Tormod Landet

Articles tagged with English

  1. A linear 2D sloshing solver in FEniCS

    In the previous blog post I showed how to solve the Laplace equation in 2D with FEniCS. That example, while illustrative for how to use FEniCS, was not particularly exciting. So, I decided to show the simplest example I could think of that involves an actual example of fluid flow.

    Before we start: Writing these posts is a learning exercise for me. If you are learning FEniCS or the finite element method, please do not consider this material authoritative. I still hope this can be useful for someone else, but correctness is not guaranteed. In addition no mesh sensitivity studies or rigorous validation has been performed. This work has been done in evenings when I have felt like it, and then producing something that is much more fun than carefully testing it afterwards. Just so you know before we start on the real content of this post.


    Sloshing is the motion of a fluid with a free surface in an enclosed space, such as a tank or a glass of water. The term free surface simply means the top of the fluid is allowed to move freely.

    The simplest way to simulate sloshing with FEniCS is with a 2D rectangular tank and incompressible, irrotational and inviscid fluid flow. This is called potential flow and we only need to solve the Laplace equation for the scalar velocity potential, normally called \(\phi\), and not the velocities and the pressure which can be calculated from the derivatives of the velocity potential function. This makes potential flow solvers fast, and hence popular, but of course not applicable to all problems of fluid flow!

    \begin{equation*} \newcommand{\dif}{\mathrm{d}} \newcommand{\pdiff}[2]{\frac{\mathrm\partial#1}{\mathrm\partial#2}} \newcommand{\laplace}[1]{\nabla^2#1} \laplace{\phi} = 0 \qquad \text{(the Laplace equation)} \end{equation*}

    To further simplify our problem we assume that the motion of the free surface is so small that we do not make a large error by not moving the mesh near the surface when waves travel across it. If the waves are small then the mesh points at the still water surface are sufficiently close to the actual position of the free surface that we can get away by having a constant mesh.

    Tank coordinate system

    The tank with free surface and still water water surface marked

    We need to apply linear free surface boundary conditions to get away with not moving the mesh. A quick overview of the linear free surface boundary conditions can be found for example on the Wikipedia page for Airy wave theory.

    The free surface introduces a new unknown function, \(\eta(x,t)\) in addition to the velocity potential \(\phi\). This is the surface elevation, and in our simple problem the surface elevation is only a function of the x-position in the tank and the time, t.

    The linear kinematic free surface boundary condition says that the free surface moves up and down with the velocity of the fluid at the free surface. Particles on the free surface stay on the free surface.

    \begin{equation*} \newcommand{\dif}{\mathrm{d}} \newcommand{\pdiff}[2]{\frac{\mathrm\partial#1}{\mathrm\partial#2}} \newcommand{\laplace}[1]{\nabla^2#1} \pdiff{\eta}{t} = \pdiff{\phi}{z} \quad \text{at the free surface} \end{equation*}

    The z-derivative of the velocity potential is equal to the vertical fluid speed as described in the previous blog post.

    The dynamic free surface boundary condition is derived from Bernoulli's equation and makes sure the pressure at the free surface is constant. We assume that the atmospheric pressure is zero:

    \begin{equation*} \pdiff{\phi}{t} + g\eta = 0 \quad \text{at the free surface} \end{equation*}

    We also need to specify that there is no motion through the floor of the tank:

    \begin{equation*} \pdiff{\phi}{z} = 0 \quad \text{at the the bottom} \end{equation*}

    And finally we want to move the tank back and forth to produce some free surface motion. We do this by introducing a horizontal velocity \(U_H(t)\) on the walls:

    \begin{equation*} \pdiff{\phi}{x} = U_H(t) \quad \text{on the walls} \end{equation*}

    One nice property of our equation system is that only our free surface boundary conditions involve time, the Laplace equation in the domain itself is independent of what happened at the last time step.

