changelog.m

%% MTEX Changelog
%
%
%% MTEX 6.0.beta.4 4/2024
%
% *Pseudo 3d EBSD and Grain maps*
%
% With version 6.0, MTEX starts to support pseudo 3d EBSD data. This means
% that EBSD maps are no longer restricted to the xy-plane. For
% example it is now possible to consider EBSD maps that represent the three
% faces of a cube. To make this possible, multiple changes at the core of
% MTEX had to be introduced:
%
% * |ebsd.pos| gives the position of the EBSD measurements and is of type
% @vector3d
% * many grain properties like vertices |grains.V|, centroid |grains.centroid|
% or long axis |grains.longAxis| are now of type @vector3d.
% * |ebsd.N|, |grains.N| gives the normal direction of a EBSD map
% * it is not possible to merge EBSD maps with different normal direction
% into one variable
%
% *Free three dimensional plotting of EBSD maps, pole figures, etc.*
%
% * Plotting of EBSD and grain maps is now possible in 3d
% * The alignment of x, y and z on the screen is now controlled by an
% object of type @plottingConvention. The code
%
%   how2plot = plottingConvention
%   how2plot.outOfScreen = ebsd.N
%   how2plot.east = yvector
%   plot(ebsd, how2plot)
%
% would plot an EBSD map with its normal direction out of the screen and the
% y-vector pointing to north.
% * A default plotting convention can be stored directly in the EBSD or
% grain variable via
%
%   ebsd.plottingConvention = how2plot
%
% * The plotting convention can also be passed to any spherical plot. This
% allows e.g. to plot pole figures with an arbitrary direction pointing out
% of the screen.
%
% * As consequence |'upper'| and |'lower'| refers to the outOFScreen
% direction.
%
% *Interface to Neper*
% Neper is an open source software package for 3d polycrystal generation
% and meshing. It is now possible to call Neper from within MTEX, simulate
% micro-structures, generated slices through a 3d volume and import those
% slices into MTEX. Have a look at <NeperInterface.html NeperInterface> for
% more information.
%
%% MTEX 5.11.0 3/2024
% 
% MTEX 5.11 will be the last release before MTEX 6.0. It significantly
% improves grain reconstruction from 2d EBSD data.
%
% *Much Faster Grain Reconstruction*
%
% Thanks to using the <https://github.com/JCash/voronoi jc_voronoi> as
% tessellation method and some addition speedups grain reconstruction is
% now more than 10 times faster then previously. The method used for
% Voronoi tessellation is now specified in |mtex_settings| by the option
% |'VoronoiMethod'|. You may want to set this option to |'qhull'| if you
% experience problems with the |'jcvoronoi'| engine.
%
% *Much Better Grain Reconstruction*
%
% With MTEX 5.11 MTEX uses <https://en.wikipedia.org/wiki/Alpha_shape alpha
% shapes> to determine the shape of the grains in the presence of large
% unindexed regions. Those alpha shapes are controlled by a single
% parameter |'alpha'| with specifies to which extend indexed regions are
% allowed to grow into not indexed regions. Have a look at
% <GrainReconstruction.html grain reconstruction> for an illustration of
% the new method.
%
% *Vector Fields in Orientation Space*
%
% Functionality of <SO3FunVectorField.html Vector Fields in Orientation
% Space> has been greatly extended. It includes now functions to compute
% <SO3VectorField.div.html the divergence |div(vF)|>,
% <SO3VectorField.curl.html the curl |curl(vF)|> and the
% <SO3VectorFieldHarmonic.antiderivative.html antiderivative> of a vector
% field |vF| on orientation space. This new functionality can be used to
% efficiently model texture evolution by numerically solving the continuity
% equation as it is demonstrated for <SingleSlipModel.html the single slip
% model>. Crucial for this approach is the new command <doEulerStep.html
% |doEulerStep|> which updates an ODF or a list of orientation according to
% a vector field an orientation space which may be given e.g. by the Taylor
% model.
% 
% *Lankford Parameter*
%
% The command <orientation.calcLankford.html |calcLankford|> allows for the
% computation of the Lankford or R-value. A full discussion of the
% corresponding analysis can be found <Lankford.html here>.
%
% *Transformation ODF*
%
% The command <orientation.variants.html |variants(p2c,odfParent)|>
% takes now as a second input a parent ODF and return the child ODF under
% the assumption that all variants appear with the same frequency. This is
% in more detail explained in the section <TransformationTexture.html
% Transformation Texture>.
%
% *Inner Planes in Crystal Shapes*
%
% Using the commands <crystalShape.plotInnerFace.html |plotInnerFace|>,
% <crystalShape.plot.html |plot(cS,sS)|> and <vector3d.arrow3d.html
% |arrow3d|> it is now possible to plot internal lattice planes, directions
% or slip systems into the crystal shape. This is explained in more detail
% at <CrystalShapes.html Crystal Shapes>.
%
% *Numerous minor improvements and bug fixes*
%
% * new command <SO3Fun.transformReferenceFrame
% |transformReferenceFrame(odf,csNew)|> that allows to switch between
% different setups of the same symmetry, i.e. between 121 and 112.
% * improved h5 interface
% * new function <SO3Fun.cor.html |cor(odf1,odf2)|> to compute the
% correlation between two ODFs.
% * new function <vector3d.lineIntersect.html |lineIntersect|> to compute
% the intersection between a line and a plane.
% * new class <S1FunHarmonics.html |S1Fun|> to represent directional
% properties in the plane.
% * new function <S2Fun.volume.html |volume(S2F,center,radii)|> to compute
% the volume of a spherical function within a ball.
% * replaces |CLim| by <setColorRange.html |setColorRange|>
% * <parentGrainReconstructor.calcParentEBSD.html |calcParentEBSD|>
% computes also the variant and packet ids
% * many bug fixes
% 
%% MTEX 5.10.1 9/2023
% 
% This is mainly a bug fix release.
%
%% MTEX 5.10.0 5/2023
%
% *Weighted Burgers Vector*
%
% With the function <EBSD.weightedBurgersVec.html |weightedBurgersVec(ebsd)|>
% it is now possible to compute the weighted burgers vector both, using the
% integral approach as well as the differential approach.
%
% *Bain Group Determination* 
% 
% The function <calcVariantId.html |calcVariantId|> now returns an id for
% the variant, the packet and the Bain group. The usage of this function is
% demonstrated <MartensiteVariants.html here>.
%
% *Numerous minor addon, speed improvements, bug fixes*
%
% * New option |'max'| to <orientation.angle.html |angle(mori)|> to compute
% the largest misorientation angle. Helpful for identifying twinning.
% * Added checks for symmetry and positive definiteness when defining
% stress, strain and elasticity tensors.
% * Add morphological filter <EBSD.erode.html |erode(ebsd)|> as a simple
% method for data cleaning in EBSD maps.
% * Pseudesymmetries like 532 are now natively supported using the syntax
% |crystalSymmetry('532')|
% * |symmetrise(t,'iso')| return the isotropic portion of a tensor
% * <tensor.symmetricDecomposition.html |symmetricDecomposition|> computes
% the symmetric decomposition of a tensor
% * normalize the Taylor factor according to the strain
% * display boundary length as default output
% * better import of h5 files
% * many more fixes and speed improvements
%
%% MTEX 5.9.0 2/2023
%
% *Habit Plane Detection*
%
% MTEX 5.9 includes powerful functions for the determination of predominant
% habit planes and habit plane distributions. For the setting of a fully
% transformed microstructure the are described in the paper <Habit plane
% determination from reconstructed parent phase orientation maps>. Those
% functions include
%
% * new function <grain2d.calcTraces.html |calcTraces(grains)|> and
% <EBSD.calcTraces.html |calcTraces(ebsd)|> to compute habit plane traces
% from families of grains or EBSD data.
% * new function <calcGBND.html |calcGBND(traces,ori)|> to compute the
% grain boundary normal distribution from a list of habit plane traces and
% the corresponding grain orientations.
% * new function <grainBoundary.characteristicShape.html
% |characteristicShape(gB)|> to compute the characteristic shape from lists
% of grain boundaries
%
% *Orientation dependent functions*
%
% The orientation distribution function (ODF) describes the relative volume
% of crystal orientations within a material. As such it is a function that
% associates to each orientation a number with unit mrd (multiples of
% random distribution). However, in material science many other orientation
% depended functions are of importance, e.g., the Taylor factor with
% respect to some outer strain depends on the local orientation. While ODFs
% have ever since been at the heart of MTEX, this release is the first one
% that includes full support for orientation dependent functions. Those
% functions are called @SO3Fun and behave similar to spherical functions
% @S2Fun. In particular one can
%
% * add, subtract, multiply and divide with them
% * compare them
% * detect global and local extrema
% * visualize them in 3d and 2d sections
% * compute gradients
%
% While implementing these new features we also significantly speed up
% all operations related with ODF operations. A full documentation of these
% new features can be found <SO3FunConcept.html here>.
%
%
%% MTEX 5.8.2 11/2022
%
% This is mainly a bug fix release. New functionalities include
%
% * <fibre.fit.html |fibre.fit(ori)|> and <fibre.fit.html |fibre.fit(odf)|>
% robustly finds fibers in data sets of individual orientations and ODFs.
% * <fibre.angle.html |angle(f1,f2)|> computes the angle between two
% <OrientationFibre.html fibers>.
% * <S2Fun/calcSymAxis.html |calcSymAxis(pf)|> allows to find rotational
% symmetries in <ODFPoleFigure.html pole figures> or arbitrary
% <S2FunConcept.html spherical functions>.
%
%% MTEX 5.8.0 01/2022
%
% MTEX 5.8 improves further on parent grain reconstruction by implementing
% the novel <https://arxiv.org/abs/2201.02103 variant graph algorithm>
% which is faster and more accurate than the previous grain graph algorithm.
%
% *Improved parent grain reconstruction*
%
% Along with the new reconstruction algorithm the following new features
% have been implemented:
%
% * manual interactive parent orientation selection using
% <parentGrainReconstructor.selectInteractive.html |selectInteractive(job)|>
% * new option |'reconsiderAll'| in
% <parentGrainReconstructor.calcGBVotes.html |calcGBVotes(job)| to recheck
% all assignments of parent orientations.
% * new option |'bestFit'| in
% <parentGrainReconstructor.calcGBVotes.html |calcGBVotes(job)| to consider
% only the best fitting neighbor
% * |job.votes| is now a table which contains the parentId votes and the
% probabilities for all grains
%
% *Misc Changes*
%
% * new option |'region'| for |<EBSD.plot.html plot(ebsd)>| to plot only a
% rectangular subregion of the map
%
%% MTEX 5.7.0 05/2021
%
% MTEX 5.7 improves on parent grain reconstruction. Changes include:
%
% *Improved parent grain reconstruction*
%
% * The ordering of the variants is stored within the OR misorientation |p2c|
% as |p2c.variantMap|. In particular the variants in |p2c.variants| are
% ordered by default according to the Morito convention. This can be easily
% check by the command |round2Miller(p2c.variants)|
% * The command |job.calcGBVotes| and |job.calcTPVotes| compute votes
% associated with probabilities that are stored in |job.votes| and can
% easily be analyzed.
% * The options |'noP2C'| and |'noC2C'| have been replaced by |'p2c'| and
% |'c2c'|.
