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cosmic ray

 

n.
A stream of ionizing radiation of extraterrestrial origin, consisting chiefly of protons, alpha particles, and other atomic nuclei but including some high-energy electrons, that enters the atmosphere, collides with atomic nuclei, and produces secondary radiation, principally pions, muons, electrons, and gamma rays.


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Wiley Book of Astronomy:

cosmic rays

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Subatomic particles that move through space close to the speed of light; their origin is one of the major unsolved mysteries of astrophysics, although researchers are moving closer to a solution. Cosmic rays consist of about 85% protons, 14% alpha particles (helium nuclei), about 1% electrons and other elementary particles, and a tiny smattering of nuclei heavier than helium. Their energies range from 10 million eV to 1 million trillion eV—equivalent, at the high end, to the punch of a major league baseball pitch. Three categories of cosmic rays are recognized: solar, galactic, and extragalactic. Solar cosmic rays, with energies of 107 to 1010 eV, are ejected by the Sun during solar flares. Galactic cosmic rays, with energies of 1010 to 1015 eV and extragalactic cosmic rays, with energies up to 1018 eV, come from all parts of the sky and, at lower energies, have their original directions partially scrambled by the galactic magnetic field.

Cosmic rays in space are known as primary cosmic rays and can be detected directly only by instruments above Earth's atmosphere. When they collide with atoms and molecules in the upper atmosphere, they generate showers (known as cosmic-ray showers or air showers) of secondary cosmic rays. The initial collision produces pions, which quickly decay into muons, some of which decay further into electrons, positrons, and neutrinos. Deceleration of the electrons and positrons in the atmosphere produces a flash of light that can be observed from the ground with special telescopes; however, most of the secondary cosmic-ray particles that reach sea-level are undecayed muons. Observations of these muons and of the aerial light-flashes from electrons and positrons provide information on the primary cosmic ray that caused the cascade. Increasingly powerful equipment in space, in the atmosphere, and on the ground is helping unravel the enigma of galactic and extragalactic cosmic rays.

It had been suspected that many of the galactic variety are generated by shock waves from supernovae. Researchers had already shown that supernova remnants can accelerate electrons to cosmic-ray energies, but there was no evidence that protons are accelerated by the same mechanism. Then in 2002, a Japanese team reported that it had, for the first time, associated a supernova remnant with cosmic-ray protons. On several occasions, the team detected light showers due to protons coming from a patch of sky that contains a supernova remnant called RX J1713. 7-3946.

The origin of extragalactic cosmic rays, the most energetic particles known, is also becoming clearer. Analyzing data from high-energy cosmic-ray detectors in Japan and England, researchers announced in 2002 that they had traced the trajectories of several cosmic rays to four galaxies known to surround dead or dormant quasars, which almost certainly contain super-massive black holes. The finding fits with a scenario in which a spinning, supermassive black hole acts like a giant battery. Magnetic field lines in close contact with the rotating hole generate a billion trillion volts, which accelerate charged particles to ultrahigh energies. In this theory, the quasar must be dormant. If the cosmic rays revved up by the black hole were to collide with intense radiation from an active quasar, their energy would be drained away.

High-speed particle (atomic nucleus or electron) that travels through the Milky Way Galaxy. Some cosmic rays originate from the Sun, but most come from outside the solar system. Primary cosmic rays that reach Earth's atmosphere collide with nuclei in it, creating secondaries. Because lower-energy primaries are strongly influenced by the interplanetary magnetic field and Earth's magnetic field (see geomagnetic field), most of those detected near Earth have very high energy, corresponding to speeds about 87% that of light or more. Observations from spacecraft indicate that most cosmic rays come from the Galaxy's disk, but the highest-energy ones are probably extragalactic. Details of their production and acceleration remain unclear, but apparently expanding shock waves from supernovas can accelerate particles. From the early 1930s to the 1950s, cosmic rays were the only source of high-energy particles used in studying the atomic nucleus and its components. Short-lived subatomic particles were discovered through cosmic-ray collisions, leading to the rise of particle physics. Even powerful particle accelerators cannot impart energy anywhere near that of the highest-energy cosmic rays. See also Victor Francis Hess.

For more information on cosmic ray, visit Britannica.com.

Electrons and the nuclei of atoms—largely hydrogen—that impinge upon Earth from all directions of space with nearly the speed of light. These nuclei with relativistic speeds are often referred to as primary cosmic rays, to distinguish them from the cascade of secondary particles generated by their impact against air nuclei at the top of the terrestrial atmosphere. The secondary particles shower down through the atmosphere and are found all the way to the ground and below.

The primary cosmic rays provide the only direct sample of matter from outside the solar system. Measurement of their composition can aid in understanding which aspects of the matter making up the solar system are typical of the Milky Way Galaxy as a whole and which may be so atypical as to yield specific clues to the origin of the solar system. Cosmic rays are electrically charged; hence they are deflected by the magnetic fields which are thought to exist throughout the Galaxy, and may be used as probes to determine the nature of these fields far from Earth. Outside the solar system the energy contained in the cosmic rays is comparable to that of the magnetic field, so the cosmic rays probably play a major role in determining the structure of the field. Collisions between the cosmic rays and the nuclei of the atoms in the tenuous gas which permeates the Galaxy change the cosmic-ray composition in a measurable way and produce gamma rays which can be detected at Earth, giving information on the distribution of this gas.

Cosmic-ray detection

All cosmic-ray detectors are sensitive only to moving electrical charges. Neutral cosmic rays (neutrons, gamma rays, and neutrinos) are studied by observing the charged particles produced in the collision of the neutral primary with some type of target. At low energies the ionization of the matter through which they pass is the principal means of detection. A single measurement of the ionization produced by a particle is usually not sufficient both to identify the particle and to determine its energy. However, since the ionization itself represents a significant energy loss to a low-energy particle, it is possible to design systems of detectors which trace the rate at which the particle slows down and thus to obtain unique identification and energy measurement.

At energies above about 500 MeV per nucleon, almost all cosmic rays will suffer a catastrophic nuclear interaction before they slow appreciably. An ionization measurement is commonly combined with measurements of physical effects which vary in a different way with mass, charge, and energy. Cerenkov detectors and the deflection of the particles in the field of large superconducting magnets or the magnetic field of the Earth itself provide the best means of studying energies up to a few hundred GeV per nucleon. Detectors employing the phenomenon of x-ray transition radiation promise to be useful for measuring composition at energies up to a few thousand GeV per nucleon. See also Cerenkov radiation; Superconducting devices.

