The Mohs scale of mineral hardness (/moʊz/) is a qualitative ordinal scale, from 1 to 10, characterizing scratch resistance of various minerals through the ability of harder material to scratch softer material.
The scale was created in 1822 by German geologist
and mineralogist Friedrich Mohs; it is one of several definitions of hardness in
materials science, some of which are more quantitative.
The method of comparing hardness by
observing which minerals can scratch others is of great antiquity, having been
mentioned by Theophrastus in his treatise On Stones, c. 300 BC,
followed by Pliny the Elder in his Naturalis Historia, c. AD 77. The
Mohs scale is extremely useful for identification of minerals in the field, but
is not an accurate predictor of how well materials endure in an industrial
setting – toughness.
Uses of the Mohs Scale
Despite its lack of precision, the Mohs
scale is relevant for field geologists, who use the scale to roughly identify
minerals using scratch kits. The Mohs scale hardness of minerals can be
commonly found in reference sheets.
Mohs hardness is useful in milling. It
allows assessment of which kind of mill will best reduce a given product whose
hardness is known. The scale is used at
electronic manufacturers for testing the resilience of flat panel display
components (such as cover glass for LCDs or encapsulation for OLEDs).
The Mohs scale has been used to evaluate
the hardness of smartphone screens. Most modern smartphone displays use Gorilla
Glass that scratches at level 6 with deeper grooves at level 7 on the Mohs
scale of hardness.
Minerals Involved in Testing
The Mohs scale of mineral hardness is
based on the ability of one natural sample of mineral to scratch another
mineral visibly. The samples of matter used by Mohs are all different minerals.
Minerals are chemically pure solids found in nature. Rocks are made up of one
or more minerals. As the hardest known naturally occurring substance when the
scale was designed, diamonds are at the top of the scale. The hardness of a
material is measured against the scale by finding the hardest material that the
given material can scratch, or the softest material that can scratch the given
material. For example, if some material is scratched by apatite but not by
fluorite, its hardness on the Mohs scale would fall between 4 and 5.
"Scratching" a material for
the purposes of the Mohs scale means creating non-elastic dislocations visible
to the naked eye. Frequently, materials that are lower on the Mohs scale can
create microscopic, non-elastic dislocations on materials that have a higher
Mohs number. While these microscopic dislocations are permanent and sometimes
detrimental to the harder material's structural integrity, they are not
considered "scratches" for the determination of a Mohs scale number.
The Mohs scale is a purely ordinal scale.
For example, corundum (9) is twice as
hard as topaz (8), but diamond (10) is four times as hard as corundum.
Hardness |
Substance or mineral |
0.2–0.3 |
|
0.5–0.6 |
|
1 |
|
1.5 |
gallium, strontium, indium, tin, barium, thallium, lead, graphite, ice[17] |
2 |
hexagonal boron
nitride,[18] calcium, selenium, cadmium, sulfur, tellurium, bismuth, gypsum |
2–2.5 |
|
2.5–3 |
|
3 |
|
3.5 |
|
4 |
|
4–4.5 |
ordinary steel |
5 |
apatite (tooth
enamel), zirconium, palladium, obsidian (volcanic
glass) |
5.5 |
|
6 |
orthoclase, titanium, manganese, germanium, niobium, uranium |
6–7 |
fused
quartz, iron pyrite, silicon, ruthenium, iridium, tantalum, opal, peridot, tanzanite, rhodium, jade |
7 |
|
7.5–8 |
|
8 |
|
8.5 |
|
9 |
corundum (includes sapphire and ruby), tungsten carbide, titanium
nitride |
9–9.5 |
silicon carbide (carborundum), tantalum
carbide, zirconium carbide, alumina, beryllium carbide, titanium
carbide, aluminum boride, boron
carbide.[a][20][21] |
9.5–near 10 |
boron, boron
nitride, rhenium diboride (a-axis),[22] stishovite, titanium diboride, moissanite (crystal
form of silicon carbide) |
10 |
https://en.wikipedia.org/wiki/Mohs_scale_of_mineral_hardness
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