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Density ( volumetric mass density or specific mass) is the substance's per unit of . The symbol most often used for density is ρ (the lower case letter rho), although the Latin letter D can also be used. Mathematically, density is defined as mass divided by volume:

\rho = \frac{m}{V}

where ρ is the density, m is the mass, and V is the volume. In some cases (for instance, in the United States oil and gas industry), density is loosely defined as its per unit , although this is scientifically inaccurate – this quantity is more specifically called .

For a pure substance the density has the same numerical value as its mass concentration. Different materials usually have different densities, and density may be relevant to , purity and . and are the densest known elements at standard conditions for temperature and pressure.

To simplify comparisons of density across different systems of units, it is sometimes replaced by the quantity "" or "", i.e. the ratio of the density of the material to that of a standard material, usually water. Thus a relative density less than one relative to water means that the substance floats in water.

The density of a material varies with temperature and pressure. This variation is typically small for solids and liquids but much greater for gases. Increasing the pressure on an object decreases the volume of the object and thus increases its density. Increasing the temperature of a substance (with a few exceptions) decreases its density by increasing its volume. In most materials, heating the bottom of a fluid results in of the heat from the bottom to the top, due to the decrease in the density of the heated fluid, which causes it to rise relative to denser unheated material.

The reciprocal of the density of a substance is occasionally called its , a term sometimes used in . Density is an intensive property in that increasing the amount of a substance does not increase its density; rather it increases its mass.

Other conceptually comparable quantities or ratios include , , and .

In a well-known but probably tale, was given the task of determining whether King Hiero's was embezzling during the manufacture of a golden dedicated to the gods and replacing it with another, cheaper . Archimedes, A Gold Thief and Buoyancy – by Larry "Harris" Taylor, Ph.D. Archimedes knew that the irregularly shaped wreath could be crushed into a cube whose volume could be calculated easily and compared with the mass; but the king did not approve of this. Baffled, Archimedes is said to have taken an immersion bath and observed from the rise of the water upon entering that he could calculate the volume of the gold wreath through the displacement of the water. Upon this discovery, he leapt from his bath and ran naked through the streets shouting, "Eureka! Eureka!" (Εύρηκα! Greek "I have found it"). As a result, the term "eureka" entered common parlance and is used today to indicate a moment of enlightenment.

The story first appeared in written form in ' , two centuries after it supposedly took place. Https://" target="_blank" rel="nofollow"> Vitruvius on Architecture, Book IX, paragraphs 9–12, translated into English and in the original Latin. Some scholars have doubted the accuracy of this tale, saying among other things that the method would have required precise measurements that would have been difficult to make at the time.

Measurement of density
A number of techniques as well as standards exist for the measurement of density of materials. Such techniques include the use of a hydrometer (a buoyancy method for liquids), Hydrostatic balance (a buoyancy method for liquids and solids), immersed body method (a buoyancy method for liquids), pycnometer (liquids and solids), air comparison pycnometer (solids), oscillating densitometer (liquids), as well as pour and tap (solids).
(2012). 9789264123298
However, each individual method or technique measures different types of density (e.g. bulk density, skeletal density, etc.), and therefore it is necessary to have an understanding of the type of density being measured as well as the type of material in question.

From the equation for density ( ρ = m/ V), mass density has any unit that is mass divided by volume. As there are many units of mass and volume covering many different magnitudes there are a large number of units for mass density in use. The SI unit of per (kg/m3) and the unit of per (g/cm3) are probably the most commonly used units for density. One g/cm3 is equal to 1000 kg/m3. One cubic centimetre (abbreviation cc) is equal to one millilitre. In industry, other larger or smaller units of mass and or volume are often more practical and US customary units may be used. See below for a list of some of the most common units of density.

Homogeneous materials
The density at all points of a homogeneous object equals its total divided by its total volume. The mass is normally measured with a ; the volume may be measured directly (from the geometry of the object) or by the displacement of a fluid. To determine the density of a liquid or a gas, a , a or a Coriolis flow meter may be used, respectively. Similarly, hydrostatic weighing uses the displacement of water due to a submerged object to determine the density of the object.

Heterogeneous materials
If the body is not homogeneous, then its density varies between different regions of the object. In that case the density around any given location is determined by calculating the density of a small volume around that location. In the limit of an infinitesimal volume the density of an inhomogeneous object at a point becomes: \rho(\vec{r}) = dm/dV, where dV is an elementary volume at position r. The mass of the body then can be expressed as

m = \int_V \rho(\vec{r})\,dV.

Non-compact materials
In practice, bulk materials such as sugar, sand, or snow contain voids. Many materials exist in nature as flakes, pellets, or granules.

Voids are regions which contain something other than the considered material. Commonly the void is air, but it could also be vacuum, liquid, solid, or a different gas or gaseous mixture.

The bulk volume of a material—inclusive of the void fraction—is often obtained by a simple measurement (e.g. with a calibrated measuring cup) or geometrically from known dimensions.

Mass divided by bulk volume determines . This is not the same thing as volumetric mass density.

To determine volumetric mass density, one must first discount the volume of the void fraction. Sometimes this can be determined by geometrical reasoning. For the close-packing of equal spheres the non-void fraction can be at most about 74%. It can also be determined empirically. Some bulk materials, however, such as sand, have a variable void fraction which depends on how the material is agitated or poured. It might be loose or compact, with more or less air space depending on handling.

In practice, the void fraction is not necessarily air, or even gaseous. In the case of sand, it could be water, which can be advantageous for measurement as the void fraction for sand saturated in water—once any air bubbles are thoroughly driven out—is potentially more consistent than dry sand measured with an air void.

