Newtonian fluid: Difference between revisions
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A '''Newtonian fluid''' is a [[fluid]] in which the [[viscous stress tensor|viscous stresses]] arising from its [[Fluid dynamics|flow]] are at every point linearly correlated to the local [[strain rate]] — the [[derivative (mathematics)|rate of change]] of its [[deformation (mechanics)|deformation]] over time.<ref>{{cite book |first=Ronald L. |last=Panton |title=Incompressible Flow |edition=Fourth |year=2013 |publisher=John Wiley & Sons |location=Hoboken |page=114 |isbn=978-1-118-01343-4 }}</ref><ref name=Batchelor>{{cite book |first= G. K. |last=Batchelor |author-link=George Batchelor |title= An Introduction to Fluid Dynamics |publisher= Cambridge Mathematical Library series, Cambridge University Press |year=2000 |orig-year= 1967 |url= https://books.google.com/books?id=Rla7OihRvUgC&pg=PP1 |isbn=978-0-521-66396-0}}</ref><ref name=Kundu>{{cite book |last1= Kundu |first1=P. |last2=Cohen |first2=I. |title= Fluid Mechanics |page= (page needed)}}</ref><ref name=Kirby>{{cite book |last= Kirby |first=B. J. |title= Micro- and Nanoscale Fluid Mechanics: Transport in Microfluidic Devices |url= http://www.kirbyresearch.com/textbook | year= 2010| publisher=Cambridge University Press |isbn=978-0-521-11903-0| via= kirbyresearch.com}}</ref> Stresses are proportional to the rate of change of the fluid's [[velocity|velocity vector]]. |
A '''Newtonian fluid''' is a [[fluid]] in which the [[viscous stress tensor|viscous stresses]] arising from its [[Fluid dynamics|flow]] are at every point linearly correlated to the local [[strain rate]] — the [[derivative (mathematics)|rate of change]] of its [[deformation (mechanics)|deformation]] over time.<ref>{{cite book |first=Ronald L. |last=Panton |title=Incompressible Flow |edition=Fourth |year=2013 |publisher=John Wiley & Sons |location=Hoboken |page=114 |isbn=978-1-118-01343-4 }}</ref><ref name=Batchelor>{{cite book |first= G. K. |last=Batchelor |author-link=George Batchelor |title= An Introduction to Fluid Dynamics |publisher= Cambridge Mathematical Library series, Cambridge University Press |year=2000 |orig-year= 1967 |url= https://books.google.com/books?id=Rla7OihRvUgC&pg=PP1 |isbn=978-0-521-66396-0}}</ref><ref name=Kundu>{{cite book |last1= Kundu |first1=P. |last2=Cohen |first2=I. |title= Fluid Mechanics |page= (page needed)}}</ref><ref name=Kirby>{{cite book |last= Kirby |first=B. J. |title= Micro- and Nanoscale Fluid Mechanics: Transport in Microfluidic Devices |url= http://www.kirbyresearch.com/textbook | year= 2010| publisher=Cambridge University Press |isbn=978-0-521-11903-0| via= kirbyresearch.com}}</ref> Stresses are proportional to the rate of change of the fluid's [[velocity|velocity vector]]. |
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A fluid is Newtonian only if the [[tensor]]s that describe the viscous stress and the strain rate are related by a constant [[viscosity|viscosity tensor]] that does not depend on the stress state and velocity of the flow. If the fluid is also [[isotropic]] (mechanical properties are the same along any direction), the viscosity tensor reduces to two real coefficients, describing the fluid's resistance to continuous [[Shearing (physics)|shear deformation]] and continuous [[compression (physical)|compression]] or expansion, respectively. |
A fluid is Newtonian only if the [[tensor]]s that describe the viscous stress and the strain rate are related by a constant [[viscosity|viscosity tensor]] that does not depend on the stress state and velocity of the flow. If the fluid is also [[isotropic]] (i.e., its mechanical properties are the same along any direction), the viscosity tensor reduces to two real coefficients, describing the fluid's resistance to continuous [[Shearing (physics)|shear deformation]] and continuous [[compression (physical)|compression]] or expansion, respectively. |
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Newtonian fluids are the easiest [[mathematical model]]s of fluids that account for viscosity. While no real fluid fits the definition perfectly, many common liquids and gases, such as water and air, can be assumed to be Newtonian for practical calculations under ordinary conditions. However, [[non-Newtonian fluid]]s are relatively common and include [[Non-newtonian fluid#Oobleck|oobleck]] (which becomes stiffer when vigorously sheared) and non-drip [[paint]] (which becomes [[shear thinning|thinner when sheared]]). Other examples include many [[polymer]] solutions (which exhibit the [[Weissenberg effect]]), molten polymers, many solid suspensions, blood, and most highly viscous fluids. |
Newtonian fluids are the easiest [[mathematical model]]s of fluids that account for viscosity. While no real fluid fits the definition perfectly, many common liquids and gases, such as water and air, can be assumed to be Newtonian for practical calculations under ordinary conditions. However, [[non-Newtonian fluid]]s are relatively common and include [[Non-newtonian fluid#Oobleck|oobleck]] (which becomes stiffer when vigorously sheared) and non-drip [[paint]] (which becomes [[shear thinning|thinner when sheared]]). Other examples include many [[polymer]] solutions (which exhibit the [[Weissenberg effect]]), molten polymers, many solid suspensions, blood, and most highly viscous fluids. |
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===Incompressible isotropic case=== |
===Incompressible isotropic case=== |
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For an [[incompressible]] and isotropic Newtonian fluid in '''laminar flow only in the direction x''' (i.e. where viscosity is isotropic in the fluid) |