Above about 1012 eV, direct detection of individual particles is no longer possible since they are so rare. Such particles are studied by observing the large showers of secondaries they produce in Earth's atmosphere. These showers are detected either by counting the particles which survive to strike ground-level detectors or by looking at the flashes of light the showers produce in the atmosphere with special telescopes and photomultiplier tubes. See also Particle detector; Photomultiplier.

Atmospheric cosmic rays

The primary cosmic-ray particles coming into the top of the terrestrial atmosphere make inelastic collisions with nuclei in the atmosphere. When a high-energy nucleus collides with the nucleus of an air atom, a number of things usually occur. Rapid deceleration of the incoming nucleus leads to production of pions with positive, negative, or neutral charge. A few protons and neutrons (in about equal proportions) may be knocked out with energies up to a few GeV. They are called knock-on protons and neutrons.

All these protons, neutrons, and pions generated by collision of the primary cosmic-ray nuclei with the nuclei of air atoms are the first stage in the development of the secondary cosmic-ray particles observed inside the atmosphere. Since several secondary particles are produced by each collision, the total number of energetic particles of cosmic-ray origin will increase with depth, even while the primary density is decreasing.

The uncharged π0 mesons decay into two gamma rays with a life of about 8 × 10−17 s. The two gamma rays each produce a positron-electron pair. Upon passing sufficiently close to the nucleus of an air atom deeper in the atmosphere, the electrons and positrons convert their energy into bremsstrahlung. The bremsstrahlung in turn create new positron-electron pairs, and so on. This cascade process continues until the energy of the initial π0 has been dispersed into a shower of positrons, electrons, and photons with insufficient individual energies (≤1 MeV) to continue the pair production. The electrons and photons of such showers are referred to as the soft component of the atmospheric (secondary) cosmic rays. See also Electron-positron pair production.

The π± mesons produced by the primary collisions have a life of about 2.6 × 10−8 s before they decay into muons. Most low-energy π± decay into muons before they have time to undergo nuclear interactions. Except at very high energy (above 500 GeV), muons interact relatively weakly with nuclei, and are too massive (207 electron masses) to produce bremsstrahlung. They lose energy mainly by the comparatively feeble process of ionizing an occasional air atom as they progress downward through the atmosphere. Because of this ability to penetrate matter, they are called the hard component.

The high-energy nucleons—the knock-on protons and neutrons—produced by the primary-particle collisions and a few pion collisions proceed down into the atmosphere. They produce nuclear interactions of the same kind as the primary nuclei, though of course with diminished energies. This cascade process constitutes the nucleonic component of the secondary cosmic rays.

Solar modulation

The cosmic-ray intensity is lower during the years of high solar activity and sunspot number, which follow an 11-year cycle. This effect has been extensively studied with ground-based and spacecraft instruments.

The primary cause of solar modulation is the solar wind, a highly ionized gas (plasma) which boils off the solar corona and propagates radially from the Sun at a velocity of about 250 mi/s (400 km/s). The wind is mostly hydrogen, with typical density of 80 protons per cubic inch (5 protons per cubic centimeter). This density is too low for collisions with cosmic rays to be important. Rather, the high conductivity of the medium traps part of the solar magnetic field and carries it outward.

In addition to the bulk sweeping action, another effect of great importance occurs in the solar wind, adiabatic deceleration. Because the wind is blowing out, only those particles which chance to move upstream fast enough are able to reach Earth. However, because of the expansion of the wind, particles interacting with it lose energy. Thus, particles observed at Earth with energy of 10 MeV per nucleon actually started out with several hundred MeV per nucleon in nearby interstellar space, and those with initial energy of only 100–200 MeV per nucleon probably never reach Earth at all.

Composition of cosmic rays

Nuclei ranging from protons to lead have been identified in the cosmic radiation. The relative abundances of the elements may be compared with the best estimate of the “universal abundances” obtained by combining measurements of solar spectra, lunar and terrestrial rocks, meteorites, and so forth. Most obvious is the similarity between the two distributions. However, a systematic deviation is quickly apparent: the elements lithium-boron and scandium-manganese as well as most of the odd-charged nuclei are vastly overabundant in the cosmic radiation. This effect has a simple explanation: the cosmic rays travel great distances in the galaxy and occasionally collide with atoms of interstellar gas—mostly hydrogen and helium—and fragment. This fragmentation, or spallation as it is called, produces lighter nuclei from heavier ones but does not change the energy per nucleon very much. Thus the energy spectra of the secondaries are similar to those of the primaries. Calculations involving reaction probabilities determined by nuclear physicists show that the overabundances of the secondary elements can be explained by assuming that cosmic rays pass through an average of about 1 oz per square inch (5 g per square centimeter) of material on their way to Earth.

When spallation has been corrected for, differences between cosmic-ray abundances and solar-system or universal abundances still remain. The most important question is whether these differences are due to the cosmic rays having come from a special kind of material (such as would be produced in a supernova explosion), or simply to the fact that some atoms might be more easily accelerated than others.

Cosmic-ray electron measurements pose other problems of interpretation, partly because electrons are nearly 2000 times lighter than protons, the next lightest cosmic-ray component. Protons with kinetic energy above 1 GeV are about 100 times as numerous as electrons above the same energy, with the relative number of electrons decreasing slowly at higher energies. But it takes about 2000 GeV to give a proton the same velocity as a 1-GeV electron. Viewed in this way electrons are several thousand times more abundant than protons. It is thus quite possible that cosmic electrons have a different source entirely from the nuclei.

Age

Another important result which can be derived from detailed knowledge of cosmic-ray isotopic composition is the “age” of cosmic radiation. Certain isotopes are radioactive, such as beryllium-10 with a half-life of 1.6 × 106 years. Since Be is produced entirely by spallation, study of the relative abundance of 10Be to the other Be isotopes, particularly as a function of energy to utilize the relativistic increase in this lifetime, will yield a number related to the average time since the last nuclear collision. Measurements show that 10Be is nearly absent at low energies and yield an estimate of the age of the cosmic rays of approximately 107 years. An implication of this result is that the cosmic rays propagate in a region in space which has an average density of 1.5–3 atoms per cubic inch (0.1–0.2 atom per cubic centimeter). This is consistent with some astronomical observations of the immediate solar neighborhood.

Origin

Although study of cosmic rays has yielded valuable insight into the structure, operation, and history of the universe, their origin has not been determined. The problem is not so much to devise processes which might produce cosmic rays, but to decide which of many possible processes do in fact produce them.

