Ito E, Akaogi M, Topor L, Navrotsky A
Science. 1990 Sep 14;249(4974):1275-8. doi: 10.1126/science.249.4974.1275.
A new and sensitive differential drop solution calorimetric technique was developed for very small samples. A single experiment using one 5.18-milligram sample of perovskite, synthesized at 25 gigapascals and 1873 Kelvin, gave 110.1 +/- 4.1 kilojoules per mole for the enthalpy of the ilmenite-pervoskite transition in MgSiO(3). The thermodynamics of the reaction of MgSiO(3) (ilmenite) to MgSiO(3) (perovskite) and of Mg(2)SiO(4) (spinel) to MgSiO(3) (pervoskite) and MgO (periclase) were assessed. Despite uncertainties in heat capacity and molar volume at high pressure and temperature, both reactions clearly have negative pressure-temperature slopes, -0.005 +/- 0.002 and -0.004 +/- 0.002 gigapascals per Kelvin, respectively. The latter may be insufficiently negative to preclude whole-mantle convection.
一种针对极少量样品开发的新型灵敏的差滴溶液量热技术。使用一个在25吉帕斯卡和1873开尔文条件下合成的5.18毫克钙钛矿样品进行的单次实验,得出MgSiO₃中钛铁矿 - 钙钛矿转变的焓为每摩尔110.1±4.1千焦。评估了MgSiO₃(钛铁矿)转变为MgSiO₃(钙钛矿)以及Mg₂SiO₄(尖晶石)转变为MgSiO₃(钙钛矿)和MgO(方镁石)的反应热力学。尽管在高压和高温下的热容和摩尔体积存在不确定性,但这两个反应的压力 - 温度斜率均明显为负,分别为-0.005±0.002和-0.004±0.002吉帕斯卡每开尔文。后者的负值可能不足以排除全地幔对流。