A burbon on the rocks exists because ice is less dense than water

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SUMMARY

A bourbon on the rocks exists because ice is less dense than water, a phenomenon attributed to the unique molecular structure of water. When water freezes, it forms a hexagonal crystalline structure due to hydrogen bonding, resulting in a lower density compared to liquid water. Specifically, in liquid water, each molecule is hydrogen bonded to approximately 3.4 other molecules, while in ice, each molecule bonds with four others. This structural arrangement creates open spaces, leading to ice's lower density at temperatures below 0°C.

PREREQUISITES
  • Understanding of molecular bonding, specifically hydrogen bonding
  • Basic knowledge of density and temperature relationships in substances
  • Familiarity with the phase changes of water (solid, liquid, gas)
  • Awareness of the unique properties of water compared to other substances
NEXT STEPS
  • Research the molecular structure of ice and its implications on density
  • Study the effects of temperature on the density of various substances
  • Explore the concept of hydrogen bonding in different chemical compounds
  • Investigate the phase diagram of water and its unique properties
USEFUL FOR

This discussion is beneficial for chemistry students, educators, and anyone interested in the physical properties of water and its behavior in different states. It is particularly relevant for those studying molecular chemistry and thermodynamics.

sanjuro
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I am fairly new to chemistry, so this might seem like a stupid question, but I am still interested nonetheless. A burbon on the rocks exists because ice is less dense than water, but how can this be the case when the molecules in a solid are closer together?
 
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Hi Sanjuro :)

You are true for most substance: when the temperature of a substance increases, the density decreases due to the violent motion of the molecules. When the temperature decreases, the density increases, since molecules are more closely packed.

This doesn't hold true for water, where the density will actually DECREASE when the temperature DECREASES.

The reason for this is that at a lower temperature, the water molecules are allowed to form hydrogen bonds, which allows it to form a hexagonal crystalline structure with many open spaces.

To illustrate: in liquid water, each molecule is hydrogen bonded to approximately 3.4 water molecules. In ice this is 4 other molecules.

This page has a nice figure: http://tidepool.st.usm.edu/pix/ice.gif You can see that the lowest density (at low temperature) is at 0 oC and the highest density is at 3.97 oC, that is when the hydrogen bonds are broken, and the water 'collapses' on itself.
 
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