For an [[incompressible]] and isotropic Newtonian fluid in '''laminar flow only in the direction x''' (i.e. where viscosity is isotropic in the fluid), the shear stress is related to the strain rate by the simple [[constitutive equation]] |
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<math display="block">\tau = |
<math display="block">\tau = \mu \frac{du}{dy}</math> |
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where |
where |
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*<math>\tau</math> is the [[shear stress]] ("[[drag (physics)|skin drag]]") in the fluid, |
*<math>\tau</math> is the [[shear stress]] ("[[drag (physics)|skin drag]]") in the fluid, |
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In case of a general 2D incompressibile flow in the plane x, y, the Newton constitutive equation become: |
In case of a general 2D incompressibile flow in the plane x, y, the Newton constitutive equation become: |
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<math display="block">\tau_{xy} = |
<math display="block">\tau_{xy} = \mu \left( \frac{\partial u}{\partial y} +\frac{\partial v}{\partial x} \right)</math> |
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where: |
where: |
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*<math>\tau_{xy}</math> is the [[shear stress]] ("[[drag (physics)|skin drag]]") in the fluid, |
*<math>\tau_{xy}</math> is the [[shear stress]] ("[[drag (physics)|skin drag]]") in the fluid, |
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*<math>\frac{\partial u}{\partial y}</math> is the [[partial derivative]] in the direction y of the [[flow velocity]] component u that is oriented along the direction x. |
*<math>\frac{\partial u}{\partial y}</math> is the [[partial derivative]] in the direction y of the [[flow velocity]] component u that is oriented along the direction x. |
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*<math>\frac{\partial v}{\partial x}</math> is the partial derivative in the direction x of the flow velocity component v that is oriented along the direction y. |
*<math>\frac{\partial v}{\partial x}</math> is the partial derivative in the direction x of the flow velocity component v that is oriented along the direction y. |
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However, there are in this case two more components of the shear stress, that are described by Newton's constitutive equation: |
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<math display="block">\tau_{xx} = - 2 \mu \frac{\partial u}{\partial x}</math> |
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and: |
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<math display="block">\tau_{yy} = - 2 \mu \frac{\partial v}{\partial y}</math> |
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Note that in the previous case these components were identically 0: <math>\tau_{xx}=0</math> since the x component of the velocity was constant along the direction x, and <math>\tau_{yy}=0</math> since the y component of the velocity was zero in every point of the flow (the flow was only in the x direction). |
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We can now generalize to the case of an [[incompressible fluid|incompressible flow]] with a general direction in the 3D space, the above constitutive equation becomes |
We can now generalize to the case of an [[incompressible fluid|incompressible flow]] with a general direction in the 3D space, the above constitutive equation becomes |
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<math display="block">\tau_{ij} = |
<math display="block">\tau_{ij} = \mu \left(\frac{\partial v_i}{\partial x_j} + \frac{\partial v_j}{\partial x_i} \right)</math> |
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where |
where |
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*<math>x_j</math> is the <math>j</math>th spatial coordinate |
*<math>x_j</math> is the <math>j</math>th spatial coordinate |
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or written in more compact tensor notation |
or written in more compact tensor notation |
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<math display="block">\boldsymbol{\tau} = |
<math display="block">\boldsymbol{\tau} = \mu\left(\nabla\mathbf{u}+\nabla\mathbf{u}^{T}\right)</math> |
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where <math>\nabla \mathbf{ |
where <math>\nabla \mathbf{u}</math> is the flow velocity gradient. |
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An alternative way of stating this constitutive equation is: |
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{{Equation box 1 |
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|indent=: |
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|title='''Stokes' stress [[constitutive equation]]''' ''(expression used for incompressible elastic solids)'' |
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|equation=:<math>\boldsymbol \tau = 2 \mu \boldsymbol \varepsilon</math> |
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}} |
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where |
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<math display="block">\boldsymbol{\varepsilon} = \tfrac{1}{2} \left( \mathbf{\nabla u} + \mathbf{\nabla u}^\mathrm{T} \right)</math> |
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is the rate-of-[[strain tensor]]. So this decomposition can be made explicit as:<ref name=Batchelor_142_148>Batchelor (1967) pp. 137 & 142.</ref> |
