
A rice cooker has no sensor that can “taste” the rice. In a simple mechanical model, the useful signal is the temperature at the base of the inner pot, with water providing the physical reference.
As the rice and water heat up, they approach water’s boiling point at the local air pressure. Much of the continuing energy then changes liquid water into vapour instead of rapidly raising its temperature. While plenty of free water remains, the pot base therefore stays close to that boiling temperature. The value is not universally 100°C, because boiling point changes with atmospheric pressure and altitude.
Once most of the water has been absorbed by the rice or evaporated, this temperature buffer disappears and the pot base can heat beyond the earlier plateau. In a traditional cooker, a thermostat and mechanical linkage against the inner pot detect that rise, release the cooking switch and move the appliance to a lower-power keep-warm state. The cooker is not proving that every grain is done; it is detecting that little free water remains. An incorrect rice-to-water ratio can still produce rice that is too firm or too soft even when the switch operates normally.
Modern electronic and induction models may use several sensors and programmed heating stages, but the central clue remains similar: water’s phase change constrains the temperature for a time, then the curve changes as free water runs out. What looks like a timer is really a response to a thermodynamic signal.
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