EGU2020-13709, updated on 12 Jun 2020
https://doi.org/10.5194/egusphere-egu2020-13709
EGU General Assembly 2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.

The effect of the cooling on a dry storage cask for spent nuclear fuel by different wind speed

LinYing Cheng1 and Chi-Ming Lai2
LinYing Cheng and Chi-Ming Lai
  • 1National Cheng Kung University, Civil Engineering, Taiwan (linying0318@gmail.com)
  • 2National Cheng Kung University, Civil Engineering, Taiwan (cmlai@mail.ncku.edu.tw)

In this study, we considered different the wind speeds affects the thermal performance when the dry storage cask for spent nuclear fuel , which used NAC- MAGNASTOR cask of system, and placed outdoors. We Ddiscuss the dry storage cask for spent nuclear fuel cooling by the thermal buoyancy ventilation of cask. Firstly, Compare the experimental data of low-speed wind tunnel experiments with the result of from a commercial software PHOENICS CFD (Computational Fluid Dynamics) for heat flow analysis, and confirm the reliability of the CFD simulation results of the software. Then we used the software to simulate higher wind speeds to understand the thermal performance of the cask for spent nuclear fuel by various wind speeds. With external wind speed is was more much faster, channel airflow of the cask hads increased, especially upper channel airflow of the cask and near steel cylindrical. The temperature of the windward side of the cask hads also been significantly reduced, The lee side hads a slower wind speed and a smaller temperature drop, and generates an eddy below the lee side, which helpeds to dissipate .heat,. However, as the wind speed gradually increases, the lee side changed to a downdraft, and the temperature drop was also slowed down. It is noticeable that the situation may occur when a typhoon comes.

How to cite: Cheng, L. and Lai, C.-M.: The effect of the cooling on a dry storage cask for spent nuclear fuel by different wind speed, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-13709, https://doi.org/10.5194/egusphere-egu2020-13709, 2020