Water, one liter
School order for water: 1 kg in 0.001 m³. The quotient 1 / 0.001 is 1,000 kg/m³, or 1 g/cm³. This is the reference example on this page.
ρ = 1,000 kg/m³
Enter mass in kilograms and volume in cubic meters. The calculator finds density with ρ = m/V and also shows grams per cubic centimeter and the volume of one kilogram. For 1 kg and 0.001 m³ the result is 1,000 kg/m³. The model does not include specific weight γ = ρg or a temperature correction for gases.
Enter a mass and a volume. Density, grams per cubic centimeter, and the ρ(V) chart will appear here.
On the neighboring pages density is an input, not the result: buoyant force uses F = ρ·V·g, and hydrostatic pressure uses p = ρ·g·h.
Density is mass per volume. The formula ρ = m/V divides mass by volume. The SI unit is the kilogram per cubic meter. For 1 kg and 0.001 m³, one liter, the quotient is 1,000 kg/m³. That same number is 1 g/cm³ and 1 kg per liter. One kilogram of that sample occupies 0.001 m³.
The calculator uses mass m in kilograms and volume V in cubic meters. Enter 1 L as 0.001, and 1 cm³ as 0.000001. One hundred liters is 0.1 m³. 250 ml is 0.00025 m³. A comma and a period are the same decimal separator. Volume does not switch to cubic feet.
What the result panel shows. Besides density in kg/m³, the calculator shows the same value in g/cm³, the volume of one kilogram equal to 1/ρ, the mass used in the division, and the volume in cubic meters. For 1 kg and 0.001 m³ the panel shows 1,000 kg/m³, 1 g/cm³, and 0.001 m³ per kilogram. The chart draws ρ against volume at that same mass, from one quarter of the entered volume to four times that volume. The middle point is the pair you entered.
Limits of the model. The result is the quotient of the numbers you entered. It is not a measurement of temperature, moisture, or porosity. Water in school problems is on the order of 1,000 kg/m³. Near 4 °C it is close to 1,000 kg/m³, and near 20 °C it is closer to 998 kg/m³. The calculator does not apply that correction. The concrete example, 2.4 kg in 0.001 m³, gives 2,400 kg/m³ as a school order for ordinary concrete, not as a mix certificate. Lightweight concrete and reinforced concrete sit in other ranges.
Density does not depend on g. Specific weight is ρ·g, force per volume. Buoyant force F = ρ·V·g is on the buoyant-force page, and fluid-column pressure p = ρ·g·h is on the hydrostatic-pressure page. There, ρ is an input. If you already know ρ and V, mass is m = ρ·V. This calculator goes the other way and has no field for a ready-made density.
The unit switch in the header changes mass to pounds and converts a number already entered in the mass field. It does not convert volume: volume stays in m³. Density stays in kg/m³. Figures in the text stay in SI as the reference. The button “Fill this example” enters the mass in the header unit and refreshes the panel and the chart. The fields start empty.
ρ = m / V
[ρ] = kg / m³; 1 g/cm³ = 1,000 kg/m³ = 1 kg/L
Model: the definition of density as mass per volume. No single author wrote ρ = m/V. Vitruvius describes comparing densities by the volume of water displaced, in the story of Archimedes. This calculator returns only ρ. Order of operations: mass in kilograms, volume in cubic meters, then the quotient.
The density of a uniform body is ρ = m/V. It is mass per volume, not a force and not a pressure. The SI unit kg/m³ follows from the kilogram and the meter. Those unit definitions are in the SI Brochure (BIPM, 9th edition). In the United States, NIST SP 330 is the guide to the SI. 1,000 kg/m³ is 1 g/cm³ and also 1 kg per liter, because 1 m³ = 1,000 L = 1,000,000 cm³.
For 1 kg and 0.001 m³ the path is short. Step 1: the mass is 1 kg. Step 2: the volume is 0.001 m³. Step 3: the quotient 1 / 0.001 = 1,000 kg/m³. The volume of one kilogram is then 1/ρ = 0.001 m³.
In De architectura, Vitruvius tells that Archimedes compared a crown with a lump of gold of the same mass by the water each one displaced. That story is about equal volumes, and therefore about density, but it is not the algebraic line ρ = m/V. The calculator does not measure a water level and does not estimate the makeup of a crown. It uses the mass and the volume you enter.
The examples on this page are quotients of specific numbers, not a laboratory certificate. Water: 1 kg in 0.001 m³ gives 1,000 kg/m³. Ice: 0.92 kg in 0.001 m³ gives 920 kg/m³. Oil: 0.9 kg in 0.001 m³ gives 900 kg/m³. Air: 1.2 kg in 1 m³ gives 1.2 kg/m³, the order of dry air at room temperature. Wood: 0.6 kg in 0.001 m³ gives 600 kg/m³. Concrete: 2.4 kg in 0.001 m³ gives 2,400 kg/m³. Aluminum: 2.7 kg in 0.001 m³ gives 2,700 kg/m³. Steel: 7.8 kg in 0.001 m³ gives 7,800 kg/m³. Copper: 8.9 kg in 0.001 m³ gives 8,900 kg/m³. One gram of water in one cubic centimeter is 0.001 kg in 0.000001 m³ and is 1,000 kg/m³ again.
A real sample depends on composition, moisture, and temperature. Ordinary concrete is often in this 2,400 kg/m³ range, but lightweight concrete is clearly lighter and reinforced concrete is heavier. Tool steel and structural steel do not share one number either. The calculator does not open a materials table.
Specific weight γ = ρ·g has the unit N/m³. At g = 9.81 m/s², water at 1,000 kg/m³ has a specific weight of about 9,810 N/m³. This form does not compute that product. Buoyant force and the pressure of a liquid column use density as an input. They are on separate pages. Specific gravity relative to water at 1,000 kg/m³ equals the number of g/cm³: concrete at 2.4 g/cm³ is 2.4 times as dense as that school value for water.