It is thought that cosmic rays are produced by mechanisms operating within galaxies and are confined almost entirely to the galaxy of their production, trapped by the galactic magnetic field. The intensity in intergalactic space would only be a few percent of the typical galactic intensity, and would be the result of a slow leakage of the galactic particles out of the magnetic trap.


Notionally, the cause of bit rot. However, this is a semi-independent usage that may be invoked as a humorous way to handwave away any minor randomness that doesn't seem worth the bother of investigating. “Hey, Eric — I just got a burst of garbage on my tube, where did that come from?” “Cosmic rays, I guess.” Compare sunspots, phase of the moon. The British seem to prefer the usage cosmic showers; alpha particles is also heard, because stray alpha particles passing through a memory chip can cause single-bit errors (this becomes increasingly more likely as memory sizes and densities increase).

Factual note: Alpha particles cause bit rot, cosmic rays do not (except occasionally in spaceborne computers). Intel could not explain random bit drops in their early chips, and one hypothesis was cosmic rays. So they created the World's Largest Lead Safe, using 25 tons of the stuff, and used two identical boards for testing. One was placed in the safe, one outside. The hypothesis was that if cosmic rays were causing the bit drops, they should see a statistically significant difference between the error rates on the two boards. They did not observe such a difference. Further investigation demonstrated conclusively that the bit drops were due to alpha particle emissions from thorium (and to a much lesser degree uranium) in the encapsulation material. Since it is impossible to eliminate these radioactives (they are uniformly distributed through the earth's crust, with the statistically insignificant exception of uranium lodes) it became obvious that one has to design memories to withstand these hits.


Columbia Encyclopedia:

cosmic rays

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cosmic rays, charged particles moving at nearly the speed of light reaching the earth from outer space. Primary cosmic rays consist mostly of protons (nuclei of hydrogen atoms), some alpha particles (helium nuclei), and lesser amounts of nuclei of carbon, nitrogen, oxygen, and heavier atoms. These nuclei collide with nuclei in the upper atmosphere, producing secondary cosmic rays of protons, neutrons, mesons, electrons, and gamma rays of high energy, which in turn hit nuclei lower in the atmosphere to produce more particles (see elementary particles). These cascade processes continue until all the energy of the primary particle is dissipated. The secondary particles shower down through the atmosphere in diminishing intensity to the earth's surface and even penetrate it. The size of the shower indicates the energy of the primary ray, which may be as high as 1020 electron volts (eV) or more, almost a billion times higher than the highest energy yet produced in a man-made particle accelerator; however, cosmic rays of lower energy predominate. Cosmic rays were long used as a source of high-energy particles in the study of nuclear reactions. The positron, the muon, the pion (or pi meson), and some of the so-called strange particles were initially discovered in studies of this radiation. Cosmic rays were first found to be of extraterrestrial origin by Victor F. Hess (c.1912) when he recorded them with electrometers carried to high altitudes in balloons, an achievement for which he won the Nobel Prize in 1936. They were so named in 1925 by R. A. Millikan, who did extensive research on them. Since then much pertinent information has been collected that have been of use in studying the chemical composition of the universe, but the origin of cosmic rays remains a mystery. However, when they react with interstellar gases, the result is a gamma ray that can be traced back. Spacecraft results indicate that many of the gamma rays appear to come from the direction of supernova remnants. The nature of the acceleration processes by which the primary particles achieve great velocities (very nearly the speed of light) is also still highly speculative. Modern electronic detectors called charge coupled devices (CCDs) are effective cosmic ray detectors; a ray can strike a single pixel, making it much brighter than the surrounding ones. Cosmic rays play a significant role in the natural mutation and evolution of life on earth.

Bibliography

See B. B. Rossi, Cosmic Rays (1964); L. I. Dorman, Cosmic Rays (1974); M. W. Friedlander, Cosmic Rays (1989).


Cosmic Lexicon:

Cosmic rays

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Extremely high-energy subatomic particles that continuously bombard Earth from all directions. Most cosmic rays hit and break up atomic nuclei in the upper atmosphere.

Elementary particles, mainly protons, that are produced by the sun and other stars and then strike the upper atmosphere of the Earth. Some of these particles are absorbed, some help form the Van Allen belt, and some reach the Earth's surface, where they form a part of the background radiation that constantly surrounds us.

Oxford Dictionary of English:

Cosmic Radiation

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→ noun [mass noun] radiation consisting of cosmic rays.

Ionizing irradiation from outer space bombarding the earth and its atmosphere. They contribute to the background radiation that is always present at the earth's surface.


n

Radiation that originates outside the earth’s atmosphere. Cosmic rays have extremely short wavelengths. They are able to produce ionization as they pass through the air and other matter and are capable of penetrating many feet of material such as lead and rock. The primary cosmic rays probably consist of atomic nuclei (mainly protons), some of which may have energies of the order of 1010 to 1015 eV. Secondary cosmic rays are produced when the primary cosmic rays interact with nuclei and electrons (for example, in the earth’s atmosphere). Secondary cosmic rays consist mainly of mesons, protons, neutrons, electrons, and photons that have less energy than the primary rays. Practically all the primary cosmic rays are absorbed in the upper atmosphere. Almost all cosmic radiation observed at the earth’s surface is of the secondary type.

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Wikipedia on Answers.com:

Cosmic ray

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The energy spectrum for cosmic rays

Cosmic rays are energetic charged subatomic particles, originating in outer space. They may produce secondary particles that penetrate the Earth's atmosphere and surface. The term ray is historical as cosmic rays were thought to be electromagnetic radiation. Most primary cosmic rays (those that enter the atmosphere from deep space) are composed of familiar stable subatomic particles that normally occur on Earth, such as protons, atomic nuclei, or electrons. However, a very small fraction are stable particles of antimatter, such as positrons or antiprotons, and the precise nature of this remaining fraction is an area of active research.

About 89% of cosmic rays are simple protons or hydrogen nuclei, 10% are helium nuclei or alpha particles, and 1% are the nuclei of heavier elements. These nuclei constitute 99% of the cosmic rays. Solitary electrons (much like beta particles, although their ultimate source is unknown) constitute much of the remaining 1%.