    Solution algorithm

    From the above we can decide on the following way to make a simulator for this problem:

    1. We need a Laplace solver that can calculate the velocity potential given a position of the free surface and a wall velocity, \(U_H\). We specify the value of the velocity potential at the free surface by using the dynamic free surface boundary condition.
    2. We need to update the free surface height function \(\eta(x,t)\) by using the kinematic free surface condition.
    3. We need to advance our solution in time and run the above in a loop.

    For point 1 we can use the previously shown FEniCS Laplace solver, with some small modifications. For point 2 we need to find a way to get the vertical derivative of the velocity potential at the free surface. For the last point we will use the built in time integration routines in SciPy so that we do not have to worry about selecting an appropriately small time step.

    We will not apply any filtering of high frequent noise on the free surface function \(\eta\), something which is common to do in Laplace equation solvers with a free surface. We will hence need a quite fine time step to avoid numerical problems. The SciPy routines have automatic time step control which avoids this problem by reducing the time step when noise is trying to sneak in. This simplification in the implementation makes our code a bit slower that it could have been.

    For the purpose of time stepping we define \(2 N\) unknowns, where \(N\) is the number of vertices on the free surface. The first half of the unknowns are the free surface elevations, while the second half is the velocity potential at the free surface:

    \begin{align*} \pdiff{\eta}{t} &= \pdiff{\phi}{z} &\qquad \text{At each of the N free surface vertices}\\ \pdiff{\phi}{t} &= - g\eta &\qquad \text{At each of the N free surface vertices} \end{align*}

    We take the initial velocity potential to be zero throughout the domain and the surface elevation is also zero at the start of the simulation.


    Finding derivatives of the computed unknown function is covered in the FEniCS tutorial. Basically you can find the derivative \(w\) of the unknown function \(u\) by solving:

    \begin{equation*} w = \pdiff{u}{t} \end{equation*}

    which has the following weak form

    \begin{equation*} \int_\Omega w\,v\,\dif \Omega = \int_\Omega \pdiff{u}{t}\,v\,\dif \Omega \end{equation*}

    This can be written as follows in FEniCS:

    # The z-derivative or the velocity potential
    u2 = df.TrialFunction(V)
    v2 = df.TestFunction(V)
    a2 = u2*v2*df.dx
    L2 = df.Dx(phi, 1)*v2*df.dx

    This allows us to solve for the z-derivative of the solution, phi, in the whole domain. We only really need the derivative at the free surface, but for this demo I did not bother to spend time to figure out how do that.


    The complete code is available from here. I have tried to comment the code well so I hope it is relatively understandable, at least after reading these two blog posts.

    If you look carefully you will see that the mesh has been slightly changed from the last post. The diagonals of the triangular elements are now alternating to left and right. Since the problem is highly symmetric this seemed to give significantly better results, at least for the test case I used while developing the code. Testing with higher order elements and quadrilaterals instead of triangles would be interesting, but has not been done.

    At resonance the solution does not converge, the motion amplitudes are growing linearly with time, which is expected. Below I have shown surface elevation amplitudes as function of the excitation frequency. It is simply the elevation amplitude in the last oscillation cycle that is shown, so the results around resonances depend on how many oscillations have been run. Some damping could be added to the free surface boundary condition to get converged results.

    Some results

    The results for a selected test case can be seen below in terms of surface elevation and the velocity potential:

    Free surface elevation

    Animation of the free surface elevation

    Free surface elevation time series

    Elevation at each end of the tank as a function of time

    Velocity potential

    Snapshot of the velocity potential at t=100

    A series of simulations were performed and the amplitudes of the free surface motion close to the walls was extracted. The results can be seen below. The resonant periods calculated by analytical formula have also been added for comparison:

    RAO for free surface elevation

    Transfer function for free surface elevation at the walls. Elevation amplitude divided by the forced motion amplitude.

    Analytical natural frequencies can be found from the following formula [Faltinsen09]:

    \begin{equation*} \omega_n = \sqrt{g\,k_n\,\tanh(k_n\,h)} \end{equation*}

    where \(k_n = n \pi / L\). The mode number is \(n\) where 1 gives the first natural mode, corresponding to a standing half sine wave. The dimensions involved are the length \(L\) and the height of the tank, \(h\).