% * New option |job.useBoundaryMisorienation| which makes the parent grain
% reconstructor to use the misorientations along the grain boundaries
% instead of the misorientations between the grain mean orientations.
% * added ShojiNishiyama orientation relationship.
%
% *Other Changes*
%
% * The command |findByOrientation| accepts a fiber as input.
% * The antipodal |axisAngleColorKey| allows for option |'antipodal'|.
% 
%
%% MTEX 5.6.1 03/2021
%
% This is mainly a bug fix release.
%
%% MTEX 5.6.0 01/2021
%
% MTEX 5.6 greatly simplifies parent grain reconstruction by introducing
% the class <parentGrainReconstructor.parentGrainReconstructor.html
% |parentGrainReconstructor|>. During the reconstruction procedure this
% class keeps track of the correspondence between measured child grains and
% the reconstructed parent grains. It provides the following functions for
% recovering parent orientations which can be applied multiple times and in
% any order to achieve the best possible reconstruction.
%
% * <parentGrainReconstructor.calcParent2Child.html |calcParent2Child|> - optimize parent to child orientation relationship
% * <parentGrainReconstructor.calcGBVotes.html |calcGBVotes|> - compute votes from child/child and parent/child grain boundaries
% * <parentGrainReconstructor.calcTPVotes.html |calcTPVotes|> - compute votes from child/child/child triple points
% * <parentGrainReconstructor.calcParentFromVote.html |job.calcParentFromVote|> - recover parent orientations from votes
% * <parentGrainReconstructor.calcParentFromGraph.html |job.calcParentFromGraph|> - recover parent orientations from graph clusteres
% * <parentGrainReconstructor.mergeSimilar.html |job.mergeSimilar|> - merge similar parent grains
% * <parentGrainReconstructor.mergeInclusions.html |job.mergeInclusions|> - merge inclusions
% * <parentGrainReconstructor.revert.html |job.revert|> - undo parent grain reconstructions
%
% The usage of this new class is demonstrated in <TiBetaReconstruction.html
% Beta Titanium Reconstruction> and <MaParentGrainReconstruction.html
% Parent Martensite Reconstruction>.
%
% *Compatibility fixes*
%
% MTEX 5.6 fixes several incompatibilities with MATLAB versions earlier
% then 2019b.
%
%% MTEX 5.5.0 11/2020
%
% *Orientation Embedding*
%
% Orientational embeddings are tensorial representations of orientations
% with the specific property that each class of symmetrically equivalent
% orientations has a unique tensor representation. In contrast to the well
% known representation by Rodrigues vectors those embeddings do not suffer
% from boundary effects, i.e., the Euclidean distance between the tensors
% is always close to the misorientation angle. This allows to lift any
% method that works for multivariate data to orientations. More details of
% this representation can be found in the chapter
% <OrientationEmbeddings.html orientation embeddings> and the paper
%
% * R. Hielscher, L. Lippert, _Isometric Embeddings of Quotients of the
% Rotation Group Modulo Finite Symmetries_,
% <https://arxiv.org/abs/2007.09664 arXiv:2007.09664>, 2020.
%
% *Low Angle Boundaries*
%
% With MTEX 5.5 we make low angle grain boundary analysis much more straight
% forward by allowing to pass to the command <EBSD.calcGrains.html
% |calcGrains|> two thresholds, i.e.,
%
%   grains = calcGrains(ebsd,'threshold',[10*degree 1*degree])
% 
% generates grains bounded by high angle grain boundaries with a threshold
% of 10 degree and inner low angle boundaries with an threshold of 1
% degree. The latter ones are stored as |grains.innerBoundary|. In order to
% estimate the density of inner boundaries per grain the commands
% <grain2d.subBoundaryLength.html |subBoundaryLength|> and
% <grain2d.subBoundarySize.html |subBoundarySize|> have been introduced.
% The documentation page <SubGrainBoundaries.html Subgrain Boundaries>
% describes the analysis of low angle boundaries in more detail.
%
% *New Functionalities*
%
% * For single phase EBSD maps you can access the orientations now more
% easily by |ebsd.orientations| instead of |ebsd('indexed').orientations|.
% Orientations corresponding to not indexed pixels will be returned as NaN
% and thus automatically ignored during any further computation.
% * <grain2d.isBoundary |grains.isBoundary|> checks grains to be
% boundary grains
% * <grain2d.isInclusion |grains.isInclusion|> checks grains to be
% inclusions
% * <grain2d.merge.html |merge(grains,'inclusions')|> merges inclusions
% into their hosts
% * <grain2d.merge.html |merge(grains,'threshold',delta)|> merges grains
% with a certain misorientation angle
% * interpolation of EBSD maps at arbitrary coordinates by the command
% <EBSD.interp.html |interp|> works now for hexagonal grids as well. In
% particular this allows to remap EBSD data from hexagonal to square grids
% and vice versa. Have a look at the chapter <EBSDInter.html Interpolation>
% for more details.
% * <EBSD.calcMis2Mean.html |calcMis2Mean|> computes the misorientation to
% a grain reference orientation, i.e., the <EBSDGROD.html grain reference
% orientation deviation (GROD)>.
% * KAM computation has been speed up significantly for hexagonal and
% square grids. Make sure to use the command |ebsd = ebsd.gridify| before
% the KAM computation.
% * new option |'edgeAlpha'| to control the transparency of grain
% boundaries, e.g. in dependency of the misorientation angle.
% * more easily add new / change phases in an EBSD map by one of the
% following commands
%
%   ebsd(ind).orientations = orientation.byEuler(0,0,0,CSNew)
%   ebsd(ind).CS = CSNew
%
% * new option to plot arrows in spherical plots by
%
%   plot([vector3d.Z, vector3d.Z + 0.5 * vector3d.rand],'arrow')
%
% * <EBSD.export.html |export(ebsd,fileName)|> allows to export to EBSD
% data to |.ang|, |.ctf|, |.crc| and |.hdf5| files, thanks to Azdiar Gazder
% * new function <rotation.fit.html |rot = fit(l,r)|> to compute the
% rotations that best rotates all the vectors |l| onto the vectors |r|
%
% * <orientation.load.html |orientation.load|> and <vector3d.load.html
% |vector3d.load|> allows now to import additional properties.
%
% *Important Bug Fixes*
%
% * <SO3Fun.volume.html |volume(odf)|> gave wrong results in the presence of
% specimen symmetry and for centers close to the boundary of the
% fundamental region.
%
% * <slipSystem.symmetrise.html |slipSystem.symmetrise|> gave
% incorrect number of slipsystems due to a rounding error
%
%% MTEX 5.4.0 7/2020
%
% *Parent Grain Reconstruction*
%
% MTEX now includes a number of functions for variant analysis and to
% recover parent grain structure. Examples include
% <TiBetaReconstruction.html beta phase reconstruction in Titanium> and
% <MaParentGrainReconstruction.html Martensite reconstruction from
% Austenite grains>. The reconstruction is mainly build around the
% following new commands
%
% * <calcParent.html |calcParent|> computes the best fitting parent
% orientations from child orientations
% * <calcChildVariants.html |calcChildVariants|> separates child variants
% into packets
% * <calcParent2Child.html |calcParent2Child|> computes best fitting parent
% to child orientation relationship from child to child misorientations
% * <variants.html |variants|> computes all parent or child variants
%
% *New Functionalities*
%
% * new function <EBSD.interp.html |ebsd.interp|> to interpolate EBSD maps
% at arbitrary x,y coordinates, <EBSDInter.html example>
% * <grain2d.smooth.html |smooth(grains)|> keeps now triple points and outer
% boundary fixed by default
% * the field |grains.triplePoints.angles| returns the angles between the
% boundaries at the triple points
% * new option |'removeQuadruplePoints'| to |<EBSD.calcGrains.html
% calcGrains>|
% * harmonic approximation of spherical functions respecting symmetry
% * |export(ebsd,'fileName.ang')| exports to .ang files
% * <grain2d.neighbours.html |neighbours(grains)|> now returns a list of
% pairs of neighboring grains
% * <grain2d.numNeighbours.html |grains.numNeighbours|> returns the number
% of neighboring grains
% * <grainBoundary.selectByGrainId.html |selectByGrainId|> allows to select
% boundary segments by pairs of grains
% * new helper function <majorityVote.html |majorityVote|> 
% * new option |'noAntipodal'| for many commands like |symmetrise|,
% |unique|, |dot|, |angle|
% * new predefined orientation relationship |orientation.Burgers|
%
%% MTEX 5.3.1 6/2020
% 
% *New Functions*
%
% * <EBSDSquare.interp.html interp> to interpolate EBSD maps
% * grain properties <grain2d.longAxis.html longAxis>, <grain2d.shortAxis.html shortAxis>
% * <BoundaryCurvature.html grain boundary curvature>
%
% *Bug Fixes*
%
% * loading ang files
% * importing ODFs
% * inverse pole figures misses orientations
% * <grain2d.hull convex hull> of grains has now correct boundaries
%
% * Other Changes*
%
% * <vector3d.mean.html vector3d/mean> now returns not normalized vectors
% * new flag |noAntipodal| to supress antipodal symmetry in calculations
%
%% MTEX 5.3.0 4/2020
%
% MTEX 5.3 is a humble release without big shiny improvements. On the other
% hand is has seen some internal changes which lead to significant speed
% improvements in some functions. Technically speaking the class @symmetry
% is not derived from @rotation anymore but is a handle class. From the
% users perspective almost no change will be noticed. Developers should
% replace |length(cs)| by |numSym(cs)|.
%
% *Much Better and Faster Halfquadratic Filter* 
%
% Denoising of EBSD data using the
% <https://mtex-toolbox.github.io/EBSDDenoising.html#10
% |halfQuadraticFilter|> is now about 10 times faster, handles outliers
% much better and runs native on hexagonal grids.
%
% *New Functions*
%
% * <stiffnessTensor.plotWaveVelocities.html |plotWaveVelocities|>
% illustrates anisotropy of seismic waves
% * <EBSD.grainMean.html |grainMean|> grain averages of arbitrary properties
% * shape functions <grain2d.surfor.html |surfor|>, <grain2d.paror.html
% |paror|>, <grain2d.caliper.html |caliper|>
% * <Miller.multiplicity.html |multiplicity|> for Miller, orientation and
% fiber
%
%% MTEX 5.2.3 11/2019
%
% * replaced |calcODF(ori)| by |<orientation.calcDensity.html calcDensity(ori)>|
% * bug fix in ODF reconstruction from XRD data
% * bug fix in EBSD export to ctf
% * bug fix in grain reconstruction
% * some more minor bug fixes
%
%% MTEX 5.2.0 10/2019
%
% *New Documentation*
%
% MTEX got a new homepage which was needed to include a much more
% exhaustive online documentation which has now
%
% * a sidebar for quick navigation
% * a search field
% * a complete function reference to all MTEX functions and classes
% * UML diagrams illustrating the hierarchy of the classes
% * much more content
%
% The new documentation is not yet perfect though we are working hard to
% improve it. That's why we are extremely happy for everybody who contributes
% additions to the documentation. This includes the correction of spelling
% errors, theoretical parts, examples etc. Check out <Contribute2Doc.html
% how to contribute to the documentation>.
