Pyroelectric coefficients were measured from a series of natural tourm
aline crystals between similar to 170 and similar to 500 K to quantify
the variation of the pyroelectric effect with chemical composition. T
he amount of Fe in tourmaline has a prominent influence on the pyroele
ctricity. Fe content linearly decreases the pyroelectric coefficient i
n the composition range between 0.01(1) and 14.6(2) wt% FeO. Thus, to
a first approximation, tourmaline pyroelectric coefficients may be pre
dicted directly from the chemical composition derived by routine elect
ron probe microanalysis. The relationships between pyroelectricity and
chemistry indicate that the pyroelectric coefficient is influenced to
different extents by the occupancies of the X, Y, and Z cation sites
in the tourmaline structure. The octahedral Y site occupancy strongly
influences the pyroelectric coefficient due to the preference of Fe fo
r this site. This work further suggests that the addition of Fe and Mg
cations to the smaller Z octahedral site causes the pyroelectric coef
ficient to increase. However, because an extended suite of samples is
not available in which the Z site contains ions other than Al, this pr
oposed trend has not been experimentally determined. The chemistry of
the ninefold coordinated X site and the population of this site do not
influence the pyroelectric coefficients of tourmaline.