15.1. Quasi-1-dimensional flows#

Assumptions. Whenever no explict assumption is made in this section, the following assumptions are made:

  • uniform properties on each section of the stream tube

  • negligible viscous and conductivity (non-ideal flows: friction-dominated (Fanno), with heat transfer (Rayleigh))

  • negligible radial velocity component

  • no azimuthal component

  • cylindrical symmetry of streamtube

15.1.1. Steady flow#

Integral balance equations.

\[\begin{split}\begin{aligned} & \dfrac{d}{dt} \int_{v_t} \rho + \oint_{\partial v_t} \rho \mathbf{u}^{rel} \cdot \hat{\mathbf{n}} = 0 \\ & \dfrac{d}{dt} \int_{v_t} \rho \mathbf{u} + \oint_{\partial v_t} \rho \mathbf{u} \mathbf{u}^{rel} \cdot \hat{\mathbf{n}} = \int_{v_t} \rho \mathbf{g} + \oint_{\partial v_t} \mathbf{t}_{\mathbf{n}} \\ & \dfrac{d}{dt} \int_{v_t} \rho e^t + \oint_{\partial v_t} \rho e^t \mathbf{u}^{rel} \cdot \hat{\mathbf{n}} = \int_{v_t} \rho \mathbf{g} \cdot \mathbf{u} + \oint_{\partial v_t} \mathbf{t}_{\mathbf{n}} \cdot \mathbf{u} - \oint_{\partial v_t} \mathbf{q} \cdot \hat{\mathbf{n}} \\ \end{aligned}\end{split}\]

For a control volume \(v_t = V\) at rest, \(\mathbf{u}_b = \mathbf{0}\) and \(\mathbf{u}^{rel} = \mathbf{u}\). Neglecting the volume force \(\mathbf{g} = \mathbf{0}\), and integrating over an elementary control volume \(\Delta V\) cutting a streamtube at coordinates \(z\), \(z + \Delta z\), under steady conditions

\[\begin{split}\begin{aligned} & \oint_{\partial \Delta V} \rho \mathbf{u} \cdot \hat{\mathbf{n}} = 0 \\ & \oint_{\partial \Delta V} \rho \mathbf{u} \mathbf{u} \cdot \hat{\mathbf{n}} = \oint_{\partial \Delta V} \mathbf{t}_{\mathbf{n}} \\ & \oint_{\partial \Delta V} \rho e^t \mathbf{u} \cdot \hat{\mathbf{n}} = \oint_{\partial \Delta V} \mathbf{t}_{\mathbf{n}} \cdot \mathbf{u} \end{aligned}\end{split}\]

Differential equations. Assuming uniform properties on each section,

\[\begin{split}\begin{aligned} & \dfrac{d}{dz} \left( \rho u A \right) = 0 \\ & \dfrac{d}{dz} \left( \rho u^2 A + p A \right) - p A' = 0 \\ & \dfrac{d}{dz} \left[ \rho \left( e^t + \frac{p}{\rho} \right) u A \right] = 0 \ . \end{aligned}\end{split}\]

Thus, momentum equation can be recast as

\[0 = \left( \rho u^2 A \right)' + p' A \ .\]
Momentum equation
\[\begin{split}\begin{aligned} \mathbf{0} & = \oint_{\partial \Delta V} \rho \mathbf{u} \mathbf{u} \cdot \hat{\mathbf{n}} - \oint_{\partial \Delta V} \mathbf{t}_{\mathbf{n}} = \\ & = \int_{A(z)} \rho \mathbf{u} \mathbf{u} \cdot \hat{\mathbf{n}} + p \hat{\mathbf{n}} + \int_{A(z+\Delta z)} \rho \mathbf{u} \mathbf{u} \cdot \hat{\mathbf{n}} + p \hat{\mathbf{n}} + \int_{\Delta A^{lat}} p \hat{\mathbf{n}} \ . \end{aligned}\end{split}\]