%
% *More Colors*
%
% All plotting commands in MTEX support now much more colors. By default
% all the color names of the CSS palette can be chosen, e.g., aqua,
% orange, gold, goldenrod, etc. To see a full list of supported colors do
%
%  colornames_view
%
% The following function have been included to handle colors more
% efficiently
%
% * <str2rgb.html |str2rgb|> convert color str to RGB color
% * <ind2color.html |ind2color|> convert index to distrinct RGB colors,
% good for loops
%
% *Improved Import Wizard*
% 
% Importing EBSD data using the import wizard allows to interactively
% realign the data and check with respect to the pole figures.
%
% *Speed Improvements*
%
% * much faster visualization of the large EBSD maps if <EBSD.gridify.html
% |gridify|> is used
% * faster Fourier transforms on the sphere and the orientation space
% * support for <MOSEK
% https://docs.mosek.com/9.0/toolbox/install-interface.html> as faster
% replacement for linprog from the Optimization Toolbox
%
% *Support for hexagonal EBSD grids*
%
% The function <EBSD.gridify.html |gridify|> now works also for EBSD data
% measured on a hexagonal grid. As a consequence denoising and GND
% computation for those data is also on the way.
%
%
% *Plastic Deformations*
%
% MTEX 5.2. introduces a bunch of new tensor classes to make modelling of
% plastic deformations more straight forward.
%
% * <velocityGradientTensor.velocityGradientTensor.html Velocity Gradient Tensors>
% * <strainRateTensor.strainRateTensor.html strain rate tensor>
% * <deformationGradientTensor.deformationGradientTensor.html deformation gradient tensor>
% * <spinTensor.spinTensor.html spin tensor>
%
% The relationships between those tensors are explained in the section
% <PlasticDeformation.html plastic deformations>.
%
%
% *Spherical Bingham Distribution* 
%
% Native support for spherical <BinghamS2.BinghamS2.html Bingham distributions>,
% including the ability to <BinghamS2.fit.html fit> them to directional
% distributions.
%
% *Tensors*
%
% * Improved methods for the visualization of elastic properties, see
% <SeismicVelocitySingleCrystalDemo2d.html Seismic demo>
% * several new functions like <tensor.trace.html |trace|>,
% <tensor.svd.html |svd|>, <tensor.det.html |det|>, <tensor.colon.html
% double dot product |:|>
% * the function <tensor.mean.html |mean|> computes now Voigt, Reuss, Hill
% and geometric means
%
% *Improved Figure Layout*
%
% * fix layout
% * plot at fixed positions
%
% *Misc Changes*
%
% * allow to export EBSD data to |.ctf| thanks to Frank Niessen
% * compute the volume of a crystal shape
% * label crystal faces in crystal shapes
% * new function <orientation_std.html |std|> for computing the standard
% deviation of orientations
% * new function <calcKearnsFactor.html |calcKearnsFactor|>
% * |grainBoundary.ebsdId| is now the id and not the index of the EBSD data
% * allow to index ebsd data and grains by id using |{}| brackets
%
%   ebsd{id}
%   grains{id}
%
% * new options to scatter
%
%   scatter(v,'numbered')               % plot vectors with numbers
%   scatter(v,'MarkerFaceColor','none') % plot vectors with colored empty marks
%
%% MTEX 5.1.0 04/2018
%
% *Dislocation systems*
%
% Starting with version 5.1 MTEX introduces a class representing
% dislocation systems. Dislocation systems may be lists of edge or screw
% dislocations and are either defined by its burgers and line vectors
%
%   cs = crystalSymmetry('432')
%   b = Miller(1,1,0,cs,'uvw')
%   l = Miller(1,-1,-2,cs,'uvw')
%   dS = dislocationSystem(b,l)
%
% by a family of slipsystems
%
%   sS = slipSystem.fcc(cs)
%   dS = dislocationSystem(sS)
%
% or as the family of predefined dominant dislocation systems by
%
%   dS = dislocationSystem.fcc(cs)
%
% More information how to calculate with dislocation systems can be found
% <dislocationSystem.dislocationSystem.html here>.
%
% *Geometrically neccesary dislocations*
%
% The newly introduced dislocation systems play an important role when
% computing geometrically neccesary dislocations from EBSD data. The
% workflow is illustrate the script <GND.html GND> and consists
% of the following steps:
%
% # define the dominant <dislocationSystem.dislocationSystem.html
% dislocation systems>
% # transform the dislocation systems into specimen coordinates for each
% pixel of the EBSD map
% # compute the <curvatureTensor.curvatureTensor.html curvature tensor> for
% each pixel in the EBSD map
% # <curvatureTensor.fitDislocationSystems.html fit the dislocation
% systems> to the curvature tensors.
% # compute the total energy in each pixel
%
% *Tensor arithmetics*
%
% <dyad.html |dyad|>, <tensor.trace.html |trace|>, <tensor.det.html
% |det|>, <tensor.mean.html |mean|>, <tensor.diag.html
% |diag|>, <tensor.eye.html |eye|>, <tensor.sym.html |sym|>
%
% *Birefringence*
%
% MTEX 5.1 includes some basic methods to analyze and simulate optically
% isotropic materials. This includes the computation of the optical axis,
% birefringence and spectral transmission. The new features are
% demonstrated in <BirefringenceDemo.html BirefringenceDemo>.
%
% *Color Keys*
%
% In MTEX 5.1 the color keys used for coloring EBSD have been a bit
% reorganised.
%
% * seperate classes for directional color keys. So far these classes are
% <HSVDirectionKey.html |HSVDirectionKey|>, <HKLDirectionKey.html
% |HKLDirectionKey|>, <TSLDirectionKey.html |TSLDirectionKey|>. This has
% become neccesary as some orientation color keys depend directional color
% keys with different symmetry.
%
% * new color key <axisAngleColorKey.html |axisAngleColorKey|> that
% implements the coloring described in K. Thomsen, K. Mehnert, P. W. Trimby
% and A. Gholinia: Quaternion-based disorientation coloring of orientation
% maps, Ultramicroscopy, 2017. In central idea is to colorise the
% misorientation axis with respect to the specimen reference system.
%
% * The existing color keys have been renamed for better consistency. The
% new names are <BungeColorKey.html |BungeColorKey|>, <ipfHSVKey.html
% |ipfHSVKey|>, <ipfHKLKey.html |ipfHKLKey|>, <ipfTSLKey.html |ipfTSLKey|>,
% <ipfSpotKey.html |ipfSpotKey|>, <spotColorKey.html |spotColorKey|>,
% <PatalaColorKey.PatalaColorKey.html |PatalaColorKey|>
%
% *Spherical functions*
%
% * new function <S2Fun.discreteSample.html |discreteSample|> to compute
% random samples from spherical density functions
% * new option to <S2FunHarmonic.symmetrise.html |symmetrise|> to
% symmetrise a spherical function with respect to an axis
%
% *Misc*
%
% * new fuction <grain2d.fitEllipse.html |fitEllipse|> to assign ellipses
% to grains
% * the functions <tensor.symmetrise.html |symmetrise(tensor)|> and
% <S2FunHarmonic.symmetrise.html |symmetrise(S2F)|> do support
% symmetrisation with respect to a certain axis.
% * the function <quaternion.export.html |export(ori)|> allows to export
% arbitrary additional properties together with the Euler angles, e.g. the
% half axes and orientation of the grain ellipses
% * the function <loadOrientation_generic.html |loadOrientation_generic|>
% allows to import arbitrary additional properties together with the
% orientations, e.g., weights
% * new option |logarithmic|
% * new function <SO3Fun.grad.html |grad|> to compute the gradient of and ODF
% at a certain orientation
% * explicitely set the number of rows and columns in a MTEXFigure plot
% with
% * EBSD hdf5 interface works now for Bruker data as well
%
%% MTEX 5.0.0 03/2018
%
% *Replace all executables by two mex files*
%
% In MTEX many functionalities are based on the non equispaced fast Fourier
% transform (<http://www.nfft.org NFFT>). Until now this dependency was kept under
% the hood, or more precisely, hidden in external executable files which often
% caused troubles on MAC systems. Starting with MTEX 5.0. all the executables
% have been replaced by two mex files provided by the NFFT package. This
% change (hopefully) comes with the following advantages
%
% * better compatibility with MAC systems, no SIP disabled required
% * increased performance, e.g., due to multi core support
% * better maintainability, as all MTEX code is now Matlab code
% * the pole figure to ODF inversion algorithm is now entirely implemented
% in Matlab making it simple to tweak it or add more sophisticated
% inversion algorithms
%
% *Spherical functions*
%
% Many functions in MTEX compute directional dependent properties, e.g.
% pole figures, inverse pole figures, wave velocities, density distribution
% of misorientation axis or boundary normals. Until now those functions
% took as an input an of vector of directions and gave as an output a
% corresponding vector of function values, e.g. the command
%
%   pfi = calcPDF(odf,Miller(1,0,0,odf.CS),r)
%
% returns for a list of specimen directions |r| the corresponding list of
% pole figure intensities |pfi| for the ODF |odf|. Starting with MTEX 5.0 it
% is possible to ommit the list of specimen directions |r| or replace it by
% an empty list |[]|. In this case the command
%
%   pdf = calcPDF(odf,Miller(1,0,0,odf.CS))
%
% returns a <S2FunHarmonic.S2FunHarmonic.html spherical function> |pdf| also called
% pole density function. One can evaluate this spherical function using the
% command <S2FunHarmonic.eval.html eval> at the list of specimen directions
% |r| to obtain the pole figure intensities
%
%   pfi = pdf.eval(r)
%
% However, there are many more operations that can be performed on
% spherical functions:
%
%   % compute with spherical functions as with ordinary numbers
%   pdf3 = 5 * pdf1 + 3 * pdf2
%   pdf = max(pdf,0) % repace of negative entries by 0
%   pdf = abs(pdf) % take the absolute value
%   sum(pdf) % the integral of the pole figure
%   sum(pdf.^2) % the integral of the pole figure squares - also called pole figure index
%
%   % plotting
%   plot(pdf)
%   plot3(pdf) % plot in 3d
%
%   % detect maximum value
%   [value,pos] = max(pdf)
%
%   % compute the eigen values and eigen vectors
%   [e,v] = eig(pdf)
%
% For a complete list of functions read <S2FunHarmonic.S2FunHarmonic.html here>.
%
% *Symmetry aware spherical functions*
%
% Since most of the directional dependent properties obey additional
% symmetry properties the class <S2FunHarmonic.S2FunHarmonic.html
% S2FunHarmonic> has been extended to respect symmetry in the class
% <S2FunHarmonicSym.S2FunHarmonicSym.html S2FunHarmonicSym>.
%
% *Multivariate spherical functions, vector fields and spherical axis fields*
%
% In some cases it is useful that a spherical function gives not only one
% value for a certain direction but several values. This is equivalent to
% have concatenate several univariate spherical function to one
% multivariate function. This can be accomplished by
%
%   S2Fmulti = [S2F1,S2F2,S2F3]
%
% which gives a spherical function with 3 values per direction. More
% information how to work multivariate functions can be found
% <S2FunMultivariate.html here>.