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{{Equation box 1 |
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|indent=: |
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|title='''Stokes's stress constitutive equation''' ''(expression used for incompressible viscous fluids)'' |
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|equation=:<math>\boldsymbol \tau = \mu \left[\nabla\mathbf{u} + (\nabla\mathbf{u}) ^\mathrm{T}\right]</math> |
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}} |
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This constitutive equation is also called the '''Newton law of viscosity'''. |
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The total [[Cauchy stress tensor|stress tensor]] <math>\boldsymbol{\sigma}</math> can always be decomposed as the sum of the [[hydrostatic stress|isotropic stress]] tensor and the [[deviatoric stress tensor]] (<math>\boldsymbol \sigma '</math>): |
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<math>\boldsymbol \sigma = \frac 1 3 \operatorname{tr}(\boldsymbol \sigma) \mathbf I + \boldsymbol \sigma'</math> |
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In the incompressible case, the isotropic stress is simply proportional to the thermodynamic [[pressure]] <math>p</math>: |
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<math display="block">p = - \frac 1 3 \operatorname{tr}(\boldsymbol \sigma) = - \frac 1 3 \sum_k \sigma_{kk}</math> |
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and the deviatoric stress is coincident with the shear stress tensor <math>\boldsymbol \tau</math>: |
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<math display="block">\boldsymbol \sigma' = \boldsymbol \tau = \mu\left(\nabla\mathbf{u}+\nabla\mathbf{u}^{T}\right)</math> |
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The stress [[constitutive equation]] then becomes |
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<math display="block"> \sigma_{ij} = p \delta_{ij} |
<math display="block"> \sigma_{ij} = - p \delta_{ij} + \mu \left(\frac{\partial v_i}{\partial x_j} + \frac{\partial v_j}{\partial x_i} \right)</math> |
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or written in more compact tensor notation |
or written in more compact tensor notation |
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<math display="block">\boldsymbol{\sigma} = p \mathbf{I} |
<math display="block">\boldsymbol{\sigma} = - p \mathbf{I} + \mu\left(\nabla\mathbf{u}+\nabla\mathbf{u}^{T}\right)</math> |
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where <math>\mathbf{I}</math> is the identity tensor. |
where <math>\mathbf{I}</math> is the identity tensor. |
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=== |
===General compressible case=== |
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The Newton's constitutive law for a compressible flow results from the following assumptions on the Cauchy stress tensor:<ref name="Batchelor_142_148"/> |
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For a generic compressible and isotropic Newtonian fluid, one additional term is involved in describing the shear stress [[constitutive equation]]. |
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This term depends on the flow compressibility, i.e. the flow velocity divergence<ref>Bird, Stewart, Lightfoot, Transport Phenomena, equation 3.2-11a</ref>: |
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<ul> |
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<math display="block">\Delta \tau_{ij} =\left(\frac 2 3 \mu - \kappa \right) \delta_{ij} \sum_a \frac{\partial v_a}{\partial x_a} </math> |
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<li>the stress is '''[[Galilean invariance|Galilean invariant]]''': it does not depend directly on the flow velocity, but only on spatial derivatives of the flow velocity. So the stress variable is the tensor gradient <math display="inline">\nabla \mathbf{u}</math>, or more simply the rate-of-[[strain tensor]]: <math display="inline">\boldsymbol{\varepsilon}\left(\nabla \mathbf{u}\right) \equiv \frac{1}{2}\nabla \mathbf{u} + \frac{1}{2} \left(\nabla \mathbf{u}\right)^T</math></li> |
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<li>the deviatoric stress is '''linear''' in this variable: <math display="inline">\boldsymbol{\sigma}(\boldsymbol \varepsilon) = -p \mathbf I + \mathbf{C} : \boldsymbol \varepsilon</math>, where <math display="inline">p</math> is independent on the strain rate tensor, <math display="inline">\mathbf{C}</math> is the fourth-order tensor representing the constant of proportionality, called the viscosity or [[elasticity tensor]], and : is the [[Dyadics#Double-dot product|double-dot product]].</li> |
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<li>the fluid is assumed to be [[isotropic]], as with gases and simple liquids, and consequently <math display="inline">\mathbf{C}</math> is an isotropic tensor; furthermore, since the deviatoric stress tensor is symmetric, by [[Helmholtz decomposition]] it can be expressed in terms of two scalar [[Lamé parameters]], the [[second viscosity]] <math display="inline">\lambda</math> and the [[dynamic viscosity]] <math display="inline">\mu</math>, as it is usual in [[linear elasticity]]: |
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{{Equation box 1 |
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|indent=: |
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|title='''Linear stress [[constitutive equation]]''' ''(expression similar to the one for elastic solid)'' |
