A-level Chemistry/OCR (Salters)/Silicates
Silicates are the largest and most important group of minerals in nature. Silicates account for around 95% of all the rocks of the Earth's crust, and the soils, clays and sands formed when those rocks break down.
Silicates are so ubiquitous that oxygen is the most abundant element in the Earth's crust by mass, with silicon in second place: oxygen makes up 46% of the mass of the Earth's crust, while silicon is responsible for 27%. Silicon and oxygen together therefore account for 73% of the crust.
The basic building block of all silicate minerals is the [SiO4]4− tetrahedron. There are four covalent Si−O bonds. Each oxygen atom forms one vertex of the tetrahedron. The silicon to oxygen ratio is 1:4.
Silicate minerals containing isolated [SiO4]4− tetrahedra are called nesosilicates or orthosilicates.
If two [SiO4]4− tetrahedra share an oxygen atom at one common vertex, an [Si2O7]6− ion is formed. The silicon to oxygen ratio is 2:7.
Silicate minerals containing isolated [Si2O7]6− double tetrahedra are called sorosilicates.
Silicate minerals containing chains are termed inosilicates.
(SiO32−)n. The silicon to oxygen ratio is 1:3.
(Si4O116−)n. The silicon to oxygen ratio in double chains is 4:11.
Asbestos (from Greek ἅσβεστος, unquenchable) is a group of fibrous silicate minerals containing double chains. Prolonged exposure to dust containing fibres from certain types of asbestos is now known to cause scarring of the lungs, lung cancer, and a particularly aggressive cancer called mesothelioma. Mesothelioma is almost always fatal, with a median survival time of 11 months. Due to the exceptional danger posed by some absestos, all work involving asbestos in the UK must be done by specialist companies. The vast majority of asbestos is the so-called white form, which is not known to pose any real danger.
SiO4 tetrahedra can be arranged to form sheets, as illustrated to the right. The formula of such a sheet can be written (Si2O52−)n.
Silicate minerals containing sheets are termed phyllosilicates.
Perhaps the most structurally complicated silicates are those based on networks of Si and O that extend in all three dimensions. Examples of such minerals include quartz, zeolites and feldspars.
Silicate minerals containing three-dimensional frameworks are termed tectosilicates.