Activity coefficients of La(NO3)3, La(ClO4)3, and La2(SO4)3 are determined using the method of liquid membrane cells, which allows us to study high dilution levels previously unattainable (10-4 to 10-5 mol kg-1 depending on the salt). Literature values are found to be correct for La(ClO4)3, moderately biased for La(NO3)3 and completely incorrect for La2(SO4)3. This last salt in the diluted regions displays dramatic negative deviations not recognized earlier because the measurements terminated at ca. 10-3 mol kg-1, where a Debye-Huckel-like misleading trend occurs. Numerical integration of the Poisson Boltzmann equation and Bjerrum's theory of ion pairing show an astounding ability to reproduce the trend of La2(SO4)3; however, there is evidence of short-range interactions that add to long-range interactions for lanthanum and bivalent metal sulfates, as if sulfate ions were displacing water from the hydration shells of the cations. Pitzer's equation parameters that reproduce the activity and osmotic coefficients of the three salts and those (recalculated) of LaCl3 are reported.

Activity coefficients of lanthanum salts at 298.15 K

Fanelli N
2002

Abstract

Activity coefficients of La(NO3)3, La(ClO4)3, and La2(SO4)3 are determined using the method of liquid membrane cells, which allows us to study high dilution levels previously unattainable (10-4 to 10-5 mol kg-1 depending on the salt). Literature values are found to be correct for La(ClO4)3, moderately biased for La(NO3)3 and completely incorrect for La2(SO4)3. This last salt in the diluted regions displays dramatic negative deviations not recognized earlier because the measurements terminated at ca. 10-3 mol kg-1, where a Debye-Huckel-like misleading trend occurs. Numerical integration of the Poisson Boltzmann equation and Bjerrum's theory of ion pairing show an astounding ability to reproduce the trend of La2(SO4)3; however, there is evidence of short-range interactions that add to long-range interactions for lanthanum and bivalent metal sulfates, as if sulfate ions were displacing water from the hydration shells of the cations. Pitzer's equation parameters that reproduce the activity and osmotic coefficients of the three salts and those (recalculated) of LaCl3 are reported.
2002
Istituto per i Processi Chimico-Fisici - IPCF
4
121
126
activity coefficient
electrolyte solution
liquid membrane cell
electrolyte theories
I coefficienti d’attività hanno ovvia importanza per chi s’interessa di reazioni che coinvolgono specie ioniche in soluzione. Esclusi gli elettroliti a bassa carica sufficientemente coperti da dati sperimentali e teorie, in tutti gli altri casi i soli dati finora disponibili erano i cosiddetti coefficienti d’attività relativi di soluzioni a concentrazione medio-alta, quasi inutili perché, in mancanza di dati per soluzioni molto diluite, era impossibile ricavarne i coefficienti d’attività veri e propri. Solo di recente il nuovo metodo delle celle a membrane liquide ha permesso di spingere le misure di potenziale chimico degli elettroliti sino a livelli di diluizione estrema, .00001 mol/kg e oltre. Ciò ha permesso d’identificare i coefficienti d’attività anche per elettroliti sinora impossibili da studiare, come il solfato di lantanio, e di controllare la consistenza dei risultati con cicli termodinamici di matching delle forze elettromotrici di celle relative ad elettroliti più semplici
1
info:eu-repo/semantics/article
262
Malatesta F.; Bruni F.; Fanelli N.
01 Contributo su Rivista::01.01 Articolo in rivista
none
File in questo prodotto:
Non ci sono file associati a questo prodotto.

I documenti in IRIS sono protetti da copyright e tutti i diritti sono riservati, salvo diversa indicazione.

Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/20.500.14243/437746
Citazioni
  • ???jsp.display-item.citation.pmc??? ND
  • Scopus ND
  • ???jsp.display-item.citation.isi??? ND
social impact