CS Friends, For a while now I've been using the HVDC generator designed by Terry Chamberlain, happy that I get good quality, 10 to 20 ppm CS. Now I'm experimenting to see if longer brewing time will boost the ppm, to the point where it's concentrated enough for saturating ceramic water filters. For that I need 100 ppm, or maybe 50 ppm. But I'm getting some confusing readings on the Hanna PWT.
I've just used enough starter CS to begin with 3 micro Siemans, and at the end of 78 minutes the reading was 25, so 25 ppm. I removed the oxide branches from the annode (cathode?), stirred the solution and restarted the electrolysis. After another 33 minutes (for a total of 111 minutes) I shut the generator off, etc., but then ended up with about the same PWT reading. I'm finding this confusing, since I could definitely see additional, new ion clouds coming off of the cathode (annode?). So why do I get the same PWT reading? Shouldn't I be getting increasing ppm? For one thing I do know that my converter is not the best, reading 110v at the betgining and about 65v after one hour. Nevertheless I'm thinking the new ion clouds alone should be indication of further ppm. (I do plan on hooking up my new, constant voltage converter fairly soon, but have some how become accustomed to the old one.) I tried this same experiment about a year ago, trying to boost ppm, long before getting hold of the PWT, and followiing that experiment, the next day found that the CS had gone unstable, ending up as silver oxide sediment. This time I'm not worried about that, if only I can boost ppm. My intent would be to saturate candles immediately after brewing, before any instability could come about. Any insights would be appreciated. Reid -- The silver-list is a moderated forum for discussion of colloidal silver. Instructions for unsubscribing may be found at: http://silverlist.org To post, address your message to: silver-list@eskimo.com Silver-list archive: http://escribe.com/health/thesilverlist/index.html List maintainer: Mike Devour <mdev...@eskimo.com>
