体稳定均匀流动的影响。采用拉克斯-弗里德里希方案求解SWE系统,并允许采用剪切速率公式。进行了实验测试,并对假设场景进行了数值模拟。结果表明,非参数化公式与理论解在正向深度上的偏差达14%,而基于Herschel-Bulkley模型的公式与理论解的一致性较好,这一点得到了计算流体动力学模拟(偏差小于2%)和实验数据的证实。两种剪切速率公式的比值与法向深度的偏差有很强的相关性,表明非参数化剪切速率函数在稳定均匀流动中不能提供可接受的结果。
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Evaluation of shear rate formulations through steady uniform non-Newtonian fluid flows in the context of shallow-water equations
ABSTRACT Non-Newtonian rheology effects, such as pseudoplasticity and viscoplasticity, are understood as shear stresses, incorporated to the energy slope term in the Shallow-Water Equations (SWE). However, non-Newtonian shear stresses are dependent of the shear rate, whose formulation is a function of the gradient of the velocity profile in the bottom. This study investigated two shear rate formulations that are commonly applied in the SWE literature: 1) a non-parameterized function; and 2) a function based on the Herschel-Bulkley rheological model. Their influence in steady uniform flows of non-Newtonian fluids was evaluated through numerical-theoretical comparisons. A Lax-Friedrichs scheme was implemented to solve the SWE system and allowed employing the shear rate formulations. Experimental tests were carried out and numerical simulations of hypothetical scenarios were performed. It was found that the non-parameterized formulation presented deviation in normal depth up to 14% in comparison with theoretical solution, while the formulation based on the Herschel-Bulkley model provided a good agreement, corroborated by punctual Computational Fluid Dynamics simulations (deviation less than 2%) and experimental data. The ratio of both shear rate formulations is strongly correlated to the deviation of normal depth, indicating that the non-parameterized shear rate function does not provide an acceptable result in the steady uniform flow.
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