リン灰石 化学特性,用途語,生産方法
解説
りん灰石の別名.なお,アパタイトとりん灰石はともに学術用語である.
森北出版「化学辞典(第2版)
化学的特性
Color variable.
物理的性質
Habit: prismatic, colloform, massive, granular, earthy.
Color: white, yellow, green, red,
or blue (the color is often due to the presence of rare earths).
Diaphaneity: transparent
to translucent.
Luster: subresinous.
Streak: white. Cleavage: (0001) indistinct, (1010)
indistinct.
Fracture: conchoidal.
Chemical: soluble in HCl, and HNO3.
Occurrence: found
in all type of rocks (igneous, sedimentary, and metamorphic).
使用
Source of phosphorus and phosphoric acid, manufacture of fertilizers, laser crystals.
定義
A natural calcium phosphate (usually containing fluorine) occurring in the earth’s crust as phosphate rock. It is also the chief component of the bony structure of teeth.
农业用途
Apatite is a highly complex hexagonal structured mineral
form of calcium phosphate [Ca
5(PO
4)
3.(OH,F,Cl)]
2. It
is the most common of all phosphate minerals.
Depending upon the dominance of fluorine, chlorine or
hydroxide, apatite is called fluorapatite, chlorapatite or
hydroxyapatite, respectively.
Apatite often occurs widely as an accessory
mineral with igneous rocks, such as pegmatite. It also
occurs in regional and contact metamorphic rock,
especially limestone. Large deposits of apatite are found
in Russia.
Apatite, a major source of phosphorus, is used in the
production of fertilizers. Enamel of the teeth is composed
chiefly of apatite.
リン灰石 上流と下流の製品情報
原材料
準備製品