Arsenopyrite: Difference between revisions
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[[File:Arsenopyrite.jpg|thumb|right|frame|Arsenopyrite from Carharrack Mine, Gwennap]] | |||
[[File:Arsenopyrite-penlee.png|right|frame|A curve trace of arsenopyrite from Penlee beach]] | [[File:Arsenopyrite-penlee.png|right|frame|A curve trace of arsenopyrite from Penlee beach]] | ||
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* Fracture:Irregular/Uneven | * Fracture:Irregular/Uneven | ||
[https://www.mindat.org | [https://www.mindat.org Data from mindat.org] | ||
Arsenopyrite is the most common form of arsenic in Cornwall, and is extremely common on the mine waste dumps. Part of the reason may be that it seems to degrade | Arsenopyrite is the most common form of arsenic in Cornwall, and is extremely common on the mine waste dumps. Part of the reason may be that it seems to degrade much more slowly than either [[pyrite]] or [[chalcopyrite]]. Easily recognised by it's diamond shaped cross sections, it can also form long 'acicular' crystals. | ||
As a semiconductor it is similar to pyrite, | As a semiconductor it is similar to pyrite, can be reluctant to semiconduct, and with an overall higher resistance and fairly leaky. It doesn't seem to differ much across different mines or areas of Cornwall. Some [[negative resistance]] has been observed, but this needs more investigation. Can be prone to added capacitance, this is shown in the curve plot being 'artificially' low on the left hand side, as the saw tooth wave resets at the start of the cycle. | ||
===Pages | ===Pages mentioning arsenopyrite=== | ||
{{Special:WhatLinksHere/Arsenopyrite}} | {{Special:WhatLinksHere/Arsenopyrite}} | ||
Latest revision as of 10:13, 1 July 2026
- Lustre:Metallic, Sub-Metallic
- Transparency:Opaque
- Colour:Silver-white to steel-gray, may have a slight yellow appearance
- Comment:Tarnished material common, some iridescent
- Streak:Gray-black
- Hardness:5½ - 6 on Mohs scale
- Tenacity:Brittle
- Cleavage:Distinct/Good Distinct on {001}; {010} in traces
- Fracture:Irregular/Uneven
Arsenopyrite is the most common form of arsenic in Cornwall, and is extremely common on the mine waste dumps. Part of the reason may be that it seems to degrade much more slowly than either pyrite or chalcopyrite. Easily recognised by it's diamond shaped cross sections, it can also form long 'acicular' crystals.
As a semiconductor it is similar to pyrite, can be reluctant to semiconduct, and with an overall higher resistance and fairly leaky. It doesn't seem to differ much across different mines or areas of Cornwall. Some negative resistance has been observed, but this needs more investigation. Can be prone to added capacitance, this is shown in the curve plot being 'artificially' low on the left hand side, as the saw tooth wave resets at the start of the cycle.