    The calculations can be seen to be predicting roughly the physics they are intended to, but for high frequent motion the resulting velocity potential is not captured well by the selected discretization and these results are probably not very reliable.

    Calculating the above transfer function with 300 excitation periods and 20 oscillations for each period on a 40 by 20 mesh with linear triangle elements took more that 12 hours on my laptop. For this specific problem it would probably take much less time to look up and implement the analytical solution, which is not terribly hard to do. The accuracy would also be much better.

    I expect that the results given in the plot above are quite unreliable. This could easily be verified by comparing to the analytical solution, but I have not bothered with this here, as the intention was to test FEniCS for a simple dynamic problem, not promote a hopelessly inefficient method of analyzing linear sloshing in a rectangular tank.

    I do, however, believe that the method presented can be made sufficiently accurate with the right mesh and/or higher order elements and perhaps more carefull treatment of the derivative of the velocity potential on the free surface. It is then possible to incorporate nonlinear free surface boundary conditions, find solutions for non-regular tank geometries and in general quite easily find answers to questions that are very hard to find by analytical work only.

    I hope you have found this and the previous article usefull. I will probably restrict myself to smaller, bite sized, chunks if I am to continue with these posts. The topic of this article took more than one evening to code and write, and I am not sure I will devode that much time to this blog in the future. There is simply too much else to do and so many things to learn! Explaining something is still a great way to learn, so we will see if there is a follow up. Maybe the same problem, just with a discontinous Galerkin implementation instead of a continous? Time will tell.

    [Faltinsen09]Faltinsen, OM and AN Timokha, Sloshing, Cambridge University Press, 2009
  2. Solving the Laplace equation with FEniCS

    I have found that explaining something is a good way to learn. As I am currently reading some books on the finite element method to refresh my rusting memories from math courses at university I thought it would be a good idea to write a summary of some of the basics. This post will explain how to use the finite element method and FEniCS for solving partial differential equations. FEniCS is a collection of tools for automated, efficient solution of partial differential equations using the finite element method.


    I will show how to apply FEniCS to a simple partial differential equation. I will also explain the solution method employed in the finite element method to solve the selected equation, the Laplace equation:

    \begin{equation*} \newcommand{\dif}{\mathrm{d}} \newcommand{\pdiff}[2]{\frac{\mathrm\partial#1}{\mathrm\partial#2}} \newcommand{\laplace}[1]{\nabla^2#1} \laplace{\phi} = 0 \end{equation*}

    When a fluid is incompressible, inviscid and the flow can be assumed to be irrotational then the Laplace equation shown above describes the fluid flow. The fluid velocities, \({\bf U} = (U_x, U_y, U_z)\), can be calculated from the velocity potential \(\phi\) as follows:

    \begin{equation*} U_x = \pdiff{\phi}{x} \qquad U_y = \pdiff{\phi}{x} \qquad U_z = \pdiff{\phi}{x} \end{equation*}

    Our domain, \(\Omega\), is a 2D square with \(x \in [0, 2]\) and \(y \in [0, 1]\). For the boundary conditions, let's say that we know the value of \(\phi\) at that the short boundaries and the normal derivative at the long edges is zero. The complete equation system can then be for example:

    \begin{align*} &\laplace{\phi} = 0 \\ \ \\ &\phi = -1.0 \quad &\text{on} \quad x = 0.0 \\ &\phi = +1.0 \quad &\text{on} \quad x = 2.0 \\ &\pdiff{\phi}{\bf n} = 42 \quad &\text{on} \quad \Gamma_L \\ \end{align*}

    where we define \(\Gamma_L\) to be the long edge boundaries \(y=0\) and \(y=1\). The normal vector on the boundary is \(\bf n\) and \(\pdiff{}{\bf n}\) is the normal derivative at the boundary. It is common to use \(\Omega\) to denote the domain and \(\Gamma\) to denote the boundary.


