Hi all, first time here - not sure where the right place to post this is, but I've been playing with simple DIY semiconductors a little.
I happen to live in a place (Cornwall) with a lot of naturally occurring minerals - more specifically a lot of non-ferrous metallic ores, which happen to have semiconductor properties. Historically material like galena (lead ore) was used to create the diodes in crystal radios.
I've been messing around a lot with pyrites and galena, but recently tried chalcocite (a secondary copper mineral) and noticed something interesting. Below is a curve trace in the way I think you 'normally' do it, using a sawtooth rising from -2.5V and 2.5V and plotting it against the current that passes through the crystal and a point contact 'cat's whisker':
![](https://static.thentrythis.org/data/tri.png)
It's a bit rough and ready but we see (I think) is a rectifying behaviour where reverse voltage is (more or less) blocked and forward voltage starts conducting at a point between 1.5 and 2.5V.
I guess these relatively giant instabilities are to be expected in a few hundred million year old, naturally grown crystal that's been sitting in the rain on a mine dump for a few hundred years!
At some point I made a mistake and passed a sinewave through the crystal instead of a sawtooth, and I've noticed that the crystal does not "turn off" symmetrically, when the crystal is "turned on" and the voltage is dropping, it doesn't exhibit this threshold:
![](https://static.thentrythis.org/data/sine.png)
I presume this is a well known effect, I just can't find much about it online - or what it would be called.