The variety of particle energies reflects the wide variety of sources. The origins range from processes on the Sun (and presumably other stars as well), to as yet unknown physical mechanisms in the farthest reaches of the observable universe. There is evidence that very high energy cosmic rays are produced over far longer periods than the explosion of a single star or sudden galactic event, suggesting multiple accelerating processes that cover very long distances with regard to the size of stars. The obscure mechanism of cosmic ray production at galactic distances is partly a result of the fact that (unlike other radiations) magnetic fields in our galaxy and other galaxies bend cosmic ray direction severely, so that they arrive nearly randomly from all directions, hiding any clue of the direction of their initial sources. Cosmic rays can have energies of over 1020 eV, far higher than the 1012 to 1013 eV that Terrestrial particle accelerators can produce. There has been interest in investigating cosmic rays of even greater energies.[1]

Cosmic rays are enriched in lithium, beryllium, and boron with regard to the relative abundance of these elements in the universe compared to hydrogen and helium, and thus are thought to have a primary role in the synthesis of these three elements through the process of "cosmic ray nucleosynthesis". They also produce some so-called cosmogenic stable isotopes and radioisotopes on Earth, such as carbon-14.[2] In the history of particle physics, cosmic rays were the source of the discovery of the positron, muon, and pi meson.

Cosmic rays compose a part of natural background radiation on Earth, averaging about 10-15% of it. However, persons living at higher altitude can obtain several times more cosmic radiation than at sea level, and long distance airline crews can double their yearly ionizing radiation exposure due to this source. Since the intensity of cosmic rays is much larger outside the Earth's atmosphere and magnetic field, it is expected to have a major impact on the design of spacecraft that can safely transport humans in interplanetary space.

Contents

Composition

Cosmic rays may broadly be divided into two categories: primary and secondary. The cosmic rays that originate from astrophysical sources are primary cosmic rays; these primary cosmic rays interact with interstellar matter creating secondary cosmic rays. The Sun also emits low energy cosmic rays associated with solar flares. Almost 90% of cosmic rays are protons, about 9% are helium nuclei (alpha particles) and nearly 1% are electrons. The ratio of hydrogen to helium nuclei (28%) is about the same as the primordial elemental abundance ratio of these elements (24%).[citation needed]

The remaining fraction is made up of the other heavier nuclei that are nuclear synthesis end products, products of the Big Bang, primarily lithium, beryllium, and boron. These light nuclei appear in cosmic rays in much greater abundance (~1%) than in the solar atmosphere, where their abundance is about 10−9% that of helium.

This abundance difference is a result of the way secondary cosmic rays are formed. Carbon and oxygen nuclei collide with interstellar matter to form lithium, beryllium and boron in a process termed cosmic ray spallation. Spallation is also responsible for the abundances of scandium, titanium, vanadium, and manganese ions in cosmic rays produced by collisions of iron and nickel nuclei with interstellar matter. See Natural Environmental Radioactivity.

Satellite experiments have found evidence of a few antiprotons and positrons in primary cosmic rays, although there is no evidence of complex antimatter atomic nuclei, such as anti-helium nuclei (anti-alpha) particles. Antiprotons arrive at Earth with a characteristic energy maximum of 2 GeV, indicating their production in a fundamentally different process from cosmic ray protons.[3]

Flux

The flux of incoming cosmic rays at the upper atmosphere is dependent on the solar wind, the Earth's magnetic field, and the energy of the cosmic rays.

The solar wind decelerates the incoming particles and blocks some of the particles with energies below about 1 GeV. The amount of solar wind is not constant due to changes in solar activity. Thus, the level of the cosmic ray flux varies with solar activity. The Earth's magnetic field deflects some of the cosmic rays, giving rise to the observation that the flux is apparently dependent on latitude, longitude, and azimuth angle. The magnetic field lines deflect the cosmic rays towards the poles, giving rise to the aurora.

At distances of ~94 AU from the Sun, the solar wind undergoes a transition, called the termination shock, from supersonic to subsonic speeds. The region between the termination shock and the heliopause acts as a barrier to cosmic rays, decreasing the flux at lower energies by about 90%.

In the past, it was believed that the cosmic ray flux remained fairly constant over time. However, recent research suggests 1.5 to 2-fold millennium-timescale changes in the cosmic ray flux in the past forty thousand years.[4]

The magnitude of the energy of cosmic ray flux in interstellar space is very comparable to that of other deep space energies: cosmic ray energy density averages about one electron-volt per cubic centimeter of interstellar space, or ~1 eV/cm3, which is comparable to the energy density of visible starlight at 0.3 eV/cm3, the galactic magnetic field energy density (assumed 3 microgauss) which is ~0.25 eV/cm3, or the cosmic microwave background (CMB) radiation energy density at ~ 0.25 eV/cm3.[5]

However, cosmic rays, unlike the other energy components above, are composed of ionizing particles, and this is far more damaging to biological processes than simple energies suggest. As noted below, cosmic rays make up on average 10 to 15% of background ionizing radiation to humans on Earth, but this component can be several times larger for persons living at higher altitudes.

Detection

The Moon's cosmic ray shadow, as seen in secondary muons detected 700 m below ground, at the Soudan 2 detector
The Moon as seen by the Compton Gamma Ray Observatory, in gamma rays of greater than 20 MeV. These are produced by cosmic ray bombardment of its surface.[6]

Cosmic rays collide with the nuclei of atmospheric gases, producing a shower of, among others, pions and kaons, that decay into muons. These muons are able to reach the surface of the Earth, and even penetrate for some distance into shallow mines. Muons are easily detected by many types of particle detectors such as cloud chambers or bubble chambers or scintillation detectors. Several muons observed by separated detectors at the same instant indicates that they have been produced in the same shower event.

Cosmic rays impacting other planetary bodies in the Solar System are detected indirectly by observing high energy gamma ray emissions by gamma-ray telescope. These are distinguished from radioactive decay processes by their higher energies above  about 10 MeV.

Detection by particle track-etch technique

Cosmic rays can also be detected directly by particle detectors aboard satellites or high altitude balloons. In a pioneering technique developed by Robert Fleischer, P. Buford Price, and Robert M. Walker,[7] sheets of clear plastic, like 1/4 mil Lexan polycarbonate, are stacked together and exposed directly to cosmic rays in space or high altitude. The nuclear charge causes chemical bond breaking or ionization in the plastic. At the top of the plastic stack, the ionization is less due to the high cosmic ray speed. As the cosmic ray speed decreases due to deceleration in the stack, the ionization increases along the path. The resulting plastic sheets are "etched" or slowly dissolved in warm caustic sodium hydroxide solution, that removes the surface material at a slow, known rate. The caustic sodium hydroxide dissolves at a faster rate along the path of the ionized plastic. The net result is a conical shaped pit or etch pit in the plastic. The etch pits are measured under a high power microscope (typically 1600X oil-immersion), and the etch rate is plotted as a function of the depth in the stacked plastic. This yields a unique curve for each atomic nucleus of Z from 1 to 92, allowing identification of both the charge and energy of the cosmic ray that traverses the plastic stack. The more extensive the ionization along the path; the higher the charge.

