How do minerals get their physical and chemical properties?

Question

Minerals are a mixture of various elements...so how do we determine there chemical ...and also physical properties?

Answer 1

Physical properties of minerals-

Classifying minerals can range from simple to very difficult. A mineral can be identified by several physical properties, some of them being sufficient for full identification without equivocation. In other cases, minerals can only be classified by more complex chemical or X-ray diffraction analysis; these methods, however, can be costly and time-consuming.

Physical properties commonly used are-

Crystal structure and habit: See the above discussion of crystal structure. A mineral may show good crystal habit or form, or it may be massive, granular or compact with only microscopically visible crystals.

Talc -
Rough diamond.Hardness: the physical hardness of a mineral is usually measured according to the |Mohs scale. This scale is relative and goes from 1 to 10. Minerals with a given Mohs hardness can scratch the surface of any mineral that has a lower hardness than itself.

Moh's Hardness scale:[6]
Talc Mg3Si4O10(OH)2
Gypsum CaSO4·2H2O
Calcite CaCO3
Fluorite CaF2
Apatite Ca5(PO4)3(OH,Cl,F)
Orthoclase KAlSi3O8
Quartz SiO2
Topaz Al2SiO4(OH,F)2
Corundum Al2O3
Diamond C (pure carbon)
Luster indicates the way a mineral's surface interacts with light and can range from dull to glassy (vitreous).
Metallic -high reflectivity like metal: galena and pyrite
Sub-metallic -slightly less than metallic reflectivity: magnetite
Non-metallic lusters:
Adamantine - brilliant, the luster of diamond also cerussite and anglesite
Vitreous -the luster of a broken glass: quartz
Pearly - iridescent and pearl-like: talc and apophyllite
Resinous - the luster of resin: sphalerite and sulfur
Silky - a soft light shown by fibrous materials: gypsum and chrysotile
Dull/earthy -shown by finely crystallized minerals: the kidney ore variety of hematite
Color indicates the appearance of the mineral in reflected light or transmitted light for translucent minerals (i.e. what it looks like to the naked eye).
Irridescence - the play of colors due to surface or internal interference. Labradorite exhibits internal irridescence whereas hematite and sphalerite often show the surface effect.
Streak refers to the color of the powder a mineral leaves after rubbing it on an unglazed porcelain streak plate. Note that this is not always the same color as the original mineral.
Cleavage describes the way a mineral may split apart along various planes. In thin section, cleavage is visible as thin parallel lines across a mineral.
Fracture describes how a mineral breaks when broken contrary to its natural cleavage planes.
Chonchoidal fracture is a smooth curved fracture with concentric ridges of the type shown by glass.
Hackley is jagged fracture with sharp edges.
Fibrous
Irregular

Specific gravity relates the mineral mass to the mass of an equal volume of water, namely the density of the material. While most minerals, including all the common rock-forming minerals, have a specific gravity of 2.5 - 3.5, a few are noticeably more or less dense, e.g. several sulfide minerals have high specific gravity compared to the common rock-forming minerals.
Other properties: fluorescence (response to ultraviolet light), magnetism, radioactivity, tenacity (response to mechanical induced changes of shape or form), piezoelectricity and reactivity to dilute acids.

Chemical properties of minerals-

Minerals may be classified according to chemical composition. They are here categorized by anion group. The list below is in approximate order of their abundance in the Earth's crust. The list follows the Dana classification system.

Silicate class-
quartzThe largest group of minerals by far are the silicates (most rocks are >95% silicates), which are composed largely of silicon and oxygen, with the addition of ions such as aluminium, magnesium, iron, and calcium. Some important rock-forming silicates include the feldspars, quartz, olivines, pyroxenes, amphiboles, garnets, and micas.

Carbonate class-
The carbonate minerals consist of those minerals containing the anion (CO3)2- and include calcite and aragonite (both calcium carbonate), dolomite (magnesium/calcium carbonate) and siderite (iron carbonate). Carbonates are commonly deposited in marine settings when the shells of dead planktonic life settle and accumulate on the sea floor. Carbonates are also found in evaporitic settings (e.g. the Great Salt Lake, Utah) and also in karst regions, where the dissolution and reprecipitation of carbonates leads to the formation of caves, stalactites and stalagmites. The carbonate class also includes the nitrate and borate minerals.

