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En Física y por extensión , también se suele denominar así al espacio ultra alto vacío donde hay poca energía. El espacio ultra alto vacío surge como consecuencia de la transformación de ésta energía, compuesta por patrones de ondas superpuestas y entrelazadas entre sí, que experimentan un impulso de repulsión, si no consiguen liberarse de ese solapamiento se debe al empuje de las unidades adyacentes . Por extensión se suelen denominar vacío, a los espacios cuya densidad de aire y partículas es muy baja, como, por ejemplo, el espacio interestelar o vacío interestelar pero su verdadera denominación es "alto vacío". Por extensión también se denomina vacío, al lugar donde la presión que se mide es menor que la presión atmosférica normal. Hay diferentes clases de vacío: grueso o primario, medio, alto y ultra alto, y en cada caso, la presión es cada vez menor (o el vacío es cada vez más alto). Cada régimen de vacío tiene un comportamiento diferente, y sobre todo, un cierto tipo de aplicaciones, que son las que hacen del vacío algo tan importante.

Existe gran variedad de usos del vacío que son de importancia para muchas industrias y desarrollos tecnológicos, para la ciencia y para la vida diaria. El vacío se aprovecha en diversas industrias, que van desde la alimenticia hasta la automovilística, la aviación, la obtención de medicamentos, etc.

Se puede decir que el área de influencia del vacío afecta a la mayoría de las industrias, lo cual le da un lugar preeminente en el desarrollo tecnológico de un país.

Definición [editar]

De acuerdo con la definición de la Sociedad Americana de Vacío o AVS (1958), el término vacío se refiere a cierto espacio lleno con gases a una presión total menor que la presión atmosférica, por lo que el grado de vacío se incrementa en relación directa con la disminución de presión del gas residual. Esto significa que en cuanto más disminuyamos la presión, mayor vacío obtendremos, lo que nos permite clasificar el grado de vacío en correspondencia con intervalos de presiones cada vez menores. Cada intervalo tiene características propias.

Medición del vacío [editar]

La presión atmosférica es la que ejerce la atmósfera o aire sobre la Tierra. A temperatura ambiente y presión atmosférica normal, un metro cúbico de aire contiene aproximadamente 2 × 1025 moléculas en movimiento a una velocidad promedio de 1600 kilómetros por hora. Una manera de medir la presión atmosférica es con un barómetro de mercurio, su valor se expresa en términos de la altura de la columna de mercurio de sección transversal unitaria y 760 mm de alto. Con base en esto decimos que una atmósfera estándar es igual a 760 mm Hg. Utilizaremos por conveniencia la unidad Torricelli (torr) como medida de presión; 1 torr = 1 mm Hg, por lo que 1 atm = 760 torr; por lo tanto 1 torr = 1/760 de una atmósfera estándar, o sea 1 torr =1,136 × 10–3 atm (1 × 10–3 es igual a 0,001 o igual a un milésimo).

Medición de bajas presiones. Pirani construyó el primer aparato capaz de medir presiones muy pequeñas, menores de 10–5 torr; está basado en que la conductividad térmica de un gas sometido a presiones inferiores a la décima de torr es una función lineal de la presión. Se dispone entonces un filamento metálico caliente en una ampolla de vidrio, unida a la bomba de vacío. La velocidad con que el calor pasa del filamento a las paredes de la ampolla determina la temperatura del filamento y, por tanto, su resistencia eléctrica, que es, en definitiva, la magnitud física que se mide y que suministra el valor de la presión.

Medidas de ionización. Tienen el mismo fundamento que las bombas de ionización, hasta el punto que éstas pueden considerarse como una consecuencia de aquéllas. Cuando se trata de medir u.h.v. se utilizan las variantes propuestas por Bayard-Alpert de aquellos aparatos, capaces de suministrar con gran exactitud presiones de hasta 10–12 torr.

El aire está compuesto por varios gases, los más importantes son el nitrógeno y el oxígeno, pero también contiene en menores concentraciones gases como dióxido de carbono, argón, neón, helio, criptón, xenón, hidrógeno, metano, óxido nitroso y vapor de agua.