This technique has been used with great success for detecting not only cosmic rays, but fission product nuclei for neutron detectors.

Detection by air shower

When cosmic rays enter the Earth's atmosphere they collide with molecules, mainly oxygen and nitrogen, to produce a cascade of billions of lighter particles, a so-called air shower.

Atmospheric Collision.svg

All of the produced particles stay within about one degree of the primary particle's path. Typical particles produced in such collisions are charged mesons e.g. positive and negative pions and kaons. These subsequently decay into muons that are easily detected by many types of particle detectors.

Research and experiments

There are a number of cosmic ray research initiatives. These include, but are not limited to:

History

After the discovery of radioactivity by Henri Becquerel in 1896, it was generally believed that atmospheric electricity, ionization of the air, was caused only by radiation from radioactive elements in the ground or the radioactive gases or isotopes of radon they produce. Measurements of ionization rates at increasing heights above the ground during the decade from 1900 to 1910 showed a decrease that could be explained as due to absorption of the ionizing radiation by the intervening air.

In 1909 Theodor Wulf developed an electrometer, a device to measure the rate of ion production inside a hermetically sealed container, and used it to show higher levels of radiation at the top of the Eiffel Tower than at its base. However, his paper published in Physikalische Zeitschrift was not widely accepted. In 1911 Domenico Pacini observed simultaneous variations of the rate of ionization over a lake, over the sea, and at a depth of 3 meters from the surface. Pacini concluded from the decrease of radioactivity underwater that a certain part of the ionization must be due to sources other than the radioactivity of the Earth.[8]

Pacini makes a measurement in 1910.

Then, in 1912, Victor Hess carried three enhanced-accuracy Wulf electrometers[9] to an altitude of 5300 meters in a free balloon flight. He found the ionization rate increased approximately fourfold over the rate at ground level.[9] Hess also ruled out the Sun as the radiation's source by making a balloon ascent during a near-total eclipse. With the moon blocking much of the Sun's visible radiation, Hess still measured rising radiation at rising altitudes.[9] He concluded "The results of my observation are best explained by the assumption that a radiation of very great penetrating power enters our atmosphere from above." In 1913–1914, Werner Kolhörster confirmed Victor Hess' earlier results by measuring the increased ionization rate at an altitude of 9 km.

Increase of ionization with altitude as measured by Hess in 1912 (left) and by Kolhörster (right)

Hess received the Nobel Prize in Physics in 1936 for his discovery.[10][11]

Hess lands after his balloon flight in 1912.

The term "cosmic rays" was coined by Robert Millikan who confirmed in 1925 they were extraterrestrial in origin, and not produced by atmospheric electricity. Millikan believed that cosmic rays were high-energy photons with some secondary electrons produced by Compton scattering of gamma rays. Compton himself held the (correct) belief that cosmic rays were primarily charged particles. During the decade from 1927 to 1937, a wide variety of experimental investigations demonstrated that the primary cosmic rays are mostly positively charged particles, and the secondary radiation observed at ground level is composed primarily of electrons, photons and muons. In 1948, observations with nuclear emulsions carried by balloons to near the top of the atmosphere by Gottlieb and Van Allen showed that the primary cosmic particles are mostly protons with some helium nuclei (alpha particles) and a small fraction heavier nuclei.

In 1934, Bruno Rossi reported an observation of near-simultaneous discharges of two Geiger counters widely separated horizontally during a test of equipment he was using in a measurement of the so-called east-west effect. In his report on the experiment, Rossi wrote "...it seems that once in a while the recording equipment is struck by very extensive showers of particles, which causes coincidences between the counters, even placed at large distances from one another." In 1937 Pierre Auger, unaware of Rossi's earlier report, detected the same phenomenon and investigated it in some detail. He concluded that extensive particle showers are generated by high-energy primary cosmic-ray particles that interact with air nuclei high in the atmosphere, initiating a cascade of secondary interactions that ultimately yield a shower of electrons, photons, and muons that reach ground level.

Attempts were made to measure the primary cosmic ray component at very high altitude. Soviet physicist Sergey Vernov was the first to use radiosondes to perform cosmic ray readings. On April 1, 1935, he took measurements at heights up to 13.6 kilometers using a pair of Geiger counters in an anti-coincidence circuit to avoid counting secondary ray showers.[12][13]

Homi J. Bhabha derived an expression for the probability of scattering positrons by electrons, a process now known as Bhabha scattering. His classic paper, jointly with Walter Heitler, published in 1937 described how primary cosmic rays from space interact with the upper atmosphere to produce particles observed at the ground level. Bhabha and Heitler explained the cosmic ray shower formation by the cascade production of gamma rays and positive and negative electron pairs.

Measurements of the energy and arrival directions of the ultra-high energy primary cosmic rays by the techniques of "density sampling" and "fast timing" of extensive air showers were first carried out in 1954 by members of the Rossi Cosmic Ray Group at the Massachusetts Institute of Technology. The experiment employed eleven scintillation detectors arranged within a circle 460 meters in diameter on the grounds of the Agassiz Station of the Harvard College Observatory. From that work, and from many other experiments carried out all over the world, the energy spectrum of the primary cosmic rays is now known to extend beyond 1020 eV. A huge air shower experiment called the Auger Project is currently operated at a site on the pampas of Argentina by an international consortium of physicists, led by James Cronin, 1980 Nobel Prize in Physics of the University of Chicago and Alan Watson of the University of Leeds. Their aim is to explore the properties and arrival directions of the very highest energy primary cosmic rays. The results are expected to have important implications for particle physics and cosmology, due to a theoretical Greisen–Zatsepin–Kuzmin limit to the energies of cosmic rays from long distances (about 160 million light years) which occurs above 1020 eV.

In November, 2007 preliminary results were announced showing direction of origination of the 27 highest energy events were strongly correlated with the locations of active galactic nuclei [AGN], where bare protons are believed to be accelerated by strong magnetic fields associated with the large black holes at the AGN centers to energies of 1020 eV and higher.

Effects

Changes in atmospheric chemistry

Cosmic rays ionize the nitrogen and oxygen molecules in the atmosphere, which leads to a number of chemical reactions. One of the reactions results in ozone depletion. Cosmic rays are also responsible for the continuous production of a number of unstable isotopes in the Earth’s atmosphere, such as carbon-14, via the reaction:

n + \mathrm{N}^{14} \rightarrow p + \mathrm{C}^{14}

Cosmic rays kept the level of carbon-14 [2] in the atmosphere roughly constant (70 tons) for at least the past 100,000 years, until the beginning of above-ground nuclear weapons testing in the early 1950s. This is an important fact used in radiocarbon dating used in archaeology.