Sulfate class-
Sulfates all contain the sulfate anion, SO42-. Sulfates commonly form in evaporitic settings where highly saline waters slowly evaporate, allowing the formation of both sulfates and halides at the water-sediment interface. Sulfates also occur in hydrothermal vein systems as gangue minerals along with sulfide ore minerals. Another occurrence is as secondary oxidation products of original sulfide minerals. Common sulfates include anhydrite (calcium sulfate), celestine (strontium sulfate), barite (barium sulfate), and gypsum (hydrated calcium sulfate). The sulfate class also includes the chromate, molybdate, selenate, sulfite, tellurate, and tungstate minerals.

Halide class-
HaliteThe halides are the group of minerals forming the natural salts and include fluorite (calcium fluoride), halite (sodium chloride), sylvite (potassium chloride), and sal ammoniac (ammonium chloride). Halides, like sulfates, are commonly found in evaporitic settings such as playa lakes and landlocked seas such as the Dead Sea and Great Salt Lake. The halide class includes the fluoride, chloride, and iodide minerals.

Oxide class-
Oxides are extremely important in mining as they form many of the ores from which valuable metals can be extracted. They also carry the best record of changes in the Earth's magnetic field. They commonly occur as precipitates close to the Earth's surface, oxidation products of other minerals in the near surface weathering zone, and as accessory minerals in igneous rocks of the crust and mantle. Common oxides include hematite (iron oxide), magnetite (iron oxide), chromite (iron chromium oxide), spinel (magnesium aluminium oxide - a common component of the mantle), ilmenite (iron titanium oxide), rutile (titanium dioxide), and ice (hydrogen oxide). The oxide class includes the oxide and the hydroxide minerals.

Sulfide class-
Many sulfide minerals are economically important as metal ores. Common sulfides include pyrite (iron sulfide - commonly known as fools' gold), chalcopyrite (copper iron sulfide), pentlandite (nickel iron sulfide), and galena (lead sulfide). The sulfide class also includes the selenides, the tellurides, the arsenides, the antimonides, the bismuthinides, and the sulfosalts (sulfur and a second anion such as arsenic).

Phosphate class-
The phosphate mineral group actually includes any mineral with a tetrahedral unit AO4 where A can be phosphorus, antimony, arsenic or vanadium. By far the most common phosphate is apatite which is an important biological mineral found in teeth and bones of many animals. The phosphate class includes the phosphate, arsenate, vanadate, and antimonate minerals.

Element class-
The Elemental group includes metals and intermetallic elements (gold, silver, copper), semi-metals and non-metals (antimony, bismuth, graphite, sulfur). This group also includes natural alloys, such as electrum (a natural alloy of gold and silver), phosphides, silicides, nitrides and carbides (which are usually only found naturally in a few rare meteorites).

Organic class-
The organic mineral class includes biogenic substances in which geological processes have been a part of the genesis or origin of the existing compound. Minerals of the organic class include various oxalates, mellitates, citrates, cyanates, acetates, formates, hydrocarbons and other miscellaneous species. Examples include whewellite, moolooite, mellite, fichtelite, carpathite and abelsonite..

Answer 2

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RE:
How do minerals get their physical and chemical properties?
Minerals are a mixture of various elements...so how do we determine there chemical ...and also physical properties?

Answer 3

Minerals are also chemical compounds although there are some variation. So its chemical and physical properties are determined by its molecular arrangement. Take, for example the physical property called hardness. It is determined by chemical bonding, The stronger the bond, the harder the substance become. The diamond, with its covalent bonding of satisfied carbons is the hardest of all. The physical property, cleavage is also determined by the molecular structure. Mica, with its van der waal bonding between two layers forms a cleavage. This way, for each chemical and physical properties, you can find an explanation due to the mineral's molecular structure and chemical property of the substance, respectively.

Answer 4

Minerals like bauxite etc are not mixtures but chemical compounds so they can have any physical and chemical properties.

Answer 5

the minerals
extract physical property by the nature itself
it has colour volume and state

they extrct thier chemical property
by thier chemical bond and also by the mixing of various chemicals