Key examples — intermolecular forces
Where the chapter’s machinery shows up across the bookshelf.
Example 1: water’s bulk modulus from molecular parameters
Estimating for water with (hydrogen-bond energy), (O–O separation) gives . Measured value: 2.2 GPa. The factor-of-2 agreement is remarkable for a one-line dimensional argument and represents one of the few cases where a macroscopic acoustic quantity is calculable directly from molecular-scale parameters. See Cavitation Ch 1.1.
Example 2: the tensile-strength puzzle
Spinodal-limit calculations give in-principle tensile strengths of for water at room temperature. Carefully prepared samples in laboratory have reached ; ordinary water fails at or less. The three-orders-of-magnitude gap motivates the heterogeneous-nucleation story of Cavitation Ch 2.2: real liquids contain pre-existing gas-filled crevices on surfaces that fail far below the homogeneous spinodal.
Example 3: high surface tension of water from hydrogen bonds
Surface tension is approximately the cohesive-energy density times molecular separation: . For water at room temperature, and give — matching the measured 72 mN/m. The directionality of hydrogen bonds, captured in the chapter’s HydrogenBondAngle visualisation, is what makes water’s surface tension exceptional among common liquids (most others sit at ). See surface-tension chapter.
Example 4: van der Waals coexistence and Maxwell construction
For temperatures below the critical , the van der Waals isotherm has a region — unstable. The Maxwell equal-area construction on the isotherm gives the coexistence pressure: a horizontal line drawn so the two areas above and below it (between the line and the isotherm) are equal. The endpoints of this line are the equilibrium densities of liquid and vapour. This is the operative tool for predicting liquid-vapour phase diagrams from molecular-level parameters and .
Example 5: density anomaly of water and ice
Water has a density maximum at 4°C — it expands on cooling below this temperature. Ice is less dense than liquid water. Both anomalies trace to the tetrahedral hydrogen-bond geometry: ice’s open, four-coordinated structure has lower density than the partially-disordered liquid where some hydrogen bonds are broken and molecules pack more closely. This is uniquely consequential for biology (ice floats on lakes) and for the climate.
Cross-book backlinks
- Cavitation Ch 1.1 — what a liquid is: bulk modulus from molecular parameters.
- Cavitation Ch 1.2 — tensile strength in principle: spinodal limit.
- Cavitation Ch 1.3 — the pathetic measured strength: why real water fails so much earlier.
- Cavitation Ch 2.2 — heterogeneous & crevice nucleation: gas-pocket model.
- Physics surface-tension — chapter: from cohesive energy.