The definition and the unit come from textbooks and from metrology: D. Halliday, R. Resnick, and J. Walker, Fundamentals of Physics, the chapter on density and pressure; H. D. Young and R. A. Freedman, University Physics, the chapter on fluids; Vitruvius, De architectura, the story of Archimedes; BIPM, SI Brochure, 9th edition; NIST Special Publication 330. This page is for educational purposes.
ρ is density, m is mass, and V is volume. For 1 kg and 0.001 m³ the result is 1,000 kg/m³.
School order for water: 1 kg in 0.001 m³. The quotient 1 / 0.001 is 1,000 kg/m³, or 1 g/cm³. This is the reference example on this page.
ρ = 1,000 kg/m³
Lighter than the school value for water: 0.9 kg in 0.001 m³. The quotient is 900 kg/m³. That is the order of many oils, not a certificate for a particular bottle.
ρ = 900 kg/m³
Dry air at room temperature: 1.2 kg in 1 m³. The quotient is 1.2 kg/m³. Moisture and pressure change a real sample.
ρ = 1.2 kg/m³
School order for steel: 7.8 kg in 0.001 m³. The quotient is 7,800 kg/m³, or 7.8 g/cm³. The grade of steel moves that number.
ρ = 7,800 kg/m³
Order of dry wood, for example pine: 0.6 kg in 0.001 m³. The quotient is 600 kg/m³. Wet wood is heavier at the same volume.
ρ = 600 kg/m³
Lighter than water: 0.92 kg in 0.001 m³. The quotient is 920 kg/m³. That is why ice floats, but buoyancy is a different page.
ρ = 920 kg/m³
School order for ordinary concrete: 2.4 kg in 0.001 m³. The quotient is 2,400 kg/m³, or 2.4 times water at 1,000 kg/m³. This is not a mix certificate.
ρ = 2,400 kg/m³
School order for copper: 8.9 kg in 0.001 m³. The quotient is 8,900 kg/m³. Pure copper in tables is often closer to 8,960 kg/m³.
ρ = 8,900 kg/m³
School order for aluminum: 2.7 kg in 0.001 m³. The quotient is 2,700 kg/m³. Aluminum alloys have a different density.
ρ = 2,700 kg/m³
The same water as the first example, from one cubic centimeter: 0.001 kg in 0.000001 m³. The quotient is 1,000 kg/m³ again. A 1 in the volume field is not 1 cm³.
ρ = 1,000 kg/m³
The calculator finds density from ρ = m/V. It divides mass in kilograms by volume in cubic meters. For 1 kg and 0.001 m³ the result is 1,000 kg/m³.
Enter mass in kilograms and volume in cubic meters. The result is in kg/m³. After the header switches to US units, mass is in pounds and the calculator converts a number you already entered. Volume stays in m³, and density stays in kg/m³. A comma and a period are the same decimal separator.
1 L = 0.001 m³. One hundred liters is 0.1 m³. 250 ml is 0.00025 m³. 1 cm³ = 0.000001 m³. Enter cubic meters in the volume field. There is no separate field for liters or milliliters.
No. Density is the quotient m/V. The acceleration g enters hydrostatic pressure and buoyant force, not this quotient. Specific weight is ρ·g, a different quantity, in N/m³.
Density is in kg/m³. Specific weight ρ·g is force per volume. Buoyant force F = ρ·V·g is on a separate page, and column pressure p = ρ·g·h is on the hydrostatic-pressure page. This calculator stays with m/V.
Zero volume and a negative volume are rejected, because the calculator divides by V. Zero mass and a negative mass are rejected too. Both fields need a number greater than zero before the panel appears.
No. This form computes ρ from m and V. Mass from a known density is recovered with m = ρ·V, but there is no field for a ready-made density. The calculator does not look up a materials table.
The panel reports density in kg/m³, the same value in g/cm³, the volume of one kilogram 1/ρ, mass in kilograms, and volume in cubic meters. The g/cm³ number equals kilograms per liter. The chart draws ρ against V at constant mass. The button “Fill this example” enters the example numbers and refreshes the panel and the chart. The fields start empty.
No. That is what the numbers 1 kg and 0.001 m³ produce. Water in school problems is on the order of 1,000 kg/m³, and near 20 °C it is closer to 998 kg/m³. The calculator does not correct for temperature, salt, or porosity. The concrete example, 2.4 kg in 0.001 m³, gives 2,400 kg/m³ as an order for ordinary concrete, not as a mix certificate.
No. They are school orders of magnitude entered as mass and volume: water 1,000, oil 900, air 1.2, steel 7,800, wood 600, ice 920, concrete 2,400, copper 8,900, and aluminum 2,700, all in kg/m³. One gram of water in 1 cm³ is 1,000 again. A real sample depends on composition, moisture, and temperature.
Divide mass by volume in coherent SI units. For 1 kg and 0.001 m³: 1/0.001 = 1,000 kg/m³.
1,000 kg/m³, or 1 g/cm³. That is the order of a liter of water under typical school conditions.
Multiply by 1,000: 1 g/cm³ = 1,000 kg/m³. The panel shows both units next to the kg/m³ result.
Comparing the numbers alone, 900 < 1,000, so the average density is lower than water. This calculator does not compute buoyancy F = ρVg or floating stability.
No. ρ = m/V is the quotient of the numbers you enter. For gases density depends strongly on T and p; there is no equation of state or temperature correction here.
The definition, the unit, and the historical note come from physics and metrology. This page does not invent publication identifiers.
Page updated November 3, 2026.