Aplicaciones de las técnicas de vacío [editar]

Aplicaciones técnicas del vacío
Situación física Objetivo Aplicaciones
Baja presión Se obtiene una diferencia de presión Sostenimiento, elevación, transporte (neumático, aspiradores, filtrado), moldeado
Baja densidad molecular Eliminar los componentes activos de la atmósfera Lámparas (incandescentes, fluorescentes, tubos eléctricos), fusión, sinterización, empaquetado, ecapsulado, detección de fugas

Extracción del gas ocluido o disuelto Desecación, deshidratación, concentración, Liofiliación, Degasificación, impregnación

Disminución de la transferencia de energía Aislamiento térmico, aislamiento eléctrico, microbalanza de vacío, simulación espacial
Gran recorrido libre medio Evitar colisiones Tubos electrónicos, rayos catódicos, TV, fotocélulas, fotomultiplicadores, tubos de rayos X, aceleradores de partículas, espectrómetros de masas, separadores de isótopos, microscopios electrónicos, soldadura por haz de electrones, metalización (evaporación, pulverización catódica), destilación molecular
Tiempo largo de formación de una monocapa Superficies limpias Estudio de la fricción, adhesión, corrosión de superficies. Prueba de materiales para experiencias espaciales.

Historia [editar]

Barómetro de mercurio de Torricelli, que produjo el primer vacío en un laboratorio.

Barómetro de mercurio de Torricelli, que produjo el primer vacío en un laboratorio.

Durante toda la Antigüedad y hasta el Renacimiento se desconocía la existencia de la presión atmosférica. No podían por tanto dar una explicación de los fenómenos debidos al vacío. En Grecia se enfrentaron por ello dos teorías. Para Epicuro y sobre todo Demócrito (420 a. C.) y su escuela, la materia no era un todo contínuo sino que estaba compuesta por pequeñas partículas indivisibles (átomos) que se movían en un espacio vacío y que con su distinto ordenamiento dan lugar a los distintos estados físicos. Por el contrario Aristóteles excluía la noción de vacío y para justificar los fenómenos que su propia Física no podía explicar recurría al célebre aforismo según el cual "la Naturaleza siente horror al vacío" (teoría que resultó dominante durante la Edad Media y hasta el descubrimiento de la presión).

Este término de "horror vacui" fue el utilizado incluso por el propio Galileo a comienzos del siglo XVII al no poder explicar ante sus discípulos el hecho de que una columan de agua en un tubo cerrado por su extremo no se desprenda, si el tubo ha sido invertido estando sumergido el extremo libre del mismo dentro de agua. Sin embargo, supo transmitir a sus discípulos la inquietud por explicar el hecho anterior y asociado a él, porque las bombas aspirantes-impelentes (inventadas por Ctesilio, contemporáneo de Aquímedes) no podían hacer subir el agua de los pozos a una altura superior a los 10 m.

Fue hasta mediados del siglo XVII cuando el italiano Gasparo Berti realizó el primer experimento con el vacío (1640). Motivado por un interés en diseñar un experimento para el estudio de los sifones, Berti pretendía aclarar el fenómeno como una manifestación de diferencia de presión de aire en la atmósfera. Creó lo que constituye, primordialmente, un barómetro de agua, el cual resultó capaz de producir vacío.

Al analizar el informe experimental de Berti, Evangelista Torricelli captó con claridad el concepto de presión de aire, por lo que diseñó, en 1644, un dispositivo para demostrar los cambios de presión en el aire. Construyó un barómetro que en lugar de agua empleaba mercurio, y de esta manera, sin proponérselo, comprobó la existencia del vacío.

El barómetro de Torricelli constaba de un recipiente y un tubo lleno de mercurio (Hg) cerrado en uno de sus extremos. Al invertir el tubo dentro del recipiente se formaba vacío en la parte superior del tubo. Esto era algo difícil de entender en su época, por lo que se intentó explicarlo diciendo que esa región del tubo contenía vapor de mercurio, argumento poco aceptable ya que el nivel de mercurio en el tubo era independiente del volumen del mismo utilizado en el experimento.

La aceptación del concepto de vacío se dio cuando en 1648, Blaise Pascal subió un barómetro con 4 kg de mercurio a una montaña a 1000 metros sobre el nivel del mar. Sorprendentemente, cuando el barómetro estaba en la cima, el nivel de la columna de Hg en el tubo era mucho menor que al pie de la montaña. Torricelli aseguraba la existencia de la presión de aire y decía que debido a ella el nivel de Hg en el recipiente no descendía, lo cual hacía que el tamaño de la columna de mercurio permaneciera constante dentro del tubo. Así pues, al disminuir la presión del aire en la cima de la montaña, el nivel de Hg en el recipiente subió y en la columna dentro del tubo bajó inmediatamente (se vació de manera parcial).