%
% If we interpret the 3 values of |S2Fmulti| as $x$, $y$, and, $z$ coordinate of
% a 3 dimensional vector, the function |S2Fmulti| can essentially be seen as
% a spherical vector field associating to each direction a three
% dimensional vector. The most important example of such a vector field is
% the gradient of a spherical function:
%
%   g = S2F1.grad
%
% The resulting variable |g| is of type <S2VectorField.S2VectorField.html
% S2VectorField>. A complete list of functions available for vector fields
% can be found  <S2VectorField.S2VectorField.html here>.
%
% Another example for vector fields are polarisation directions |pp|,
% |ps1|, |ps2| as computed by
%
%   [vp,vs1,vs2,pp,ps1,ps2] = velocity(C)
%
% The main difference is, that polarisation directions are antipodal, i.e.
% one can not distinguish between the polarisation direction |d| and |-d|.
% In MTEX we call vector fields with antipodal values are represented by
% variables of type <S2AxisFieldHarmonic.S2AxisFieldHarmonic.html AxisField>.
%
% *Scalar tensor properties are returned as spherical functions*
%
% Any scalar or vectorial property of a tensor is not returned as a
% spherical function or spherical vector field. Examples are the velocity
% properties mentioned above, Youngs modulus, shear modulus, Poisson ration
% etc. In particular, plotting those directional dependend quantities is as
% simple as
%
%   plot(C.YoungsModulus)
%
% This makes the old syntax
%
%   plot(C,'plotType','YoungsModulus')
%
% obsolete. It is not supported anymore.
%
% *Crystal shapes*
%
% MTEX 5.0 introduces a new class <crystalShape.crystalShape.html crystalShape>.
% This class allows to plot 3-dimensional representations of crystals on
% top of EBSD maps, pole figures and ODF sections. The syntax is as follows
%
%   % define the crystal symmetry
%   cs = loadCIF('quartz');
%
%   % define the faces of the crystal
%   m = Miller({1,0,-1,0},cs);  % hexagonal prism
%   r = Miller({1,0,-1,1},cs);  % positive rhomboedron, usally bigger then z
%   z = Miller({0,1,-1,1},cs);  % negative rhomboedron
%   s2 = Miller({1,1,-2,1},cs); % right tridiagonal bipyramid
%   x2 = Miller({5,1,-6,1},cs); % right positive Trapezohedron
%   N = [m,r,z,s2,x2];
%
%   % define the crystal shape
%   habitus = 1.2; % determines the overal shape
%   extension = [1,1.2,1]; % determines the extension of the crystal in x,y,z direction
%   cS = crystalShape(N,habitus,extension);
%
%   plot(cS)
%   plot(x,y,cS)
%   plot(grains,cS)
%   plot(ebsd,cS)
%   plotPDF(ori,ori*cS)
%
% *ODF component analysis*
%
% MTEX 5.0 allows for decomposing ODF into components using the command
% <SO3Fun.calcComponents.html calcComponents>. In its simplest form
%
%   [mods,weights] = calcComponents(odf)
%
% returns a list of modal orientaions |mods| and a list of weights which
% sum up to one. A more advanced call is
%
%   [modes, weights,centerId] = calcComponents(odf,'seed',oriList)
%
% which returns in centerId also for each orientation from |oriList| to
% which component it belongs.
%
% *Clustering of orientations*
%
% The ODF component analysis is used as the new default algorithm in
% <orientation.calcCluster.html calcCluster> for orientations. The idea is
% to compute an ODF out of the orientations and call
% <SO3Fun.calcComponents.html calcComponents> with
%
%   [center,~,centerId] = calcComponents(odf,'seed',ori)
%
% Then |center| are the clusters center and |centerId| gives for each
% orientation to which cluster it belongs. Substantional in this method is
% the choise of the kernel halfwidth used for ODF computation. This can be
% adjusted by
%
%   [c,center] = calcCluster(ori,'halfwidth',2.5*degree)
%
% *New tensor classes*
%
% With MTEX 5.0 we start introducing specific tensor classes. So far we
% included the following classes
%
% * <stiffnessTensor.stiffnessTensor.html stiffnessTensor>
% * <complianceTensor.complianceTensor.html complianceTensor>
% * <strainTensor.strainTensor.html strainTensor>
% * <stressTensor.stressTensor.html stressTensor>
% * <ChristoffelTensor.ChristoffelTensor.html ChristoffelTensor>
%
% more tensors are supposed to be included in the future. The central
% advantage is that tensor specific behaviour and functions can now better
% be implemented and documented, e.g., that the inverse of the compliance
% tensor is the stiffness tensor and vice versa. For user the important
% change is that e.g. the stiffness tenssor is now defined by
%
%   C = stiffnessTensor(M,cs)
%
% instead of the depreciated syntax
%
%   C = tensor(M,cs,'name','elastic stiffness','unit','GPA')
%
% *Improved spherical plotting*
%
% In MTEX 4.X it was not possible to display the upper and lower hemisphere
% in pole figure plots, inverse pole figure plots or ODF section plots.
% This was a server restriction as for certain symmetries both hemispheres
% do not have to coincide. In MTEX 5.0 this restriction has been overcome.
% MTEX automatically detects whether the upper and lower hemisphere are
% symmetrically equivalent and decides whether both hemispheres needs to be
% plotted. As in the previous version of MTEX this can be controlled by the
% options |upper|, |lower| and |complete|.
%
% As a consequence the behaviour of MTEX figures have changed slightly. By
% default MTEX now always plots into the last axis. In order to annotate
% orintations or directions to all axes in a figure use the new option
% |add2all|.
%
%  plotIPDF(SantaFe,[xvector,yvector+zvector])
%  [~,ori] = max(SantaFe)
%  plot(ori,'add2all')
%
% We also introduced two new functions <S2Fun.plotSection.html plotSection>
% and <S2Fun.quiverSection.html quiverSection> to visualize spherical
% functions restricted to a plane. As an exaple one can now plot the
% slowness surfaceses of wave velocities in the plane perpendicular to Y
% with
%
%   plotSection(1./vp,vector3d.Y)
%
% see <AnisotropicTheory.html here> for more information.
%
% *Other new functions*
%
% * <SO3Fun.grad.html odf.grad> computes the gradient of an ODF at some
% orientation
% * <grain2d.hist.html grain2d.hist> can now plot histogram of arbitrary
% properties
% * <SO3Fun.fibreVolume.html  |fibreVolume|> works also for specimen symmetry
% * allow to change the length of the scaleBar in EBSD plots
%
%% MTEX 4.5.2 11/2017
%
% This is mainly a bug fix release
%
% * some more functions get tab completetion for input arguments
% * the option 'MarkerSize' can also be a vector to allow for varying Markersize
% * new option 'noSymmetry' for plotPDF and plotSection
%
% *orientation relation ships*
%
% * new functions for computing variants and parents for a orientation
% relation ship *
% * new predefined orientation relation ship
%
%   gT = GreningerTrojano(csAlpha,csGamma)
%   ori_childs = ori_parent * inv(gT.variants)
%   ori_parents = ori_child * gT.parents
%
%
%% MTEX 4.5.1 08/2017
%
% This is mainly a bug fix release
%
% * some functions get tab completetion for input arguments
% * allow different colormaps in one figure
% * updated interfaces
% * added Levi Civita permutation tensor
% * improved round2Miller
% * grains.boundary('phase2','phase1') rearranges the misorientation to be
% from phase2 to phase 1
%
%% MTEX 4.5 03/2017
%
% *3d orientation plots*
%
% MTEX 4.5 supports plotting of orientations, fibres, and ODFs in 3d in
% various projections like
%
% * Bunge Euler angles
% * Rodrigues Frank space
% * axis angles space
%
% *Misorientations*
%
% * MTEX introduces <orientation.round2Miller.html round2Miller> which
% determines to an arbitrary misorientation |mori| two pairs of lower order
% Miller indeces such that which are aligned by |mori|
%
% * MTEX includes now some of the important misorientation
% relationsships like
%
%   orientation.Bain(cs)
%   orientation.KurdjumovSachs(cs)
%   orientation.NishiyamaWassermann(cs)
%   orientation.Pitch(cs)
%
% *Grain Reconstruction*
%
% New option to handle non convex other shapes of EBSD data sets
%
%   calcGrains(ebsd,'boundary','tight')
%
% * Grain boundary indexing*
% The commands
%   gB('phase1','phase2').misorientation
% returns now always a misorientation from phase1 to phase2
%
% *Tensors*
%
% New functions <tensor.diag.html diag>, <tensor.trace.html trace>,
%
% *EBSD*
%
% Rotating, flipping of EBSD data is now done with respect to the center of
% the map. Previously all these opertions where done relatively to the
% point (0,0). Use
%
%   rotate(ebsd,180*degree,'center',[0,0])
%
% to get back the behavior of previous versions.
%
% *Colorbar*
%
% |MTEXColorbar| allows now to have a title next to it. Use
%
%   mtexColorbar('Title','this is a title')
%
% *Bug Fix*
% This release contains several important bug fixes compare to MTEX 4.4.
%
%% MTEX 4.4   01/2017
%
% *Slip Systems*
%
% MTEX 4.4 introduces support for <SlipSystems.html slip systems>. Slip
% systems are defined by a plane normal and a slip direction
%
%   sSFCC = slipSystem(Miller(0,1,-1,cs,'uvw'),Miller(1,1,1,cs,'hkl'));
%
% Slip systems are instrumental for computating the following properties
%
% * <slipSystem.SchmidFactor.html Schmid factor>
% * <TaylorModel.html Taylor factor>
% * <StrainAnalysis.html Strain transmission through grain boundaries>
%
% *Fibres*
%
% MTEX 4.4 adds support for fibres in orientation space. As an
% example the alpha fibre in cubic materials can be defined in the
% following ways
%
% * as a predefined fibre
%
%   cs = crystalSymmetry('m-3m')
%   f  = fibre.alpha(cs)
%
% * by a pair of directions
%
%   f = fibre(Miller(1,0,0,cs),vector3d.X)
%
% * by two orientations
%
%   ori1 = orientation('Miller',[0 0 1],[1 1 0],cs);
%   ori2 = orientation('Miller',[1 1 1],[1 1 0],cs);
%
%   f = fibre(ori1,ori2)
%
% * by a list of orientations
%
%   f = fibre.fit([ori1,ori2,mean(ori1,ori2)])
%
% All commands that took a pair of directions to specify a fibre, e.g.,
% <fibreODF.html fibreODF>, <SO3Fun.fibreVolume.html fibreVolume>,
% <SO3Fun.plotFibre.html plotFibre> have been rewritten to accept a fibre as a
% single input argument. I.e. a fibre ODF is now defined by
%
%   odf = fibreODF(fibre.alpha(cs))
%
% Up to now the following functions are implemented for fibres
%
% * plot to Rodrigues space, Euler space, pole figures, inverse pole
% figures
%
%    oR = fundamentalRegion(cs,cs)
%    f = fibre(oR.V(1),oR.V(2))
%    plot(oR)
%    hold on
%    plot(fibre,'color','r','linewidth',2)
%    hold off
%
% * compute the angle between orientation and fibre
%
%   angle(f,ori)
%
% *Ignore Symmetry*
%
% Many functions support now the flag |noSymmetry|. Among them are |angle|,
% |axis|, |dot|, |cunion|.
%
% *Clustering of orientations*
%
% The new command <orientation.calcCluster.html calcCluster> allows to
% cluster a given set of orientations into a given number of clusters.
