Look at Ice Through a Microscope - Charlie

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    Ice Microscope
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Looking at ice through a standard microscope reveals that the crystalline atomic structure is generally too small to be seen, as structures below about 1/4 micron are not visible with light. However, one can observe the agglomerated structure, including trapped air bubbles and dirt. The clarity of ice, whether cloudy or clear, is influenced by the freezing process, with clear ice typically requiring degassed water. Slow freezing allows air to escape from the solution, contributing to clearer ice. Understanding these factors can enhance the study of ice's physical properties.
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hi every1

what do you see if you look at ice through a standard microscope? is the structure too small to be seen?

thanks

charlie
 
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Which structure- the crystalline atomic structure, the grain bounderies, the aggregations, the inclusions?
 
i meant the crystalline atomic structure, but would also be interested to know what the aggregations and the inclusions are.

thanks :)
 
Structures below about 1/4 micron are too small to see with visible light, given a proper definition of 'see'. Depending on the specific ice sample, you may be able to determine the agglomerated structure, and could most likely see all the trapped air bubbles and dirt.
 
ok thanks! I've always wondered what makes the difference between cloudy and clear ice. Does it depend how quickly the ice is frozen?
 
Good question- I don't know. All I know is that to get clear ice, one must degas the water. I guess if the ice feezes slowly enough, in the right geometry, the air can come out of solution and escape the liquid water.
 
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