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|equation=<math>\boldsymbol \sigma(\boldsymbol \varepsilon) = - p \mathbf I + \lambda \operatorname{tr} (\boldsymbol \varepsilon) \mathbf I + 2 \mu \boldsymbol \varepsilon</math> |
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}} |
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where <math display="inline">\mathbf{I}</math> is the [[Identity matrix|identity tensor]], and <math display="inline">\operatorname{tr} (\boldsymbol \varepsilon)</math> is the [[trace (linear algebra)|trace]] of the rate-of-strain tensor. So this decomposition can be explicitly defined as: |
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<math display="block">\boldsymbol \sigma = -p \mathbf I + \lambda (\nabla\cdot\mathbf{u}) \mathbf I + \mu \left(\nabla\mathbf{u} + ( \nabla\mathbf{u} )^\mathrm{T}\right).</math> |
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</li> |
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</ul> |
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Since the [[trace (linear algebra)|trace]] of the rate-of-strain tensor in three dimensions is the [[divergence]] (i.e. rate of expansion) of the flow: |
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where |
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<math display="block">\operatorname{tr} (\boldsymbol \varepsilon) = \nabla\cdot\mathbf{u}.</math> |
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*<math>x_j</math> is the <math>j</math>th spatial coordinate |
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*<math>v_i</math> is the fluid's velocity in the direction of axis <math>i</math> |
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*<math>\Delta \tau_{ij}</math> is the <math>j</math>-th component of the stress acting on the faces of the fluid element perpendicular to axis <math>i</math> due to the flow compressibility. It is the ij-th component of the shear stress tensor part due to the flow compressibility |
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*<math>\kappa</math> is the [[bulk viscosity]] of the flow, that is zero for example for monoatomic gases at low density |
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*<math>\delta_{ij}</math> is the [[Kronecker delta]] of ''i'' and ''j'' |
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Given this relation, and since the trace of the identity tensor in three dimensions is three: |
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Moreover, note that the sum: |
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<math display="block">\operatorname{tr} (\boldsymbol I) = 3.</math> |
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is the [[divergence]] of the [[flow velocity]]. |
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the trace of the stress tensor in three dimensions becomes: |
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<math display="block">\operatorname{tr} (\boldsymbol \sigma ) = -3p + (3 \lambda + 2 \mu )\nabla\cdot\mathbf{u}.</math> |
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So by alternatively decomposing the stress tensor into '''isotropic''' and '''deviatoric''' parts, as usual in fluid dynamics:<ref>{{cite book |last1=Chorin |first1=Alexandre E. |last2=Marsden |first2=Jerrold E. |date=1993 |title=A Mathematical Introduction to Fluid Mechanics |page=33}}</ref> |
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This additional compressibility term of the shear stress, written in more compact tensor notation is: |
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<math display="block">\ |
<math display="block">\boldsymbol \sigma = - \left[ p + \left(\lambda + \tfrac23 \mu\right) \left(\nabla\cdot\mathbf{u}\right) \right] \mathbf I + \mu \left(\nabla\mathbf{u} + \left( \nabla\mathbf{u} \right)^\mathrm{T} - \tfrac23 \left(\nabla\cdot\mathbf{u}\right)\mathbf I\right)</math> |
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where: |
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Introducing the [[volume viscosity|bulk viscosity]] <math display="inline">\zeta</math>, |
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*<math>\nabla \mathbf{v}</math> is the flow velocity gradient |
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<math display="block"> \zeta \equiv \lambda + \tfrac23 \mu ,</math> |
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*<math>\nabla \cdot \mathbf{v}</math> is the flow velocity divergence |
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*<math>\mathbf{I}</math> is the [[identity matrix]] |
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we arrive to the linear [[constitutive equation]] in the form usually employed in [[thermal hydraulics]]:<ref name=Batchelor_142_148/> |
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{{Equation box 1 |
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|indent=: |
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|title='''Linear stress constitutive equation''' ''(expression used for fluids)'' |
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|equation=<math>\boldsymbol \sigma = -[ p - \zeta (\nabla\cdot\mathbf{u})] \mathbf I + \mu \left[\nabla\mathbf{u} + ( \nabla\mathbf{u} )^\mathrm{T} - \tfrac23 (\nabla\cdot\mathbf{u})\mathbf I\right]</math> |
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which can also be arranged in the other usual form:<ref>Bird, Stewart, Lightfoot, Transport Phenomena, 1st ed., 1960, eq. (3.2-11a)</ref> |
