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Incompressible Newtonian and barotropic inviscid fluid constitutive models

Definition

Let I⊆R be a nonempty open interval, let O⊆R3 be open, and let u:I×O→R3 be a C1 spatial velocity field with the conventions of Euclidean spatial calculus: gradient, divergence and material derivative. Write Du(t,x) for the total derivative in the spatial variable and div⁡u=tr⁡(Du) (The trace tr⁡(A) as the sum of the diagonal entries). For A∈M3(R) define its transpose by (AT)ij:=Aji for 1≤i,j≤3, using the same one-based component labels; call A symmetric when Aij=Aji for every such pair.

(a) Incompressible Newtonian fluid. Model data are a C1 scalar field p:I×O→R (pressure) and a real number η>0 (dynamic viscosity; a dimensionless mathematical parameter until a unit system is fixed). The model consists of the incompressibility constraint

div⁡u(t,x)=0((t,x)∈I×O)

and the Newtonian stress field

σ(t,x):=−p(t,x)I3+η(Du(t,x)+Du(t,x)T)∈M3(R),

with (Du(t,x)T)ij=∂iuj(t,x) and I3 the identity (Rectangular matrix multiplication and the identity matrix In, including zero-sized shapes, The vector space Mm×n(F):=F m×n of m by n matrices over a field, with entrywise operations). The entries of the second term are η(∂jui+∂iuj), so σ is symmetric for every (t,x).

(b) Barotropic inviscid fluid. Model data are a C1 function p:(0,∞)→R (pressure law) and a C1 scalar map V:I×O→R. Calling V a body-force potential means that its associated vector field is defined by b(t,x):=−∇xV(t,x); this field is continuous, and in a consuming momentum equation the body-force density is ρb=−ρ∇xV. This datum is separate from the stress law. The enthalpy of the pressure law is the C1 function

h(ρ):=∫1ρp′(s)s ds(ρ>0),

which is characterised by h(1)=0 and h′(ρ)=p′(ρ)/ρ for every ρ>0 (The integral function F(x):=∫axf of an integrable f, The first fundamental theorem: if f is integrable on [a,b] and continuous at c, then F′(c)=f(c); in particular a continuous f has F as a primitive). For a C1 positive density field ρ:I×O→(0,∞) the branch's stress field is

σ(t,x):=−p(ρ(t,x))I3,

and the branch is inviscid (no velocity-gradient term) and barotropic (the stress depends on position and time only through the density).

Remarks

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