El paso final que dio Torricelli fue la construcción de un barómetro de mercurio que contenía en la parte vacía del tubo, otro barómetro para medir la presión de aire en esa región. Se hicieron muchas mediciones y el resultado fue que no había una columna de Hg en el tubo del barómetro pequeño porque no se tenía presión de aire. Esto aclaró que no existía vapor de mercurio en la parte vacía del tubo. Así, se puso en evidencia la presión del aire y, lo más importante, la producción y existencia del vacío.

Entonces después de varios experimentos se puede explicar bien el funcionamiento del barómetro de Torricelli: la atmósfera ejerce una presión, lo cual impide que el mercurio salga del tubo y del recipiente, es decir, cuando la presión atmosférica se iguale a la presión ejercida por la columna de mercurio, el mercurio no podrá salir del tubo. Cuando el aire pesa más, soporta una columna mayor de mercurio; y cuando pesa menos, no es capas de resistir la misma columna de mercurio, así que se escapa un poco de mercurio del tubo.

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A vacuum is a volume of space that is essentially empty of matter, such that its gaseous pressure is much less than atmospheric pressure. [1] The word comes from the Latin term for "empty," but in reality, no volume of space can ever be perfectly empty. A perfect vacuum with a gaseous pressure of absolute zero is a philosophical concept that is never observed in practice. Physicists often discuss ideal test results that would occur in a perfect vacuum, which they simply call "vacuum" or "free space" in this context, and use the term partial vacuum to refer to real vacuum. The Latin term in vacuo is also used to describe an object as being in what would otherwise be a vacuum.

The quality of a vacuum refers to how closely it approaches a perfect vacuum. The residual gas pressure is the primary indicator of quality, and is most commonly measured in units called torr, even in metric contexts. Lower pressures indicate higher quality, although other variables must also be taken into account. Quantum theory sets limits for the best possible quality of vacuum, predicting that no volume of space can be perfectly empty. Outer space is a natural high quality vacuum, mostly of much higher quality than can be created artificially with current technology. Low quality artificial vacuums have been used for suction for many years.

Vacuum has been a frequent topic of philosophical debate since Ancient Greek times, but was not studied empirically until the 17th century. Evangelista Torricelli produced the first laboratory vacuum in 1643, and other experimental techniques were developed as a result of his theories of atmospheric pressure. Vacuum became a valuable industrial tool in the 20th century with the introduction of incandescent light bulbs and vacuum tubes, and a wide array of vacuum technology has since become available. The recent development of human spaceflight has raised interest in the impact of vacuum on human health, and on life forms in general.

A large vacuum chamber

[edit] Uses

Light bulbs contain a partial vacuum, usually backfilled with argon, which protects the tungsten filament

Light bulbs contain a partial vacuum, usually backfilled with argon, which protects the tungsten filament

Vacuum is useful in a variety of processes and devices. Its first widespread use was in the incandescent light bulb to protect the filament from chemical degradation. Its chemical inertness is also useful for electron beam welding, cold welding, vacuum packing and vacuum frying. Ultra-high vacuum is used in the study of atomically clean substrates, as only a very good vacuum preserves atomic-scale clean surfaces for a reasonably long time (on the order of minutes to days). High to ultra-high vacuum removes the obstruction of air, allowing particle beams to deposit or remove materials without contamination. This is the principle behind chemical vapor deposition, physical vapor deposition, and dry etching which are essential to the fabrication of semiconductors and optical coatings, and to surface science. The reduction of convection provides the thermal insulation of thermos bottles. Deep vacuum promotes outgassing which is used in freeze drying, adhesive preparation, distillation, metallurgy, and process purging. The electrical properties of vacuum make electron microscopes and vacuum tubes possible, including cathode ray tubes. The elimination of air friction is useful for flywheel energy storage and ultracentrifuges.

Vacuums are commonly used to produce suction, which has an even wider variety of applications. The Newcomen steam engine used vacuum instead of pressure to drive a piston. In the 19th century, vacuum was used for traction on Isambard Kingdom Brunel's experimental atmospheric railway.