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<math display="block">\boldsymbol \sigma = -p \mathbf I + \mu \left(\nabla\mathbf{u} + ( \nabla\mathbf{u} )^\mathrm{T}\right) + \left(\zeta - \frac 2 3 \mu \right) (\nabla\cdot\mathbf{u}) \mathbf I.</math> |
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Note that in the compressible case the pressure is no more proportional to the [[hydrostatic stress|isotropic stress]] term, since there is the additional bulk viscosity term: |
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<math>p = - \frac 1 3 \operatorname{tr} (\boldsymbol \sigma) + \zeta (\nabla\cdot\mathbf{u})</math> |
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and the [[deviatoric stress tensor]] <math>\boldsymbol \sigma'</math> is still coincident with the shear stress tensor <math>\boldsymbol \tau</math> (i.e. the deviatoric stress in a Newtonian fluid has no normal stress components), and it has a compressibility term in addition to the incompressible case, which is proportional to the shear viscosity: |
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Then the Newton's constitutive equation for the shear stress becomes: |
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<math |
<math>\boldsymbol \sigma' = \boldsymbol \tau = \mu \left[\nabla\mathbf{u} + ( \nabla\mathbf{u} )^\mathrm{T} - \tfrac23 (\nabla\cdot\mathbf{u})\mathbf I\right]</math> |
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Note that the incompressible case correspond to the assumption that the pressure constrains the flow so that the volume of [[fluid element]]s is constant: [[isochoric process|isochoric flow]] resulting in a [[Solenoidal vector field|solenoidal]] velocity field with <math display="inline"> \nabla \cdot \mathbf{u} = 0</math>.<ref>Batchelor (1967) p. 75.</ref> |
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Or, written in more compact tensor notation, it is: |
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So one returns to the expressions for pressure and deviatoric stress seen in the preceding paragraph. |
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<math display="block">\boldsymbol{\tau} = - \mu\left(\nabla\mathbf{v}+\nabla\mathbf{v}^{T}\right) + \left(\frac 2 3 \mu - \kappa \right) (\nabla \cdot \mathbf v) \mathbf{I}</math> |
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Both bulk viscosity <math display="inline">\zeta</math> and dynamic viscosity <math display="inline">\mu</math> need not be constant – in general, they depend on two thermodynamics variables if the fluid contains a single chemical species, say for example, pressure and temperature. Any equation that makes explicit one of these [[transport coefficient]] in the [[conservation variable]]s is called an [[equation of state]].<ref name="Batchelor 1967 p. 165">Batchelor (1967) p. 165.</ref> |
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The general Newton's constitutive equation for the total stress is correspondingly: |
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Apart from its dependence of pressure and temperature, the second viscosity coefficient also depends on the process, that is to say, the second viscosity coefficient is not just a material property. Example: in the case of a sound wave with a definitive frequency that alternatively compresses and expands a fluid element, the second viscosity coefficient depends on the frequency of the wave. This dependence is called the ''dispersion''. In some cases, the [[volume viscosity|second viscosity]] <math display="inline">\zeta</math> can be assumed to be constant in which case, the effect of the volume viscosity <math display="inline">\zeta</math> is that the mechanical pressure is not equivalent to the thermodynamic [[pressure]]:<ref>Landau & Lifshitz (1987) pp. 44–45, 196</ref> as demonstrated below. |
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<math display="block"> \sigma_{ij} = \left( p + \left(\frac 2 3 \mu - \kappa \right) \sum_a \frac{\partial v_a}{\partial x_a} \right) \delta_{ij} - \mu \left(\frac{\partial v_i}{\partial x_j} + \frac{\partial v_j}{\partial x_i} \right)</math> |
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<math display="block">\nabla\cdot(\nabla\cdot \mathbf u)\mathbf I=\nabla (\nabla \cdot \mathbf u),</math><math display="block"> \bar{p} \equiv p - \zeta \, \nabla \cdot \mathbf{u} ,</math> |
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or written in more compact tensor notation: |
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However, this difference is usually neglected most of the time (that is whenever we are not dealing with processes such as sound absorption and attenuation of shock waves,<ref>White (2006) p. 67.</ref> where second viscosity coefficient becomes important) by explicitly assuming <math display="inline">\zeta = 0</math>. The assumption of setting <math display="inline">\zeta = 0</math> is called as the '''Stokes hypothesis'''.<ref>Stokes, G. G. (2007). On the theories of the internal friction of fluids in motion, and of the equilibrium and motion of elastic solids.</ref> The validity of Stokes hypothesis can be demonstrated for monoatomic gas both experimentally and from the kinetic theory;<ref>Vincenti, W. G., Kruger Jr., C. H. (1975). Introduction to physical gas dynamic. Introduction to physical gas dynamics/Huntington.</ref> for other gases and liquids, Stokes hypothesis is generally incorrect. |
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<math display="block">\boldsymbol{\sigma} = - \left( p + \left(\frac 2 3 \mu - \kappa \right) \nabla \cdot \mathbf v \right) \mathbf I - \mu\left(\nabla\mathbf{v}+\nabla\mathbf{v}^{T}\right)</math>. |
