Density is a measure of how much mass is contained in a given volume. It is calculated by dividing the mass of an object by its volume. The formula for density is:
center;">Density = Mass / Volume
Density is a fundamental property of matter and can be used to identify and compare different substances. It is typically measured in units such as grams per cubic centimeter (g/cm3) for solids and liquids, and kilograms per cubic meter (kg/m3) for gases.
Factors Affecting Density
The density of a substance can be affected by changes in temperature and pressure. Generally, as the temperature of a substance increases, its density decreases, and as the pressure increases, the density also increases.
Examples of Density
Some common examples of density include:
Ice has a lower density than water, which is why it floats.
Iron has a higher density than wood, which is why iron sinks while wood floats.
Heliumgas has a lower density than air, which is why helium-filled balloons float in air.
Applications of Density
The concept of density has wide-ranging applications in various fields, such as:
Identifying unknown substances through density measurements.
Determining the purity of a substance by comparing its measured density to the known density of the pure material.
Represent data in graphical displays to reveal patterns of daily changes in length and direction of shadows, day and night, and the seasonal appearance of some stars in the night sky.
Earth’s Systems
Students who demonstrate understanding can:
Develop a model using an example to describe ways the geosphere, biosphere, hydrosphere, and/or atmosphere interact.