[edit] Outer space

Main article: Outer space
Outer space is not a perfect vacuum, but a tenuous plasma awash with charged particles, electromagnetic fields, and the occasional star.

Outer space is not a perfect vacuum, but a tenuous plasma awash with charged particles, electromagnetic fields, and the occasional star.

Outer space has very low density and pressure, and is the closest physical approximation of a perfect vacuum. It has effectively no friction, allowing stars, planets and moons to move freely along ideal gravitational trajectories. But no vacuum is truly perfect, not even in interstellar space where there are still a few hydrogen atoms per cubic centimeter. The deep vacuum of space could make it an attractive environment for certain industrial processes, for instance those that require ultraclean surfaces; however, it is much less costly to create an equivalent vacuum on Earth than to leave the Earth's gravity well.

Stars, planets and moons keep their atmospheres by gravitational attraction, and as such, atmospheres have no clearly delineated boundary: the density of atmospheric gas simply decreases with distance from the object. The Earth's atmospheric pressure drops to about 1 Pa (10-3 Torr) at 100 km of altitude, the Kármán line which is a common definition of the boundary with outer space. Beyond this line, isotropic gas pressure rapidly becomes insignificant when compared to radiation pressure from the sun and the dynamic pressure of the solar wind, so the definition of pressure becomes difficult to interpret. The thermosphere in this range has large gradients of pressure, temperature and composition, and varies greatly due to space weather. Astrophysicists prefer to use number density to describe these environments, in units of particles per cubic centimetre.

But although it meets the definition of outer space, the atmospheric density within the first few hundred kilometers above the Kármán line is still sufficient to produce significant drag on satellites. Most artificial satellites operate in this region called low earth orbit and must fire their engines every few days to maintain orbit. The drag here is low enough that it could theoretically be overcome by radiation pressure on solar sails, a proposed propulsion system for interplanetary travel. Planets are too massive for their trajectories to be affected by these forces, although their atmospheres are eroded by the solar winds.

All of the observable universe is filled with large numbers of photons, the so-called cosmic background radiation, and quite likely a correspondingly large number of neutrinos. The current temperature of this radiation is about 3 K, or -270 degrees Celsius or -454 degrees Fahrenheit.

[edit] Effects on humans and animals

See also: Human adaptation to space
This painting, An Experiment on a Bird in the Air Pump by Joseph Wright of Derby, 1768, depicts an experiment performed by Robert Boyle in 1660.

This painting, An Experiment on a Bird in the Air Pump by Joseph Wright of Derby, 1768, depicts an experiment performed by Robert Boyle in 1660.

Humans and animals exposed to vacuum will lose consciousness after a few seconds and die of hypoxia within minutes, but the symptoms are not nearly as graphic as commonly shown in pop culture. Blood and other body fluids do boil when their pressure drops below 6.3 kPa, (47 Torr,) the vapour pressure of water at body temperature.[2] This condition is called ebullism. The steam may bloat the body to twice its normal size and slow circulation, but tissues are elastic and porous enough to prevent rupture. Ebullism is slowed by the pressure containment of blood vessels, so some blood remains liquid.[3][4] Swelling and ebullism can be restrained by containment in a flight suit. Shuttle astronauts wear a fitted elastic garment called the Crew Altitude Protection Suit (CAPS) which prevents ebullism at pressures as low as 2 kPa (15 Torr).[5] Rapid evaporative cooling of the skin will create frost, particularly in the mouth, but this is not a significant hazard.

Animal experiments show that rapid and complete recovery is the norm for exposures shorter than 90 seconds, while longer full-body exposures are fatal and resuscitation has never been successful.[6] There is only a limited amount of data available from human accidents, but it is consistent with animal data. Limbs may be exposed for much longer if breathing is not impaired.[2] Robert Boyle was the first to show in 1660 that vacuum is lethal to small animals. In 1942, in one of a series of experiments on human subjects for the Luftwaffe, the Nazi regime tortured Dachau concentration camp prisoners by exposing them to vacuum in order to determine the human body's capacity to survive high-altitude conditions.

