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Water (H2O) has several physical properties that appear contradictory if you only consider its small molar mass (Mr = 18):
Each of these is explained by the extensive hydrogen bonding in liquid and solid water.
Consider the Group 16 hydrides: H2O, H2S, H2Se, H2Te. Based on molecular mass alone, one would expect boiling points to rise steadily down the group as London forces increase. The actual data tell a very different story:
| Hydride | Mr | Boiling point (degC) |
|---|---|---|
| H2O | 18 | +100 |
| H2S | 34 | -61 |
| H2Se | 81 | -41 |
| H2Te | 130 | -2 |
If water followed the trend of the other hydrides, extrapolation gives a predicted boiling point of around -80 degC. The observed +100 degC is ~180 degC higher than expected.
This enormous difference is because liquid water contains extensive hydrogen bonding networks, which H2S and the heavier hydrides lack (S, Se, Te are less electronegative and larger, so they do not support hydrogen bonding). Water molecules need far more energy to escape into the gas phase.
Each H2O molecule can form up to four hydrogen bonds: the O has two lone pairs (acceptors) and two H atoms (donors).
H
\
O . . . H
/ \
H O -- H
. /
. H
.
O -- H
/
H
The result is a 3D network in which each molecule is H-bonded to several neighbours. To melt ice or boil water you must supply enough energy to break or disrupt these H bonds - hence the high m.p. (0 degC) and b.p. (100 degC).
Numerically: a hydrogen bond in water is about 20 kJ mol-1; there are on average about 3-4 per molecule in liquid water, contributing roughly 40 kJ mol-1 to the enthalpy of vaporisation of 41 kJ mol-1.
For almost all substances, the solid is denser than the liquid because particles pack more closely in the ordered solid. Water is the striking exception: ice at 0 degC has a density of 0.917 g cm-3, while liquid water at 0 degC is 1.000 g cm-3. Ice therefore floats.
In ice, each water molecule forms 4 hydrogen bonds to its neighbours in a tetrahedral arrangement around O. This rigid geometry gives a very open, hexagonal lattice with large gaps between the molecules.
H H
| |
H - O . . . H - O - H
| :
: :
H H
| |
H - O . . . H - O - H
| |
When ice melts, the tetrahedral lattice partially collapses - about 10% of the H bonds break - allowing water molecules to pack more efficiently. The liquid is therefore denser than the solid.
Liquid water actually reaches its maximum density at ~4 degC, not at 0 degC. Between 0 and 4 degC, collapse of residual ice-like structure dominates, increasing density. Above 4 degC, ordinary thermal expansion dominates, decreasing density.
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