A common clay mineral belonging to the kaolin
group, with the chemical formula Al2Si2O5(OH)4. Consisting
of sheets of tetrahedrally coordinated silicon joined by oxygen
shared with octahedrally coordinated aluminum, kaolinite
does not expand with the addition of water and does not
exchange magnesium or iron. A high-alumina clay mineral and
one of the most common of the clay minerals, it often occurs
with quartz, iron oxides, pyrite, and siderite and is formed by
the weathering of feldspars and other silicate minerals.














Tidak ada komentar:
Posting Komentar
Catatan: Hanya anggota dari blog ini yang dapat mengirim komentar.