Cold or oxygen-rich atmospheres can sustain life at pressures much lower than atmospheric, as long as the density of oxygen is similar to that of standard sea-level atmosphere. The colder air temperatures found at altitudes of up to 3 km generally compensate for the lower pressures there.[2] Above this altitude, oxygen enrichment is necessary to prevent altitude sickness, and spacesuits are necessary to prevent ebullism above 19 km.[2] Most spacesuits use only 20 kPa (150 Torr) of pure oxygen, just enough to sustain full consciousness. This pressure is high enough to prevent ebullism, but simple evaporation of blood can still cause decompression sickness and gas embolisms if not managed.

Rapid decompression can be much more dangerous than vacuum exposure itself. Even if the victim does not hold his breath, venting through the windpipe may be too slow to prevent the fatal rupture of the delicate alveoli of the lungs.[2] Eardrums and sinuses may be ruptured by rapid decompression, soft tissues may bruise and seep blood, and the stress of shock will accelerate oxygen consumption leading to hypoxia.[7] Injuries caused by rapid decompression are called barotrauma. A pressure drop as small as 100 Torr, (13 kPa,) which produces no symptoms if it is gradual, may be fatal if occurs suddenly.[2]

Some extremophile microrganisms, such as Tardigrades, can survive vacuum for a period of years.

[edit] Historical interpretation

Historically, there has been much dispute over whether such a thing as a vacuum can exist. Ancient Greek philosophers did not like to admit the existence of a vacuum, asking themselves "how can 'nothing' be something?". Plato found the idea of a vacuum inconceivable. He believed that all physical things were instantiations of an abstract Platonic ideal, and he could not conceive of an "ideal" form of a vacuum. Similarly, Aristotle considered the creation of a vacuum impossible — nothing could not be something. Later Greek philosophers thought that a vacuum could exist outside the cosmos, but not within it.

Hero of Alexandria was the first to challenge this belief in the first century AD, but his attempts to create an artificial vacuum failed.[8] The philosopher Al-Farabi (872 - 950 CE) appears to have carried out the first experiments concerning the existence of vacuum, in which he investigated handheld plungers in water.[9] He concluded that air's volume can expand to fill available space, and he suggested that the concept of perfect vacuum was incoherent.[10]

Torricelli's mercury barometer produced one of the first sustained vacuums in a laboratory.

Torricelli's mercury barometer produced one of the first sustained vacuums in a laboratory.

In the Middle Ages, the Catholic Church held the idea of a vacuum to be immoral or even heretical. The absence of anything implied the absence of God, and harkened back to the void prior to the creation story in the book of Genesis. Medieval thought experiments into the idea of a vacuum considered whether a vacuum was present, if only for an instant, between two flat plates when they were rapidly separated. There was much discussion of whether the air moved in quickly enough as the plates were separated, or, as Walter Burley postulated, whether a 'celestial agent' prevented the vacuum arising. The commonly held view that nature abhorred a vacuum was called horror vacui. This speculation was shut down by the 1277 Paris condemnations of Bishop Etienne Tempier, which required there to be no restrictions on the powers of God, which led to the conclusion that God could create a vacuum if he so wished.[11] René Descartes also argued against the existence of a vacuum, arguing along the following lines:“Space is identical with extension, but extension is connected with bodies; thus there is no space without bodies and hence no empty space (vacuum)”. In spite of this, opposition to the idea of a vacuum existing in nature continued into the Scientific Revolution, with scholars such as Paolo Casati taking an anti-vacuist position. Jean Buridan reported in the 14th century that teams of ten horses could not pull open bellows when the port was sealed, apparently because of horror vacui.[8]

The Crookes tube, used to discover and study cathode rays, was an evolution of the Geissler tube.

The Crookes tube, used to discover and study cathode rays, was an evolution of the Geissler tube.

The belief in horror vacui was overthrown in the 17th century. Water pump designs had improved by then to the point that they produced measurable vacuums, but this was not immediately understood. What was known was that suction pumps could not pull water beyond a certain height: 18 Florentine yards according to a measurement taken around 1635. (The conversion to metres is uncertain, but it would be about 9 or 10 metres.) This limit was a concern to irrigation projects, mine drainage, and decorative water fountains planned by the Duke of Tuscany, so the Duke commissioned Galileo to investigate the problem. Galileo advertised the puzzle to other scientists, including Gaspar Berti who replicated it by building the first water barometer in Rome in 1639.[12] Berti's barometer produced a vacuum above the water column, but he could not explain it. The breakthrough was made by Evangelista Torricelli in 1643. Building upon Galileo's notes, he built the first mercury barometer and wrote a convincing argument that the space at the top was a vacuum. The height of the column was then limited to the maximum weight that atmospheric pressure could support. Some people believe that although Torricelli's experiment was crucial, it was Blaise Pascal's experiments that proved the top space really contained vacuum.

