Mineral compositions of the heated coal fly ash

석탄회의 가열에 따른 광물조성 변화

In order to clarify the part of thermal properties of coal fly ash, the change of mineral compositions of the heated coal fly ash was investigated by XRD, TG - DTA and SEM. It was found that the mineral composition of coal fly ash was quartz, mullite and glassy phase ( a b. 20 ~ 25 wt % ), and had no difference in the range of 105 to $1000^{\circ}C $. Only in the case of Ansan coal fly ash, calcite was detected besides the crystalline of quartz and mullite. And anorthite was produced by the reaction between thermal- decomposed calcite, quartz and $Al_2O_3$component in the glassy phase at $1200^{\circ}C $.

석탄회의 성상 해명의 일환으로서, 석회석의 열처리 조건과 광물조성의 관계를 검토했다. 석탄회의 주 광물조성은 mullite, quartz 및 유리상(약 20 ~ 25wt%)이었으며, $1000^{\circ}C $ 까지는 거의 변화가 없었다. 안산의 석탄회 중에는 calcite가 함유되었으며, $1200^{\circ}C $ 에서 calcite 분해로부터 온 CaO, quartz 및 유리상 중의$Al_2O_3$가 반응하여 anorthite($CaO{\cdot}Al_2O_3{\cdot}2SiO_2$)로 바뀌는 것을 알 수 있었다.