%
%   % generate orientation clustered around 5 centers
%   cs = crystalSymmetry('m-3m');
%   center = orientation.rand(5,cs);
%   odf = unimodalODF(center,'halfwidth',5*degree)
%   ori = odf.calcOrientations(3000);
%
%   % find the clusters and its centers
%   [c,centerRec] = cluster(ori,'numCluster',5);
%
%   % visualize result
%   oR = fundamentalRegion(cs);
%   plot(oR)
%
%   hold on
%   plot(ori.project2FundamentalRegion,c)
%   caxis([1,5])
%   plot(center.project2FundamentalRegion,'MarkerSize',10,'MarkerFaceColor','k','MarkerEdgeColor','k')
%   plot(centerRec.project2FundamentalRegion,'MarkerSize',10,'MarkerFaceColor','r','MarkerEdgeColor','k')
%   hold off
%
%% MTEX 4.3.2 07/2016
%
% *Alignment of Miller plots*
%
% You can now specify the alignment of the crystal a-axis or b-axis in
% Miller plots by
%
%   plota2north, plota2east, plota2south, plota2west
%   plotb2north, plotb2east, plotb2south, plotb2west
%
% This might also be specify in <matlab:edit mtex_settings.m
% mtex_settings>.
%
%% MTEX 4.3 - 03/2016
%
% *Alignment of Miller plots*
%
% Starting with MTEX 4.3 plots with respect to the crystal coordinate
% system, i.e., inverse pole figure plots, misorientation axis plot, ipf
% keys, are always aligned such that the b-axis points towards east. This
% follows the convention given in the International Table of
% Crystallography. The alignment can be adjusted using the
% option |xAxisAlignment|
%
%   plot(Miller(1,0,0,cs),'xAxisAlignment',30*degree)
%
% *Plotting vector fields at grain centers or grain boundaries*
%
% There are three new commands
%
% * <EBSD.quiver.html quiver(ebsd,dir)>
% * <grain2d.quiver.html quiver(grains,dir)>
% * <grainBoundary.quiver.html quiver(grains.boundary,dir)>
%
% that allow visualizing directions for EBSD data, grains and at grain
% boundaries. The input argument |dir| should be a list of |vector3d| and
% may represent e.g. slip directions, polarization direction, etc.
%
% *EBSD data in raster format*
%
% Until MTEX 4.2 EBSD data have been always considered as a one-dimensional
% list of data, i.e., the often present structure of a regular grid was
% completely ignored. Starting with MTEX 4.3 EBSD data can be converted in
% a regular grid by
%
%   ebsd = ebsd.gridify
%
% Missing data are represented as NaN in the regular representation.
% Gridified EBSD data may be addressed analogously like matrixes, i.e.,
%
%   ebsd(100,200)
%
% will give pixel 100 in the y-direction and 200 in the x-direction. Analogously.
%
%   ebsd(50:100,:)
%
% will give the stripe if pixels with y coordinate between 50 and 100.
%
% *Orientation gradients and GND*
%
% Gridified EBSD data allows also to compute orientation gradients by
%
%   ebsd.gradientX
%   ebsd.gradientY
%
% as well as an estimate of the geometrically necessary dislocation
% density (GND) using the command <EBSDsquare.calcGND.html calcGND>
%
%   ebsd.calcGND
%
% *Auxilary new functionality*
%
% * grain2d.calcParis - Percentile Average Relative Indented Surface
% * tensor.diag
% * <EBSD.reduce.html reduce> works now also for EBSD data on Hex grids
%
%% MTEX 4.2 - 11/2015
%
% MTEX 4.2 introduces basic functionality for triple junction analysis in
% grain maps.
%
% *Triple points*
%
% Triple points are automatically computed during grain reconstruction and
% can be accessed by
%
%   grains.triplePoints
%   grains.boundary.triplePoints
%
% More details on how to work with triple points can be found
% <TriplePoints.html here>.
%
% *large EBSD data sets*
%
% Analyzing large EBSD data sets may be quite annoying due to memory
% consumption and slow plotting. As a work around MTEX includes a new
% function <EBSD.reduce.html reduce> which allows reducing the data set to
% each n-th pixel, i.e.,
%
%   ebsd_small = reduce(ebsd,2)
%
% contains only 25 percent of the data of the original data set. This
% functionality is assumed to be used for experimenting around with the
% data set and setting up a proper analysis script. The final analysis
% should, if possible, be done with the entire data set.
%
% *New option to ignore symmetry*
%
% When computing the angle between crystal directions, the misorientation
% angle between orientations and the misorientation axis symmetry can be
% ignored with the flag |noSymmetry|
%
%   angle(Miller(1,0,0,cs),Miller(0,1,0,cs),'noSymmetry')
%   angle(mori,'noSymmetry')
%   axis(mori,'noSymmetry')
%
% *Axis distributions in specimen coordinates*
%
% In order to plot axis distributions in specimen coordinates, you can now
% do
%
%   [ori1,ori2] = calcMisorientation(ebsd('phaseName'))
%   plotAxisDistribution(ori1,ori2,'contourf')
%
% or
%
%   ori = ebsd(grains.boundary('indexed').ebsdId).orientations
%   plotAxisDistribution(ori(:,1),ori(:,2),'contourf')
%
% *New option to work around Matlab opengl bug*
%
% In <matlab:edit mtex_settings.m mtex_settings> there is a new option that
% may help to work around the Matlab opengl bug. Switching it of may give
% nicer graphics.
%
%   setMTEXpref('openglBug',true)
%
% *CSL misorientations*
%
% The function <CSL.html CSL> requires now as a mandatory argument the
% crystal symmetry of the phase, i.e.
%
%   CSL(3,crystalSymmetry('m-3m'))
%
% *Grain boundaries*
%
% Grain boundaries segments have a new option |midPoint| which may be used
% for attaching a vector displaying the misorientation axis or some other
% direction.
%
% *More ODF sections*
%
% * phi1
% * Phi
% * gamma
% * omega
%
% Along with the old syntax, there is now a new syntax that allows for more
% fine control of the ODF sections.
%
%   oS = phi2Sections(odf.CS,odf.SS)
%   oS.phi2 = [ 10*degree, 30*degree, 90*degree ];
%
%   plot(odf,oS)
%
% *Ordering of crystal symmetries*
%
% One can now check whether a crystal symmetry |cs1| is a subgroup of
% crystal symmetry |cs2| by
%
%   cs1 <= cs2
%
% Further, the largest proper subgroup of some crystal symmetry |cs| is now
% accessible by
%
%  cs.properSubGroup
%
%% MTEX 4.1 - 09/2015
%
% MTEX 4.1 introduces new possibilities to the analysis of misorientations.
% For the first time, it covers all geometric aspects of misorientations
% between arbitrary crystal symmetries. Furthermore, MTEX 4.1 introduces
% filters to smooth EBSD data.
%
% *Smoothing of EBSD Data*
%
% Smoothing of EBSD data might be necessary if the orientation data are
% corrupted by noise which influences the estimation of orientation
% dependent properties like KAM or GND. The general syntax for smoothing
% EBSD data is
%
%   ebsd = smooth(ebsd)
%
% This applies the spline filter to the orientation data. Beside the spline
% filter, many other filters are available. A general discussion on this
% topic can be found <EBSDDenoising.html here>. To make use of a different
% than the default filter use the syntax
%
%   F = medianFilter
%   F.numNeighbours = 2 % this way options for the filter can be set
%   ebsd = smooth(ebsd,F)
%
% The command smooth can also be used to fill not indexed measurement
% points. This behavior is enabled by the option |fill|
%
%   ebsd = smooth(ebsd,F,'fill')
%
% *Support for antipodal symmetry for misorientations*
%
% When working with boundary misorientations between the same phase one can
% not distinguish between a misorientation |mori| and its inverse
% |inv(mori). Starting with MTEX 4.1 this symmetry is supported for
% misorientations and misorientation distribution functions.
%
%   mori = inv(ori1) * ori2;
%   mori.antipodal = true;
%
%   mdf = calcMDF(odf1,odf2,'antipodal')
%
% Antipodal symmetry effects the asymmetric region in orientation space as
% described below, as well as the distance between misorientations. Boundary
% misorientations between the same phase have set the flag |antipodal| by
% default.
%
% *Asymmetric regions in orientation space*
%
% MTEX 4.1 has now full support of asymmetric regions in orientation space.
% For any combination of crystal symmetries they can be defined by
%
%   oR = fundamentalRegion(cs1,cs2)
%
% and visualized by
%
%   plot(oR)
%
% One can check, whether an orientation is within the fundamental region by
%
%   oR.checkInside(ori)
%
% similarly as for a sphericalRegion. The fundamental region with antipodal
% symmetry is defined by.
%
%   oR = fundamentalRegion(cs1,cs2,'antipodal')
%
% For a fixed rotational angle |omega|, the intersection of the fundamental
% region with the sphere with radius omega gives the fundamental sector for
% the corresponding rotational axes. The axis sector can be computed by
%
%   sR = oR.axisSector(omega)
%
% *Axis and angle distributions*
%
% Thanks to the implementation of the asymmetric region
% |plotAxisDistribution| and |plotAngleDistribution| works in MTEX 4.1 for
% any combination of crystal symmetries.
%
% The following syntax is obsolete
%
%   plotAxisDistribution(grains.boundary('phase1','phase2'))
%   plotAngleDistribution(grains.boundary('phase1','phase2'))
%   plotAngleDistribution(ebsd)
%
% As replacement use the more verbose syntax
%
%   plotAxisDistribution(grains.boundary('phase1','phase2').misorientation)
%   plotAngleDistribution(grains.boundary('phase1','phase2').misorientation)
%
%   mori = calcMisorientation(ebsd('phase1'),ebsd('phase2'))
%   plotAngleDistribution(mori)
%   plotAxisDistribution(mori)
%
% *Rotational axis in specimen coordinates*
%
% It is now possible to compute the misorientation axis between two
% orientations in specimen coordinate system. This is done by
%
%   axis(ori1,ori2)
%
% To do so with random misorientations from an EBSD data set do
%
%   [ori1,ori2] = calcMisorientation(ebsd('phase1'),ebsd('phase2'))
%   plot(axis(ori1,ori2))
%
% *Axis angle plots*
%
% (Mis)Orientation, ODFs, and MDFs can now be plotted in axis angles
% sections. Those plots respect the fundamental sector depending on the
% misorientation angle and for all combinations of crystal symmetries. The
% angle sections are scaled such that they represent the corresponding
% volume in orientation space. This can be switch off as described below
%
%   plotSection(mori,'axisAngle',55*degree)
%   plotSection(mdf,'axisAngle',(15:10:55)*degree)
%   plotSection(mdf,'axisAngle',(15:10:55)*degree,'volumeScaling',false)
%   plotSection(mdf,'axisAngle',(15:10:55)*degree,'antipodal')
%
% *Replace plotODF by a plotSection*
%
% In most cases, you can replace |plotODF| by a|plot|. Only for
% misorientations, the default plot is |scattered|.
%
% *More default settings for EBSD maps and pole figure plots*
%
% * new MTEXpref to show/hide the micronbar in EBSD maps. The default is
% set in |mtex_settings.m| to |on|. The following command switches them
% off.