In 1654, Otto von Guericke invented the first vacuum pump and conducted his famous Magdeburg hemispheres experiment, showing that teams of horses could not separate two hemispheres from which the air had been evacuated. Robert Boyle improved Guericke's design and conducted experiments on the properties of vacuum. Robert Hooke also helped Boyle produce an air pump which helped to produce the vacuum. The study of vacuum then lapsed until 1855, when Heinrich Geissler invented the mercury displacement pump and achieved a record vacuum of about 10 Pa (0.1 Torr). A number of electrical properties become observable at this vacuum level, and this renewed interest in vacuum. This, in turn, led to the development of the vacuum tube.

While outer space has been likened to a vacuum, early theories of the nature of light relied upon the existence of an invisible, aetherial medium which would convey waves of light (Isaac Newton relied on this idea to explain refraction and radiated heat).[13] This evolved into the luminiferous aether of the 19th century, but the idea was known to have significant shortcomings - specifically that if the Earth were moving through a material medium, the medium would have to be both extremely tenuous (because the Earth is not detectably slowed in its orbit), and extremely rigid (because vibrations propagate so rapidly). An 1891 article by William Crookes noted: "the [freeing of] occluded gases into the vacuum of space".[14] Even up until 1912, astronomer Henry Pickering commented: "While the interstellar absorbing medium may be simply the ether, [it] is characteristic of a gas, and free gaseous molecules are certainly there".[15]

In 1887, the Michelson-Morley experiment, using an interferometer to attempt to detect the change in the speed of light caused by the Earth moving with respect to the aether, was a famous null result, showing that there really was no static, pervasive medium throughout space and through which the Earth moved as though through a wind. While there is therefore no aether, and no such entity is required for the propagation of light, space between the stars is not completely empty. Besides the various particles which comprise cosmic radiation, there is a cosmic background of photonic radiation (light), including the thermal background at about 2.7 K, seen as a relic of the Big Bang. None of these findings affect the outcome of the Michelson-Morley experiment to any significant degree.

Einstein argued that physical objects are not located in space, but rather have a spatial extent. Seen this way, the concept of empty space loses its meaning.[16] Rather, space is an abstraction, based on the relationships between local objects. Nevertheless, the general theory of relativity admits a pervasive gravitational field, which, in Einstein's words[17], may be regarded as an "aether", with properties varying from one location to another. One must take care, though, to not ascribe to it material properties such as velocity and so on.

In 1930, Paul Dirac proposed a model of vacuum as an infinite sea of particles possessing negative energy, called the Dirac sea. This theory helped refine the predictions of his earlier formulated Dirac equation, and successfully predicted the existence of the positron, discovered two years later in 1932. Despite this early success, the idea was soon abandoned in favour of the more elegant quantum field theory.

The development of quantum mechanics has complicated the modern interpretation of vacuum by requiring indeterminacy. Niels Bohr and Werner Heisenberg's uncertainty principle and Copenhagen interpretation, formulated in 1927, predict a fundamental uncertainty in the instantaneous measurability of the position and momentum of any particle, and which, not unlike the gravitational field, questions the emptiness of space between particles. In the late 20th century, this principle was understood to also predict a fundamental uncertainty in the number of particles in a region of space, leading to predictions of virtual particles arising spontaneously out of the void. In other words, there is a lower bound on the vacuum, dictated by the lowest possible energy state of the quantized fields in any region of space.

[edit] Quantum-mechanical definition

For more details on this topic, see vacuum state.

In quantum mechanics, the vacuum is defined as the state (i.e. solution to the equations of the theory) with the lowest energy. To first approximation, this is simply a state with no particles, hence the name.

Even an ideal vacuum, thought of as the complete absence of anything, will not in practice remain empty. Consider a vacuum chamber that has been completely evacuated, so that the (classical) particle concentration is zero. The walls of the chamber will emit light in the form of black body radiation. This light carries momentum, so the vacuum does have a radiation pressure. This limitation applies even to the vacuum of interstellar space. Even if a region of space contains no particles, the Cosmic Microwave Background fills the entire universe with black body radiation.

