“…For a given cation, exchange of the anions yields different crystal structures with different densities, e.g., SrC 2 O 4 ·H 2 O, SrCO 3 , and SrSO 4 have densities of 2.85, 3.78, and 3.95 g cm −3 , respectively. Sulphates (with the exception of gypsum), generally have higher densities for their respective cations (CaSO 4 ·2H 2 O, SrSO 4 , and BaSO 4 ρ = 2.32, 3.95, and 4.48 g cm −3 ), followed by carbonates (CaCO 3 , SrCO 3 , and BaCO 3 ρ = 2.71, 3.78, and 4.3 g cm −3 ) and finally oxalates (CaC 2 O 4 ·H 2 O, SrC 2 O 4 ·H 2 O, and BaC 2 O 4 ·0.5H 2 O ρ = 2.21, 2.85 45 , and 3.45 46 g cm −3 ). The relative RTP intensities follow this pattern, where they increase exponentially with density until a threshold (100%) relative RTP intensity is attained (Fig.…”