%
%   setMTEXpref('showMicronBar','off')
%
% * new MTEXpref to show/hide the coordinates in EBSD maps. The default is
% set in |mtex_settings.m| to |off|. The following command switches them
% on.
%
%   setMTEXpref('showCoordinates','off')
%
% * new MTEXpref to display coordinates in pole figure plot. The default is
% set in |mtex_settings.m| to display the directions |X| and |Y|. The
% following command switches it to |RD| and |ND|.
%
%   pfAnnotations = @(varargin) text([vector3d.X,vector3d.Y],{'RD','ND'},...
%    'BackgroundColor','w','tag','axesLabels',varargin{:});
%   setMTEXpref('pfAnnotations',pfAnnotations);
%
% *Other improvements since MTEX 4.0.0*
%
% During the minor revisions of MTEX also several minor improvements have
% been added which are summarized below
%
% * check for inclusions in grains: the following command returns a list of
% true/false depending whether a grain in |grainList| is an inclusion in
% |hostGrain|
%
%   hostGrain.checkInside(grainList)
%
% * allow syntax
%
%   plot(odf,pf.h,'superposition',pf.c)
%
% * allow to show / hide the scale bar by the MTEX menu or by
%
%   [~,mP] = plot(ebsd)
%   mP.micronBar.visible = 'off'
%
% * allow to place labels above/below the marker by
%
%   plot(xvector,'label','RD','textAboveMarker')
%
% * new EBSD interface to ACOM Nanomegas *.ang files
%
% * plot relative to the crystal coordinate system are now always aligned
% such that x points to the east and y points to north
%
% * misorientation axis with respect to crystal and specimen reference
% frame
%
%   a = axis(o1,o2)  % misorientation axis with respect to sample coordinate system
%
%   a = axis(inv(o2)*o1)  % misorientation axis with respect to crystal coordinate system
%
% * new function |intersect| to compute intersections between grain
% boundary segments an a line
%
%   [x,y] = grains.boundary.intersect(xy1,xy2);
%
% * option for plotting angle distributions in percent
%
%   plotAngleDsitribution(mori,'percent')
%
% * reintroduced min/max in pole figure like plot
%
%   plot(pf,'minmax')
%
% * 3d plots of pole figures can now be simultanously rotated
% * you can now restrict an EBSD data set to a line to plot profiles
%
%   ebsd_prof = ebsd.spatialProfile(ebsd,some_line)
%
% * additional syntax to define a list if Miller indices
%
%   h = Miller({1,0,0},{1,1,1},{2,3,4},CS,'uvw')
%
% * interface to Bruker phl files
% * new properties for grainBoundary |gB|
%
%   gB.segmentLength % length of the corresponding connected segment
%   gB.isTwinning(mori,threshold) % check boundary for twinning
%
% * for a crystal symmetry |cs| you can access a, b ,c and reciprocal axes
% by
%
%   cs.Aaxis
%   cs.AaxisRec
%
% * compute KAM with misorientation angle threshold or grain boundary threshold
%
%
%% MTEX 4.0.0 - 10/2014
%
% MTEX 4 is a complete rewrite of the internal class system which was
% required to keep MTEX compatible with upcoming Matlab releases. Note
% that MTEX 3.5 will not work on Matlab versions later than 2014a. As a
% positive side effect, the syntax has been made more consistent and
% powerful. On the bad side MTEX 3.5. code will need some
% adaption to run on MTEX 4. There are two general principles to consider
%
% *Use dot indexing instead of getting and setting methods*
%
% The syntax
%
%   h = get(m,'h')
%   m = set(m,'h',h+1)
%
% is obsolete. |set| and |get| methods are not longer supported by any MTEX
% class. Instead use dot indexing
%
%   h = m.h
%   m.h = h + 1
%
% Note, that this syntax can be nested, i.e., one can write
%
%   ebsd('Forsterite').orientations.angle
%
% to get the rotational angle of all Forsterite orientations, or,
%
%   cs.axes(1).x
%
% to get the x coordinate of the first crystallographic coordinate axis -
% the a-axis. As a nice bonus, you can now use TAB completion to cycle
% through all possible properties and methods of a class.
%
% *Use camelCaseCommands instead of under_score_commands*
%
% Formerly, MTEX used different naming conventions for functions. Starting
% with MTEX 4.0 all function names consisting of several words, have the
% first word spelled with lowercase letters and the consecutive words
% starting with a capital letter. Most notable changes are
%  * |plotPDF|
%  * |plotIPDF|
%  * |plotODF|
%  * |calcError|
%
% *Grain boundaries are now directly accessible*
%
% MTEX 4.0 introduces a new type of variables called |grainBoundary| which
% allows to represent arbitrary grain boundaries and to work with them as
% with grains. The following lines give some examples. Much more is possible.
%
%   % select boundary from specific grains
%   grains.boundary
%
%   % select boundary by phase transition
%   gB = grains.boundary('Forstarite','Enstatite')
%
%   % select boundary by misorientation angle
%   gB(gB.misorientation.angle>100*degree)
%
%   % compute misorientation angle distribution for specific grain boundaries
%   plotAngleDistribution(gB)
%
% *Plotting EBSD, grain, grainBoundary data has different syntax*
%
% The syntax of the plot commands has made more consistent throughout MTEX.
% It is now
%
%   plot(obj,data)
%
% where obj is the object to be plotted, i.e., EBSD data, grains,
% grain boundaries, spherical vectors, pole figures, etc., and the data are
% either pure numbers or RGB values describing the color. Examples are
%
%   % plot MAD values of EBSD data
%   plot(ebsd,ebsd.mad)
%
%   % colorize grains according to area
%   plot(grains,grains.area)
%
%   % colorize grain boundary according to misorientation angle
%   gB = grains.boundary('Forsterite','Enstatite')
%   plot(gB,gB.misorientation.angle)
%
% Colorization according to phase or phase transition is the new default
% when calling |plot| without data argument, i.e., the following results in
% a phase plot
%
%   plot(ebsd)
%
% In order to colorize ebsd data according to orientations, one has first to
% define an orientationMapping by
%
%   oM = ipdfHSVOrientationMapping(ebsd('Forsterite'))
%
% Then one can use the command |oM.orientation2color| to compute RGB values
% for the orientations
%
%   plot(ebsd('Forsterite'),oM.orientation2color(ebsd('Forsterite').orientations))
%
% The orientation mapping can be visualized by
%
%   plot(oM)
%
% *EBSD data are always spatially indexed*
%
% Starting with MTEX 4.0 EBSD data always have to have x and y coordinates.
% EBSD data without spatial coordinates are imported simply as orientations.
% As a consequence, all orientation related functionalities of EBSD data
% have been moved to |orientations|, i.e., you can not do anymore
%
%   plotpdf(ebsd('Fo'),Miller(1,0,0,CS))
%   calcODF(ebsd('Fo'))
%   volume((ebsd('Fo'))
%
% But instead you have to explicitly state that you operate on the
% orientations, i.e.
%
%   plotpdf(ebsd('Fo').orientations,Miller(1,0,0,ebsd('Fo').CS))
%   calcODF(ebsd('Fo').orientations)
%   volume((ebsd('Fo').orientations)
%
% This makes it more easy to apply the same functions to misorientations
% to grain mean orientations |grains.meanOrientation|, ebsd misorientation
% to mean |mean |ebsd.mis2mean| or boundary misorientations
% |grains.boundary.misorientation|
%
% *Different syntax for reconstructing grains from EBSD data*
%
% In MTEX 3.5 the command
%
%   grains = calcGrains(ebsd)
%
% duplicates the ebsd data into the grain variable allowing to access the
% EBSD data belonging to a specific grain by
%
%   get(grains(1),'EBSD')
%
% In MTEX 4.0 the command |calcGrains| returns as an additional output the
% list of grainIds that is associated with the EBSD data. When storing
% these grainIds directly inside the EBSD data, i.e., by
%
%   [grains,ebsd.grainId] calcGrains(ebsd)
%
% one can access the EBSD data belonging to a specific grain by the command
%
%   ebsd(grains(1))
%
% *MTEX 4.0 distinguishes between crystal and specimen symmetry*
%
% In MTEX 4.0 two new variable types |specimenSymmetry| and
% |crystalSymmetry| have been introduced to distinguish clearly between
% these two types of symmetry. Calling
%
%   cs = symmetry('m-3m')
%   ss = symmetry('triclinic')
%
% is not allowed anymore! Please use instead
%
%   cs = crystalSymmetry('m-3m','mineral','phaseName')
%   ss = specimenSymmetry('triclinic')
%
% *Pole figure indexing is now analogously to EBSD data*
%
% You can now index pole figure data by conditions in the same manner as
% EBSD data. E.g. the condition
%
%   condition = pf.r.theta < 80 * degree
%
% is an index to all pole figure data with a polar angle smaller than 80
% degree. To restrict the pole figure variable |pf| to the data write
%
%   pf_restrcited = pf(condition)
%
% In the same manner, we can also remove all negative intensities
%
%   condition = pf.intensities < 0
%   pf(condition) = []
%
% In order to address individual pole figures within a array of pole
% figures |pf| use the syntax
%
%   pf('111')
%
% or
%
%   pf(Miller(1,1,1,cs))
%
% The old syntax
%
%   pf(1)
%
% for accessing the first pole figure will not work anymore as it now refers to
% the first pole figure measurement. The direct replacement for the above
% command is
%
%   pf({1})
%
% *MTEX 4.0 supports all 32 point groups*
%
% In MTEX 4.0 it is for the first time possible to calculate with
% reflections and inversions. As a consequence, all 32 point groups are
% supported. This is particularly important when working with
% piezoelectric tensors and symmetries like 4mm. Moreover, MTEX
% distinguishes between the point groups 112, 121, 112 up to -3m1 and -31m.
%
% Care should be taken, when using non-Laue groups for pole figure or EBSD
% data.
%
% *Support for three-digit notation for Miller indices of trigonal
% symmetries*
%
% MTEX 4.0 understands now uvw and UVTW notation for trigonal symmetries.
% The following two commands define the same crystallographic direction,
% namely the a1-axis
%
%   Miller(1,0,0,crystalSymmetry('-3m'),'uvw')
%
%   Miller(2,-1,-1,0,crystalSymmetry('-3m'),'UVTW')
%
% *Improved graphics*
%
% MTEX can now display colorbars next to pole figure, tensor or ODF plots
% and offers much more powerful options to customize the plots with titles,
% legends, etc.
%
% *Functionality that has been (temporarily) removed*
%
% This can be seen as a todo list.
%
% * 3d EBSD data handling + 3d grains
% * some grain functions like aspectRatio, equivalent diameter
% * logarithmic scaling of plots
% * 3d plot of ODFs
% * some of the orientation color maps
% * fibreVolume in the presence of specimen symmetry
% * Dirichlet kernel
% * patala colorcoding for some symmetry groups
% * v.x = 0
% * misorientation analysis is not yet complete
% * some colormaps, e.g. blue2red switched
% * histogram of volume fractions of CSL boundaries
% * remove id from EBSD?
% * changing the phase of a grain should change phases in the boundary
% * KAM and GOSS may be improved
% * write import wizard for orientations, vectors, tensors.