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Finally, note that Stokes hypothesis is less restrictive that the one of incompressible flow. In fact, in the incompressible flow both the bulk viscosity term, and the shear viscosity term in the divergence of the flow velocity term disappears, while in the Stokes hypothesis the first term also disappears but the second one still remains. |
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===For anisotropic fluids=== |
===For anisotropic fluids=== |
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There is general formula for friction force in a liquid: The vector [[Differential (mathematics)|differential]] of friction force is equal the viscosity tensor increased on [[vector product]] differential of the area vector of adjoining a liquid layers and [[Rotor (mathematics)|rotor]] of velocity: |
There is general formula for friction force in a liquid: The vector [[Differential (mathematics)|differential]] of friction force is equal the viscosity tensor increased on [[vector product]] differential of the area vector of adjoining a liquid layers and [[Rotor (mathematics)|rotor]] of velocity: |
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<math display="block"> d \mathbf{F} = \mu _ {ij} \, d\mathbf{S} \times\ |
<math display="block"> d \mathbf{F} = \mu _ {ij} \, d\mathbf{S} \times\nabla\times \, \mathbf {u} </math> |
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where <math> \mu _ {ij} </math> is the viscosity [[tensor]]. The diagonal components of viscosity tensor is molecular viscosity of a liquid, and not diagonal components – [[turbulence eddy viscosity]].<ref name=Volobuev>{{cite book | first=A. N. |last=Volobuev| title=Basis of Nonsymmetrical Hydromechanics| publisher=[[Nova Science Publishers, Inc.]] |location=New York | year=2012 | isbn=978-1-61942-696-2}}</ref> |
where <math> \mu _ {ij} </math> is the viscosity [[tensor]]. The diagonal components of viscosity tensor is molecular viscosity of a liquid, and not diagonal components – [[turbulence eddy viscosity]].<ref name=Volobuev>{{cite book | first=A. N. |last=Volobuev| title=Basis of Nonsymmetrical Hydromechanics| publisher=[[Nova Science Publishers, Inc.]] |location=New York | year=2012 | isbn=978-1-61942-696-2}}</ref> |
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== |
== Newton's law of viscosity == |
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The following equation illustrates the relation between shear rate and shear stress '''for |
The following equation illustrates the relation between shear rate and shear stress '''for a fluid with laminar flow only in the direction x''': |
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<math display="block">\tau_{xy} = \mu \frac{ \mathrm{d} v_x }{ \mathrm{d} y },</math> |
<math display="block">\tau_{xy} = \mu \frac{ \mathrm{d} v_x }{ \mathrm{d} y },</math> |
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where: |
where: |
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* [[Fluid mechanics]] |
* [[Fluid mechanics]] |
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* [[Non-Newtonian fluid]] |
* [[Non-Newtonian fluid]] |
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* [[Strain rate tensor]] |
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* [[Viscosity]] |
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* [[Viscous stress tensor]] |
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==References== |
==References== |
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{{Non-Newtonian fluids}} |
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Latest revision as of 09:09, 29 November 2024
Part of a series on |
Continuum mechanics |
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A Newtonian fluid is a fluid in which the viscous stresses arising from its flow are at every point linearly correlated to the local strain rate — the rate of change of its deformation over time.[1][2][3][4] Stresses are proportional to the rate of change of the fluid's velocity vector.
A fluid is Newtonian only if the tensors that describe the viscous stress and the strain rate are related by a constant viscosity tensor that does not depend on the stress state and velocity of the flow. If the fluid is also isotropic (i.e., its mechanical properties are the same along any direction), the viscosity tensor reduces to two real coefficients, describing the fluid's resistance to continuous shear deformation and continuous compression or expansion, respectively.
Newtonian fluids are the easiest mathematical models of fluids that account for viscosity. While no real fluid fits the definition perfectly, many common liquids and gases, such as water and air, can be assumed to be Newtonian for practical calculations under ordinary conditions. However, non-Newtonian fluids are relatively common and include oobleck (which becomes stiffer when vigorously sheared) and non-drip paint (which becomes thinner when sheared). Other examples include many polymer solutions (which exhibit the Weissenberg effect), molten polymers, many solid suspensions, blood, and most highly viscous fluids.
Newtonian fluids are named after Isaac Newton, who first used the differential equation to postulate the relation between the shear strain rate and shear stress for such fluids.
Definition
[edit]An element of a flowing liquid or gas will endure forces from the surrounding fluid, including viscous stress forces that cause it to gradually deform over time. These forces can be mathematically first order approximated by a viscous stress tensor, usually denoted by .
