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Originally Posted by Kaiser
A.J do you have practical observations to support this? I know we do have a disagreement on this and your understanding of the underlying chemistry is greater than mine.
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The 'observation' that it will taste chalky is not mine but rather what I have been told by people who have put lots of chalk into beer and, of course, Gordon's statements about alka selzer which is in his book and which he has mentioned in a couple of talks he has given. The rest is my attempt to explain why this might happen. If you have chalk in an acidic medium it is going to dissolve. Mash and wort contain a fair amount of acid. At pH 5.5 88% of the carbo will be in the form of CO2. In hot mash or the kettle CO2 isn't very soluble so a lot of that gas will escape. If gas escapes then the balance between carbonic, bicarbonate and carbonate is upset and can only be restored if more carbo is supplied by the system or the pH goes up. Both of these happen but the mash is a buffer so that the pH doesn't change that much but it does change some and will continue to do so until the system comes to equilibrium with atmospheric CO2 which will never happen until the pH reaches the vicinity of 8.4.
Quote:
Originally Posted by Kaiser
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I would really expect most of the undissolved chalk to be trapped in the filter bed. Certainly if you are withdrawing bright wort that should be the case. So that leaves the time in the mash tun which is usually an hour for ales but could be several hours in a decoction mash. CaCO3 seems to react slowly and so even does bicarbonate as I was surprised to discover when I recorded pH continuously during an alkalinity titration (
http://www.wetnewf.org/pdfs/measuring-alkalinity.html). So perhaps that's what is preventing much from dissolving. Or perhaps, even if some extra dissolves the yeast, which strive to maintain a pH they like, simply put more effort into secreting the acids they need in order to overcome the additional buffering imposed by the dissolved chalk (which in itself should be an argument for getting or keeping the chalk out).
But if the chalk isn't dissolving, how do we explain the chalky taste?
Quote:
Originally Posted by Kaiser
Yes, there are bicarbonates in beer. If you have 2 atm CO2 pressure and a pH of 4.5 you need about 60 ppm HCO3 for equilibrium. But those 60 ppm are only a function of the CO2 content and the pH and not the original brewing water.
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Good point. I get 72 ppm for the bicarb content at 2 Atm and pH 4.5 (I get about the same number as you do if I use ideally dilute chemistry). But if I increase the pH to 4.7 the bicarb zooms to 115 i.e. about doubles. Base purely on my line of reasoning I would suggest that the stress of the extra alkalinity would result in a higher pH for the beer but that's essentially saying that the yeast are unable to handle the extra alkalinity and I don't know that. The usual reason for controlling water alkalinity is for the benefit of the enzymes in the mash tun. I certainly have no experimental data correlating start and finish fermentation pH's for unusually alkaline worts.
Let's assume that more calcium carbonate is dissolving (I think that part has to be true if enough time is involved) and that this appears in the fermenter and that the yeast can handle the extra buffering load. That leaves the calcium as a possible explanation. Perhaps Gordon's "AlkaSelzer" is more apt than "chalky". Perhaps the guys (I think of my LHBS operator in particular) that use that phrase are victims of confirmation bias "I used chalk and the beer tastes chalky." But then any beer loaded with calcium and bicarbonate would taste like AlkaSelzer and I guess they do.
Quote:
Originally Posted by Kaiser
I agree that chalk can have a negative impact on beer taste but I don’t thinks it happens via that way you described it and maybe we can discuss this.
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I'm not going to pound my fist on the table and declare my explanation gospel. There certainly are questions