For 2-dimensional flows,

\[\hat{\mathbf{z}} \cdot \int_{\Delta A^{lat}} p \hat{\mathbf{n}} = - \Delta z \int_{\ell^{lat}} p \hat{\mathbf{n}} \cdot \hat{\mathbf{z}} \simeq - \Delta z \, p \, \frac{A'(z) \Delta z}{\Delta z} = - p(z) A'(z) \Delta z \ . \]

For 3-dimensional flows,…

Using mass equation, \(( \rho u A )' = 0\), \(\rho u A =: \dot{m}\), momentum and total energy equations become

\[\begin{split}\begin{aligned} & \rho u A u' + p' A = 0 \\ & \rho u A h^{t \, '} = 0 \ , \end{aligned}\end{split}\]

or, simplifying momentum equation for the area of the section of the stream-tube and total energy equation for a mass flux \(\dot{m} \ne 0\),

\[\begin{split}\begin{aligned} & \rho u u' + p' = 0 \\ & h^{t \, '} = 0 \ . \end{aligned}\end{split}\]

15.1.1.1. Mach dependence#

Subsonic and supersonic flows show different behavior. If the differential equations hold (no shock, homoentropic flow, \(ds = 0\)), pressure derivative is proportional to density derivative through the square of the speed of sound,

\[d p = a^2(\rho, \overline{s}) d \rho \ .\]
\[\begin{split}\begin{aligned} \frac{A'}{A} & = \left( M^2 - 1 \right) \frac{u'}{u} \\ & = - \frac{ M^2 - 1 }{M^2} \frac{\rho'}{\rho} \\ \end{aligned}\end{split}\]
Details

Thus,

\[\begin{split}\begin{aligned} 0 & = \rho u u' + a^2 \rho' && \text{(momentum)} \\ 0 & = \frac{\rho'}{\rho} + \frac{u'}{u} + \frac{A'}{A} && \text{(mass)} \\ & = - \frac{u u'}{a^2} + \frac{u'}{u} + \frac{A'}{A} \\ \end{aligned}\end{split}\]

and thus

  • velocity

    \[\left( M^2 - 1 \right) \frac{u'}{u} = \frac{A'}{A} \ .\]

    Thus,

    • in a subsonic flow \(M < 1\), velocity increases as the section of the stream-tube decreases

    • in a supersonic flow \(M > 1\), velocity increases as the section of the stream-tube increases

  • density

    \[\begin{split}\begin{aligned} \frac{\rho'}{\rho} & = - \frac{u^2}{a^2} \frac{u'}{u} \\ - \frac{M^2 - 1}{M^2} \frac{\rho'}{\rho} & = - \frac{A'}{A} \\ \end{aligned}\end{split}\]

    Thus,

    • in a subsonic flow \(M < 1\), density decreases as the section of the stream-tube decreases

    • in a supersonic flow \(M > 1\), density decreases as the section of the stream-tube increases

  • pressure

  • temperature

15.1.2. Unsteady flow#

todo For a generic control volume \(v_t\)… It could be useful for mechanical/multi-field system dynamics…

Integral equations.

\[\begin{split}\begin{aligned} & \dfrac{d}{dt} \int_{v_t} \rho + \oint_{\partial v_t} \rho \mathbf{u}^{rel} \cdot \hat{\mathbf{n}} = 0 \\ & \dfrac{d}{dt} \int_{v_t} \rho \mathbf{u} + \oint_{\partial v_t} \rho \mathbf{u} \mathbf{u}^{rel} \cdot \hat{\mathbf{n}} = \int_{v_t} \rho \mathbf{g} + \oint_{\partial v_t} \mathbf{t}_{\mathbf{n}} \\ & \dfrac{d}{dt} \int_{v_t} \rho e^t + \oint_{\partial v_t} \rho e^t \mathbf{u}^{rel} \cdot \hat{\mathbf{n}} = \int_{v_t} \rho \mathbf{g} \cdot \mathbf{u} + \oint_{\partial v_t} \mathbf{t}_{\mathbf{n}} \cdot \mathbf{u} - \oint_{\partial v_t} \mathbf{q} \cdot \hat{\mathbf{n}} \\ \end{aligned}\end{split}\]