    Now, to solve the equation with boundary conditions we need a discretized domain. This can be created by using the FEniCS Python package dolfin like this:

    import dolfin as df
    start_x, end_x, n_elem_x = 0.0, 2.0, 4
    start_y, end_y, n_elem_y = 0.0, 1.0, 2
    mesh = df.RectangleMesh(start_x, start_y, end_x, end_y, n_elem_x, n_elem_y)

    Running df.plot(mesh) will show the following:

    The mesh

    An example mesh with triangular elements

    We discretize our domain \(\Omega\) into discrete elements and obtain \(\hat \Omega\). I will use the "hat" to denote discretized values. We use linear elements which means we will approximate the unknown function with piecewise linear functions, \(\phi \approx \hat \phi\). They look like this for a 1D domain with two elements and three vertices (nodes):

    Linear shape functions in 1D

    1D domain with three shape functions, \(N_1(x)\), \(N_2(x)\) and \(N_3(x)\)

    We have one shape function \(N_i\) for each vertex in the mesh. The shape functions are equal to 1.0 at the corresponding vertex and 0.0 at all other vertices. In 2D a standard bi-linear shape function looks as follows:

    Linear shape function in 2D

    2D domain with a bi-linear shape function shown for one of the vertices on the boundary

    Marking the boundaries

    We know how to make a mesh of the domain. We also need to tell FEniCS about the different parts of the boundary. We do this by giving the boundaries different unique integer numbers and marking the boundaries with a mesh function:

    # Each part of the mesh gets its own ID
    boundary_parts = df.MeshFunction("size_t", mesh, mesh.topology().dim()-1)
    # Define the boundaries
    GEOM_TOL = 1e-6
    define_boundary(lambda x, on_boundary: on_boundary and x[0] < start_x + GEOM_TOL, boundary_parts, ID_LEFT_SIDE)
    define_boundary(lambda x, on_boundary: on_boundary and x[0] > end_x - GEOM_TOL, boundary_parts, ID_RIGHT_SIDE)
    define_boundary(lambda x, on_boundary: on_boundary and x[1] < start_y + GEOM_TOL, boundary_parts, ID_BOTTOM)
    define_boundary(lambda x, on_boundary: on_boundary and x[1] > end_y - GEOM_TOL, boundary_parts, ID_TOP)

    The define_boundary function is just a small utility I made to make it easier to mark the boundaries. Normally you need to create a class for each boundary and implement a method, inside, on this class. My function accepts a lambda expression which is used instead:

    def define_boundary(defining_func, boundary_parts, boundary_id):
        Define a boundary
        - defining_func is used instead of the normal SubDomain inside method: defining_func(x, on_boundary)
        - boundary_parts is a MeshFunction used to distinguish parts of the boundary from each other
        - boundary_id is the id of the new boundary in the boundary_parts dictionary
        class Boundary(df.SubDomain):
            def inside(self, x, on_boundary):
                return defining_func(x, on_boundary)
        boundary = Boundary()
        boundary.mark(boundary_parts, boundary_id)
        return boundary

    The solution method

    The simplest variant of the finite element method to describe is probably the Galerkin weighted residuals method. The core of the method is described below.

    The unknown function \(\phi\) is written as a sum of \(M\) shape functions and a set of unknown coefficients, \(a_i\). There is one unknown coefficient for each shape function:

    \begin{equation*} \hat \phi(x,y) = \sum_{i=0}^{M} a_i N_i(x,y) \end{equation*}

    Suppose we guess some coefficients \(a_i\). We can then integrate our trial function, \(\hat \phi\) over the domain, but since the discretization is not perfect we get a residual and not zero as the equation was supposed to give:

    \begin{equation*} \int_{\Omega} \laplace{\hat \phi} \ \dif \Omega = R \end{equation*}

    To be able to fix this and find some coefficients \(a_i\) that gives zero residual we need a set of equations. This is done by multiplying the above integral with a set of weighing functions, \(w_i(x,y)\). The number of weighting functions is equal to the number of unknowns, so we get a fully determined set of linear equations. In the Galerkin method the weighting functions are taken equal to the shape functions, \(N_i\) except that we do not include shape functions corresponding to vertices where we know the solution \(\phi(x,y)\) from the Dirichlet boundary conditions.

