Talk:Amorphous ice: Difference between revisions
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:This sounds like [[supercooling]] to me. If you carefully cool water in a smooth container to below its freezing point but above its [[glass transition temperature]], it will remain liquid. A supercooled liquid will crystallize suddenly if it's disturbed and heat up in the process ([[heat of fusion]]). Amorphous ice is what you get if you continue cooling it past the glass transition temperature of water (which is difficult to measure but it's definitely colder than it ever gets outdoors). Because it gets easier to crystallize as the temperature decreases, it's practically impossible to reach the glass transition temperature unless you do it really fast, hence the difficulty of making amorphous ice. —[[User:Keenan Pepper|Keenan Pepper]] 16:24, 7 October 2005 (UTC) |
:This sounds like [[supercooling]] to me. If you carefully cool water in a smooth container to below its freezing point but above its [[glass transition temperature]], it will remain liquid. A supercooled liquid will crystallize suddenly if it's disturbed and heat up in the process ([[heat of fusion]]). Amorphous ice is what you get if you continue cooling it past the glass transition temperature of water (which is difficult to measure but it's definitely colder than it ever gets outdoors). Because it gets easier to crystallize as the temperature decreases, it's practically impossible to reach the glass transition temperature unless you do it really fast, hence the difficulty of making amorphous ice. —[[User:Keenan Pepper|Keenan Pepper]] 16:24, 7 October 2005 (UTC) |
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:: Thanks for the explanation :) [[User:Saigon from europe|Saigon from europe]] 21:29, 9 October 2005 (UTC) |
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==Relevance== |
==Relevance== |
Revision as of 21:29, 9 October 2005
I merged these 5 articles into one because they were redundant and having separate articles was stupid, but then I googled and realized all the content was just cut-and-pasted from http://www.lsbu.ac.uk/water/amorph.html. I'm working on writing some original content (at Amorphous ice/Temp) now. —Keenan Pepper 16:14, 3 October 2005 (UTC)
Creation of amorphous ice at home
It happens from time to time glass/bottle of water to be found liquid-like if left outdoors when temperature moves from above 0 to below 0 C. On first touch, bottle suddenly freezes. We were explained that this is because water acquired same structure as glass (i.e. Amorphous ice), and then it changed to real cristal-ice. But as I read this article, this does not match -- amorphous ice requires sudden, not slow temperature change. Could someone explain me mentioned phenomenon? Saigon from europe 15:15, 7 October 2005 (UTC)
- This sounds like supercooling to me. If you carefully cool water in a smooth container to below its freezing point but above its glass transition temperature, it will remain liquid. A supercooled liquid will crystallize suddenly if it's disturbed and heat up in the process (heat of fusion). Amorphous ice is what you get if you continue cooling it past the glass transition temperature of water (which is difficult to measure but it's definitely colder than it ever gets outdoors). Because it gets easier to crystallize as the temperature decreases, it's practically impossible to reach the glass transition temperature unless you do it really fast, hence the difficulty of making amorphous ice. —Keenan Pepper 16:24, 7 October 2005 (UTC)
- Thanks for the explanation :) Saigon from europe 21:29, 9 October 2005 (UTC)
Relevance
Is there any utility to amorphous glass, or is it solely a curiosity? Perhaps this ice has some interesting properties? All I really know at this point is its definition and how to make it.
- Amorphous glass or amorphous ice? All glass is an amorphous solid, as far as I know... so its utility is for things like Window and Eyeglasses.
- I don't know if amorphous ice has any utility. :) --Syrthiss 19:47, 7 October 2005 (UTC)
- And if you would like to make sinking ice cubes this might help... --Mac Davis 12:51, 8 October 2005 (UTC)
Units
I've just gone ahead and changed the units to something more sensible (Kelvins, with Celcius and Fahrenheit in parentheses). Also fixed botched conversion from GPa to kilobars --Sander Pronk 21:11, 7 October 2005 (UTC)
Density
Does anybody know the actual densities of low and high density amorphous ice?
- LDA, 0.94 g cm^-3
- HDA, 1.17 g cm^-3
- VHDA, 1.26 g cm^-3
What I don't understand is how the denisties are less than that of normal liquid water, which is 1 g/cm^3. Ice Ih would be denser, and common sense tells us amorphous ice is even denser. --Mac Davis 07:54, 8 October 2005 (UTC)
- Well, water is an odd substance. Normal water ice (ala Ice cubes) is less dense than liquid water. I don't know the density of normal water ice, but I would suspect maybe 0.9. --Syrthiss 13:49, 8 October 2005 (UTC)
- Sorry, I really do know that ice is less dense than water. The ice article, puts it at 0.917 g/cm³ at 0 °C, whereas water has a density of 0.9998 g/cm³ at the same temperature.
- "Liquid water is most dense, essentially 1.00 g/cm³, at 4 °C and becomes less dense as the water molecules begin to form the hexagonal crystals of ice as the temperature drops to 0 °C."
- So, it is not that difficult to understand why solid ice is less dense, because there is so much empty space in between the hexagonal crystals of ice Ih. But amorphous ice has no crystals, and that would mean there as not as much empty space, therefore the density is greater. The density is much less though, why? --Mac Davis 07:54, 9 October 2005 (UTC)