Viscoelastic flow of an Oldroyd-B fluid through a slowly varying contraction-expansion channel: pressure drop and elastic stress relaxation
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| Format: | Preprint |
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2025
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| _version_ | 1866915539586121728 |
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| author | Kedem, Yali Mahapatra, Bimalendu Boyko, Evgeniy |
| author_facet | Kedem, Yali Mahapatra, Bimalendu Boyko, Evgeniy |
| contents | Viscoelastic fluid flows in narrow non-uniform geometries are ubiquitous in various engineering applications and physiological flow systems. For such flows, one of the key interests is understanding how fluid viscoelasticity affects the flow rate-pressure drop relation, which remains not fully understood. We analyze the flow of the Oldroyd-B fluid in slowly varying contraction-expansion channels, commonly referred to as constrictions. Unlike most previous theoretical studies focusing on contracting channels, we consider a constriction geometry and present a theory for calculating the elastic stresses and flow rate-pressure drop relation at low and high Deborah ($De$) numbers. We apply lubrication theory and consider the ultra-dilute limit, in which the velocity approximates a parabolic and Newtonian profile. This results in a one-way coupling between the velocity and elastic stresses, allowing us to derive closed-form expressions for the elastic stresses and pressure drop for arbitrary values of $De$. We validate our theoretical predictions with numerical simulations, finding excellent agreement. We identify the physical mechanisms governing the pressure drop behavior and compare our results for the constriction with previous predictions for the contraction. At low $De$, the pressure drop in the constriction monotonically decreases with $De$, similar to the contraction. However, at high $De$, in contrast to a linear decrease for the contraction, the pressure drop across the constriction reaches a plateau due to the vanishing contribution of elastic normal stresses, leaving elastic shear stresses as the sole driver of the reduction. Furthermore, we elucidate the spatial relaxation of elastic stresses and pressure gradient in the exit channel following both constriction and contraction geometries, showing that the relaxation length is significantly shorter in the case of a constriction. |
| format | Preprint |
| id |
arxiv_https___arxiv_org_abs_2510_07166 |
| institution | arXiv |
| publishDate | 2025 |
| record_format | arxiv |
| spellingShingle | Viscoelastic flow of an Oldroyd-B fluid through a slowly varying contraction-expansion channel: pressure drop and elastic stress relaxation Kedem, Yali Mahapatra, Bimalendu Boyko, Evgeniy Fluid Dynamics Viscoelastic fluid flows in narrow non-uniform geometries are ubiquitous in various engineering applications and physiological flow systems. For such flows, one of the key interests is understanding how fluid viscoelasticity affects the flow rate-pressure drop relation, which remains not fully understood. We analyze the flow of the Oldroyd-B fluid in slowly varying contraction-expansion channels, commonly referred to as constrictions. Unlike most previous theoretical studies focusing on contracting channels, we consider a constriction geometry and present a theory for calculating the elastic stresses and flow rate-pressure drop relation at low and high Deborah ($De$) numbers. We apply lubrication theory and consider the ultra-dilute limit, in which the velocity approximates a parabolic and Newtonian profile. This results in a one-way coupling between the velocity and elastic stresses, allowing us to derive closed-form expressions for the elastic stresses and pressure drop for arbitrary values of $De$. We validate our theoretical predictions with numerical simulations, finding excellent agreement. We identify the physical mechanisms governing the pressure drop behavior and compare our results for the constriction with previous predictions for the contraction. At low $De$, the pressure drop in the constriction monotonically decreases with $De$, similar to the contraction. However, at high $De$, in contrast to a linear decrease for the contraction, the pressure drop across the constriction reaches a plateau due to the vanishing contribution of elastic normal stresses, leaving elastic shear stresses as the sole driver of the reduction. Furthermore, we elucidate the spatial relaxation of elastic stresses and pressure gradient in the exit channel following both constriction and contraction geometries, showing that the relaxation length is significantly shorter in the case of a constriction. |
| title | Viscoelastic flow of an Oldroyd-B fluid through a slowly varying contraction-expansion channel: pressure drop and elastic stress relaxation |
| topic | Fluid Dynamics |
| url | https://arxiv.org/abs/2510.07166 |