An ideal vacuum cannot exist even inside of a molecule. Each atom in the molecule exists as a probability function of space, which has a certain non-zero value everywhere in a given volume. Thus, even "between" the atoms there is a certain probability of finding a particle, so the space cannot be said to be a vacuum.

More fundamentally, quantum mechanics predicts that vacuum energy will be different from its naive, classical value. The quantum correction to the energy is called the zero-point energy and consists of energies of virtual particles that have a brief existence. This is called vacuum fluctuation. Vacuum fluctuations may also be related to the so-called cosmological constant in cosmology. The best evidence for vacuum fluctuations is the Casimir effect and the Lamb shift.[11]

In quantum field theory and string theory, the term "vacuum" is used to represent the ground state in the Hilbert space, that is, the state with the lowest possible energy. In free (non-interacting) quantum field theories, this state is analogous to the ground state of a quantum harmonic oscillator. If the theory is obtained by quantization of a classical theory, each stationary point of the energy in the configuration space gives rise to a single vacuum. String theory is believed to have a huge number of vacua - the so-called string theory landscape.

[edit] Pumping

The manual water pump draws water up from a well by creating a vacuum that water rushes in to fill. In a sense, it acts to evacuate the well, although the high leakage rate of dirt prevents a high quality vacuum from being maintained for any length of time.

The manual water pump draws water up from a well by creating a vacuum that water rushes in to fill. In a sense, it acts to evacuate the well, although the high leakage rate of dirt prevents a high quality vacuum from being maintained for any length of time.
Main article: Vacuum pump

Fluids cannot be pulled, so it is technically impossible to create a vacuum by suction. Suction can spread and dilute a vacuum by letting a higher pressure push fluids into it, but the vacuum has to be created first before suction can occur. The easiest way to create an artificial vacuum is to expand the volume of a container. For example, the diaphragm muscle expands the chest cavity, which causes the volume of the lungs to increase. This expansion reduces the pressure and creates a partial vacuum, which is soon filled by air pushed in by atmospheric pressure.

To continue evacuating a chamber indefinitely without requiring infinite growth, a compartment of the vacuum can be repeatedly closed off, exhausted, and expanded again. This is the principle behind positive displacement pumps, like the manual water pump for example. Inside the pump, a mechanism expands a small sealed cavity to create a vacuum. Because of the pressure differential, some fluid from the chamber (or the well, in our example) is pushed into the pump's small cavity. The pump's cavity is then sealed from the chamber, opened to the atmosphere, and squeezed back to a minute size.

A cutaway view of a turbomolecular pump, a momentum transfer pump used to achieve high vacuum

A cutaway view of a turbomolecular pump, a momentum transfer pump used to achieve high vacuum

The above explanation is merely a simple introduction to vacuum pumping, and is not representative of the entire range of pumps in use. Many variations of the positive displacement pump have been developed, and many other pump designs rely on fundamentally different principles. Momentum transfer pumps, which bear some similarities to dynamic pumps used at higher pressures, can achieve much higher quality vacuums than positive displacement pumps. Entrapment pumps can capture gases in a solid or absorbed state, often with no moving parts, no seals and no vibration. None of these pumps are universal; each type has important performance limitations. They all share a difficulty in pumping low molecular weight gases, especially hydrogen, helium, and neon.

The lowest pressure that can be attained in a system is also dependent on many things other than the nature of the pumps. Multiple pumps may be connected in series, called stages, to achieve higher vacuums. The choice of seals, chamber geometry, materials, and pump-down procedures will all have an impact. Collectively, these are called vacuum technique. And sometimes, the final pressure is not the only relevant characteristic. Pumping systems differ in oil contamination, vibration, preferential pumping of certain gases, pump-down speeds, intermittent duty cycle, reliability, or tolerance to high leakage rates.

In ultra high vacuum systems, some very odd leakage paths and outgassing sources must be considered. The water absorption of aluminium and palladium becomes an unacceptable source of outgassing, and even the adsorptivity of hard metals such as stainless steel or titanium must be considered. Some oils and greases will boil off in extreme vacuums. The permeability of the metallic chamber walls may have to be considered, and the grain direction of the metallic flanges should be parallel to the flange face.

