ljm
Member
None of the SG hydrometers I have found are calibrated to 20C. I have been thinking about a method or methods to do this conversion, but can't try them without, for example, both gravities for a 10P solution.
The more complicated nerdy method starts with equality of mass of extract (wex):
wex = d15 * SG15 * P * V15 = d20 * SG20 * P * V20
where
d15 = density of water at 15C
V15 = volume of wort at 15C
SG 15 = specific gravity of wort at 15C = SG(15/15)
etc.
Then a little algebra gives
SG20 = d15/d20 * SG15 * V15/V20
To get the volume ratio I could use the cubic coefficient of expansion for water (k) (or better yet for wort). And this the first problem - for water at 20C k = 2.07E-4; at 15C k=1.51E-4
Anyway,substituting the volume ratio with V15/V20 = exp(k*(20-15)) ought to give me an answer for SG(20/20). Except (1) I can't find any SG(15/15) and SG(20/20) for the same Plato and (2) k is clearly not even close to constant which is important since the none of the multiplicative factors in the SG20 equation are very far from 1.
I also thought perhaps if there were reliable SG20 and SG15 data the equation could be used to find an optimal k to force the conversion to work for other solution concentrations.
The easiest way might be to multiply SG(15) by the density ratio of water at the two temperatures. But what fun is that? And I still need some data for comparison.
Any help?
The more complicated nerdy method starts with equality of mass of extract (wex):
wex = d15 * SG15 * P * V15 = d20 * SG20 * P * V20
where
d15 = density of water at 15C
V15 = volume of wort at 15C
SG 15 = specific gravity of wort at 15C = SG(15/15)
etc.
Then a little algebra gives
SG20 = d15/d20 * SG15 * V15/V20
To get the volume ratio I could use the cubic coefficient of expansion for water (k) (or better yet for wort). And this the first problem - for water at 20C k = 2.07E-4; at 15C k=1.51E-4
Anyway,substituting the volume ratio with V15/V20 = exp(k*(20-15)) ought to give me an answer for SG(20/20). Except (1) I can't find any SG(15/15) and SG(20/20) for the same Plato and (2) k is clearly not even close to constant which is important since the none of the multiplicative factors in the SG20 equation are very far from 1.
I also thought perhaps if there were reliable SG20 and SG15 data the equation could be used to find an optimal k to force the conversion to work for other solution concentrations.
The easiest way might be to multiply SG(15) by the density ratio of water at the two temperatures. But what fun is that? And I still need some data for comparison.
Any help?