Quoting thekrib (reflective of my current knowlege)...
"When the aquarium has some carbonate buffering in it, the bicarbonate ions will combine with the excess hydrogen ions to form carbonic acid (H2CO3) which then slowly breaks down into CO2 and water. Since the excess hydrogen ions are used in the reaction, the pH does not change very much. Over time, as the carbonate ions are used up, the buffering capacity will drop and larger pH changes will be noted. From this it is clear why aquariums with low KH seem unstable -as acid is produced by biological action, the KH is used up; when it is gone, the pH is free to drop rapidly as H+ ions are generated."
--end quote (from http:// aquaticconcepts.thekrib.com/Articles/ Water_Chemistry.htm ; copyright 2000 George and Karla Booth)
So what else do we know now, as technology and science have advanced over the several years period (more than a decade) between the time when that was writen and today?
What more can anyone add to that? The replies we've seen in this thread thus far don't take us much further than the above cited article. Is there more to be known?
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