    We then get a set of \(M\) equations:

    \begin{equation*} \int_{\Omega} \laplace{\hat \phi} w_i \ \dif \Omega = 0 \end{equation*}

    which is the same as:

    \begin{equation*} \int_{\Omega} \laplace{\left(\sum_{j=0}^M a_j N_j\right)} N_i \dif \Omega = 0 \end{equation*}

    Since the integral will only be non-zero for vertices that are close in the mesh, i.e. \(N_i\) and \(N_j\) have some overlap, we end up with a quite sparse equation system. Very efficient solvers exist for the types of equation systems that come out of the Galerkin method.

    Solving the equation system with FEniCS

    In the standard finite element terminology our unknown function \(\phi\) is called the trial function and denoted \(u\) while the weighting function is called the test function and denoted \(v\). We switch to this terminology to be compatible with the FEniCS tutorial. We call this equation the weak form:

    \begin{equation*} \int_{\Omega} \laplace{(u)}\,v \ \dif \Omega = 0 \end{equation*}

    Before we are done we need to modify the equation a bit. As written it makes little sense since the Laplacian of the bi-linear function \(N_j(x,y)\) will always be zero. We modify our weak form by performing integration by parts. The formula for this in higher dimensions is:

    \begin{equation*} \int_\Omega \pdiff{f}{x_i}\,g \ \dif \Omega = \int_\Gamma f\,g\,n_i\ \dif \Gamma - \int_\Omega f \pdiff{g}{x_i} \ \dif \Omega \end{equation*}

    where \(n_i\) is the \(i\)-th component of the outwards normal vector on \(\Gamma\). I do not think I ever learned that at school? Maybe it's just my rusty memory, but thanks to Wikipedia we will not let lacking education and/or failing memory stop us, now will we? We get this when applying integration by parts to our integral:

    \begin{equation*} \int_\Omega \laplace{(u)}\,v \ \dif \Omega = \int_\Gamma \nabla(u)\,v\,n_i\ \dif \Gamma - \int_\Omega \nabla (u)\cdot\nabla(v) \ \dif \Omega \end{equation*}

    I guess now is the time for me to remember to mention that the test function \(v\) is always zero at the Dirichlet boundaries. Dirichlet boundaries are boundaries where we have Dirichlet boundary conditions, which means we know the value of \(\phi\), i.e. the short edges of our mesh in this case. No reason to have a weight function there, right? We now have the final expression for the weak form:

    \begin{align*} \int_{\Omega} \nabla u \cdot \nabla v \ \dif \Omega &= \int_{\Gamma_N} \laplace{(u)}\,v\,n_i\ \dif \Gamma_N \\ &= \int_{\Gamma_N} \pdiff{u}{\bf n}\,v\ \dif \Gamma_N \end{align*}

    The long edges were we prescribe the normal velocity (normal derivative of the velocity potential \(\phi\)) are now denoted \(\Gamma_N\) since this type of boundary condition is called a Neumann boundary condition.

    FEniCS understands equations such as the above and calls them forms. To describe the equations we use UFL, Uniform Form Language which is a Python API for defining forms. When interacting with FEniCS through Python we can use UFL through the dolfin package just like the mesh facilities. UFL can also be directly imported, import ufl.

