A report
is given of the first detailed investigation of the relation
of structure to the germanate anomaly in alkaline earth germanate
glasses. Pulsed neutron diffraction and high-energy X-ray diffraction
measurements on calcium germanate glasses (22 to 41 mol % CaO, roller-quenched)
show that the average Ge–O coordination number, n
GeO, and average bond length, r
GeO, exhibit broad maxima at ∼28 mol % CaO. Maxima in the mass
density, atom number density, and glass-transition temperature also
occur at a similar composition and are characteristic of the germanate
anomaly. The anomalies occur at a higher modifier oxide content for
alkaline earth (Ae) germanate glasses than for alkali (A) germanate
glasses, attributed to the higher bond strengths within Ae-O polyhedra
compared to those in A-O polyhedra. Consequently, the stabilization
of [GeO6] octahedra and/or bridges between higher-coordinated
[GeO
m
] units (m = 5,
6) is a feature of AeO–GeO2 glasses, in contrast
to the existence of only [GeO4] tetrahedra and [GeO5] units proposed in alkali (Cs) germanate glasses. At high
CaO content, n
GeO behaves as in thallium
germanate glasses because of the very similar metal–oxygen
bond strengths within [CaO7] polyhedra and [TlO3] units. The composition dependence of the atom number density at
low modifier content follows a common trend for Ca, Sr, and Ba germanate
glasses because modifier cations fill germanate network cages. Our
results show that the germanate anomaly for calcium germanate glasses
is related to both a packing effect and a structural change in the
germanate network; there is not a simple dichotomy whereby only one
of these factors is of significance for the germanate anomaly.