%
%% MTEX 3.5.0 - 12/2013
%
% *Misorientation colorcoding*
%
% * Patala colormap for misorientations
% * publication:  S. Patala, J. K. Mason, and C. A. Schuh, Improved
% representations of misorientation information for grain boundary,
% science, and engineering, Prog. Mater. Sci., vol. 57, no. 8, pp. 1383-1425, 2012.
% * implementation: Oliver Johnson
% * syntax:
%
%   plotBoundary(grains('Fo'),'property','misorientation','colorcoding','patala')
%
% *Fast multiscale clustering (FMC) method for grain reconstruction*
%
% * grain reconstruction algorithm for highly deformed materials without
% sharp grain boundaries
% * publication: C. McMahon, B. Soe, A. Loeb, A. Vemulkar, M. Ferry,
% L. Bassman, Boundary identification in EBSD data with a generalization of
% fast multiscale clustering, Ultramicroscopy, 2013, 133:16-25.
% * implementation: Andrew Loeb
% * syntax:
%
%   grains = calcGrains(ebsd,'FMC')
%
% *Misc changes*
%
% * one can now access the grain id by
%
%   get(grains,'id')
%
% * the flags |'north'| and |'south'| are obsolete and have been replaced
% by |'upper'| and |'lower'|
% * you can specify the outer boundary for grain reconstruction in
% non-convex EBSD data set by the option |'boundary'|
%
%   poly = [ [x1,y1];[x2,y2];[xn,yn];[x1,y1] ]
%   grains = calcGrains(ebsd,'boundary',poly)
%
% * you can select a polygon interactively with the mouse using the command
%
%   poly = selectPolygon
%
% *Bug fixes*
%
% * .osc, .rw1 interfaces improved
% * .ang, .ctf interfaces give a warning if called without one of the
% options |convertSpatial2EulerReferenceFrame| or
% |convertEuler2SpatialReferenceFrame|
% * fixed: entropy should never be imaginary
% * removed function |SO3Grid/union|
% * improved MTEX startup
% * many other bug fixes
% * MTEX-3.5.0 should be compatible with Matlab 2008a
%
%% MTEX 3.4.2 - 06/2013
%
% *bugfix release*
%
% * fixed some inverse pole figure color codings
% * option south is working again in pole figure plots
% * geometric mean in tensor averagin, thanks to Julian Mecklenburgh
% * improved support of osc EBSD format
% * tensor symmetry check error can be turned of and has a more detailed
% error message
% * improved syntax for Miller
%   Miller(x,y,z,'xyz',CS)
%   Miller('polar',theta,rho,CS)
% * ensure same marker size in EBSD pole figure plots
% * allow plotting Schmid factor for grains and EBSD data
% * allow to annotate Miller to AxisDistribution plots
% * improved figure export
% * allow for negative phase indices in EBSD data
% * bug fix: https://code.google.com/p/mtex/issues/detail?id=115
% * improved ODF fibre plot
%
%% MTEX 3.4.1 - 04/2013
%
% *bugfix release*
%
% * much improved graphics export to png and jpg files
% * improved import wizard
% * Miller(2,0,0) is now different from Miller(1,0,0)
% * new EBSD interfaces h5, Bruker, Dream3d
% * various speedups
% * fix: startup error http://code.google.com/p/mtex/issues/detail?id=99
% * fix: Rigaku csv interface
%
%% MTEX 3.4.0 - 03/2013
%
% *New plotting engine*
%
% MTEX 3.4 features a completely rewritten plotting engine. New features
% include
%
% * The alignment of the axes in the plot is now described by the options
% |xAxisDirection| which can be |north|, |west|, |south|, or |east|, and
% |zAxisDirection| which can be |outOfPlane| or |intoPlane|. Accordingly,
% there are now the commands
%
%   plotzOutOfPlane, plotzIntoPlane
%
% * The alignment of the axes can be changed interactively using the new
% MTEX menu which is located in the menubar of each figure.
% * northern and southern hemisphere are now separate axes that can be
% stacked arbitrarily and are marked as north and south.
% * Arbitrary plots can be combined in one figure. The syntax is
%
%   ax = subplot(2,2,1)
%   plot(ax,xvector)
%
% * One can now arbitrarily switch between scatter, contour and smooth
% plots for any data. E.g. instead of a scatter plot the following command
% generates now a filled contour plot
%
%   plotpdf(ebsd,Miller(1,0,0),'contourf')
%
% * obsolete options: |fliplr|, |flipud|, |gray|,
%
% *Colormap handling*
%
% * User defined colormap can now be stored in the folder |colormaps|, e.g.
% as |red2blueColorMap.m| and can set interactively from the MTEX menu or
% by the command
%
%   mtexColorMap red2blue
%
% *ODF*
%
% * The default ODF plot is now phi2 sections with plain projection and (0,0)
% being at the top left corner. This can be changed interactively in the
% new MTEX menu.
% * The computation of more than one maximum is back. Use the command
%
%   [modes, values] = calcModes(odf,n)
%
% *EBSD data*
%
% * MTEX is now aware about the inconsistent coordinate system used in CTF and
% HKL EBSD files for Euler angles and spatial coordinates. The user can now
% convert either the spatial coordinates or the Euler angles such that they
% become consistent. This can be easily done by the import wizard or via
% the commands
%
%   % convert spatial coordinates to Euler angle coordinate system
%   loadEBSD('filename','convertSpatial2EulerReferenceFrame')
%
%   % convert Euler angles to spatial coordinate system
%   loadEBSD('filename','convertEuler2SpatialReferenceFrame')
%
% * It is now possible to store a color within the variable describing a
%  certain mineral. This makes phase plots of EBSD data and grains more
%  consistent and customizable.
%
%   CS = symmetry('cubic','mineral','Mg','color','red')
%
% * A better rule of thumb for the kernel width when computing an ODF from
% individual orientations via kernel density estimation.
% * inpolygon can be called as
%
%   inpolygon(ebsd,[xmin ymin xmax ymax])
%
% *Tensors*
%
% * new command to compute the Schmid tensor
%
%   R = SchmidTensor(m,n)
%
% * new command to compute Schmid factor and active slip system
%
%   [tauMax,mActive,nActive,tau,ind] = calcShearStress(stressTensor,m,n,'symmetrise')
%
% * it is now possible to define a tensor only by its relevant entries.
% Missing entries are filled such that the symmetry properties are
% satisfied.
%
% * faster, more stable tensor implementation
% * new syntax in tensor indexing to be compatible with other MTEX classes.
% For a 4 rank thensor |C|, we have now
%
%   % extract entry 1,1,1,1 in tensor notation
%   C{1,1,1,1}
%
%   % extract entry 1,1 in Voigt notation
%   C{1,1}
%
% * For a list of tensors |C| we have
%
%   % extract the first tensor
%   C(1)
%
% *Import / Export*
%
% * command to export orientations
%
%   export(ori,'fname')
%
% * command to import vector3d
%
%   v = loadVector3d('fname','ColumnNames',{'x','y','z'})
%   v = loadVector3d('fname','ColumnNames',{'latitude','longitude'})
%
% * new interface for DRex
% * new interface for Rigaku
% * new interface for Saclay
%
% *General*
%
% * improved instalation / uninstalation
% * new setting system
%
%   setpref('mtex','propertyName','propertyValue')
%
% has been replaced by
%
%   setMTEXpref('propertyName','propertyValue')
%
%
%% MTEX 3.3.2 - 01/2013
%
% *bugfix release*
%
% * fix: better startup when using different MTEX versions
% * fix: backport of the tensor fixes from MTEX 3.4
% * fix: show normal colorbar in ebsd plot if scalar property is plotted
% * fix: http://code.google.com/p/mtex/issues/detail?id=82
% * fix: http://code.google.com/p/mtex/issues/detail?id=76
% * fix: http://code.google.com/p/mtex/issues/detail?id=48
% * fix: http://code.google.com/p/mtex/issues/detail?id=71
% * fix: http://code.google.com/p/mtex/issues/detail?id=70
% * fix: http://code.google.com/p/mtex/issues/detail?id=69
% * fix: http://code.google.com/p/mtex/issues/detail?id=65
% * fix: http://code.google.com/p/mtex/issues/detail?id=68
%
%% MTEX 3.3.1 - 07/2012
%
% *bugfix release*
%
% * fix: single/double convention get sometimes wrong with tensors
% * fix: tensor checks did not respect rounding errors
% * fix: ingorePhase default is now none
% * fix: calcAngleDistribution works with ODF option
% * fix: respect rounding errors when importing pole figures and ODFs
%
%% MTEX 3.3.0 - 06/2012
%
% *Grains: change of internal representation*
%
% Reimplementation of the whole *grain* part:
%
% * The classes @grain, @polygon, @polyeder do not exist any longer. The
% functionality of the classes is mainly replaced by the classes @GrainSet,
% @Grain2d and @Grain3d
% * The class @GrainSet explicitly stores @EBSD. To access @EBSD data
% within a single grain or a set of grains use
%
%   get(grains,'EBSD')
%
% * the grain selector tool for spatial grain plots was removed,
% nevertheless, grains still can be <SelectingGrains.html selected
% spatially>.
% * scripts using the old grain engine may not work properly, for more
% details of the functionalities and functioning of the @GrainSet please
% see the documentation.
% * new functionalities: merge grains with certain boundary.
%
% *EBSD*
%
% The behavior of the |'ignorePhase'| changed. Now it is called in general
% |'not indexed'| and the not indexed data <EBSDImport.html is imported
% generally>. If the crystal symmetry of an @EBSD phase is set to a string
% value, it will be treated as not indexed. e.g. mark the first phase as
% |'not indexed'|
%
%   CS = {'not indexed',...
%         symmetry('cubic','mineral','Fe'),...
%         symmetry('cubic','mineral','Mg')};
%
% By default, |calcGrains| does also use the |'not Indexed'| phase.
%
% * create customized orientation colormaps
%
% *Other*
%
% * the comand |set_mtex_option| is obsolete. Use the matlab command
% |setMTEXpref(...)| instead. Additionally, one can now see all options
% by the command |getpref('mtex')|
%
%% MTEX 3.2.3 - 03/2012
%
% *bugfix release*
%
% * allow zooming for multiplot objects again; change the z-order of axes
% * symmetries allows now options a | | x additional to x | | a
% * fix http://code.google.com/p/mtex/issues/detail?id=35
% * fix http://code.google.com/p/mtex/issues/detail?id=38
% * fix http://code.google.com/p/mtex/issues/detail?id=28
% * fix export odf
%
%% MTEX 3.2.1 - 11/2011
%
% *New Features*
%
% * Import and Export to VPSC
% * export EBSD data with all properties
% * improved ODF calculation from pole figures by using quadrature weights
% for the pole figure grid
% * implemented spherical Voronoi decomposition and computation of
% spherical quadrature weights
% * plot odf-space in omega-sections, the i.e. generalization of sigma-sections
%
% *Bug Fixes*
%
% * S2Grid behaves more like vector3d
% * vector3d/eq takes antipodal symmetry into account
% * Euler angle conversion was sometimes wrong
% * tensors multiplication was sometimes wrong
% * rank 3 tensors get options 'doubleConvention' and 'singleConvention'
% for the conversion into the Voigt matrix representation
% * documentation fixes
% * Miller('[100]') gives not the correct result
% * import wizard now generates correct CS definition
% * import filter for uxd files should now work more reliable
%
%% MTEX 3.2 - 05/2011
%
% *3d EBSD Analysis*
%
% This release for the first time supports 3d EBSD data. In particular,
% MTEX is now able to
%
% * import 3d EBSD data from stacked files
% * visualize 3d EBSD data by plotting interactive slices through the
% specimen
% * 3d grain detection
% * the topology of 3d grains, i.e. boundaries, neighboring grains, etc.
