1981 年 8 巻 3 号 p. 106-114
Resolution of excess heat capacities of many types of transitions-whether structural or electronic, or otherwise-requires a reliable estimate of the lattice contribution. This besetting problem has confronted thermophysicists for decades. Corresponding state theories have been less than satisfactory; Lindemann schemes are suggestive. For chemical thermodynamic purposes use of a volume-weighted scheme over the range where entropy development largely occurs is demonstrated to provide resolution of Schottky contributions for Ln (OH)3 and LnCl3 systems and has been shown to be superior to other approaches. Application to estimation of heat capacities (entropies, etc.) and to extrapolation of results to pure end-member composition in geothermodynamic problems are considered.