For a control volume \(v_t = V\) at rest, \(\mathbf{u}_b = \mathbf{0}\) and \(\mathbf{u}^{rel} = \mathbf{u}\). Neglecting the volume force \(\mathbf{g} = \mathbf{0}\), and integrating over an elementary control volume \(\Delta V\) cutting a streamtube at coordinates \(z\), \(z + \Delta z\), under steady conditions

\[\begin{split}\begin{aligned} & \frac{d}{dt} \int_{\Delta V} \rho + \oint_{\partial \Delta V} \rho \mathbf{u} \cdot \hat{\mathbf{n}} = 0 \\ & \frac{d}{dt} \int_{\Delta V} \rho \mathbf{u} + \oint_{\partial \Delta V} \rho \mathbf{u} \mathbf{u} \cdot \hat{\mathbf{n}} = \oint_{\partial \Delta V} \mathbf{t}_{\mathbf{n}} \\ & \frac{d}{dt} \int_{\Delta V} \rho e^t + \oint_{\partial \Delta V} \rho e^t \mathbf{u} \cdot \hat{\mathbf{n}} = \oint_{\partial \Delta V} \mathbf{t}_{\mathbf{n}} \cdot \mathbf{u} \end{aligned}\end{split}\]

Differential equations. Assuming uniform properties on each section,

\[\begin{split}\begin{aligned} & \partial_t \left( \rho A \right) + \partial_z \left( \rho u A \right) = 0 \\ & \partial_t \left( \rho u A \right) + \partial_z \left[ \left( \rho u^2 + p \right) A \right] - p \partial_z A = 0 \\ & \partial_t \left( \rho e^t A \right) + \partial_z \left[ \rho \left( e^t + \frac{p}{\rho} \right) u A \right] = 0 \ . \end{aligned}\end{split}\]

Assuming here rigid stream-tube with known section \(A(z)\), constant in time \(\partial_t A(z,t) = 0\), the differential equations can be recast as a set of PDE, with primary unknowns \((\rho A, m A, E^t A)\) whose

  • conservative form reads

    \[\begin{split} \partial_t \begin{bmatrix} \rho A \\ \rho u A \\ \rho e^t A \end{bmatrix} + \partial_z \begin{bmatrix} \rho u A \\ \frac{( \rho u A )^2}{\rho A} + p A \\ \frac{ (\rho e^t A + p A) (\rho u A) }{ \rho A } \end{bmatrix} = \begin{bmatrix} 0 \\ p \partial_z A \\ 0 \end{bmatrix} \end{split}\]
  • conservative quasi-linear form reads

    \[\begin{split} \partial_t \begin{bmatrix} \rho A \\ \rho u A \\ \rho e^t A \end{bmatrix} + \begin{bmatrix} \cdot & 1 & \cdot \\ - \frac{(\rho u A)^2}{(\rho A)^2} + \partial_{\rho A} (pA) & 2 \frac{\rho u A}{\rho A} + \partial_{\rho u A} (pA) & \partial_{\rho e^t A} (pA) \\ - \frac{(\rho h^t A)(\rho u A)}{(\rho A)^2} + \partial_{\rho A} (pA) \frac{\rho u A}{\rho A} & \frac{\rho h^t A}{\rho A} + \partial_{\rho u A} ( \rho h^t A ) \frac{\rho u A}{\rho A} & \frac{\rho u A}{\rho A} \left( 1 + \partial_{\rho e^t} ( pA ) \right) \end{bmatrix} \partial_z \begin{bmatrix} \rho A \\ \rho u A \\ \rho e^t A \end{bmatrix} = \begin{bmatrix} 0 \\ p \partial_z A \\ 0 \end{bmatrix} \end{split}\]
  • convective form reads

    \[\begin{split}\begin{cases} A \partial_t \rho + A ( \rho \partial_z u + u \partial_z \rho ) = - \rho u \partial_z A \\ \rho A \partial_t u + \rho A u \partial_z u + A \partial_z p = 0 \\ \rho A \partial_t e^t + \rho A u \partial_z e^t + A \left( u \partial_z p + p \partial_z u \right) = - p u \partial_z A \ . \end{cases}\end{split}\]

