Water density is a crucial property that plays a vital role in various scientific, industrial, and everyday applications. It is defined as the mass of water per unit volume. The density of water is affected by factors such as temperature and pressure.
At standard temperature and pressure (STP) of 20°C (68°F) and 1 atmosphere (atm), the density of pure water is approximately:
1 gram per cubic centimeter (g/cm³) or 1 kilogram per liter (kg/L)
8.34 pounds per gallon (lb/gal)
The density of water is not constant and varies with temperature. As water temperature increases, its density decreases slightly. This is because the molecules become more energetic and move further apart.
The following table shows the density of water at different temperatures at atmospheric pressure:
Temperature (°C) | Density (lb/gal) |
---|---|
0 | 8.37 |
10 | 8.33 |
20 | 8.34 |
30 | 8.31 |
40 | 8.28 |
50 | 8.24 |
At constant temperature, the density of water increases slightly with increasing pressure. However, this change is relatively small and is not typically significant in most applications.
The density of water is essential in numerous fields, including:
The concept of water density has inspired novel applications, including:
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