Reaction products of primary cosmic rays, radioisotope lifetime, and production reaction.[14]
  • Tritium (12.3 years): 14N(n, 3H)12C (Spallation)
  • Beryllium-7 (53.3 days)
  • Beryllium-10 (1.6 million years): 14N(n,p α)10Be (Spallation)
  • Carbon-14 (5730 years): 14N(n, p)14C (Neutron activation)
  • Sodium-22 (2.6 years)
  • Sodium-24 (15 hours)
  • Magnesium-28 (20.9 hours)
  • Silicon-31 (2.6 hours)
  • Silicon-32 (101 years)
  • Phosphorus-32 (14.3 days)
  • Sulfur-35 (87.5 days)
  • Sulfur-38 (2.8 hours)
  • Chlorine-34 m (32 minutes)
  • Chlorine-36 (300,000 years)
  • Chlorine-38 (37.2 minutes)
  • Chlorine-39 (56 minutes)
  • Argon-39 (269 years)
  • Krypton-85 (10.7 years)

Role in ambient radiation

Cosmic rays constitute a fraction of the annual radiation exposure of human beings on the Earth, averaging 0.39 mSv out of a total of 3 mSv per year (13% of total background) for the Earth's population. However, the background due to cosmic rays can vary from 0.3 mSv/year at sea level to 1.0 mSv per year in high-altitude cities, which would raise cosmic radiation exposure to a quarter of the total background. Airline crews flying long distance high-altitude routes can be exposed to 2.2 mSv of extra radiation each year due to cosmic rays, which nearly doubles their total ionizing radiation exposure. The following table compares cosmic radiation doses to other sources of background radiation:

Average annual radiation exposure (millisievert)
Radiation UNSCEAR[15][16] Princeton[17] Wa State[18] MEXT[19]
Type Source World
average
Typical range USA USA Japan remark
Natural Air 1.26 0.2-10.0a 2.29 2.00 0.40 mainly from Radon, (a)depend on indoor accumulation of radon gas
Internal 0.29 0.2-1.0b 0.16 0.40 0.40 mainly from food (K-40, C-14, etc.) (b)Depend on diets
Terrestrial 0.48 0.3-1.0c 0.19 0.29 0.40 (c)depend on soil and building material
Cosmic 0.39 0.3-1.0d 0.31 0.26 0.30 (d)from sea level to high elevation
sub total 2.40 1.0-13.0 2.95 2.95 1.50
Man made Medical 0.60 0.03-2.0 3.00 0.53 2.30
Fallout 0.007 0 - 1+ - - 0.01 peak at 1963 and spike at 1986. still high near test and accident sites. US; Fallout is included in others
others 0.0052 0-20 0.25 0.13 0.001 average occupational exposure 0.7mSv, mining workers are high, population near Nuclear plant 0.02mSv
sub total 0.6 0 to tens 3.25 0.66 2.311
Total 3.00 0 to tens 6.20 3.61 3.81
figures are pre "2011 Fukushima Nuclear Plant Accident"
Human-made values at UNCEAR are from Japan NIRS which summarized UNCEAR data.

Effect on electronics

Cosmic rays have sufficient energy to alter the states of elements in electronic integrated circuits, causing transient errors to occur, such as corrupted data in electronic memory devices, or incorrect performance of CPUs, often referred to as "soft errors" (not to be confused with software errors caused by programming mistakes/bugs). This has been a problem in extremely high-altitude electronics, such as in satellites, but with transistors becoming smaller and smaller, this is becoming an increasing concern in ground-level electronics as well.[20] Studies by IBM in the 1990s suggest that computers typically experience about one cosmic-ray-induced error per 256 megabytes of RAM per month.[21]

To alleviate this problem, the Intel Corporation has proposed a cosmic ray detector that could be integrated into future high-density microprocessors, allowing the processor to repeat the last command following a cosmic-ray event.[22]

Cosmic rays are suspected as a possible cause of an in-flight incident in 2008 where an Airbus A330 airliner of Qantas twice plunged hundreds of feet after an unexplained malfunction in its flight control system. Many passengers and crew members were injured, some seriously. After this incident, the accident investigators determined that the airliner's flight control system had received a data spike that could not be explained, and that all systems were in perfect working order. This has prompted a software upgrade to all A330 and A340 airliners, worldwide, so that any data spikes in this system are filtered out electronically.[23]

Significance to space travel

Galactic cosmic rays are one of the most important barriers standing in the way of plans for interplanetary travel by crewed spacecraft. Cosmic Rays also place a threat to electronics placed aboard outgoing probes. In 2010, a malfunction aboard the Voyager 2 space probe was credited to a single flipped bit, probably caused by a cosmic ray.

Role in lightning

Cosmic rays have been implicated in the triggering of electrical breakdown in lightning. It has been proposed that essentially all lightning is triggered through a relativistic process, "runaway breakdown", seeded by cosmic ray secondaries. Subsequent development of the lightning discharge then occurs through "conventional breakdown" mechanisms.[24]

Role in climate change

A role of cosmic rays directly or via solar-induced modulations in climate change was suggested by Edward P. Ney in 1959[25] and by Robert Dickinson in 1975. In recent years, the idea has been revived most notably by Henrik Svensmark; the most recent IPCC study disputed the mechanism,[26] while the most comprehensive review of the topic to date states: "evidence for the cosmic ray forcing is increasing as is the understanding of its physical principles."[27]

Suggested mechanisms

Henrik Svensmark et al. have argued that solar variations modulate the cosmic ray signal seen at the Earth and that this would affect cloud formation and hence climate. Cosmic rays have been experimentally determined capable of producing ultra-small aerosol particles,[28] orders of magnitude smaller than cloud condensation nuclei (CCN).

