摘要
应用联氨,使珍珠陶石形成其夹层物,然后再用水洗获得水合珍珠陶石。这种水合珍珠陶石具有十分特征的0.835umX射线衍射峰。而高岭石族的其它矿物却保持不变。利用这一明显的特征,可以容易地区分出混合在高岭石中的少量珍珠陶石。
An intercalation complex of hydrated nacrite is formed by initial nacrite intercalated withhydrazine, and then replaced with water tholecules by washing with water. The nacrite intercalatedcomplex is of cbaracteristic of 0. 835 nm diffraction peak,while other minerals of the kaolinite family rfmain unchanged. This is an unambiguous way to distinguish minor nacrite component from themixture of kaolinite minerals.
出处
《矿物学报》
CAS
CSCD
北大核心
1996年第1期89-91,共3页
Acta Mineralogica Sinica