aluminossilicato
Sign in to saveAlso known as aluminium silicate, aluminium silicates, aluminum silicate, aluminum silicates
Aluminosilicate refers to materials containing anionic Si-O-Al linkages. Commonly, the associate cations are sodium (Na+), potassium (K+) and protons (H+). Such materials occur as minerals, coal combustion products and as synthetic materials, often in the form of zeolites. Both synthetic and natural aluminosilicates are of technical significance as structural materials, catalysts, and reagents.
Research
2,906 papers- Application of aluminosilicate clay mineral-based composites in photocatalysis.Journal of environmental sciences (China) · 2022
- Aluminosilicate and zeolitic materials synthesis using alum sludge from water treatment plants: Challenges and perspectives.Waste management (New York, N.Y.) · 2024
- Mesopore Engineering for Well-Defined Mesoporosity in Al-Rich Aluminosilicate Zeolites.Chemistry (Weinheim an der Bergstrasse, Germany) · 2019
- The pozzolanic activity of calcined oil-based drilling cuttings-aluminosilicate composites.Environmental science and pollution research international · 2022
- Aluminosilicate Nanosponges: Synthesis, Properties, and Application Prospects.Inorganic chemistry · 2021
via PubMed
Wikidata facts
- Instance of
- mineral group
- Subclass of
- silicate mineral
Show 1 more fact
- topic's main category
- Category:Aluminosilicates
Sources (2)
via Wikidata · CC0
Article · Português
Minerais de aluminossilicato são compostos de alumínio, silício e oxigênio. Eles são um importante componente do caulino e outros minerais de argila. Andaluzita, cianita e silimanita são minerais de aluminossilicato de ocorrência natural, que possuem a composição Al2SiO5. O ponto triplo dos três polimorfos encontra-se à temperatura de 500 ºC e à pressão em 0,4 GPa. Estes três minerais são comumente usados como em rochas metamórficas. Os minerais de aluminossilicatos hidratados são referidos como zeólitos e são estruturas porosas que são materiais que ocorrem naturalmente.
Abstract from DBpedia / Wikipedia · CC BY-SA