Difference between revisions of "Fluorescent minerals"
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| − | [[File: | + | [[File:Fluorescent-minerals.jpg|thumb|Fluorescent minerals]] |
== Description == | == Description == | ||
| − | Minerals that have the unique physical property to absorb light and one wavelength and instantaneously release it at a different wavelength, resulting in a temporary color change to the eye of the human observer. Only about 15% of minerals are able to fluoresce. The fluorescence is usually due to a cation activator, such as: tungsten, molybdenum, lead, boron, titanium, manganese, uranium, and chromium, but some rare earth elements are also able to contribute to the phenomenon. Most minerals fluoresce a single color, but some may have multiple colors; for example calcite can fluoresce red, blue, white, pink, green and orange. | + | Minerals that have the unique physical property to absorb light and one wavelength and instantaneously release it at a different wavelength, resulting in a temporary color change to the eye of the human observer. Only about 15% of minerals are able to fluoresce. The fluorescence is usually due to a cation activator, such as: tungsten, molybdenum, lead, boron, titanium, manganese, uranium, and chromium, but some rare earth elements are also able to contribute to the phenomenon. Some trace elements, such as iron or copper, can quench the fluorscence. Most minerals fluoresce a single color, but some may have multiple colors; for example calcite can fluoresce red, blue, white, pink, green and orange. Because of the potential for many varying factors, the fluorescence of mineral is not typically used for its identification. |
| − | + | * '''Phosphorescence:''' | |
| + | While fluorescent minerals stop glowing when the light source is turned off, minerals that are phosphorescent continue to emit light. Minerals that can sometimes exhibit phosphorescence are: calcite, celestite, colemanite, fluorite, sphalerite, and willemite. | ||
| + | * '''Thermoluminescence:''' | ||
| + | Heating a mineral to temperatures as low as 50-200 degrees Celsius may also produce the emission of light. Some minerals that exhibit thermoluminescence are: apatite, calcite, chlorophane, fluorite, lepidolite, scapolite, and some feldspars. | ||
| + | * '''Triboluminescence:''' | ||
| + | Additionally, some mineral may emit light due to a mechanical energy, such as striking, crushing, or scratching. Potential triboluminescent minerals are: amblygonite, calcite, fluorite, lepidolite, pectolite, quartz, sphalerite, and some feldspars. | ||
| − | + | == Examples == | |
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{| class="wikitable" | {| class="wikitable" | ||
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! scope="row"| Mineral | ! scope="row"| Mineral | ||
| − | | Composition | + | | '''Composition''' |
| − | | Visible color | + | | '''Visible color''' |
| − | | Fluorescent color | + | | '''Fluorescent color''' |
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|- | |- | ||
! scope="row"| Apatite | ! scope="row"| Apatite | ||
| − | | | + | | Ca5(PO4)3(F,Cl,OH) |
| − | | | + | | pale green to purple |
| − | | | + | | pink, blue, greenish yellow |
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|- | |- | ||
! scope="row"| Calcite | ! scope="row"| Calcite | ||
| − | | | + | | CaCO3 |
| colorless to white | | colorless to white | ||
| − | | | + | | red, blue, pink, green, orange |
|- | |- | ||
! scope="row"| Cerrusite | ! scope="row"| Cerrusite | ||
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|- | |- | ||
! scope="row"| Chalcedony | ! scope="row"| Chalcedony | ||
| − | | | + | | SiO2 |
| − | | | + | | white, blue, pink |
| − | | | + | | variable |
|- | |- | ||
! scope="row"| Corundum | ! scope="row"| Corundum | ||
| − | | | + | | Al2O3 |
| − | | | + | | red (ruby), blue (sapphire) |
| − | | | + | | red (ruby), none (sapphire) |
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|- | |- | ||
! scope="row"| Fluorite | ! scope="row"| Fluorite | ||
| − | | | + | | CaF2 |
| − | | colorless | + | | colorless, white, pale blue, green |
| − | | | + | | blue-violet |
|- | |- | ||
! scope="row"| Quartz | ! scope="row"| Quartz | ||
| − | | | + | | SiO2 |
| − | | colorless | + | | colorless, purple |
| − | | | + | | variable |
|- | |- | ||
| − | ! scope="row"| | + | ! scope="row"| Scheelite |
| − | | | + | | CaWO4 |
| − | | colorless | + | | colorless, white, gray brown, yellow, orange, red, green |
| − | | | + | | bright blue, white, yellow |
|- | |- | ||
| − | ! scope="row"| | + | ! scope="row"| Sphalerite |
| − | | | + | | (Zn,Fe)S |
| − | | | + | | yellow, brown, gray, black |
| − | | yellowish | + | | lighter specimens = yellowish |
|- | |- | ||
! scope="row"| Willemite | ! scope="row"| Willemite | ||
| − | | | + | | Zn2SiO4 |
| − | | colorless | + | | colorless, white, gray, red, brown |
| − | | green | + | | strong white, green |
|- | |- | ||
|} | |} | ||
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== Comparisons == | == Comparisons == | ||
Latest revision as of 11:06, 25 July 2022
Description
Minerals that have the unique physical property to absorb light and one wavelength and instantaneously release it at a different wavelength, resulting in a temporary color change to the eye of the human observer. Only about 15% of minerals are able to fluoresce. The fluorescence is usually due to a cation activator, such as: tungsten, molybdenum, lead, boron, titanium, manganese, uranium, and chromium, but some rare earth elements are also able to contribute to the phenomenon. Some trace elements, such as iron or copper, can quench the fluorscence. Most minerals fluoresce a single color, but some may have multiple colors; for example calcite can fluoresce red, blue, white, pink, green and orange. Because of the potential for many varying factors, the fluorescence of mineral is not typically used for its identification.
- Phosphorescence:
While fluorescent minerals stop glowing when the light source is turned off, minerals that are phosphorescent continue to emit light. Minerals that can sometimes exhibit phosphorescence are: calcite, celestite, colemanite, fluorite, sphalerite, and willemite.
- Thermoluminescence:
Heating a mineral to temperatures as low as 50-200 degrees Celsius may also produce the emission of light. Some minerals that exhibit thermoluminescence are: apatite, calcite, chlorophane, fluorite, lepidolite, scapolite, and some feldspars.
- Triboluminescence:
Additionally, some mineral may emit light due to a mechanical energy, such as striking, crushing, or scratching. Potential triboluminescent minerals are: amblygonite, calcite, fluorite, lepidolite, pectolite, quartz, sphalerite, and some feldspars.
Examples
| Mineral | Composition | Visible color | Fluorescent color |
|---|---|---|---|
| Apatite | Ca5(PO4)3(F,Cl,OH) | pale green to purple | pink, blue, greenish yellow |
| Calcite | CaCO3 | colorless to white | red, blue, pink, green, orange |
| Cerrusite | PbCO3 | colorless to white | yellowish |
| Chalcedony | SiO2 | white, blue, pink | variable |
| Corundum | Al2O3 | red (ruby), blue (sapphire) | red (ruby), none (sapphire) |
| Fluorite | CaF2 | colorless, white, pale blue, green | blue-violet |
| Quartz | SiO2 | colorless, purple | variable |
| Scheelite | CaWO4 | colorless, white, gray brown, yellow, orange, red, green | bright blue, white, yellow |
| Sphalerite | (Zn,Fe)S | yellow, brown, gray, black | lighter specimens = yellowish |
| Willemite | Zn2SiO4 | colorless, white, gray, red, brown | strong white, green |
Comparisons
Properties of Common Abrasives
Properties of Common Gemstones
Natural and Simulated Diamonds