Aluminosilicate chemistry - Revision history

Rasmus: links

2016-08-13T17:21:27Z

links

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	Aluminosilicate chemistry is the inorganic counterpart to organic chemistry, based on the manipulation of the many varieties of silica and alumina containing materials on earth. Although not as reactive as hydrocarbons, Alumiosilicates are vastly more available than petroleum and form a wide variety of materials with useful structural, thermal, chemical and electrical properties.		Aluminosilicate chemistry is the inorganic counterpart to organic chemistry, based on the manipulation of the many varieties of silica and alumina containing materials on earth. Although not as reactive as hydrocarbons, [https://en.wikipedia.org/wiki/Aluminosilicate Alumiosilicates] are vastly more available than petroleum and form a wide variety of materials with useful structural, thermal, chemical and electrical properties.

	Silica (Si02) is one of the most abundant molecules on the surface of the earth. Alumina (Al2O3) is also widely distributed. Most minerals exist as complexes of Silicon, Aluminum, and Oxygen, as well as Iron and other less abundant elements. Kaolin clay for example, which is used by ceramicists is often dug locally, consists of hydrated silica and alumina (Al2Si2O5(OH)4). The various Feldspars, which comprise about 60% of the earth's surface, are variations on a common aluminosilicate theme, with various alkali and alkali earth components.		Silica (Si02) is one of the most abundant molecules on the surface of the earth. Alumina (Al2O3) is also widely distributed. Most minerals exist as complexes of Silicon, Aluminum, and Oxygen, as well as Iron and other less abundant elements. Kaolin clay for example, which is used by ceramicists is often dug locally, consists of hydrated silica and alumina (Al2Si2O5(OH)4). The various Feldspars, which comprise about 60% of the earth's surface, are variations on a common aluminosilicate theme, with various alkali and alkali earth components.
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	The smelting of aluminum and silicon from rocks, the purification of silica (fused quartz) for lenses, windows, containers, et cetera, and the polymerization of aluminosilicates ([[Geopolymers]]) are members of the field of aluminosilicate chemistry.		The smelting of aluminum and silicon from rocks, the purification of silica (fused quartz) for lenses, windows, containers, et cetera, and the polymerization of aluminosilicates ([[Geopolymers]]) are members of the field of aluminosilicate chemistry.

	[[Category:Metalworks]][[Category:Materials]]		==Related Pages==
			* [[Zeolite]]
			* [[Green Chemistry]]

			[[Category:Metalworks]]
			[[Category:Materials]]

Rasmus: categorization

2011-01-21T02:52:25Z

categorization

← Older revision		Revision as of 02:52, 21 January 2011
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	Aluminosilicate chemistry is the inorganic counterpart to organic chemistry, based on the manipulation of the many varieties of silica and alumina containing materials on ~~the~~ earth. Although not as reactive as hydrocarbons, ~~Aaumiosilicates~~ are vastly more available than petroleum and form a wide variety of materials with useful structural, thermal, chemical and electrical properties.		Aluminosilicate chemistry is the inorganic counterpart to organic chemistry, based on the manipulation of the many varieties of silica and alumina containing materials on earth. Although not as reactive as hydrocarbons, Alumiosilicates are vastly more available than petroleum and form a wide variety of materials with useful structural, thermal, chemical and electrical properties.

	Silica (Si02) is one of the most abundant molecules on the surface of the earth. Alumina (Al2O3) is also widely distributed. Most minerals exist as complexes of Silicon, Aluminum, and Oxygen, as well as Iron and other less abundant elements. Kaolin clay for example, which is used by ceramicists is often dug locally, consists of hydrated silica and alumina (Al2Si2O5(OH)4). The various Feldspars, which comprise about 60% of the earth's surface, are variations on a common aluminosilicate theme, with various alkali and alkali earth components.		Silica (Si02) is one of the most abundant molecules on the surface of the earth. Alumina (Al2O3) is also widely distributed. Most minerals exist as complexes of Silicon, Aluminum, and Oxygen, as well as Iron and other less abundant elements. Kaolin clay for example, which is used by ceramicists is often dug locally, consists of hydrated silica and alumina (Al2Si2O5(OH)4). The various Feldspars, which comprise about 60% of the earth's surface, are variations on a common aluminosilicate theme, with various alkali and alkali earth components.
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	The smelting of aluminum and silicon from rocks, the purification of silica (fused quartz) for lenses, windows, containers, et cetera, and the polymerization of aluminosilicates ([[Geopolymers]]) are members of the field of aluminosilicate chemistry.		The smelting of aluminum and silicon from rocks, the purification of silica (fused quartz) for lenses, windows, containers, et cetera, and the polymerization of aluminosilicates ([[Geopolymers]]) are members of the field of aluminosilicate chemistry.

	[[Category:Metalworks]]		[[Category:Metalworks]][[Category:Materials]]

Rasmus at 02:36, 15 January 2011

2011-01-15T02:36:41Z

← Older revision		Revision as of 02:36, 15 January 2011
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	The smelting of aluminum and silicon from rocks, the purification of silica (fused quartz) for lenses, windows, containers, et cetera, and the polymerization of aluminosilicates ([[Geopolymers]]) are members of the field of aluminosilicate chemistry.		The smelting of aluminum and silicon from rocks, the purification of silica (fused quartz) for lenses, windows, containers, et cetera, and the polymerization of aluminosilicates ([[Geopolymers]]) are members of the field of aluminosilicate chemistry.

			[[Category:Metalworks]]

Offonoffoffonoff: New page: Aluminosilicate chemistry is the inorganic counterpart to organic chemistry, based on the manipulation of the many varieties of silica and alumina containing materials on the earth. Altho...

2008-05-26T21:50:36Z

New page: Aluminosilicate chemistry is the inorganic counterpart to organic chemistry, based on the manipulation of the many varieties of silica and alumina containing materials on the earth. Altho...

New page

Aluminosilicate chemistry is the inorganic counterpart to organic chemistry, based on the manipulation of the many varieties of silica and alumina containing materials on the earth. Although not as reactive as hydrocarbons, Aaumiosilicates are vastly more available than petroleum and form a wide variety of materials with useful structural, thermal, chemical and electrical properties.

Silica (Si02) is one of the most abundant molecules on the surface of the earth. Alumina (Al2O3) is also widely distributed. Most minerals exist as complexes of Silicon, Aluminum, and Oxygen, as well as Iron and other less abundant elements. Kaolin clay for example, which is used by ceramicists is often dug locally, consists of hydrated silica and alumina (Al2Si2O5(OH)4). The various Feldspars, which comprise about 60% of the earth's surface, are variations on a common aluminosilicate theme, with various alkali and alkali earth components.

The smelting of aluminum and silicon from rocks, the purification of silica (fused quartz) for lenses, windows, containers, et cetera, and the polymerization of aluminosilicates ([[Geopolymers]]) are members of the field of aluminosilicate chemistry.