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Including operators and expressions in a multiphysics simulation is easier than you think.

Posted: 8 months ago by: Linus Andersson, COMSOL Employee | 8 Comments |

As most skilled COMSOL users, I am sure you know that you are not limited to just selecting what is in our drop-down lists. Say that you have invented your own measure of structural stress. You want it to be equal to the quadratic mean of the Tresca and von Mises stresses. Go to Plot Parameters to find out what these predefined stresses are called (tresca_smsld and mises_smsld if you are modeling in 3D with the Structural Mechanics Module). Now all you need to do is enter sqrt(0.5*(tresca_smld^2+mises_smld^2)) in any of the Expression fields and click OK to see your new stress distribution.

You probably didn't think of it, but in the expression I just mentioned, sqrt, ^, and even + are all examples of operators. COMSOL offers a whole range of useful ones, not all equally obvious. Did you for instance know that the letter d will differentiate any variable or expression with respect to time or space? d(c,z) gives the derivative of a concentration c with respect to the z-coordinate. d(sqrt(0.5*(tresca_smld^2+mises_smld^2)),t) is the time-derivative of your stress. If you have created your own subdomain expression my_stress containing your stress definition, d(my_stress,t) gives the same results.

The at operator lets you access the solution at any time in postprocessing. This is handy if you want to see changes over a time interval. Plotting the expression at(20,p)-at(10,p) overrides the Solution at time setting and shows you the pressure increase between 10 and 20 seconds. The with operator lets you postprocess more than one parametric or eigensolution in a similar fashion.

Another handy pair of operators is up and down. They live on boundaries and help you evaluate anything with discontinuities. Consider for example a temperature gradient on a boundary between two subdomains with different conductivities. gradT_ht will silently evaluate this gradient on both sides of the boundary and give you the average. With up(gradT_ht) and down(gradT_ht) however, you can decide which side you are interested in.

If you work with electromagnetics, you might have plotted the magnetic field in an eigenmode analysis only to find that it appears to be identically zero. Chances are it is non-zero but perfectly imaginary due to its 90-degree phase difference with a real-valued electric field. Use the imag operator to show its imaginary part, abs to plot the norm, or arg to see the phase angle. Note that the default plot for complex fields shows the real part.

This is just the tip of the iceberg. You can find the complete list of mathematical and other operators in the COMSOL Multiphysics Quick Start and Quick Reference.