Amorphous ice is less dense than crystalline, why?

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    Amorphous Ice
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SUMMARY

Amorphous ice exhibits a lower density than crystalline ice due to its less ordered structure, which allows for more voids and air pockets. The densities of various forms of amorphous ice, such as Low-Density Amorphous (LDA) and High-Density Amorphous (HDA) ice, are confirmed to be accurate and not typographical errors. Crystalline ice, with its geometric arrangement, traps air between intermolecular hydrogen bonds, resulting in a fixed density. The packing efficiency of crystalline structures is generally superior to that of amorphous forms, leading to a more compact arrangement of molecules.

PREREQUISITES
  • Understanding of molecular structures and bonding, particularly hydrogen bonds.
  • Familiarity with concepts of density and packing efficiency in materials science.
  • Knowledge of the differences between crystalline and amorphous solids.
  • Basic principles of thermodynamics related to compression and phase changes.
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  • Research the properties and applications of Low-Density Amorphous (LDA) and High-Density Amorphous (HDA) ice.
  • Explore the role of hydrogen bonding in determining the physical properties of water and ice.
  • Investigate the effects of pressure on the structural integrity of crystalline ice.
  • Study the packing factors of various crystalline structures to understand their efficiency.
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Researchers in materials science, chemists studying phase transitions, and professionals in engineering fields focused on the properties of ice and water. This discussion is particularly beneficial for those examining the implications of ice density in natural and industrial processes.

Mk
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http://www.lsbu.ac.uk/water/amorph.html puts the densities of various forms of amorphous ice at densities that are very low. g/cm-3 in fact. Is this a typographical error? If not why is it so dense? Crystalline ice's densities are attributed to all the empty space in-between crystals, amorphous ices have much less empty space.
 
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Mk said:
amorphous ices have much less empty space.

And this is based on what?
 
Hi Mk,

Imagine you have to fill a given box with small rigid cubes. Firstly you trow (fast and randomly) the cubes in the box and secondly you arrange them one by one.
 
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Which one is the amorphous and crystalline? I'm assuming the first is amorphous, that's why its dess dense?
 
According to the article, there's LDA and HDA. Which are you asking about ?
 
Mk said:
http://www.lsbu.ac.uk/water/amorph.html puts the densities of various forms of amorphous ice at densities that are very low. g/cm-3 in fact. Is this a typographical error? If not why is it so dense? Crystalline ice's densities are attributed to all the empty space in-between crystals, amorphous ices have much less empty space.

So amorphous is a bit more dense than crystalline, if remember its density about right ... the differences are of the order of some tens or percents depending on what forms of ice in question ... doesn't appear a typo to me.
 
I would have thought that amorphous (having no crystalline structure) has a larger opportunity for trapping air, whereas crystalline being geometric contains a fixed amount.

ie, the crystalline ice traps air between the intermolecular (H) bonds, and as such has a fixed density, while amorphous ice has a random element (in molecular alignment) leaving extraneous spaces between said molecules.

The analogy above is intuitive - being a random pile (amorphous) allows more gaps so more air and thus less density, compared to a stack with no gaps (crystal)...
 
But then, you can also compress amorphous ice and find stable configurations that lie on the other side of an energy barrier, enabling a higher final density.
 
True, but that doesn't exclude the possibility of amorphous ice having a lower density up until it is compressed. :D

How much can crystalline ice be compressed before it loses its structure?
 
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This issue is best dealt with from the standpoint of engineering or chemistry. The issue is one of crystal structure and what, exactly, different structures look like. http://www.chem.lsu.edu/htdocs/people/sfwatkins/ch4570/lattices/lattice.html" is another site showing packing factors of various crystals. It is important to note that the packing factor is the same for all materials. It is the geometric relationship between the number of particles and the volume.

Amorphous is tougher than crystalline because the density can vary, but as a general rule, ordered packing is more efficient than disordered, thus crystalline is always (afaik) more efficiently packed than amorphous. The reason has been said above: in amorphous, you get semi-random arrangements that often cause large voids.
 
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