Density Calculator
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Contact UsThe concept of density was first systematically studied by Archimedes (287-212 BCE) through his work on buoyancy. His famous "Eureka!" moment came when discovering that the volume of water displaced by an object equals the object's volume, leading to methods of measuring density. Modern understanding of density incorporates atomic theory and material science, explaining how atomic structure, electron configuration, and intermolecular forces determine a material's density.
ρ = m / V
ρrelative = ρsubstance / ρreference
ρ = ρ₀ / (1 + αΔT) [temperature dependence]
| Material Type | Density (kg/m³) | Notes |
|---|---|---|
| Air (at STP) | 1.225 | 78% N₂, 21% O₂, 1% other gases |
| Water (20°C) | 998 | Maximum density at 4°C |
| Mercury | 13,546 | Only liquid metal at room temp |
| Gold | 19,320 | One of the densest precious metals |
Most materials expand when heated, reducing their density. Water is unique because it's densest at 4°C (39.2°F). This explains why ice floats and why lakes don't freeze solid.
Density (ρ) equals mass (m) divided by volume (V): ρ = m/V. This means if you know any two values, you can calculate the third using this relationship.
Objects float when their density is less than the fluid they're in. For example, wood (density ~0.7 g/cm³) floats in water (density 1 g/cm³), while iron (density 7.87 g/cm³) sinks.
Gases are highly compressible, so their density increases significantly with pressure. Liquids and solids are nearly incompressible, so pressure has minimal effect on their density.
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