1997
DOI: 10.1006/jcht.1997.0195
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The thermodynamics of aqueous trivalent rare earth elements. Apparent molar heat capacities and volumes of Nd(ClO4)3(aq), Eu(ClO4)3(aq), Er(ClO4)3(aq), and Yb(ClO4)3(aq) from the temperatures 283 K to 328 K

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Cited by 13 publications
(10 citation statements)
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References 50 publications
(112 reference statements)
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“…The effects of the overall hydration increase on thermodynamic and transport properties have been discussed in detail previously. (11,54,66,68,69,73) Values of C p,φ for these R X 3 (aq) electrolytes exhibit slightly more complicated behavior. At constant lower molalities, the values of C p,φ for the RCl 3 (aq) (15,16) and R(ClO 4 ) 3 (aq) (56) at T = 298.15 K are nearly constant from lanthanum to neodymium, increase with atomic number between neodymium and terbium, and then remain nearly constant for the remaining RCl 3 (aq) or increase slowly with increasing atomic number for the R(ClO 4 ) 3 (aq).…”
Section: (Aq) and R(so )mentioning
confidence: 94%
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“…The effects of the overall hydration increase on thermodynamic and transport properties have been discussed in detail previously. (11,54,66,68,69,73) Values of C p,φ for these R X 3 (aq) electrolytes exhibit slightly more complicated behavior. At constant lower molalities, the values of C p,φ for the RCl 3 (aq) (15,16) and R(ClO 4 ) 3 (aq) (56) at T = 298.15 K are nearly constant from lanthanum to neodymium, increase with atomic number between neodymium and terbium, and then remain nearly constant for the remaining RCl 3 (aq) or increase slowly with increasing atomic number for the R(ClO 4 ) 3 (aq).…”
Section: (Aq) and R(so )mentioning
confidence: 94%
“…However, Xiao and Tremaine (54) have discussed the effect of changes in the hydration of the rare-earth ion on values of C • p,φ (R 3+ , aq, T ). Marcantonatos et al (74) analyzed the coupling between an inner-sphere hydration number equilibrium and an equilibrium for the formation of outer-sphere ion-pair complexes.…”
Section: (Aq) and R(so )mentioning
confidence: 98%
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