The deformation of a fluid element, relative to some previous state, can be first order approximated by a strain tensor that changes with time. The time derivative of that tensor is the strain rate tensor, that expresses how the element's deformation is changing with time; and is also the gradient of the velocity vector field at that point, often denoted .
The tensors and can be expressed by 3×3 matrices, relative to any chosen coordinate system. The fluid is said to be Newtonian if these matrices are related by the equation where is a fixed 3×3×3×3 fourth order tensor that does not depend on the velocity or stress state of the fluid.
Incompressible isotropic case
[edit]For an incompressible and isotropic Newtonian fluid in laminar flow only in the direction x (i.e. where viscosity is isotropic in the fluid), the shear stress is related to the strain rate by the simple constitutive equation where
- is the shear stress ("skin drag") in the fluid,
- is a scalar constant of proportionality, the dynamic viscosity of the fluid
- is the derivative in the direction y, normal to x, of the flow velocity component u that is oriented along the direction x.
In case of a general 2D incompressibile flow in the plane x, y, the Newton constitutive equation become:
where:
- is the shear stress ("skin drag") in the fluid,
- is the partial derivative in the direction y of the flow velocity component u that is oriented along the direction x.
- is the partial derivative in the direction x of the flow velocity component v that is oriented along the direction y.
We can now generalize to the case of an incompressible flow with a general direction in the 3D space, the above constitutive equation becomes where
- is the th spatial coordinate
- is the fluid's velocity in the direction of axis
- is the -th component of the stress acting on the faces of the fluid element perpendicular to axis . It is the ij-th component of the shear stress tensor
or written in more compact tensor notation where is the flow velocity gradient.
An alternative way of stating this constitutive equation is:
where is the rate-of-strain tensor. So this decomposition can be made explicit as:[5]
This constitutive equation is also called the Newton law of viscosity.
The total stress tensor can always be decomposed as the sum of the isotropic stress tensor and the deviatoric stress tensor ():
In the incompressible case, the isotropic stress is simply proportional to the thermodynamic pressure :
and the deviatoric stress is coincident with the shear stress tensor :
The stress constitutive equation then becomes or written in more compact tensor notation where is the identity tensor.
General compressible case
[edit]The Newton's constitutive law for a compressible flow results from the following assumptions on the Cauchy stress tensor:[5]
- the stress is Galilean invariant: it does not depend directly on the flow velocity, but only on spatial derivatives of the flow velocity. So the stress variable is the tensor gradient , or more simply the rate-of-strain tensor:
- the deviatoric stress is linear in this variable: , where is independent on the strain rate tensor, is the fourth-order tensor representing the constant of proportionality, called the viscosity or elasticity tensor, and : is the double-dot product.
- the fluid is assumed to be isotropic, as with gases and simple liquids, and consequently is an isotropic tensor; furthermore, since the deviatoric stress tensor is symmetric, by Helmholtz decomposition it can be expressed in terms of two scalar Lamé parameters, the second viscosity and the dynamic viscosity , as it is usual in linear elasticity:
Linear stress constitutive equation (expression similar to the one for elastic solid)
where is the identity tensor, and is the trace of the rate-of-strain tensor. So this decomposition can be explicitly defined as:
Since the trace of the rate-of-strain tensor in three dimensions is the divergence (i.e. rate of expansion) of the flow:
Given this relation, and since the trace of the identity tensor in three dimensions is three:
the trace of the stress tensor in three dimensions becomes:
So by alternatively decomposing the stress tensor into isotropic and deviatoric parts, as usual in fluid dynamics:[6]
Introducing the bulk viscosity ,
we arrive to the linear constitutive equation in the form usually employed in thermal hydraulics:[5]
which can also be arranged in the other usual form:[7]
Note that in the compressible case the pressure is no more proportional to the isotropic stress term, since there is the additional bulk viscosity term:
and the deviatoric stress tensor is still coincident with the shear stress tensor (i.e. the deviatoric stress in a Newtonian fluid has no normal stress components), and it has a compressibility term in addition to the incompressible case, which is proportional to the shear viscosity:
Note that the incompressible case correspond to the assumption that the pressure constrains the flow so that the volume of fluid elements is constant: isochoric flow resulting in a solenoidal velocity field with .[8] So one returns to the expressions for pressure and deviatoric stress seen in the preceding paragraph.
