MCsaxmaster
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<a href=showthread.php?s=&postid=10531583#post10531583 target=_blank>Originally posted</a> by Sk8r
Bertoni came up with an interesting observation: if you are supplementing [an dI hope I'm quoting him right] with 2-part or Kent's or whatever, you're actually adding some mg.
If you are supplementing with kalk, you are not, because there is no mg in kalk.
So if the corals are using mg, and you are not supplying it via your supplement, the net effect is that you are losing mg and need to supplement more.
That may reconcile Randy with Bertoni. Bertoni makes those comments in the thread I linked to above.
<a href=showthread.php?s=&postid=12772714#post12772714 target=_blank>Originally posted</a> by Marshall Haith
Huh--could you post a picture? Accumulating preferentially in areas of strong flow seems strange.
c j
Thanks Chris. Posted are a couple of photos, the closeup being of the center front glass. You are right. The calc buildup is actually to the side of the powerheads and below them, not in the output stream, so the water is pretty slow-moving there. In front, the output streams from the two powerheads meet, so they cancel one another, and the flow is pretty slow there also.
mh
could you possible take out an album on www.photobucket.com
<a href=showthread.php?s=&postid=10521969#post10521969 target=_blank>Originally posted</a> by Sara B
I do use a Salifert Magnesium test kit. I also run a Kalk reactor on both systems and drip with top-off water 24/7. The reactors stir the Kalk 4 times a day for 15 minutes at a time. I have a basement fishroom and my PH remains in the range of 7.8 to 8.0 as the A/C running all summer has an effect on it's level. In the fall and winter its more in the 8.2 range as I have a vent that's open for fresh air in the room.
<a href=showthread.php?s=&postid=12774694#post12774694 target=_blank>Originally posted</a> by Marshall Haith
Ok, here they are.
mh
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I would assume your low dkH values are behind the precipitation
<a href=showthread.php?s=&postid=12781414#post12781414 target=_blank>Originally posted</a> by MCsaxmaster
Marshall,
How are you measuring pH?
I would assume your low dkH values are behind the precipitation
Huh-uh. All else equal (e.g., pH, temperature, precense of nucleation sites, etc.), with lower carbonate alkalinity you'll have lower rates of CaCO3 precipitation.
The rate of precipitation depends mostly on saturation state (assuming there are available nucleation sites, which is probably a good assumption in an aquarium full of pieces of CaCO3 rock/sand ). Saturation state, at a given temperature, salinity, pressure, is described by:
omega = [Ca++][CO3=]/Ksp*
where [Ca++] is the calcium concentation, [CO3=] is the carbonate concetration, and Ksp* is the solubility product (adjusted for use in sea water). If calcium goes up, satuation state goes up proportionally. If carbonate goes up, saturation state goes up proportionally. Carbonate concentration is controlled by carbonate alkalinity and pH (all else equal). The higher the alkalinity, all else equal, the more carbonate there is. The higher the pH, all else equal, the more carbonate there is. If both alkalinity and pH go up, carbonate goes up more still. You get the idea.
<a href=showthread.php?s=&postid=12781508#post12781508 target=_blank>Originally posted</a> by capn_hylinur
gottcha---thanks very much for the detailed answer:smokin: