Stolyarova Valentina L, Vorozhtcov Viktor A, Masaki Kurata, Costa Davide
Saint Petersburg State University, Saint Petersburg, Russia.
Institute of Silicate Chemistry of RAS, Saint Petersburg, Russia.
Rapid Commun Mass Spectrom. 2020 Oct 15;34(19):e8862. doi: 10.1002/rcm.8862.
The UO -ZrO solid solution at high temperatures is the key system of modern nuclear science and technology in the context of the safety operation of nuclear cycles, the consequences of severe accidents, and the incorporation of nuclear waste. Urgent needs of the continuation of experimental studies of this system at temperatures up to 3000 K are aimed at preventing severe accidents similar to Chernobyl and Fukushima when the thermodynamic approach is used for the prediction of high-temperature behavior of materials.
This investigation was carried out using the Knudsen effusion mass spectrometric method using the MS-1301 magnetic sector mass spectrometer. The samples in the UO -ZrO system were vaporized from a tungsten effusion cell. Vapor species effusing from the cell were ionized at an electron ionization energy of 70 eV.
The vaporization and thermodynamics of pure UO and ZrO as well as of the samples in the UO -ZrO system were studied in the range 2000-2730 K. The temperature dependences of the partial vapor pressures of UO and UO over pure UO were obtained at 2060-2456 K, which agreed with the literature results. The partial vapor pressures of UO, UO , ZrO, and ZrO , the vaporization rates, and the UO and ZrO activities in the UO -ZrO solid solutions were determined at 2370, 2490, 2570, and 2730 K.
The component activities and excess Gibbs energies of the UO -ZrO system indicated a change in deviations from the ideal behavior from positive to negative with the temperature increase from 2370 to 2730 K. The thermodynamic functions of formation from the oxides of the solid solutions in the UO -ZrO system such as Gibbs energies as well as the enthalpies and entropies of formation were obtained for the first time at 2550 K in the composition range 0.89-1.00 ZrO mole fraction.
在核循环安全运行、严重事故后果以及核废料处置的背景下,高温下的UO-ZrO固溶体是现代核科学与技术的关键体系。在高达3000 K的温度下继续对该体系进行实验研究的迫切需求,旨在当采用热力学方法预测材料的高温行为时,预防类似于切尔诺贝利和福岛的严重事故。
本研究使用配备MS-1301磁扇形质谱仪的克努森喷射质谱法进行。UO-ZrO体系中的样品从钨喷射池中蒸发。从池中逸出的蒸汽物种在70 eV的电子电离能量下被电离。
在2000-2730 K范围内研究了纯UO和ZrO以及UO-ZrO体系中样品的蒸发和热力学。在2060-2456 K下获得了纯UO上UO和UO的分压随温度的变化关系,与文献结果一致。在2370、2490、2570和2730 K下测定了UO-ZrO固溶体中UO、UO、ZrO和ZrO的分压、蒸发速率以及UO和ZrO的活度。
UO-ZrO体系的组分活度和过量吉布斯自由能表明,随着温度从2370 K升高到2730 K,与理想行为的偏差从正向负向变化。首次在2550 K下,在ZrO摩尔分数为0.89-1.00的组成范围内获得了UO-ZrO体系中固溶体由氧化物形成的热力学函数,如吉布斯自由能以及形成焓和熵。