Нестационарный перенос компонентов изотопной смеси в результате изменения потоков каскада

Bibliographic Details
Parent link:Современные технологии, экономика и образование: сборник материалов II Всероссийской научно-методической конференции, г. Томск, 2-4 сентября 2020 г./ Национальный исследовательский Томский политехнический университет ; под ред. А. Г. Фефеловой, Е. А. Покровской, И. О. Болотиной [и др.]. [С. 111-112].— , 2020
Main Author: Ушаков А. А.
Corporate Author: Национальный исследовательский Томский политехнический университет Инженерная школа ядерных технологий Отделение ядерно-топливного цикла
Other Authors: Орлов А. А. Алексей Алексеевич, Совач В. П.
Summary:Заглавие с титульного экрана
The simulation of a non-stationary process caused by a change in the flows of the light and heavy fractions of cascade is carried out using the example of the separation of germanium isotopes. The character of the change in the isotope concentration in the stages and flows of the cascade is shown depending on the final values of the flows. It has been established that in the course of a nonstationary process, it is possible to obtain isotopes of intermediate masses with a concentration significantly exceeding the maximum attainable values for a threeflow cascade.
Published: 2020
Subjects:
Online Access:http://earchive.tpu.ru/handle/11683/64657
Format: Electronic Book Chapter
KOHA link:https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=632622
Description
Summary:Заглавие с титульного экрана
The simulation of a non-stationary process caused by a change in the flows of the light and heavy fractions of cascade is carried out using the example of the separation of germanium isotopes. The character of the change in the isotope concentration in the stages and flows of the cascade is shown depending on the final values of the flows. It has been established that in the course of a nonstationary process, it is possible to obtain isotopes of intermediate masses with a concentration significantly exceeding the maximum attainable values for a threeflow cascade.