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Density of water

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College Physics III – Thermodynamics, Electricity, and Magnetism

Definition

The density of water is the mass per unit volume of water, typically measured in kilograms per cubic meter (kg/m³). It varies with temperature and pressure, being approximately 1000 kg/m³ at standard conditions (4°C and 1 atm).

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5 Must Know Facts For Your Next Test

  1. The density of water reaches its maximum value at 4°C, which is approximately 1000 kg/m³.
  2. As water is heated above 4°C or cooled below this temperature, its density decreases due to thermal expansion.
  3. Ice has a lower density than liquid water, which is why it floats.
  4. The anomalous expansion of water between 0°C and 4°C prevents bodies of water from freezing solid from the bottom up.
  5. In thermodynamic calculations, variations in the density of water with temperature can significantly impact results involving buoyancy and fluid dynamics.

Review Questions

  • At what temperature does water reach its maximum density?
  • Why does ice float on liquid water?
  • How does the density of water change when it is heated from just above freezing to room temperature?

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