%
% *Misorientation Analysis*
%
% * computation of the uncorrelated misorientation distribution (MDF) for
% one or two ODFs
% * computation of the theoretical angle distribution of an ODF or MDF
% * computation of the misorientation to mean for EBSD data
%
% *New Syntax for EBSD and grain variables*
%
% EBSD and grain variables can now be indexed by phase, region or grain /
% ebsd variables. Let us assume we have a two phase ebsd variable
% containing 'Fe' and 'Mg' then can restrict our dataset to the Fe - phase
% only by writing
%
%  ebsd('Fe')
%
% The same works with grains and also with more than one phase. Please have
% a look into the documentation for information how to index ebsd and grain
% variables.
%
% Accordingly the following syntax is now depreciated.
%
%  calcODF(ebsd,'phase',2)
%
% It should be replaced by
%
%  calcODF(ebsd('Fe'))
%
%
% *Other Enhangments*
%
% * better import and export of pole figures, odfs and EBSD data
% * automatic centering of a specimen with respect to its specimen symmetry
% * download and import tensors from http://www.materialproperties.org/
% * new interfaces for Rigaku, Siemens, Bruker and many other X-ray devices
% and formats
% * support for rank three tensors, i.e, for piezo electricity tensors
% * improved documentation
% * many bug fixes
%
%% MTEX 3.1 - 03/2011
%
% *Tensor Arithmetics* This release introduces tensor analysis into MTEX,
% this includes
%
% * import of tensors via the import wizard
% * basic tensor operations: multiplication, rotation, inversion
% * advanced visualization
% * computation of averaged tensors from EBSD data and ODFs
% * computation of standard elasticity tensors like: Youngs modulus, linear
% compressibility, Christoffel tensor, elastic wave velocities
%
% *Other Enhancements*
%
% * support for different crystal reference frame conventions
% * automatic conversion between different reference frames
% * definition of crystal directions in direct and reciprocal space
% * more predefines orientations: Cube, CubeND22, CubeND45, CubeRD, Goss,
% Copper, SR, Brass, PLage, QLage, ...
% * improved EBSD and grain plots
% * new and improved interfaces
% * many bug fixes
%
%
%% MTEX 3.0 - 10/2010
%
% *Crystal Geometry*
%
% This release contains a completely redesigned crystal geometry engine
% which is thought to be much more intuitive and flexible. In particular,
% it introduces two new classes <rotation.rotation.html rotation> and
% <orientation.orientation.html orientation> which make it much easier to
% work with crystal orientations. Resulting features are
%
% * no more need for quaternions
% * support for Bunge, Roe, Matthies, Kocks, and Canova Euler angle
% convention
% * a simple definition of fibres
% * simply check whether two orientations are symmetrically equivalent
%
% *Other Enhancements*
%
% * automatic kernel selection in ODF estimation from EBSD data
% * support for Bingham model ODFs
% * estimation of Bingham parameters from EBSD data
% * faster and more accurate EBSD simulation
% * faster grain reconstruction
% * improved documentation
% * improved output
% * MTEX is now compatible with NFFT 3.1.3
%
%
%% MTEX 2.0 - 10/2009
%
% *Grain Analysis for EBSD Data*
%
% MTEX is now able to partition spatial EBSD data into grains. This allows
% for the computation of various grain characteristics, as well as the
% computation and visualization of the grain boundaries and neighborhood
% relationships. Main features are:
%
% * Grains statistics (area, diameter, mean orientation, ...)
% * Missorientation analysis
% * Interactive selection of grains by various criteria
% * ODF-calculations for any subset of grains
% * A large palette of plotting possibilities.
%
% *Visualization Improvements*
%
% * ODF fibre plot
% * support for different x-axis alignment - <plotx2north.html
% plotx2north>, <plotx2east.html plotx2east>
% * plot EBSD data with respect to arbitrary properties
% * plot zero regions of ODFs and pole figures white
% * pole figure contour plots
% * color triangle for spatial EBSD plots
%
% *General Improvements*
%
% * ODF import / export
% * rotate EBSD data
% * Pole figure normalization
% * improved interfaces and import wizard
% * speed improvement of several side-functions as well as core-functions
% of @quaternions and spherical grids.
%
% *Incompatible Changes to Previous Versions*
%
% * The flags *reduced* and *axial* have been replaced by the flag
% <VectorsAxes.html antipodal>
%
%% MTEX 1.2 - 05/2009
%
% *Improved EBSD import*
%
% * import-weighted EBSD (e.g. from odf modeling)
% * new HKL and Chanel interfaces (.ang and .ctf files)
% * import of multiple phases
% * import of arbitrary properties as MAD, detection error, etc.
%
% *Improved EBSD plotting*
%
% * plot EBSD data in axis angle and Rodrigues space
% * annotations in these spaces
% * plot arbitrary properties as MAD, detection error, etc.
% * better orientation colorcoding
% * superpose odf, pole figure and EBSD plots
% * better interpolation
%
% *General Improvements*
%
% * support for different crystal geometry setups
% * faster and more accurate volume computation
% * improved function modalorientation
% * improved documentation
%
% *Incompatible Changes to Previous Versions*
%
% * The flag *reduced* has been replaced by the flag <VectorsAxes.html
% axial>
%
%% MTEX 1.1 - 12/2008
%
% *Improved Import Wizzard*
%
% * Load CIF files to specify crystal geometry
% * Import EBSD data with coordinates
% * More options to specify the alignment of the specimen coordinate system
% * support for popla *.epf files, *.plf files, and *.nja files
%
%
% *Improved Pole Figure Analysis*
%
% * Background correction and defocusing
% * Outlier detection and elimination
%
% *Improved EBSD Data Support*
%
% * Spatial plot of EBSD data
% * Modify EBSD data in the same way as pole figures
%
% *Improved Plotting*
%
% * GUI to modify plots more easily
% * Annotate orientations into pole figure plots
% * Annotate orientations into ODF sections
% * Coordinate systems for ODF and pole figure plots
% * More flexible and consistent option system
% * Default plotting options like FontSize, Margin, ...
% * Speed improvements
%
% *Bug Fixes*
%
% * ModalOrientation works now much better
% * Plot (0,0) coordinate in ODF plot at upper left
% * Fixed a bug in ODF estimation from EBSD data
%
%
%% MTEX 1.0 - 06/2008
%
% *New Installer Including Binaries for Windows, Linux, and Max OSX*
%
% * MTEX ships now with an automated installer and binaries for Windows,
% Linux, and Mac OSX. This makes it in unnecessary to install any
% additional library and to compile the toolbox. (Thanks to F. Bachmann, C.
% Randau, and F. Wobbe)
%
% *New ODF Class*
%
% * The new function <FourierODF.html |FourierODF|> provides an easy way to
% define ODFs via their Fourier coefficients. In particular, MTEX allows now
% to calculate with those ODFs in the same manner as with any other ODFs.
%
% *New Interfaces*
%
% * New PoleFigure interface for xrdml data (F. Bachmann)
%
% *Improved Plotting*
%
% * Plot EBSD data and continuous ODFs into one plot
% * Miller indices and specimen directions can now be plotted directly into
% pole figures or inverse pole figures.
% * New plotting option north, south for spherical plots
% * Improved colorbar handling
% * Spherical grids
% * More spherical projections
%
% *Incompatible Changes With Previous Releases*
%
% * The flag *hemisphere* in <S2Grid.S2Grid.html S2Grid> has been replaced
% by *north*, *south*, and *antipodal* making it more consistent with the
% plotting routine.
%
% *Improved Documentation*
%
% MTEX comes now with over 500 help pages explaining the mathematical
% concepts, the philosophy behind MTEX and the syntax and usage of all 300
% functions available in MTEX. Furthermore, you find numerous examples and
% tutorials on ODF estimation, data import, calculation of texture
% characteristics, ODF and pole figure plotting, etc.
%
% *Bug Fixes*
%
% * Fixed zero range method
% * Fixed automatic ghost correction
% * Fixed some loadPoleFigure issues
% * Many other bug fixes.
%
%
%% MTEX 0.4 - 04/2008
%
% *Speed Improvements*
%
% * ODF reconstruction and PDF calculation are about *10 times faster* now
% (thanks to the new NFFT 4.0 library)
% * ODF plotting and the calculation of <SO3Fun.volume.html volume
% fractions>, the <textureindex.html texture index>, the
% <SO3Fun.entropy.html |entropy|> and <SO3Fun.calcFourier.html Fourier
% coefficients> is about *100 times faster*
%
% *New Support of EBSD Data Analysis*
%
% * Import EBSD data from arbitrary data formats.
% * New class <EBSD.EBSD.html EBSD> to store and manipulate with EBSD
% data.
% * Plot pole figures and inverse pole figures from EBSD data.
% * Recover ODFs from EBSD data via kernel density
% estimation.
% * Estimate Fourier coefficients from EBSD data.
% * Simulate EBSD data from ODFs.
% * Export EBSD data.
%
% *New Functions*
%
% * |fibreVolume| calculates the
% volume fraction within a fibre.
% * |plotSpektra| plots the Fourier coefficients of an ODF.
% * |setcolorrange| and the plotting option *colorrange* allow for
% consistent color coding for arbitrary plots.
% * A *colorbar* can be added to any plots.
% * |mat2quat| and |quat2mat| convert rotation matrices to quaternions and
% vice versa.
%
% *Incompatible Changes With Previous Releases*
%
% * New, more flexible syntax for the generation of S2Grids
% * Slightly changed the syntax of |unimodalODF| and |fibreODF|.
% * Default plotting options are set to {}, i.e. 'antipodal' has to add
% manually if desired
% * Crystal symmetry *triclinic* is not called *tricline* anymore.
%
%
%% MTEX 0.3 - 10/2007
%
% * new function |fourier| to calculate the
% Fourier coefficents of an arbitrary ODF
% * new option |ghost correction| in function
% <PoleFigure.calcODF.html calcODF>
% * new option |zero range| in function <PoleFigure.calcODF.html calcODF>
% * new function <EBSD.load.html loadEBSD> to import EBSD data
% * simplified syntax for the import of diffraction data
% * new import wizard for pole figure data
% * support of triclinic crystal <symmetry.symmetry.html symmetry> with
% arbitrary angles between the axes
% * default plotting options may now be specified in mtex_settings.m
% * new plot option _3d_ for a three-dimensional spherical plot of pole
% figures
% * contour levels may be specified explicitly in all plot functions
% plotodf, plotpdf and plotipdf
% * new plot option _logarithmic_
% * many bugfixes
%
%
%% MTEX 0.2 - 07/2007
%
% * new functions <textureindex.html texture index>, <SO3Fun.entropy.html
% entropy>, <SO3Fun.volume.html volume>
% * greatly improved help
% * improved installation
% * new options for plotting routines for specific ODF sections
% * many bugfixes
%
%
%% MTEX 0.1 - 03/2007
%
% * initial release
%