create_sample(geometry="layer") and are represented by 1D line-trace mesh along the normal direction of the layer(s). For this, the plane-wave Fredkin-Koehler method has been expanded to infinitely-extended layers (preprint available at arXiv, submitted to AIP Advances). See Example ...tetrax.geometries submodule:
monolayer_line_trace()bilayer_line_trace()multilayer_line_trace()sample.J1 (in J/m^2) can also have different values between different layers in a multilayered sample, by supplying a list of values (see User Guide).eigenmodes(k=k_list,...) now accepts lists or 1D arrays as a parameter for k, e.g. to specify a non-equidistant wave-vector range.ExperimentalSetup.show_mode(k=..., N=...). See User Guide for details.TetraX are often based on seminal papers. In order to give credit to these works, when conducting a numerical experiment, TetraX now saves references important for this experiment to a bibtex file called references.bib, found in the sample directory. In this file, each entry contains a comment field describing how the reference was important for the computation. When publishing results calculated with TetraX in your research, please also give credit to the works which are important for the numerical experiments you conducted.NaNs are inserted into the dispersion dataframe. Previously, this simply caused an error.round_wire_cross_section_refined which supports local mesh refinement (see documentation).ExperimentalSetup.Bext is now initialized as MeshVector filled with zeros. Previously, an error occured when not specifying any external field.eigenmodes(fname="dispersion.csv",...).e_u can now be specified as a triplet, e.g. [0, 0, 1], just like magnetization or external field. Previously, this caused complications with the possiblity to set multiple uniaxial anistropies.