Anyone measure their rate of fermentation?

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Happy Holidays tCan, I Gimped 'em for you. ;)

AlcoholVsCO2.jpg
 
...especially when the CO2 is coming out of solution faster than it's being produced.
Not so once equilibrium is reached. The outflow will then be the same as the production rate.

Curious difference of opinions here...

Now, if we were talking distilled water, I'd say ajdelange was correct, but in reality we are talking about a varying solution which probably has varying CO2 solubility. More data please.
 
Not so once equilibrium is reached. The outflow will then be the same as the production rate.

For most of the run yes. But as fermentation slows, that may not be true. Saturation does not necessarily mean equilibrium. Incredible how many factors there are to consider. I'm not hugely familiar with gas exchange in liquids so I could be wrong and it could be only a minor consideration.

For experimental purposes, an indicator might be used. Bromothymol blue is one that comes to mind. I don't know if you can drink it though. And I'm not willing to sacrifice that ability. :cross:


Happy Holidays tCan, I Gimped 'em for you. ;)

AlcoholVsCO2.jpg

YAAAY! Thanks!
 
Ultimately, of course, the solubility of CO2 in fermenting wort/beer does depend on the composition of the solution. CO2 is, for example, approximately 10 times more soluble in EtOH than it is in water and Henry coefficient depends, thus, on the mole fraction of EtOH. The equilibrium concentration of CO2 depends on the Henry coefficient, the fugacity of CO2 over the solution and the activity of carbonic acid in the solution. But Henry coefficient is, for all practical purposes, constant until the mole fraction of EtOH approaches 0.2 ( in a 5% ABV solution it is about 0.016), at 1 atmosphere fugacity is equal to pressure and, as ionic strength in beer is in the first place low and in the second place does not change appreciably over the course of fermentation and as H2CO3 is not a charged species activity coefficient for H2CO3 will be a constant very close to 1 throughout. Thus, to the level we could reasonably make measurements, solubility of CO2 is constant being determined by pressure (1 atmosphere once the surface is blanketed by CO2) and temperature. The presence of extract also has an effect on the mole fraction of the solvent but in a 12 °P maltose wort the mole fraction of water is 99.3%.

That's the theoretical evidence. Practical data can be found in the Zahm and Nagle (ASBC) table which gives volumes of dissolved CO2 in beer as a function of temperature and pressure. These tables are used for the analysis of beers of all alcoholic strengths. If ASBC had found that failure to account for alcohol content, true extract etc. caused appreciable error then they would have prepared additional tables or given correction factors based on whatever parameter was responsible for the variation.

"Equilibrium" here does not mean chemical equilibrium of the system. Clearly a system in which a reaction (fermentation) is underway cannot be at chemical equilibrium. What it does refer to is equilibrium WRT CO2. If CO2 does not escape at the rate it is formed then the chemical potential of CO2 in solution rises to the point where it exceeds the chemical potential of CO2 in the gas over the surface of the fermenting wort. This causes CO2 to move from higher to lower potential i.e. into the headspace. This continues to the point where the potentials are equalized. WRT the headspace: the total pressure in a fermenter open to the atmosphere is 1 atmosphere. Thus the maximum partial pressure of CO2 in the headspace can be no more than 1 atmosphere and that is reached when CO2 from the ferment has displaced all the air. From then on at any time the concentration of carbonic acid exceeds the Henry coefficient gas moves to the headspace. Any time [H2CO3] < Khy gas moves to the wort. Thus the equilibrium condition here represents one in which the headspace is full of CO2 at fixed pressure and temperature, the wort is at fixed temperature and CO2 is leaving the wort at the rate the yeast produce it. Note: We define the Henry coefficient here such that [H2CO3] = pCO2*Khy with the units of Khy being mg/L-atm.

WRT the indicator - I'm not sure what you would expect that to tell you. Wort pH drops appreciably in the first few hours of a fermentation as the yeast establish an environment optimum for their well being (and suboptimal for competing organisms). Thereafter the yeast tend to buffer wort pH to a constant value dependent on the strain. Thus pH is more indicative of yeast strain than CO2 content. Using the nominal 1 atm CO2 pressure over ferementing beer (resulting in about 1 volume dissolved dependent on temprature) the pH would be, in water, about 3.9. More typical beer pH would be 4.5 or so (though pH of as low as 4 are found in some ales).
 
One unaccounted variable would be pressure, using tCan's balloon method. Each time the balloon inflates, pressure increases. Each time the balloon is deflated, pressure abruptly drops to ambient pressure. And that brings up a second, unaccounted variable, barometric pressure throughout the experiment....

I'd like to straighten out the blue, mol CO2, curve in the above diagram with more accurate data. I think you'd see a smooth slope instead of the bumpy one. Maybe a cloud passed by or the weather cleared at hour 50, and/or the vessel temperature dropped, causing more CO2 to be released for a period of time...
 
The ambient temperature was also up at least 2C at that time. But I think you are correct. I'm inclined to think that the 'wave' in the data is erroneous. I'd not expect the fermentation rate to increase again after reaching it's peak. A more linear fall off, like the rest of the graph shows seems likely.

I might continue to do this under a different method. Perhaps just count the number of bubbles coming out of an airlock per minute. Waiting twenty minutes for a balloon to fill up twice is not exactly my cup of tea.
 
Still won't account for barometric pressure changes. Log that and temperature too, and correlate.
 
Still won't account for barometric pressure changes. Log that and temperature too, and correlate.

Will it not? The pressure above the water in the lock still affects the pressures inside the jug? Interesting. I guess that's right. I now remember reading about a similar set of circumstances. Maybe in my Orgo or bio book. I'll see if I can find it.
 
All I know is that my still carboys start to bubble during a low pressure system. So I assume the affect is there throughout fermentation--when the barometric pressure is low, less CO2 can stay in solution, when high more will be retained, just like fluctuations in temperature. There is no real world STP (standard temperature and pressure), it's constantly changing.
 
The airlock is a mini-manometer. The difference between the water level in the 2 arms of the U is the difference in pressure between the headspace and the atmosphere. If the water on the carboy side is 1/2" lower than the water on the open side the pressure difference is 1/2" WC (water column). As gas is evolved in the carboy this difference increases until the lock breaks (blurps) at which point the pressures are equalized and the levels return to being the same. So just after a blurp the pressure in the heaspace is the same as in the atmosphere. Practically speaking, a dramatic pressure change would be 1" out of 30 (mercury inches this time) after passage of a strong front i.e. about 3%. The equilibrium saturation level for the beer would then change by about 3%. Given the methods under discussion here I don't think that would be an appreciable source of error. Were a flow meter being used its reading would be corrected for temperature (effects density of gas and water vapor content) and barometric pressure (effects density).
 
I just re-read the thread. What fun! I said some things wrong at certain points though. IDK what I was saying! Must've been the nature of the experiment if you catch my drift. hehe.
 

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