thrlride said:
So, in other words... The longer the tank water stays in the reactor the lower the PH will be?
No, the longer the water stays in the reactor without further addition of CO2 the higher the PH will be until PH, dissolved ions, carbonic acid and dissolved CO2 achieve a balance in the water which is at the PH point were Aragonite no longer dissolves. I think is about 7.6
Lets assume the process without water flow for a moment. You have a bucket with media, you add aquarium water and then bubble CO2 trough the media and then stop the CO2.
Here is what I see happening:
CO2 dissolves in the water and turns into Carbonic Acid lowering the PH. As the Carbonic Acid dissolves the media Calcium and Bicarbonate Ions are now dissolved in the water and the PH starts to increase until everything achieves a balance (saturation) were no more Calcium and Bicarbonate Ions can be added to the water Aragonite stops dissolving (Dissolution depends on the PH level as well as the amount of alkalinity in the water), free CO2 in the water has either escaped back into the air or turned some of the Carbonic Acid into Bicarbonate Ions etc.
Now let's make it dynamic. Take some of the saturated water out, add new tank water bubble more CO2 and the reactions start again but this time you do get the water out and add new water and CO2 continuously.
The reactions will try to increase the PH but the continued addition of CO2 keeps it at a lower level thus maintaining the process going. The level at which PH stabilize will depend on the ratio of the amount of water added and removed, and the CO2 added and consumed.
For example oversimplifying if you have a water flow of 25 ml/hr and a CO2 bubble rate of 20 bpm and the PH stabilizes at 6.5, Then the PH will approx. stay at 6.5. If you double the flow to 50 ml/hr and the CO2 to 40 bpm the PH will tend to remain at 6.5
but there is a limit. You can continue increasing the flow and the CO2 and this will happen as long as the water stay in contact with the media long enough to complete the needed dissolution.
At certain point the water will pass trough the media too fast to dissolve and you will start to carry CO2 and carbonic acid out with the effluent water. The PH can stay low but the water will not be saturated with ions so the alkalinity in the effluent starts to drop.
So until the point were the flow is too high, the total amount of alkalinity added to the tank will depend of the following:
a) The higher the flow the more alkalinity
b) The lower the PH the more alkalinity
If the flow exceeds the retention time for a given PH the alkalinity in the flow starts to decrease. At one point the reduction in alkalinity in the effluent is faster than the increase in flow so the total alkalinity added starts to decrease and the non-reached Acid and undissolved CO2 starts to increase in the effluent thus starting to lower the PH of the overall tank.
Sorry it might be confusing but is difficult for me to explain how the several variables interact with each other.
This article may help to explain better than I could:
http://reefkeeping.com/issues/2002-04/rhf/feature/index.htm