Compressibility
{{#invoke:Hatnotehatnote}} {{#invoke:Hatnotehatnote}}Template:Main other {{#invoke:Sidebar collapsible  bodyclass = plainlist  titlestyle = paddingbottom:0.3em;borderbottom:1px solid #aaa;  title = Thermodynamics  imagestyle = display:block;margin:0.3em 0 0.4em;  image =  caption = The classical Carnot heat engine  listtitlestyle = background:#ddf;textalign:center;  expanded = Material properties
 list1name = branches  list1title = Branches  list1 = Template:Startflatlist
 list2name = laws  list2title = Laws  list2 = Template:Startflatlist
 list3name = systems  list3title = Systems  list3 =
State 

Processes 
Cycles 
 list4name = sysprop  list4title = System properties
 list4 =
Functions of state 

Process functions 
 list5name = material  list5title = Material properties  list5 =
 list6name = equations  list6title = Equations  list6 = Template:Startflatlist
 Maxwell relations
 Onsager reciprocal relations
 Bridgman's equations
 Table of thermodynamic equations
 list7name = potentials  list7title = Potentials  list7 = Template:Startflatlist
 list8name = hist/cult  list8title = Template:Hlist  list8 =
History 

Philosophy 
Theories 

Key publications 
Timelines 
Template:Hlist 
 list9name = scientists  list9title = Scientists  list9 = Template:Startflatlist
 Bernoulli
 Carnot
 Clapeyron
 Clausius
 Carathéodory
 Duhem
 Gibbs
 von Helmholtz
 Joule
 Maxwell
 von Mayer
 Onsager
 Rankine
 Smeaton
 Stahl
 Thompson
 Thomson
 Waterston
 below = Book:Thermodynamics
}}
In thermodynamics and fluid mechanics, compressibility is a measure of the relative volume change of a fluid or solid as a response to a pressure (or mean stress) change.
where V is volume and p is pressure.
Definition
The specification above is incomplete, because for any object or system the magnitude of the compressibility depends strongly on whether the process is adiabatic or isothermal. Accordingly isothermal compressibility is defined:
where the subscript T indicates that the partial differential is to be taken at constant temperature
Isentropic compressibility is defined:
where S is entropy. For a solid, the distinction between the two is usually negligible.
Relation to speed of sound
The speed of sound is defined in classical mechanics as:
where is the density of the material. It follows, by replacing partial derivatives, that the isentropic compressibility can be expressed as:
Relation to bulk modulus
The inverse of the compressibility is called the bulk modulus, often denoted K (sometimes B). That page also contains some examples for different materials.
The compressibility equation relates the isothermal compressibility (and indirectly the pressure) to the structure of the liquid.
Thermodynamics
{{#invoke:mainmain}} The term "compressibility" is also used in thermodynamics to describe the deviance in the thermodynamic properties of a real gas from those expected from an ideal gas. The compressibility factor is defined as
where p is the pressure of the gas, T is its temperature, and is its molar volume. In the case of an ideal gas, the compressibility factor Z is equal to unity, and the familiar ideal gas law is recovered:
Z can, in general, be either greater or less than unity for a real gas.
The deviation from ideal gas behavior tends to become particularly significant (or, equivalently, the compressibility factor strays far from unity) near the critical point, or in the case of high pressure or low temperature. In these cases, a generalized compressibility chart or an alternative equation of state better suited to the problem must be utilized to produce accurate results.
A related situation occurs in hypersonic aerodynamics, where dissociation causes an increase in the “notational” molar volume, because a mole of oxygen, as O_{2}, becomes 2 moles of monatomic oxygen and N_{2} similarly dissociates to 2N. Since this occurs dynamically as air flows over the aerospace object, it is convenient to alter Z, defined for an initial 30 gram mole of air, rather than track the varying mean molecular weight, millisecond by millisecond. This pressure dependent transition occurs for atmospheric oxygen in the 2500 K to 4000 K temperature range, and in the 5000 K to 10,000 K range for nitrogen.^{[1]}
In transition regions, where this pressure dependent dissociation is incomplete, both beta (the volume/pressure differential ratio) and the differential, constant pressure heat capacity will greatly increase.
For moderate pressures, above 10,000 K the gas further dissociates into free electrons and ions. Z for the resulting plasma can similarly be computed for a mole of initial air, producing values between 2 and 4 for partially or singly ionized gas. Each dissociation absorbs a great deal of energy in a reversible process and this greatly reduces the thermodynamic temperature of hypersonic gas decelerated near the aerospace object. Ions or free radicals transported to the object surface by diffusion may release this extra (nonthermal) energy if the surface catalyzes the slower recombination process.
The isothermal compressibility is related to the isentropic (or adiabatic) compressibility by the relation,
via Maxwell's relations. More simply stated,
where,
 is the heat capacity ratio. See here for a derivation.
Earth science
Material  β (m²/N or Pa^{−1}) 

