The thermal hydraulic characteristics in the vacuum vessel (VV) of
a fusion reactor under an ingress of coolant event (ICE) and a
loss of vacuum event (LOVA) were investigated quantitatively using
preliminary experimental apparatuses. In the ICE experiments, pressure rise characteristics in the VV were
clarified for experimental parameters of the wall temperature and water
temperature and for cases with and without a blowdown tank. In addition, the functional
performance of a blowdown tank with and without a water cooling system was examined
and it was confirmed that the blowdown tank with a water cooling system
is effective for suppressing the pressure rise during the ICE.
In the LOVA experiments, the saturation time in the VV from vacuum to
atmosphere was investigated for various breach sizes and it was found that
the saturation time is in inverse proportion to the breach size. In
addition, the characteristics of exchange flow through breaches were
clarified for the different breach positions on the VV. It was proven from
the experimental results that the exchange flow became a counter-current
flow when the breach was positioned on the top of the VV and a stratified
flow when it was formed on the side wall of the VV, and that the exchange flow
under the stratified flow condition was smoother than that of
counter-current flow. On the basis of these results, the severest breach condition in
ITER was changed from the top-break case to the side-break case.
To predict with high accuracy the thermal hydraulic
characteristics during ICEs and LOVAs under ITER conditions,
a large scale test facility will be necessary. The current
conceptual design of the combined ICE-LOVA test facility with a scaling
factor of 1/1000 in comparison with the ITER volume is presented.