
Analcime - Wikipedia
Analcime (/ əˈnælsiːm, - saɪm /; from Ancient Greek ἀνάλκιμος (análkimos) 'not strong') or analcite is a white, gray, or colorless tectosilicate mineral. Analcime consists of hydrated sodium aluminium silicate in cubic crystalline form. Its chemical formula is NaAlSi 2 O 6 · H 2 O. Minor amounts of potassium and calcium substitute for sodium.
方沸石 - 百度百科
经大连理工大学化学物理研究所试验表明,方沸石应用于农牧业、环境保护、建材三大最佳领域的项目有:利用方沸石生产离子筛及橡塑助剂、 土壤改良剂 、重金属提取剂、生产硅铝化合物、杀菌剂、特殊氧化剂等。 方沸石经过化学改性处理后,显示出独具特色的“离子筛”特性,对直径<2.6Å的重金属离子如Cu、Pb、Zn、Ag、Fe等具有选择吸附性,非常适合于此类金属的提取、熔炼及废水净化。 经改性后,方沸石的纯度及孔径均有明显改善,吸附力和离子交换力明显提 …
Analcime (analcite): The zeolite mineral analcime information …
Analcime is a member of the zeolite group, and often occurs together with other zeolites. However, it is closely related in structure to the feldspathoid group, and is occasionally also classified as a feldspathoid together with the similar mineral Leucite.
Analcime: Mineral information, data and localities. - mindat.org
According to the International Zeolite Association (http://www.iza-online.org/natural/Datasheets/Analcime/Analcime.html) the mineral has variable composition, which can be given as Na 16-x (H 2 O) 16+x [Al 16-x Si 32+x O 96], with x varying from -3.4 to +4.3. The Na content generally is ~16 atoms per formula unit, but may range from 12 to 17.
什么是方沸石? - 知乎专栏
什么是方沸石( analcime) 化学组成:Na16[Al16Si32O96]·16H2O。Si/Al=1.8~2.8, H2O/Al2O3=22.6。 等轴晶系。 晶形为四角三八面体,有时呈粒状或放射状集合体,见图1-12,图1-13。 白色或带淡灰、淡红、淡绿等色调。含…
Synthesis and characterization of analcime (ANA) zeolite using …
2021年6月28日 · Analcime is characterized by X-ray diffraction, infrared spectroscopy, scanning electron microscopy, inductively coupled plasma optical emission spectrometry and thermal analysis....
Analcime Mineral Data
Analcime Serandite Natrolite. Comments: Orange-red, blocky serandite with white, blocky natrolite and white, equant grains of analcime. Location: Mt. St. Hilaire, Canada. Scale: 4 x 3 cm. © Fabre Minerals
Analcime | Sodium Alumino-silicate, Zeolite, Hydrated | Britannica
Analcime, common feldspathoid mineral, a hydrated sodium aluminosilicate (NaAlSi2O6·H2O) that occurs in seams and cavities in basalt, diabase, granite, or gneiss and in extensive beds thought to have formed by precipitation from alkaline lakes.
Analcime - an overview | ScienceDirect Topics
Analcime is a widespread zeolite: it occurs in amygdaloidal filling of cavities in basaltic rocks, replacement of rhyolitic vitric tuff, or precipitates from hyperalkaline waters. It occurs in a few igneous rocks (reported as a primary mineral) and can be a primary constituent of volcaniclastic sediments affected by hydrothermal alteration or ...
方沸石(Analcime) - gtss.cn
什么是方沸石( analcime) 化学组成:Na16[Al16Si32O96]·16H2O。Si/Al=1.8~2.8, H2O/Al2O3=22.6。 等轴晶系。 晶形为四角三八面体,有时呈粒状或放射状集合体,白色或带淡灰、淡红、淡绿等色调。含氧化铁时则染成肉红色。玻璃光泽。 [010]解理不完全。硬度5~5.5。 相对密 …