The structural properties of katoite, Ca3Al2(O4H4)(3), are investigated as
a function of applied pressure. The calculated structure at ambient pressur
e, the bulk modulus and its pressure derivative are in good agreement with
the available experimental data. The strength of the hydrogen bond increase
s under pressure, accompanied by a lengthening of the O-H bonds. This concl
usion agrees with experimental spectroscopic data and casts serious doubts
on the reliability of neutron diffraction results that predict strong compr
ession of the O-H bonds. Calculations for Mg3Al2(O4H4)(3) have been used to
predict the structure and relative stability of the hypothetical hydropyro
pe.