ALUMINO-SILICATES 化学特性,用途語,生産方法
製造方法
From a geological point of view, clays are soft, fine-grained, and residual sedimentary rocks
resulting from the weathering of feldspars (e.g., orthoclases and plagioclases) and ferromagnesian silicates (e.g., micas, amphiboles) contained in igneous and metamorphic rocks.
Hence clays are always made of various hydrated aluminosilicates, mainly kaolinite but also
illite and montmorillonite, all exhibiting the typical structure of sheet silicates (i.e., phyllosilicates).
ALUMINO-SILICATES 上流と下流の製品情報
原材料
準備製品