Considering again the same isostructural compounds ( Figure 3 c), divided this time according to the nature of the A cation (A = K, Rb, Cs, Sr, Ba), one sees a negative trend between the a and c lattice parameters, with almost parallel slopes between the different classes.
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Report of the Double-Molybdate Phase Cs<sub>2</sub>Ba(MoO<sub>4</sub>)<sub>2</sub> with a Palmierite Structure and Its Thermodynamic Characterization.
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