Density Calculator
Calculate Density, Mass, or Volume Using ρ = m/V
Calculate Density from Mass and Volume
Calculate Mass from Density and Volume
Calculate Volume from Density and Mass
Density of Common Materials Reference
| Material | Density (kg/m³) | g/cm³ | Category | Notes |
|---|---|---|---|---|
| Air (at sea level) | 1.2 | 0.0012 | Gas | Varies with temperature, pressure |
| Water (4°C) | 1000 | 1.0 | Liquid | Reference standard density |
| Oil (typical) | 920 | 0.92 | Liquid | Less dense than water, floats |
| Cork | 240 | 0.24 | Solid | Very light, floats easily |
| Wood (pine) | 500 | 0.50 | Solid | Varies by type (400-1200 kg/m³) |
| Concrete | 2400 | 2.4 | Composite | Durable building material |
| Glass | 2500 | 2.5 | Solid | Varies by composition |
| Aluminum | 2700 | 2.7 | Metal | Light metal, used in aerospace |
| Iron | 7874 | 7.87 | Metal | Common structural metal |
| Copper | 8960 | 8.96 | Metal | Excellent conductor, valuable |
| Lead | 11340 | 11.34 | Metal | Very dense, toxic |
| Gold | 19300 | 19.3 | Metal | Precious metal, very dense |
| Mercury | 13546 | 13.55 | Liquid metal | Only liquid metal at room temp |
| The Earth | 5515 | 5.5 | Planet | Average density of entire planet |
Density is mass per unit volume, typically denoted by Greek letter ρ (rho). Fundamental property describing how much matter is packed into a given space. Intensive property: doesn't depend on amount of material. Example: gold and lead same density whether 1 gram or 1000 grams.
Key Concepts:- Intensive property: Doesn't change with quantity (1 kg or 10 kg of iron: same density)
- Material characteristic: Each pure substance has unique density
- Temperature dependent: Usually decreases with temperature (volume expands)
- Pressure dependent: Increases with pressure (volume compressed)
- Float/sink indicator: Denser than water (>1 g/cm³) sinks; less dense floats
- Gases: 0.0001 - 10 kg/m³ (hydrogen to chlorine)
- Liquids: 600 - 13600 kg/m³ (oil to mercury)
- Solids: 200 - 22600 kg/m³ (cork to platinum)
- Reference: Water = 1000 kg/m³ = 1 g/cm³ = standard baseline
Solids & Liquids: Slight density change with temperature. Density generally decreases with increasing temperature (thermal expansion). Iron: 7874 kg/m³ at 0°C → 7750 kg/m³ at 500°C. Gases: Density highly sensitive to temperature. Using ideal gas law: ρ ∝ 1/T. Doubling absolute temperature halves density at constant pressure.
Pressure Effects:Solids & Liquids: Relatively incompressible. Density increases slightly with pressure. Water: minimal change (0.5% increase at 1000 atm). Gases: Highly compressible. Density proportional to pressure at constant temperature. Using ideal gas law: ρ ∝ P. Doubling pressure doubles density.
Notable Exception - Water:Water has maximum density at 4°C (1000 kg/m³). Below 4°C, density decreases as temperature falls. At 0°C (freezing): 917 kg/m³ (ice is less dense). This anomaly causes ice to float on water. Critical for aquatic life in frozen lakes.
Practical Implications:- Always specify temperature/pressure when density values critical
- Room temperature (20°C) standard reference for most materials
- Cryogenic temperatures (very cold) increase density dramatically
- Deep ocean pressures significantly increase density of water/materials
- Altitude/atmospheric pressure variations affect gas density
Kilogram per cubic meter (kg/m³) is standard SI unit. Reference: water = 1000 kg/m³. Widely used in science and engineering. Large numbers for typical solids (iron = 7874 kg/m³).
Metric Alternative:Gram per cubic centimeter (g/cm³) = 1000 kg/m³ numerically. Convenient for smaller volumes. Commonly used in chemistry (water = 1 g/cm³). Easier mental conversion in lab work.
Imperial Units:Pound per cubic foot (lb/ft³): Common in US engineering (water ≈ 62.4 lb/ft³). Pound per cubic inch (lb/in³): Very large numbers (water ≈ 0.036 lb/in³). Used in materials science and machinining.
Key Conversion Factors:- 1 kg/m³ = 0.001 g/cm³
- 1 g/cm³ = 1000 kg/m³
- 1 lb/ft³ = 16.0185 kg/m³
- 1 kg/m³ = 0.06243 lb/ft³
- 1 lb/in³ = 27680 kg/m³