The lowest pressures currently achievable in laboratory are about 10-13 Torr.[18] However, pressures as low as 5×10-17 Torr have been indirectly measured in a 4 K cryogenic vacuum system.[19]

[edit] Outgassing

Main article: Outgassing

Evaporation and sublimation into a vacuum is called outgassing. All materials, solid or liquid, have a small vapour pressure, and their outgassing becomes important when the vacuum pressure falls below this vapour pressure. In man-made systems, outgassing has the same effect as a leak and can limit the achievable vacuum. Outgassing products may condense on nearby colder surfaces, which can be troublesome if they obscure optical instruments or react with other materials. This is of great concern to space missions, where an obscured telescope or solar cell can ruin an expensive mission.

The most prevalent outgassing product in man-made vacuum systems is water absorbed by chamber materials. It can be reduced by desiccating or baking the chamber, and removing absorbent materials. Outgassed water can condense in the oil of rotary vane pumps and reduce their net speed drastically if gas ballasting is not used. High vacuum systems must be clean and free of organic matter to minimize outgassing.

Ultra-high vacuum systems are usually baked, preferably under vacuum, to temporarily raise the vapour pressure of all outgassing materials and boil them off. Once the bulk of the outgassing materials are boiled off and evacuated, the system may be cooled to lower vapour pressures and minimize residual outgassing during actual operation. Some systems are cooled well below room temperature by liquid nitrogen to shut down residual outgassing and simultaneously cryopump the system.

[edit] Quality

The quality of a vacuum is indicated by the amount of matter remaining in the system, so that a high quality vacuum is one with very little matter left in it. Vacuum is primarily measured by its absolute pressure, but a complete characterization requires further parameters, such as temperature and chemical composition. One of the most important parameters is the mean free path (MFP) of residual gases, which indicates the average distance that molecules will travel between collisions with each other. As the gas density decreases, the MFP increases, and when the MFP is longer than the chamber, pump, spacecraft, or other objects present, the continuum assumptions of fluid mechanics do not apply. This vacuum state is called high vacuum, and the study of fluid flows in this regime is called particle gas dynamics. The MFP of air at atmospheric pressure is very short, 70 nm, but at 100 mPa (~1×10-3 Torr) the MFP of room temperature air is roughly 100 mm, which is on the order of everyday objects such as vacuum tubes. The Crookes radiometer turns when the MFP is larger than the size of the vanes.

Vacuum quality is subdivided into ranges according to the technology required to achieve it or measure it. These ranges do not have universally agreed definitions, but a typical distribution is as follows:[20][21]


  • Atmospheric pressure is variable but standardized at 101.325 kPa (760 Torr)
  • Low vacuum, also called rough vacuum or coarse vacuum, is vacuum that can be achieved or measured with rudimentary equipment such as a vacuum cleaner and a liquid column manometer.
  • Medium vacuum is vacuum that can be achieved with a single pump, but is too low to measure with a liquid or mechanical manometer. It can be measured with a McLeod gauge, thermal gauge or a capacitive gauge.
  • High vacuum is vacuum where the MFP of residual gases is longer than the size of the chamber or of the object under test. High vacuum usually requires multi-stage pumping and ion gauge measurement. Some texts differentiate between high vacuum and very high vacuum.
  • Ultra high vacuum requires baking the chamber to remove trace gases, and other special procedures. British and German standards define ultra high vacuum as pressures below 10-6 Pa (10-8 Torr).[22][23]
  • Deep space is generally much more empty than any artificial vacuum that we can create. It may or may not meet the definition of high vacuum above, depending on what region of space and astronomical bodies are being considered. For example, the MFP of interplanetary space is smaller than the size of the solar system, but larger than small planets and moons. As a result, solar winds exhibit continuum flow on the scale of the solar system, but must be considered as a bombardment of particles with respect to the Earth and Moon.
  • Perfect vacuum is an ideal state that cannot be obtained in a laboratory, nor can it be found in outer space.

[edit] Measurement

Main article: Pressure measurement

Vacuum is measured in units of pressure. The SI unit of pressure is the pascal (symbol Pa), but vacuum is usually measured in torrs (symbol Torr), named for Torricelli, an early Italian physicist (1608 - 1647). A torr is equal to the displacement of a millimeter of mercury (mmHg) in a manometer with 1 torr equaling 133.3223684 pascals above absolute zero pressure. Vacuum is often also measured using inches of mercury on the barometric scale or as a percentage of