The heat capacity of manganese monophosphide MnP has been determined by adiabatic shield calorimetry at temperatures from 5 K to 840 K. The heli-to ferromagnetic transition is noted only as a slightly enhanced heat capacity at T f 53 K. A -type heat capacity contribution with maximum at T s 289.5 K
Thermodynamic properties of scapolites at temperatures ranging from 10 K to 1000 K
β Scribed by Norikazu Komada; David P. Moecher; Edgar F. Westrum; Bruce S. Hemingway; Mikhail Yu Zolotov; Yury V. Semenov; Igor L. Khodakovsky
- Publisher
- Elsevier Science
- Year
- 1996
- Tongue
- English
- Weight
- 363 KB
- Volume
- 28
- Category
- Article
- ISSN
- 0021-9614
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β¦ Synopsis
The heat capacities of five mineral samples from the scapolite solid-solution series, Na4Al3Si9O24Cl (marialite) to Ca4Al6Si6O24CO3 (meionite), were measured by the adiabatic method from T=8 K to T=350 K and by the differential scanning calorimetry (d.s.c.) method from T = 300 K to T = 1000 K. The meionite (Me) content in per cent {Me=100 Ca*/(Ca*+Na*)} (where the asterisk indicates that possible substituents are included) and molar heat capacity (Cp,m/R) at T=298.
π SIMILAR VOLUMES
Osmotic coefficients f of aqueous solutions of 1-n-decanepyridinium chloride, 1-n-dodecanepyridinium chloride, and 1-n-hexadecanepyridinium chloride are estimated at T = 328.15 K from vapor pressure osmometric measurements. Molar integral enthalpies of dilution DdilHm have been measured for aqueous
The heat capacity of tungsten disilicide \(\mathrm{WSi}_{2.06}\) was measured over the temperature range \(5.9<(T / K)<341\) using adiabatic calorimetry. Our results show that neither a phase transition nor anomalies are present. A contribution from the electronic molar heat capacity is present and