In the case of non-compact materials, one must also take care in determining the mass of the material sample. If the material is under pressure (commonly ambient air pressure at the earth's surface) the determination of mass from a measured sample weight might need to account for buoyancy effects due to the density of the void constituent, depending on how the measurement was conducted. In the case of dry sand, sand is so much denser than air that the buoyancy effect is commonly neglected (less than one part in one thousand).

Mass change upon displacing one void material with another while maintaining constant volume can be used to estimate the void fraction, if the difference in density of the two voids materials is reliably known.

Changes of density
In general, density can be changed by changing either the or the . Increasing the pressure always increases the density of a material. Increasing the temperature generally decreases the density, but there are notable exceptions to this generalization. For example, the density of increases between its melting point at 0 °C and 4 °C; similar behavior is observed in at low temperatures.

The effect of pressure and temperature on the densities of liquids and solids is small. The for a typical liquid or solid is 10−6 bar−1 (1 bar = 0.1 MPa) and a typical thermal expansivity is 10−5 −1. This roughly translates into needing around ten thousand times atmospheric pressure to reduce the volume of a substance by one percent. (Although the pressures needed may be around a thousand times smaller for sandy soil and some clays.) A one percent expansion of volume typically requires a temperature increase on the order of thousands of degrees .

In contrast, the density of gases is strongly affected by pressure. The density of an is

\rho = \frac {MP}{RT},

where is the , is the pressure, is the , and is the absolute temperature. This means that the density of an ideal gas can be doubled by doubling the pressure, or by halving the absolute temperature.

In the case of volumic thermal expansion at constant pressure and small intervals of temperature the temperature dependence of density is

\rho = \frac{\rho_{T_0}}{1 + \alpha \cdot \Delta T},

where \rho_{T_0} is the density at a reference temperature, \alpha is the thermal expansion coefficient of the material at temperatures close to T_0.

Density of solutions
The density of a solution is the sum of mass (massic) concentrations of the components of that solution.

Mass (massic) concentration of each given component ρi in a solution sums to density of the solution,

\rho = \sum_i \varrho_i .

Expressed as a function of the densities of pure components of the mixture and their volume participation, it allows the determination of excess molar volumes:

\rho = \sum_i \rho_i \frac{V_i}{V}\, = \sum_i \rho_i \varphi_i = \sum_i \rho_i \frac{V_i}{\sum_i V_i + \sum_i {V^E}_i},
provided that there is no interaction between the components.

Knowing the relation between excess volumes and activity coefficients of the components, one can determine the activity coefficients:

\overline{V^E}_i = RT \frac{\partial\ln\gamma_i}{\partial P}.


Various materials
Selected chemical elements are listed here. For the densities of all chemical elements, see List of chemical elements

+Densities of various materials covering a range of values
Air contained in material excluded when calculating density New carbon nanotube struructure aerographite is lightest material champ . (July 13, 2012). Retrieved on July 14, 2012. Aerographit: Leichtestes Material der Welt entwickelt – SPIEGEL ONLINE . (July 11, 2012). Retrieved on July 14, 2012.
At sea level
One of the heaviest known gases at standard conditions
At approx. −255 °C
Least dense metal
Seasoned, typical
(1970). 9781315214092, CRC Press.
At temperature < 0 °C
At 4 °C, the temperature of its maximum density
At approx. −219 °C
Approx.; for and /
glycerol composition at . Retrieved on July 14, 2012.
Between 1,600 and 2000
(2023). 9780321696861, Addison-Wesley.
Liquid at room temperature
Densest natural element on Earth

Assuming 90% H, 10% He; variable T
Mean density.
Approx., as listed in .
Does not depend strongly on size of nucleus

+ Density of liquid water at 1 atm pressure

+Density of air at 1 atm pressure

Molar volumes of liquid and solid phase of elements

Common units
The SI unit for density is:

The litre and tonne are not part of the SI, but are acceptable for use with it, leading to the following units:

Densities using the following metric units all have exactly the same numerical value, one thousandth of the value in (kg/m3). Liquid has a density of about 1 kg/dm3, making any of these SI units numerically convenient to use as most and have densities between 0.1 and 20 kg/dm3.

  • kilogram per cubic decimetre (kg/dm3)
  • gram per cubic centimetre (g/cm3)
    • 1 g/cm3 = 1000 kg/m3
  • megagram (metric ton) per cubic metre (Mg/m3)

In US customary units density can be stated in:

  • Avoirdupois ounce per (1 g/cm3 ≈ 0.578036672 oz/cu in)
  • Avoirdupois ounce per (1 g/cm3 ≈ 1.04317556 oz/US fl oz = 1.04317556 lb/US fl pint)
  • Avoirdupois pound per cubic inch (1 g/cm3 ≈ 0.036127292 lb/cu in)
  • pound per (1 g/cm3 ≈ 62.427961 lb/cu ft)
  • pound per (1 g/cm3 ≈ 1685.5549 lb/cu yd)
  • pound per US liquid gallon (1 g/cm3 ≈ 8.34540445 lb/US gal)
  • pound per US (1 g/cm3 ≈ 77.6888513 lb/bu)
  • slug per cubic foot

differing from the above (as the Imperial gallon and bushel differ from the US units) in practice are rarely used, though found in older documents. The Imperial gallon was based on the concept that an Imperial fluid ounce of water would have a mass of one Avoirdupois ounce, and indeed 1 g/cm3 ≈ 1.00224129 ounces per Imperial fluid ounce = 10.0224129 pounds per Imperial gallon. The density of could conceivably be based on ounces and pounds, a possible cause of confusion.

Knowing the volume of the of a crystalline material and its formula weight (in daltons), the density can be calculated. One dalton per cubic ångström is equal to a density of 1.660 539 066 60 g/cm3.

See also

External links

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