1999
DOI: 10.1006/jcht.1999.0542
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Enthalpies of formation and heat capacity functions for maricite,NaFePO4(cr), and sodium iron(III) hydroxy phosphate,Na3Fe(PO4)2· (Na4/3H2/3O)(cr)

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Cited by 13 publications
(5 citation statements)
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“…Maricite, as opposed to olivine, is the thermodynamically stable structure for NaFePO 4 . 49,50 The maricite structure is similar to the olivine structure, except that the alkali occupies the M(2) site, and transition metal occupies the M(1) sites. Generally, they are of less interest for battery applications given that there are no obvious channels for fast alkali diffusion in these materials, unlike in the olivine structure.…”
Section: Structure Selectionmentioning
confidence: 99%
“…Maricite, as opposed to olivine, is the thermodynamically stable structure for NaFePO 4 . 49,50 The maricite structure is similar to the olivine structure, except that the alkali occupies the M(2) site, and transition metal occupies the M(1) sites. Generally, they are of less interest for battery applications given that there are no obvious channels for fast alkali diffusion in these materials, unlike in the olivine structure.…”
Section: Structure Selectionmentioning
confidence: 99%
“…For our work, taking thermodynamic data from a sole source was possible only for well-known substances (α-Fe, Li 2 CO 3 , etc) whose characteristics completely coincide in few reference books. Table presents the standard thermodynamic values needed for our calculations and taken from various sources with a necessary indication of the references and comments on how the calculated thermodynamic values have been obtained by us, if absent in the source explicitly. In every case, preference was given to the primary experimental papers containing fuller data, including the coefficients of eq .…”
Section: Results and Discussionmentioning
confidence: 99%
“…As a result of the application of a thermodynamic cycle, a close value Δ f H 298 °(FePO 4 ) = −1220.4 kJ•mol −1 was calculated on the basis of these numeric data.Due to the poorer experimental database, La Iglesia 68 describes the lithium−phosphate compounds with a lower accuracy than the soduim and potassium compounds:(h i (Li 2 O) = (−817.30 ± 12.97) kJ•mol −1 ; g i (Li 2 O) is not given). This enables us to evaluate, by this method, the standard enthalpy of formation only: Δ f H 298 °(LiFePO 4 ) = (−1591.23 ± 13) kJ•mol −1 , which is very near to the corresponding value for orthorhombic sodium iron phosphate:Δ f H 298 °(NaFePO 4 ) = −1571.8 kJ•mol −1 ,69 but is in contradiction with the value Δ f H 298 °(LiFePO 4 ) = −1392.45 kJ•mol −1 calculated from the data from ref 66. Taking various data sets and applying the quasi-additivity principle to compounds close by composition and structure, we have additionally found Δ f H 298 °(LiFePO 4 ) = −1514.8 kJ•mol −1 (from the standard enthalpies of formation of Li 3 PO 4 , NaFePO 4 , and Na 3 PO 4 ) and S 298 °(LiFePO 4 ) = 136.75 J•K −1 •mol −1 (from the standard entropies of the constituent oxides Li 2 O, P 2 O 5 , FeO).Table3presents the values of Δ f G 298 °(LiFePO 4 ) corresponding to different calculation techniques.…”
mentioning
confidence: 77%
“…Therefore, the molar ratio of Fe 2+ to Fe 3+ used in the present study was 1.4 ‫.2׃‬ In general, as long as the molar ratio of Fe 2+ to Fe 3+ is not greater than ‫,1׃1‬ the Fe 3 O 4 can be formed (He et al, 2003). Additionally, the process Fe 2+ →Fe 3+ +e -is an endothermic process and heating can accelerate oxidization of Fe 2+ into Fe 3+ , because the standard molar enthalpies of formation of Fe 2+ and Fe 3+ are −89.1 kJ mol -1 and −48.5 kJ mol -1 , respectively (Tremaine and Xiao, 1999). It was therefore necessary to keep relatively low temperature during the process of preparation of water-based ferromagnetic fluid.…”
Section: The Absolute Quantity and Relative Magneticmentioning
confidence: 99%