- Mass (kg)
- 1kg
- Volume (m³)
- 0.001m³
1,000.000kg/m³
Open with these values1,000.000kg/m³
Result: 1,000.000 kg/m³Density is mass divided by volume: 1 kg of water filling 0.001 m³ — one litre — gives 1000 kg/m³. Enter kilograms and cubic metres and the answer comes out in kg/m³. Anything lighter than 1000 kg/m³ floats on water, anything heavier sinks. Divide by 1000 for g/cm³.
1,000.000kg/m³
Open with these values2,700.000kg/m³
Open with these values7,870.000kg/m³
Open with these valuesDensity = mass ÷ volume
Density is mass divided by volume — how much matter is packed into each cubic metre. It is what separates a feather from a brick of the same size, and for a given material at a given temperature it is fixed, which is why it works as a fingerprint. Enter kilograms and cubic metres and the answer comes back in kg/m³. One kilogram of water filling a one-litre bottle is 1 ÷ 0.001 = 1000 kg/m³, which is also exactly 1 g/cm³, the unit chemistry usually prefers. The same number answers three different questions. Buoyancy: water sits at about 1000 kg/m³, so anything below that floats and anything above sinks — ice at 917 kg/m³ floats, which is why icebergs show above the sea, while aluminium at 2700, iron at 7870 and gold at 19,300 kg/m³ go straight down. Identity: a metal sample landing near 2700 kg/m³ is far more likely aluminium than steel. Logistics: because density links mass to volume, either one gives you the other. Two caveats are worth keeping. Density shifts with temperature and pressure, so published figures always state a temperature. And what you get here is an average — a porous, hollow or mixed object returns a blended value, not the density of the solid material.
Water sits at 1000 kg/m³, which is exactly 1 g/cm³. Divide by a thousand to move between the two — nothing else changes.
It tells you whether something floats, which material it probably is, and how much a given volume weighs. Water at 1000 kg/m³ is the line for the first of those.
Density shifts with temperature and pressure, which is why every table states the conditions. Comparing a warm sample against a table at 20 °C introduces an error the calculation cannot see.
The result is the density of the material.
It is the average over the whole object. Anything porous, hollow or mixed returns a blended value, not the density of the solid.
Heavy things sink, light things float.
Density decides it, not weight. A steel ship floats and a steel bolt sinks because the ship encloses air and the bolt does not.
| Mass (kg), volume (m³) | Material | Density (kg/m³) |
|---|---|---|
| 0, 1 | Empty container | 0 |
| 10, 2 | Ultralight foam | 5 |
| 1, 0.001 | Water | 1000 |
| 2700, 1 | Aluminium | 2700 |
| 7.87, 0.001 | Iron | 7870 |
Divide the mass by the volume: density = mass ÷ volume. For 1 kg of water filling 0.001 m³ (one litre), that is 1 ÷ 0.001 = 1000 kg/m³. Keep mass in kilograms and volume in cubic metres to get the result in kg/m³.
Mass in kilograms (kg), volume in cubic metres (m³), and density in kilograms per cubic metre (kg/m³). One litre is 0.001 m³, so a 1-litre bottle weighing 1 kg has a density of 1000 kg/m³.
Compare it to water, which has a density of about 1000 kg/m³. Anything less dense than water (below 1000 kg/m³) floats, and anything denser (above 1000 kg/m³) sinks. Ice at 917 kg/m³ floats; iron at 7870 kg/m³ sinks.
At room temperature: water is about 1000 kg/m³, ice 917, aluminium 2700, iron 7870, and gold 19,300 kg/m³. Comparing your result to these anchors helps you identify a material or sanity-check a measurement.
Divide by 1000: 1000 kg/m³ equals 1 g/cm³. So water is 1 g/cm³, aluminium 2.7 g/cm³, and gold 19.3 g/cm³. The g/cm³ unit is common in chemistry and is just the kg/m³ value scaled down by a thousand.
Information, not professional advice.
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