    # Define a function space of bi-linear elements on our mesh
    V = df.FunctionSpace(mesh, 'Lagrange', 1)
    # The trial and test functions are defined on the bi-linear function space
    u = df.TrialFunction(V)
    v = df.TestFunction(V)
    # Our equation is defined as a=L. We only define what is inside the integrals, and the difference
    # between integrals over the domain and the boundary is whether we use dx or ds:
    #   - the term a contains both the trial (unknown) function u and the test function v
    #   - the term L contains only test function v
    a = df.inner(df.nabla_grad(u), df.nabla_grad(v))*df.dx
    L = df.Constant(42)*v*df.ds(ID_BOTTOM) + df.Constant(42)*v*df.ds(ID_TOP)

    This is basically all there is to solving the Laplace equation in FEniCS. The complete code can be seen below. The parts I have skipped explaining above are well explained in the FEniCS tutorial.

    Complete code

    The complete code can be found on Bitbucket. The resulting plot from running the code with FEniCS 1.3 is shown below:

    Plot of the result

    Plot of the resulting \(\phi\) function

    If you have any questions to the above and how to use FEniCS you can ask here, but I would really recommend the FEniCS QA Forum where you will probably get better and faster answers.

  3. Creating a mesh in FEniCS

    I may end up doing a large project using FEniCS which is a collection of tools for automated, efficient solution of differential equations using the finite element method. While playing with implementing a simple solver for fluid flow in a tank by use of FEniCS to solve the Laplace equation I needed to create my own mesh in code.

    FEniCS is quite well documented, but I had to look at the source code for some of the mesh conversion routines to find out how to build a mesh from scratch. So, for posterity, here is a reimplementation of dolfin.RectangleMesh in a much more cumbersome (and flexible) way:

    import numpy
    import dolfin as df
    def create_mesh(length, height, nx, ny, show=False):
        Make a square mesh manually
        Should give exactly the same results as using the built in dolfin.RectangleMesh() class
        # The number of mesh entities
        nvert = nx*ny
        ncell = 2*(nx-1)*(ny-1)
        # Positions of the vertices
        xpos = numpy.linspace(0, length, nx)
        ypos = numpy.linspace(0, height, ny)
        # Create the mesh and open for editing
        mesh = df.Mesh()
        editor = df.MeshEditor(), 2, 2)
        # Add the vertices (nodes)
        i_vert = 0
        for x in xpos:
            for y in ypos:
                editor.add_vertex(i_vert, x, y)
                i_vert += 1
        # Add the cells (triangular elements)
        # Loop over the vertices and build two cells for each square
        # where the selected vertex is in the lower left corner
        i_cell = 0
        for ix in xrange(nx-1):
            for iy in xrange(ny-1):
                # Upper left triangle in this square
                i_vert0 = ix*ny + iy
                i_vert1 = ix*ny + iy+1
                i_vert2 = (ix+1)*ny + iy + 1
                editor.add_cell(i_cell, i_vert0, i_vert1, i_vert2)
                i_cell += 1
                # Lower right triangle in this square
                i_vert0 = ix*ny + iy
                i_vert1 = (ix+1)*ny + iy+1
                i_vert2 = (ix+1)*ny + iy
                editor.add_cell(i_cell, i_vert0, i_vert1, i_vert2)
                i_cell += 1
        # Close the mesh for editing
        print 'Created mesh with %d vertices and %d cells' % (nvert, ncell)
        if show:
        return mesh

    If anyone finds this by searching the web for how to build a mesh programmatically in FEniCS/dolfin, then I hope the above was understandable. The documentation is quite good when you know that you need to search for the MeshEditor class ...

  4. Sorting images

    Once upon a time, back when I was using Windows at home, I had a useful small program that helped me sort through new pictures from my camera. I have forgotten the name of the program, but basically it allowed me to sort the good pictures from the bad in a fast and efficient manner so that the really bad ones could be deleted and the good ones could be separated, maybe for sharing with others.

    I have just been on a trip where I took quite some pictures. I could have gone over the pictures and manually copied the good ones into a separate folder for sharing with friends. This would have been a bit boring, but it would only have taken about five minutes. As a programmer I of course selected to optimize this task and spent some hours recreating the program I had once used. After a thousand trips or so I will come out ahead in terms of time spent!

