Anomalous Expansion
A. The Phenomenon:
Most liquids expand continuously on heating and contract on cooling. Water behaves abnormally between $0^\circ\text{C}$ and $4^\circ\text{C}$:
- When water at $0^\circ\text{C}$ is heated, it contracts in volume until $4^\circ\text{C}$.
- At $4^\circ\text{C}$, water has its minimum volume and consequently its maximum density ($1000\text{ kg/m}^3 = 1.0\text{ g/cm}^3$).
- Above $4^\circ\text{C}$, water expands normally like any other liquid.
- Conversely, when water cools from $4^\circ\text{C}$ to $0^\circ\text{C}$, it expands!
B. Hope's Experiment:
A tall metal cylinder filled with water at room temperature ($pprox 12^\circ ext{C}$) has a central trough filled with a freezing mixture (ice + salt). Two thermometers $T_1$ (bottom) and $T_2$ (top) record temperature over time:
- Water in the central region cools. As it cools toward $4^\circ ext{C}$, its density increases, so it sinks to the bottom. Lower thermometer $T_1$ drops rapidly to $4^\circ ext{C}$ and stays locked there.
- Further cooling of the central water below $4^\circ ext{C}$ causes it to expand and become lighter. This colder, less dense water ($3^\circ ext{C}, 2^\circ ext{C}, 1^\circ ext{C}, 0^\circ ext{C}$) rises to the top!
- Upper thermometer $T_2$ drops rapidly from $4^\circ ext{C}$ to $0^\circ ext{C}$, and ice begins to form on the surface, while the bottom thermometer remains safely at $4^\circ ext{C}$!
C. Ecological Importance:
In cold winter climates, lake surfaces freeze at $0^\circ ext{C}$. Because ice is less dense than water, it floats. Furthermore, ice is a poor conductor of heat, insulating the liquid water beneath. The bottom of the lake remains at $4^\circ ext{C}$, preserving aquatic life (fish and plants) throughout the winter.