Two (2) Siruma silica samples, one raw
and the other elutriated to obtain a
particle size of 2 microns and below (2µ
>), were analyzed. The raw Siruma silica
sample was subjected to X-ray
diffraction and particle size
distribution analyses, while the 2µ >
materials was subjected
to X-ray diffraction analysis, TG-DTA,
IR, and SEM.
Results of the study shouied that the
raw Siruma silica sample is mainly
composed of quartz (SiO2) and
traces of kaolinite (Al2O3.2SiO2,
2H2O) and sericite (KAI2
(AlSi3O10(OH)2)
On the other hand, the elutriated sample
( 2 µ >) consists of clay minerals, such
as, kaolinite and
sericite and traces of very fine
particles of quartz.