According to a report about an ongoing CERN CLOUD research project[29] to detect any Cosmic ray forcing is challenging since on wide spread time scales changes in the Sun’s magnetic activity, Earth’s magnetic field, and the galactic environment must be taken into account. Empirically, increased galactic cosmic ray (GCR) flux seem to be associated with a cooler climate, a southerly shift of the ITCZ (Inter Tropical Convergence Zone)[citation needed] and a weakening of monsoon rainfalls and vice versa.[29] Claims have been made of identification of GCR climate signals in atmospheric parameters such as high latitude precipitation (Todd & Kniveton), and Svensmark's annual cloud cover variations, which were said to be correlated to GCR variation. Various proposals have been made for the mechanism by which cosmic rays might affect clouds, including ion mediated nucleation, and indirect effects on current flow density in the global electric circuit (see Tinsley 2000, and F. Yu 1999).... Other studies refer to the formation of relatively highly charged aerosols and cloud droplets at cloud boundaries, with an indirect effect on ice particle formation and altering aerosol interaction with cloud droplets.[29] Kirkby (2009) reviews developments and describes further cloud nucleation mechanisms that appear energetically favorable and depend on GCRs.,[30][31]

Geochemical and astrophysical evidence

Carbon dioxide concentrations on 500 million year scale[32]
Climate change on 500 million year scale

Nir Shaviv has argued that climate signals on geological time scales are attributable to changing positions of the galactic spiral arms of the Milky Way Galaxy, and that cosmic ray flux variability is the dominant "climate driver" over these time periods.[33] Nir Shaviv and Jan Veizer in 2003[34] argue, that in contrast to a carbon based scenario, the model and proxy based estimates of atmospheric CO2 levels especially for the early Phanerozoic (see diagrams) do not show correlation with the paleoclimate picture that emerged from geological criteria, while cosmic ray flux would do.

The 2007 IPCC reports, however, strongly attribute a major role of anthropogenic carbon dioxide in the ongoing global warming, but as "different climate changes in the past had different causes" a driving role of carbon dioxide in the geological past is neither focus of the IPCC nor purported. Similarly, according a BBC report a 2008 Lancaster University study produced "further compelling evidence showing that modern-day climate change is not caused by changes in the Sun's activity".[35]

A comprehensive study of different research institutes was published 2007 by Scherer et al. in Space Science Reviews 2007.[36] The study combines geochemical evidence both on temperature, cosmic rays influence and as well astrophysical deliberations suggesting a major role in climate variability over different geological time scales. Proxy data of CRF influence comprise among others isotopic evidence in sediments on the Earth and as well changes in (iron) meteorites.

See also

Notes

  1. ^ L. Anchordoqui, T. Paul, S. Reucroft, J. Swain (2003). "Ultrahigh Energy Cosmic Rays: The state of the art before the Auger Observatory". International Journal of Modern Physics A 18 (13): 2229. arXiv:hep-ph/0206072. Bibcode 2003IJMPA..18.2229A. doi:10.1142/S0217751X03013879. 
  2. ^ a b Trumbore, Susan (2000). Noller, J. S., J. M. Sowers, and W. R. Lettis. ed. Quaternary Geochronology: Methods and Applications. Washington, D.C.: American Geophysical Union. pp. 41–59. ISBN 0-87590-950-7. http://www.agu.org/books/rf/v004/. 
  3. ^ Secondary antiprotons and propagation of cosmic rays in the Galaxy and heliosphere. I. V. Moskalenko (NASA/GSFC), A. W. Strong (MPE, Garching), J. F. Ormes (NASA/GSFC), M. S. Potgieter (Potchefstroom U.) Astrophys.J.565:280-296,2002 cite:arXiv:astro-ph/0106567v2 [1]
  4. ^ D. Lal, A.J.T. Jull, D. Pollard, L. Vacher (2005). "Evidence for large century time-scale changes in solar activity in the past 32 Kyr, based on in-situ cosmogenic 14C in ice at Summit, Greenland". Earth and Planetary Science Letters 234 (3–4): 335–249. Bibcode 2005E&PSL.234..335L. doi:10.1016/j.epsl.2005.02.011. 
  5. ^ [2] Astrophysics of Galactic Charged Cosmic Rays. A.Castellina1, F. Donato. Review. Retrieved from ArXive Dec. 2, 2011
  6. ^ "EGRET Detection of Gamma Rays from the Moon". NASA/GSFC. 1 August 2005. http://heasarc.gsfc.nasa.gov/docs/cgro/epo/news/gammoon.html. Retrieved 2010-02-11. 
  7. ^ R.L. Fleischer, P.B. Price, R.M. Walker (1975). Nuclear tracks in solids: Principles and applications. University of California Press. 
  8. ^ D. Pacini (1912). "La radiazione penetrante alla superficie ed in seno alle acque". Il Nuovo Cimento, Series VI 3: 93–100. doi:10.1007/BF02957440. 
    Translated and commented in A. de Angelis (2010). "Penetrating Radiation at the Surface of and in Water". arXiv:1002.1810 [physics.hist-ph]. 
  9. ^ a b c Nobel Prize in Physics 1936 – Presentation Speech
  10. ^ V.F. Hess (1936). "The Nobel Prize in Physics 1936". The Nobel Foundation. http://nobelprize.org/nobel_prizes/physics/laureates/1936/index.html. Retrieved 2010-02-11. 
  11. ^ V.F. Hess (1936). "Unsolved Problems in Physics: Tasks for the Immediate Future in Cosmic Ray Studies". Nobel Lectures. The Nobel Foundation. http://nobelprize.org/nobel_prizes/physics/laureates/1936/index.html. Retrieved 2010-02-11. 
  12. ^ J.L. DuBois, R.P. Multhauf, C.A. Ziegler (2002). The Invention and Development of the Radiosonde. Smithsonian Studies in History and Technology. 53. Smithsonian Institution Press. http://www.sil.si.edu/smithsoniancontributions/HistoryTechnology/pdf_lo/SSHT-0053.pdf. 
  13. ^ S. Vernoff (1935). "Radio-Transmission of Cosmic Ray Data from the Stratosphere". Nature 135 (3426): 1072. Bibcode 1935Natur.135.1072V. doi:10.1038/1351072c0. 
  14. ^ "Natürliche, durch kosmische Strahlung laufend erzeugte Radionuklide". http://www.um.baden-wuerttemberg.de/servlet/is/34839/Natuerliche_durch_kosmische_Strahlung_laufend_erzeugte_Radionuklide.pdf?command=downloadContent&filename=Natuerliche_durch_kosmische_Strahlung_laufend_erzeugte_Radionuklide.pdf. Retrieved 2010-02-11.  (German)
  15. ^ UNSCEAR "Sources and Effects of Ionizing Radiation" page 339 retrieved 2011-6-29
  16. ^ Japan NIRS UNSCEAR 2008 report page 8 retrieved 2011-6-29
  17. ^ Princeton.edu "Background radiation" retrieved 2011-6-29
  18. ^ Washington state Dept. of Health "Background radiation" retrieved 2011-6-29
  19. ^ Ministry of Education, Culture, Sports, Science, and Technology of Japan "Radiation in environment" retrieved 2011-6-29
  20. ^ IBM experiments in soft fails in computer electronics (1978-1994), from Terrestrial cosmic rays and soft errors, IBM Journal of Research and Development, Vol. 40, No. 1, 1996. Retrieved April 16, 2008.
  21. ^ Scientific American (2008-07-21). "Solar Storms: Fast Facts". Nature Publishing Group. http://www.scientificamerican.com/article.cfm?id=solar-storms-fast-facts. Retrieved 2009-12-08. 
  22. ^ Intel plans to tackle cosmic ray threat, BBC News Online, 8 April 2008. Retrieved April 16, 2008.
  23. ^ Cosmic rays may have hit Qantas plane off the coast of North West Australia, News.com.au, 18 November 2009. Retrieved 19 November 2009.
  24. ^ Runaway Breakdown and the Mysteries of Lightning, Physics Today, May 2005.
  25. ^ Ney, Edward P. (14 February 1959). "Cosmic Radiation and the Weather". Nature 183: 451 - 452. http://www.nature.com/nature/journal/v183/n4659/abs/183451a0.html. Retrieved 2012-02-09. 
  26. ^ Changes in Atmospheric Constituents and in Radiative Forcing IPCC Fourth Assessment Report Working Group I Report "The Physical Science Basis" 2007 [3]
  27. ^ K. Scherer, H. Fichtner et al. (December, 2006). "Interstellar-Terrestrial Relations: Variable Cosmic Environments, The Dynamic Heliosphere, and Their Imprints on Terrestrial Archives and Climate". Space Science Reviews (Springer Netherlands) 127 (1–4): 327–465. Bibcode 2006SSRv..127..327S. doi:10.1007/s11214-006-9126-6. ISSN 0038-6308. 
  28. ^ Henrik Svensmark, Jens Olaf Pepke Pedersen, Nigel Marsh, Martin Enghoff and Ulrik Uggerhøj, "Experimental Evidence for the role of Ions in Particle Nucleation under Atmospheric Conditions", Proceedings of the Royal Society A, (Early Online Publishing), 2006.
  29. ^ a b c Kirkby, J. 2008. Cosmic rays and climate. Surveys in Geophysics 28: 333-375)
  30. ^ Cosmic Rays and Climate Video Jasper Kirkby, CERN Colloquium, 4 June 2009
  31. ^ Cosmic Rays and Climate Presentation Jasper Kirkby, CERN Colloquium, 4 June 2009
  32. ^ Similar displays in Veizer and Shaviv 2003 and in 2001 IPCC Mitchell report
  33. ^ [4], [5]sciencebits.com/CO2orSolar Science bit display of Nir Shaviv papers
  34. ^ N.J. Shaviv, J. Veizer (2003). "Celestial driver of Phanerozoic climate?". GSA Today 7 (7): 4–10. Bibcode 2003EAEJA....13401S. ftp://rock.geosociety.org/pub/GSAToday/gt0307.pdf. 
  35. ^ R. Black (3 April 2008). "'No Sun link' to climate change". BBC News. http://news.bbc.co.uk/1/hi/sci/tech/7327393.stm. Retrieved 2010-02-11. 
  36. ^ K. Scherer et al. (2006). "Interstellar-Terrestrial Relations: Variable Cosmic Environments, The Dynamic Heliosphere, and Their Imprints on Terrestrial Archives and Climate". Space Science Reviews 127 (1–4): 327. Bibcode 2006SSRv..127..327S. doi:10.1007/s11214-006-9126-6. 

