The Piezoelectricity Tensor edit page

In this chapter we discuss how to compute and visualize piezoellectirc properties. At first, let us import some piezoelectric contents for a quartz specimen.

CS = crystalSymmetry('32', [4.916 4.916 5.4054], 'X||a*', 'Z||c', 'mineral', 'Quartz');

fname = fullfile(mtexDataPath,'tensor', 'Single_RH_quartz_poly.P');

P = tensor.load(fname,CS,'propertyname','piecoelectricity','unit','C/N','DoubleConvention')
P = tensor (Quartz)
  propertyname    : piecoelectricity
  unit            : C/N             
  rank            : 3 (3 x 3 x 3)   
  doubleConvention: true            
 
  tensor in compact matrix form:
     0     0     0 -0.67     0   4.6
   2.3  -2.3     0     0  0.67     0
     0     0     0     0     0     0

Plotting the magnitude surface

The default plot of the magnitude, which indicates, in which direction we have the most polarization. By default, we restrict ourselves to the unique region implied by crystal symmetry

% set some colormap well suited for tensor visualisation
setMTEXpref('defaultColorMap',blue2redColorMap);

plot(P)
mtexColorbar

but also, we can plot the whole crystal behavior

close all
plot(P,'complete','smooth','upper')
mtexColorbar

Most often, the polarization is illustrated as surface magnitude

close all
surf(P.directionalMagnitude)

Note, that for directions of negative polarization the surface is mapped onto the axis of positive, which then let the surface appear as a double coverage

Quite a famous example in various standard literature is a section through the surface because it can easily be described as an analytical solution. We just specify the plane normal vector

plotSection(P.directionalMagnitude,vector3d.Z)
xlabel('x')
ylabel('y')
drawNow(gcm)

so we are plotting the polarization in the xy-plane, or the yz-plane with

plotSection(P.directionalMagnitude,vector3d.X)
ylabel('y')
zlabel('z')
drawNow(gcm)

Mean Tensor Calculation

Let us import some data, which was originally published by Mainprice, D., Lloyd, G.E. and Casey , M. (1993) Individual orientation measurements in quartz polycrystals: advantages and limitations for texture and petrophysical property determinations. J. of Structural Geology, 15, pp.1169-1187

fname = fullfile(mtexDataPath,'orientation', 'Tongue_Quartzite_Bunge_Euler');

ori = orientation.load(fname,CS, 'ColumnNames', {'Euler 1' 'Euler 2' 'Euler 3'})
ori = orientation (Quartz → y↑→x)
  size: 382 x 1

The figure on p.1184 of the publication

Pm = ori.calcTensor(P)

plot(Pm)
mtexColorbar
Pm = tensor (y↑→x)
  propertyname    : piecoelectricity
  unit            : C/N             
  rank            : 3 (3 x 3 x 3)   
  doubleConvention: true            
 
  tensor in compact matrix form: *10^-2
 -10.48   34.2 -23.72 -32.75 -64.24 -26.18
 -18.02  -3.15  21.17  62.42  29.67  44.39
 -41.35  40.44   0.91  32.48 -23.42   6.47
close all
plot(Pm)
mtexColorbar

setMTEXpref('defaultColorMap',WhiteJetColorMap)