Density formula: ρ = m / V. Enter two values to solve for the third.
| Material | Density (kg/m³) |
|---|---|
| Water | 1,000 |
| Ice | 917 |
| Air (sea level) | 1.225 |
| Aluminum | 2,700 |
| Steel | 7,850 |
| Gold | 19,320 |
| Concrete | 2,300 |
| Wood (oak) | 700 |
Density is mass per unit volume (? = m/V). Objects with density less than water (1,000 kg/m³) float. Objects denser than the surrounding fluid sink. Density varies with temperature most materials expand when heated, reducing density.
Density is a fundamental physical property that tells you how much mass is packed into a given volume: ρ = m/V. It determines whether objects float or sink, how materials behave under stress, and plays a critical role in engineering design, chemistry, and earth science.
Water is unique: its solid form (ice) is less dense than its liquid form. Ice has a density of 0.917 g/cm³ vs. liquid water at 1.0 g/cm³. This happens because water molecules form an open crystalline lattice structure when freezing, taking up more space than in the liquid state. This property is critical for aquatic life — ice forms on the surface of lakes, insulating the liquid water below and allowing fish to survive winter.
Engineers use density constantly in material selection. The strength-to-weight ratio (specific strength) is often more important than absolute strength. Aluminum (2.7 g/cm³) is used in aircraft frames over steel (7.87 g/cm³) despite being weaker, because the weight savings are enormous. Carbon fiber (1.6 g/cm³) with its exceptional strength is used in high-performance aerospace and sports applications where minimum weight is critical.
Density measures how much mass is packed into a given volume: ρ = m ÷ V (density = mass ÷ volume). In SI units, density is expressed in kg/m³ or g/cm³ (g/mL). Water's density is exactly 1 g/cm³ (1,000 kg/m³) at 4°C — this is by design, as the gram was originally defined as the mass of 1 cm³ of water. Gold has a density of 19.3 g/cm³, nearly 20× denser than water. Aluminum is 2.7 g/cm³. Lead is 11.3 g/cm³. The least dense solid element is lithium at 0.53 g/cm³ — it floats on water. Air at sea level has a density of about 1.225 kg/m³ (0.00122 g/cm³). Density determines whether objects float or sink in a fluid: an object floats if its average density is less than the fluid's density.
For most materials, density decreases as temperature increases (thermal expansion). A notable exception is water between 0°C and 4°C — water actually becomes denser as it warms from freezing to 4°C, then becomes less dense above 4°C. This is why ice floats and why lakes don't freeze solid from the bottom up. For gases, density is strongly affected by both temperature and pressure (ideal gas law: ρ = PM ÷ RT, where P is pressure, M is molar mass, R is the gas constant, T is absolute temperature). At high altitude, lower air pressure means lower air density — at 10,000 feet, air density is about 75% of sea-level density, which is why aircraft engines produce less power and baseballs travel further in Denver than at sea level.
Density is used across many practical applications: Archimedes' principle: a ship floats because its total average density (including all the air inside) is less than water's density. A solid steel ship would sink; the hollow steel hull with air inside floats. Quality control: density testing verifies material purity — gold dealers use density measurement to detect fake gold. Geology: rock density helps geologists identify mineral composition without chemical analysis. Medicine: bone mineral density (BMD) measured via DEXA scan diagnoses osteoporosis. Food science: the density of must (crushed grapes) predicts wine alcohol content (Brix scale). Brewing: specific gravity (density relative to water) measures fermentation progress in beer and wine production.