References

  • R.G. Harrison and D.B. Stephenson, Detection of a galactic cosmic ray influence on clouds, Geophysical Research Abstracts, Vol. 8, 07661, 2006 SRef-ID: 1607-7962/gra/EGU06-A-07661
  • C. D. Anderson and S. H. Neddermeyer, Cloud Chamber Observations of Cosmic Rays at 4300 Meters Elevation and Near Sea-Level, Phys. Rev 50, 263,(1936).
  • M. Boezio et al., Measurement of the flux of atmospheric muons with the CAPRICE94 apparatus, Phys. Rev. D 62, 032007, (2000).
  • R. Clay and B. Dawson, Cosmic Bullets, Allen & Unwin, 1997. ISBN 1-86448-204-4
  • T. K. Gaisser, Cosmic Rays and Particle Physics, Cambridge University Press, 1990. ISBN 0-521-32667-2
  • P. K. F. Grieder, Cosmic Rays at Earth: Researcher’s Reference Manual and Data Book, Elsevier, 2001. ISBN 0-444-50710-8
  • A. M. Hillas, Cosmic Rays, Pergamon Press, Oxford, 1972 ISBN 0-08-016724-1
  • J. Kremer et al., Measurement of Ground-Level Muons at Two Geomagnetic Locations, Phys. Rev. Lett. 83, 4241, (1999).
  • S. H. Neddermeyer and C. D. Anderson, Note on the Nature of Cosmic-Ray Particles, Phys. Rev. 51, 844, (1937).
  • M. D. Ngobeni and M. S. Potgieter, Cosmic ray anisotropies in the outer heliosphere, Advances in Space Research, 2007.
  • M. D. Ngobeni, Aspects of the modulation of cosmic rays in the outer heliosphere, M.Sc Dissertation, Northwest University (Potchefstroom campus) South Africa 2006.
  • D. Perkins, Particle Astrophysics, Oxford University Press, 2003. ISBN 0-19-850951-0
  • C. E. Rolfs and S. R. William, Cauldrons in the Cosmos, The University of Chicago Press, 1988. ISBN 0-226-72456-5
  • B. B. Rossi, Cosmic Rays, McGraw-Hill, New York, 1964.
  • Martin Walt, Introduction to Geomagnetically Trapped Radiation, 1994. ISBN 0-521-43143-3
  • M. Taylor and M. Molla, Towards a unified source-propagation model of cosmic rays, Pub. Astron. Soc. Pac. 424, 98 (2010).
  • J. F. Ziegler, The Background In Detectors Caused By Sea Level Cosmic Rays, Nuclear Instruments and Methods 191, 419, (1981).
  • TRACER Long Duration Balloon Project: the largest cosmic ray detector launched on balloons.
  • HiRes Fly's Eye
  • Carlson, Per; De Angelis, Alessandro (2011). "Nationalism and internationalism in science: the case of the discovery of cosmic rays". European Physical Journal H. Bibcode 2010EPJH...35..309C. doi:10.1140/epjh/e2011-10033-6. 

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