Plastic clay  2Template:E – 2.6Template:E 
Stiff clay  2.6Template:E – 1.3Template:E 
Mediumhard clay  1.3Template:E – 6.9Template:E 
Loose sand  1Template:E – 5.2Template:E 
Dense sand  2Template:E – 1.3Template:E 
Dense, sandy gravel  1Template:E – 5.2Template:E 
Rock, fissured  6.9Template:E – 3.3Template:E 
Rock, sound  <3.3Template:E 
Water at 25 °C (undrained)^{[3]}  4.6Template:E 
Ethyl alcohol^{[4]}  110Template:E 
Carbon disulfide^{[4]}  93Template:E 
Glycerine^{[4]}  21Template:E 
Mercury^{[4]}  3.7Template:E 
Compressibility is used in the Earth sciences to quantify the ability of a soil or rock to reduce in volume with applied pressure. This concept is important for specific storage, when estimating groundwater reserves in confined aquifers. Geologic materials are made up of two portions: solids and voids (or same as porosity). The void space can be full of liquid or gas. Geologic materials reduces in volume only when the void spaces are reduced, which expel the liquid or gas from the voids. This can happen over a period of time, resulting in settlement.
It is an important concept in geotechnical engineering in the design of certain structural foundations. For example, the construction of highrise structures over underlying layers of highly compressible bay mud poses a considerable design constraint, and often leads to use of driven piles or other innovative techniques.
Fluid dynamics
{{#invoke:mainmain}} The degree of compressibility of a fluid has strong implications for its dynamics. Most notably, the propagation of sound is dependent on the compressibility of the medium.
Aeronautical dynamics
{{#invoke:mainmain}} Compressibility is an important factor in aerodynamics. At low speeds, the compressibility of air is not significant in relation to aircraft design, but as the airflow nears and exceeds the speed of sound, a host of new aerodynamic effects become important in the design of aircraft. These effects, often several of them at a time, made it very difficult for World War II era aircraft to reach speeds much beyond 800 km/h (500 mph).
Many effects are often mentioned in conjunction with the term "compressibility", but regularly have little to do with the compressible nature of air. From a strictly aerodynamic point of view, the term should refer only to those sideeffects arising as a result of the changes in airflow from an incompressible fluid (similar in effect to water) to a compressible fluid (acting as a gas) as the speed of sound is approached. There are two effects in particular, wave drag and critical mach.
Negative compressibility
Under very specific conditions the compressibility can be negative.^{[5]}
See also
 Poisson ratio
 Mach number
 PrandtlGlauert singularity, associated with supersonic flight.
 Shear strength
References
 ↑ {{#invoke:citation/CS1citation CitationClass=book }}
 ↑ {{#invoke:Citation/CS1citation CitationClass=journal }}
 ↑ {{#invoke:Citation/CS1citation CitationClass=journal }}
 ↑ ^{4.0} ^{4.1} ^{4.2} ^{4.3} Hugh D. Young; Roger A. Freedman. University Physics with Modern Physics. AddisonWesley; 2012. ISBN 9780321696861. p. 356.
 ↑ {{#invoke:Citation/CS1citation
CitationClass=journal
}}
{{#invoke:Citation/CS1citation CitationClass=journal }}
{{#invoke:Citation/CS1citation CitationClass=journal }}
{{#invoke:Citation/CS1citation CitationClass=journal }}