Date: Mon, 8 Nov 1999 17:04:31 -0500 (EST)
From: Paul Kruse plkruse@iu.net
Nope. Go back and think about the following statement from what you wrote:
Sea ice forms first as salt-free crystals near the surface of the sea.
That is exactly what happens
Is the following then a fair world-trawler-list consensus statement (W-T-L
CS) on the subject?
This is the basis of the centigrade scale.
Seawater and brine solutions freeze at a lower temperature. Thats how you
make ice cream and why the sea doesnt freeze when the ponds do. Fahrenheit
got it down to 0 degrees with 50% salt.
Thats why icebergs are fresh water and freezing can produce fresh water
commercially.
In the open ocean the brine constituent is in equilibrium with an
essentially infinite volume and therefore stays constant even as H2O
molecules are lost to the crystalline matrix. The value of 28.6 deg F.at
35 parts / 1000 saline is obtained under these conditions.
In a container, in the freezer, as H2O is lost to the matrix the residual
water becomes less, the salt concentration therefore increases. This
depresses the freezing point below the 28.6 given above.
Respectfully,
hmp
hpollock@massmed.org writes:
Thats why icebergs are fresh water and freezing can produce fresh
water
commercially.
I'm surprised that no-one has brought on the subject of freezing
alcohol-water mixtures (i.e. wine). If you substitute the Na-Cl in
the statements above with C2-H5-OH, you get an ever increasing
concentration of alcohol. Easy and cheap way of operating a still in
your freezer. :-)
Cheers - George
Apple Jack?