    or

    \[\begin{split}\begin{cases} \partial_t \rho + \rho \partial_z u + u \partial_z \rho = - \rho u \frac{\partial_z A}{A} \\ \partial_t u + u \partial_z u + \frac{ \partial_z p }{\rho} = 0 \\ \partial_t e^t + u \partial_z e^t + \frac{u}{\rho} \partial_z p + \frac{p}{\rho} \partial_z u = - \frac{p u}{\rho} \frac{\partial_z A}{A} \ . \end{cases}\end{split}\]
Internal energy equation
\[\begin{split}\begin{aligned} \partial_t e & = \partial_t e^t - \partial_t \frac{u^2}{2} = \\ & = -u \partial_z e^t - \frac{u}{\rho}\partial_z p - \frac{p}{\rho} \partial_z u - \frac{pu}{\rho} \frac{\partial_z A}{A} + u \partial_z \frac{u^2}{2} + \frac{u}{\rho} \partial_z p = \\ & = -u \partial_z e - \frac{p}{\rho} \partial_z u - \frac{pu}{\rho} \frac{\partial_z A}{A} \ , \end{aligned}\end{split}\]

i.e.

\[ \partial_t e + u \partial_z e = - \frac{p}{\rho} \partial_z u - \frac{pu}{\rho} \frac{\partial_z A}{A} \ .\]
Entropy equation
\[\begin{split}\begin{aligned} T D_t s & = D_t e - \frac{p}{\rho^2} D_t \rho = \\ & = - \frac{p}{\rho} \partial_z u - \frac{pu}{\rho} \frac{\partial_z A}{A} - \frac{p}{\rho^2} \left( - \rho \partial_z u - \rho u \frac{\partial_z A}{A} \right) = \\ & = 0 \ , \end{aligned}\end{split}\]

or, as \(T > 0\),

\[\begin{split}\begin{aligned} 0 & = D_t s = \\ & = \partial_t s + u \partial_z s \ . \end{aligned}\end{split}\]

todo Discuss homoentropic flow, if no shock occurs

Characteristics

Quasi linear form with mass, momentum and entropy equation and \((\rho, u, s)\) primary variables reads

\[\begin{split} \partial_t \begin{bmatrix} \rho \\ u \\ s \end{bmatrix} + \begin{bmatrix} u & \rho & \cdot \\ \frac{1}{\rho}\left( \partial_\rho p \right)_s & u & \frac{1}{\rho}\left( \partial_s p \right)_\rho \\ \cdot & \cdot & u \end{bmatrix} \partial_z \begin{bmatrix} \rho \\ u \\ s \end{bmatrix} = \begin{bmatrix} - \rho u \frac{\partial_z A}{A} \\ 0 \\ 0 \end{bmatrix} \ . \end{split}\]

The derivative \((\partial_\rho p)_s = a^2\) is the square of the speed of sound, as its meaning becomes clear in the spectrum of the convection matrix. These equations looks like 1-dimensional Euler equations for compressible ideal flows, with the exception that a non-uniform section of the stream-tube acts as a source term in mass equation.

Spectrum - eigenvalues.

\[0 = |\mathbf{A}(\mathbf{u}) - s \mathbf{I}| = ( u - s )^3 - ( u - s ) a^2 \ ,\]

i.e.

\[s_{1,3} = u \mp a \quad , \quad s_2 = u \ .\]

Right eigenvectors

\[\begin{split} \mathbf{R} = \begin{bmatrix} \rho & \rho & \rho \\ -a & \cdot & a \\ \cdot & - \frac{\rho a^2}{(\partial_s p)_{\rho}} & \cdot \end{bmatrix} \end{split}\]

Left eigenvectors

\[\begin{split} \mathbf{L} = \begin{bmatrix} \frac{1}{2 \rho} & - \frac{1}{2 a} & \frac{(\partial_s p)_\rho}{2 \rho a^2} \\ \cdot & \cdot & -\frac{(\partial_s p)_\rho}{ \rho a^2} \\ \frac{1}{2 \rho} & \frac{1}{2 a} & \frac{(\partial_s p)_\rho}{2 \rho a^2} \\ \end{bmatrix} \end{split}\]