Here, we report an investigation of the gas–solid
reaction
between cesium hydroxide (CsOH) and siliceous (calcium silicate) thermal
insulation at high temperature, which is postulated as the origin
for the formation mechanism of cesium-bearing material emitted from
the Fukushima Daiichi nuclear power plant. A developed reaction furnace
consisting of two heating compartments was used to study the reaction
at temperatures of 873, 973, and 1073 K. Under the influence of hydrogen-steam
atmospheric conditions (H
2
/H
2
O = 0.2), the reaction
between cesium hydroxide vapor and solid thermal insulation was confirmed
to occur at temperatures of 973 and 1073 K with the formation of dicalcium
silicate (Ca
2
SiO
4
) and cesium aluminum silicate
(CsAlSiO
4
). Water-dissolution analyses of the reaction
products have demonstrated their stability, in particular, CsAlSiO
4
. Constituent similarity of the field-observed cesium-bearing
materials near the Fukushima Daiichi nuclear power plants with CsAlSiO
4
suggests for the first time that gaseous reaction between
CsOH with calcium silicate thermal insulation could be one of the
original formation mechanisms of the cesium-bearing materials.