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The momentum balance with Newton’s viscosity law describes an incompressible fluid of constant density and viscosity.
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Formula
ρ in kg/m3; p in Pa; μ in Pa·s; v in m/s; g in m/s2
| Symbol | Meaning | Unit |
|---|---|---|
| Constant fluid density | kg/m3 | |
| Velocity field | m/s | |
| Pressure field | Pa | |
| Dynamic viscosity | Pa·s | |
| Gravitational acceleration vector | m/s2 |
\rho(\partial_t\vec v+(\vec v\cdot\nabla)\vec v)=-\nabla p+\mu\nabla^2\vec v+\rho\vec g,\quad\nabla\cdot\vec v=0This form assumes an incompressible Newtonian fluid with constant ρ and μ; also impose ∇·v=0. It combines local momentum conservation with a linear stress–strain-rate relation. Variable viscosity, compressibility, non-Newtonian behavior or additional body forces require adjusted terms or constitutive models. Boundary and initial conditions are essential; the PDE alone does not determine a unique flow field.
This form assumes an incompressible Newtonian fluid with constant ρ and μ; also impose ∇·v=0. It combines local momentum conservation with a linear stress–strain-rate relation. Variable viscosity, compressibility, non-Newtonian behavior or additional body forces require adjusted terms or constitutive models. Boundary and initial conditions are essential; the PDE alone does not determine a unique flow field.
The momentum balance with Newton’s viscosity law describes an incompressible fluid of constant density and viscosity.
Base equation for the target quantity
Preserve signs, boundary conditions and units when rearranging.
Work through the numerical example for “Navier–Stokes equation for an incompressible Newtonian fluid” and check its unit and magnitude.
Hydrostatic check with z upward, v=0 and g⃗=−g ez gives −∂p/∂z−ρg=0, hence Δp=ρgΔh.
For water over 2.0 m, Δp≈1000·9.81·2=19.6 kPa.
Substituting a related quantity that shares the same symbol.
Use variable definitions and check: ρ in kg/m3; p in Pa; μ in Pa·s; v in m/s; g in m/s2.
Formula cluster
The momentum balance with Newton’s viscosity law describes an incompressible fluid of constant density and viscosity.
Hydrostatic check with z upward, v=0 and g⃗=−g ez gives −∂p/∂z−ρg=0, hence Δp=ρgΔh. For water over 2.0 m, Δp≈1000·9.81·2=19.6 kPa.
Place the governing equation for viscous flow, CFD, pipes and boundary layers in context.
Here is how to work through a typical Navier–Stokes equation for an incompressible Newtonian fluid (ρ Dv/Dt = −∇p + μ∇²v + ρg) task step by step:
Task
Work through the numerical example for “Navier–Stokes equation for an incompressible Newtonian fluid” and check its unit and magnitude.
Solution path
Hydrostatic check with z upward, v=0 and g⃗=−g ez gives −∂p/∂z−ρg=0, hence Δp=ρgΔh.
For water over 2.0 m, Δp≈1000·9.81·2=19.6 kPa.
A fluid particle can change velocity while moving through a spatially varying velocity field even when the field is steady in time. The term v·∇v captures that change along the particle path. Steady flow therefore does not imply zero acceleration or zero inertia. Assumptions: constant density and viscosity, incompressible Newtonian fluid; initial and boundary conditions are part of the problem. Application: Place the governing equation for viscous flow, CFD, pipes and boundary layers in context. The numerical example Hydrostatic check with z upward, v=0 and g⃗=−g ez gives −∂p/∂z−ρg=0, hence Δp=ρgΔh. For water over 2.0 m, Δp≈1000·9.81·2=19.6 kPa anchors the idea in a concrete measurement case.
The incompressible momentum equation must be coupled to ∇·v=0. This constrains the velocity field and couples pressure to velocity. Without continuity, a necessary mass-conservation condition is missing; momentum alone is not a complete flow model. Assumptions: constant density and viscosity, incompressible Newtonian fluid; initial and boundary conditions are part of the problem. The corresponding units are ρ in kg/m3; p in Pa; μ in Pa·s; v in m/s; g in m/s2. Hydrostatic check with z upward, v=0 and g⃗=−g ez gives −∂p/∂z−ρg=0, hence Δp=ρgΔh. For water over 2.0 m, Δp≈1000·9.81·2=19.6 kPa. This checks that the reference quantities are compatible.
For constant μ and incompressible flow, the divergence of Newtonian viscous stress simplifies to μ∇2v. With variable viscosity, compressibility or a different rheology, this compact form does not remain unchanged. The viscous stress term must then be derived from the appropriate constitutive law. Assumptions: constant density and viscosity, incompressible Newtonian fluid; initial and boundary conditions are part of the problem. Scope: This form assumes an incompressible Newtonian fluid with constant ρ and μ; also impose ∇·v=0. It combines local momentum conservation with a linear stress–strain-rate relation. Variable viscosity, compressibility, non-Newtonian behavior or additional body forces require adjusted terms or constitutive models. Boundary and initial conditions are essential; the PDE alone does not determine a unique flow field. A practical application is Place the governing equation for viscous flow, CFD, pipes and boundary layers in context.
Write the quantity and unit from the variable list next to every value: ρ in kg/m3; p in Pa; μ in Pa·s; v in m/s; g in m/s2. Substitute only after converting to a consistent unit system, and state sign or reference direction explicitly. The example Hydrostatic check with z upward, v=0 and g⃗=−g ez gives −∂p/∂z−ρg=0, hence Δp=ρgΔh. For water over 2.0 m, Δp≈1000·9.81·2=19.6 kPa. is a calculation check: result, unit and order of magnitude must fit the described situation. Round after intermediate calculations so small contributions are not lost prematurely. Assumptions: constant density and viscosity, incompressible Newtonian fluid; initial and boundary conditions are part of the problem.
The background states this starting condition: This form assumes an incompressible Newtonian fluid with constant ρ and μ; also impose ∇·v=0. It combines local. That limits when the result is a valid model prediction. Compare the problem’s boundary conditions with this assumption before substituting values; real components, material properties or loads can introduce additional effects. The cited reference supports the relation used here but does not remove the need to check whether the specific case fits the model. Assumptions: constant density and viscosity, incompressible Newtonian fluid; initial and boundary conditions are part of the problem.
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Curated exam set for "Navier–Stokes equation for an incompressible Newtonian fluid":
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Which formula describes Navier–Stokes equation for an incompressible Newtonian fluid?
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How do you rearrange Navier–Stokes equation for an incompressible Newtonian fluid for Base equation for the target quantity?
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Which common mistake happens with Navier–Stokes equation for an incompressible Newtonian fluid?
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Create a curated FSRS exam set for ρ Dv/Dt = −∇p + μ∇²v + ρg: formula recall, variables, derivation, rearrangement, worked example, common mistakes and exam context.
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