Both bulk viscosity and dynamic viscosity need not be constant – in general, they depend on two thermodynamics variables if the fluid contains a single chemical species, say for example, pressure and temperature. Any equation that makes explicit one of these transport coefficient in the conservation variables is called an equation of state.[9]
Apart from its dependence of pressure and temperature, the second viscosity coefficient also depends on the process, that is to say, the second viscosity coefficient is not just a material property. Example: in the case of a sound wave with a definitive frequency that alternatively compresses and expands a fluid element, the second viscosity coefficient depends on the frequency of the wave. This dependence is called the dispersion. In some cases, the second viscosity can be assumed to be constant in which case, the effect of the volume viscosity is that the mechanical pressure is not equivalent to the thermodynamic pressure:[10] as demonstrated below. However, this difference is usually neglected most of the time (that is whenever we are not dealing with processes such as sound absorption and attenuation of shock waves,[11] where second viscosity coefficient becomes important) by explicitly assuming . The assumption of setting is called as the Stokes hypothesis.[12] The validity of Stokes hypothesis can be demonstrated for monoatomic gas both experimentally and from the kinetic theory;[13] for other gases and liquids, Stokes hypothesis is generally incorrect.
Finally, note that Stokes hypothesis is less restrictive that the one of incompressible flow. In fact, in the incompressible flow both the bulk viscosity term, and the shear viscosity term in the divergence of the flow velocity term disappears, while in the Stokes hypothesis the first term also disappears but the second one still remains.
For anisotropic fluids
[edit]More generally, in a non-isotropic Newtonian fluid, the coefficient that relates internal friction stresses to the spatial derivatives of the velocity field is replaced by a nine-element viscous stress tensor .
There is general formula for friction force in a liquid: The vector differential of friction force is equal the viscosity tensor increased on vector product differential of the area vector of adjoining a liquid layers and rotor of velocity: where is the viscosity tensor. The diagonal components of viscosity tensor is molecular viscosity of a liquid, and not diagonal components – turbulence eddy viscosity.[14]
Newton's law of viscosity
[edit]The following equation illustrates the relation between shear rate and shear stress for a fluid with laminar flow only in the direction x: where:
- is the shear stress in the components x and y, i.e. the force component on the direction x per unit surface that is normal to the direction y (so it is parallel to the direction x)
- is the viscosity, and
- is the flow velocity gradient along the direction y, that is normal to the flow velocity .
If viscosity is constant, the fluid is Newtonian.
Power law model
[edit]The power law model is used to display the behavior of Newtonian and non-Newtonian fluids and measures shear stress as a function of strain rate.
The relationship between shear stress, strain rate and the velocity gradient for the power law model are: where
- is the absolute value of the strain rate to the (n−1) power;
- is the velocity gradient;
- n is the power law index.
If
- n < 1 then the fluid is a pseudoplastic.
- n = 1 then the fluid is a Newtonian fluid.
- n > 1 then the fluid is a dilatant.
Fluid model
[edit]The relationship between the shear stress and shear rate in a casson fluid model is defined as follows: where τ0 is the yield stress and where α depends on protein composition and H is the Hematocrit number.
Examples
[edit]Water, air, alcohol, glycerol, and thin motor oil are all examples of Newtonian fluids over the range of shear stresses and shear rates encountered in everyday life. Single-phase fluids made up of small molecules are generally (although not exclusively) Newtonian.
See also
[edit]References
[edit]- ^ Panton, Ronald L. (2013). Incompressible Flow (Fourth ed.). Hoboken: John Wiley & Sons. p. 114. ISBN 978-1-118-01343-4.
- ^ Batchelor, G. K. (2000) [1967]. An Introduction to Fluid Dynamics. Cambridge Mathematical Library series, Cambridge University Press. ISBN 978-0-521-66396-0.
- ^ Kundu, P.; Cohen, I. Fluid Mechanics. p. (page needed).
- ^ Kirby, B. J. (2010). Micro- and Nanoscale Fluid Mechanics: Transport in Microfluidic Devices. Cambridge University Press. ISBN 978-0-521-11903-0 – via kirbyresearch.com.
- ^ a b c Batchelor (1967) pp. 137 & 142.
- ^ Chorin, Alexandre E.; Marsden, Jerrold E. (1993). A Mathematical Introduction to Fluid Mechanics. p. 33.
- ^ Bird, Stewart, Lightfoot, Transport Phenomena, 1st ed., 1960, eq. (3.2-11a)
- ^ Batchelor (1967) p. 75.
- ^ Batchelor (1967) p. 165.
- ^ Landau & Lifshitz (1987) pp. 44–45, 196
- ^ White (2006) p. 67.
- ^ Stokes, G. G. (2007). On the theories of the internal friction of fluids in motion, and of the equilibrium and motion of elastic solids.
- ^ Vincenti, W. G., Kruger Jr., C. H. (1975). Introduction to physical gas dynamic. Introduction to physical gas dynamics/Huntington.
- ^ Volobuev, A. N. (2012). Basis of Nonsymmetrical Hydromechanics. New York: Nova Science Publishers, Inc. ISBN 978-1-61942-696-2.