    The program looks like this:

    Picster GUI

    I named it Picster, short for Picture Sorter. There is, of course, at least one other programs with that name already, but I cannot be bothered to find something better at the moment, It's just a script, after all. It is meant to be used from the keyboard, but there are also buttons for all possible actions (moving between images, categorizing images, and sorting images on disk based on category information).

    All of the GUI coding I do at work is scientific visualization, mostly using Python 2 and the wx library in some way. To try something slightly different I went with Python 3 and Qt for this program. I cannot really call myself an expert in Qt after only a couple of hours and the Picster code is probably not how a Qt expert would have written it, but it seems to work OK.

    From this brief encounter, Python Qt code seems to be a bit more verbose and tedious compared to wxPython. For example Qt/PySide is missing the nice init arguments, so all properties on an object must be set after creation through method calls. The API is not very pythonic with no use of Python properties as far as I understood. I am also missing docstring help on class and method name completion in Eclipse PyDev :-(

    Also missing as far as I understood is the wxPython ability to bind to any event from anywhere. To listen for keystrokes or window size change for example you must override virtual methods. For now I am happy with using wx at work. The Qt documentation that was rumored to be fabulous seems quite on the same level of the wx documentation as well.

    What I really liked about Qt was the Layouts which work almost exactly like Sizers in wx, except that they come with a sensible default spacing of widgets. This is a sore spot in laying out wx interfaces and always needs manual intervention to look good.

    Enough mostly unqualified statements about Qt vs. wx, here's the code for anyone interested in a picture sorting program. The code requires Python (probably works in versions 2 and 3, tested in 3.2) and PySide for Python bindings to Qt.

  5. Streaming audio from Spotify on Linux to Squeezebox

    I have tried the WaveInput route for SqueezeCenter, but due to a non-cooperative sound card and various problems with permissions related to SqueezeCenter running as a limited user I decided to go another route and stream sound from my Linux laptop via Icecast. If you want try using WaveInput and have the same problems with recording from the sound card as I have (it plain doesn't work with arecord and friends) there is a recipe here that might work for you.


    I need to use PulseAudio to get recording of sound played through the sound card to work as my Intel sound card refuses to allow me to record the sound directly. Luckily PulseAudio finally works OK for me now. I configured Wine with padsp winecfg and chose the OSS output driver for sound (ALSA works poorly at the moment). Now, run Spotify as padsp wine spotify.exe. Spotify should pop up in your PulseAudio Volume Control (pavucontrol) in the Playback tab.

    You need to define a PulseAudio sink that is different from the normal (output to PC speakers). I chose to call this sink spotify. Create the sink with the following command.

    pactl load-module module-null-sink sink_name=spotify

    The sink should pop up in the volume control under the Output Devices tab. Next, select this sink as the default for Spotify in the Playback tab (click the small down-arrow and choose Move Stream and then Null Output).


    You can run Icecast with a minimalistic configuration. I used the minimal example (/usr/share/doc/icecast2/icecast_minimal.xml.dist on Ubuntu) where I modified the passwords and the log directory (I set the log directory a directory where I have write permissions so that I can run Icecast as my own user). Start Icecast with

    icecast2 -c icecast.xml


    Finally I take the spotify PulseAudio sink and channel it to Icecast by use of Gstreamer. The magic command is (in one line).

    gst-launch-0.10 pulsesrc device=spotify.monitor ! audioconvert  ! vorbisenc bitrate=300000 ! oggmux ! shout2send ip=localhost port=8000 password=PASSWORD mount=stream.ogg

    The bit rate is set to the highest I could use without getting error messages (300kbps). I assume this is pretty transparent and does not degrade the 160kbps Spotify output much.

    Now tune your Squeezebox to URL http://ip-address-of-linux-machine:8000/stream.ogg. Modify the file name and port according to your configuration.

    Comments are disabled on this article due to problems with spam. Somehow spammers believe that link-spamming this page with praise for the article will send them lots of readers or google-points or something ...

    Update 2013: I no longer use this method and do not know if it still works or if there are better ways to do this now

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