The history of gamma-ray began with the serendipitous detection of a gamma-ray burst (GRB) on July 2, 1967, by the U.S. Vela satellites. After these satellites detected fifteen other GRBs, Ray Klebesadel of the Los Alamos National Laboratory published the first paper on the subject, Observations of Gamma-Ray Bursts of Cosmic Origin.
As more and more research was done on these mysterious events, hundreds
of models were developed in an attempt to explain their origins.
Discovery
Gamma-ray bursts were discovered in the late 1960s by the U.S. Vela
nuclear test detection satellites. The Velas were built to detect gamma
radiation pulses emitted by nuclear weapon tests in space. The United
States suspected that the USSR might attempt to conduct secret nuclear tests after signing the Nuclear Test Ban Treaty
in 1963. While most satellites orbited at about 500 miles above Earth's
surface, the Vela satellites orbited at an altitude of 65,000 miles. At
this height, the satellites orbited above the Van Allen radiation belt, which reduced the noise in the sensors. The extra height also meant that the satellites could detect explosions behind the moon, a location where the United States government
suspected the Soviet Union would try to conceal nuclear weapon tests.
The Vela system generally had four satellites operational at any given
time such that a gamma-ray signal could be detected at multiple
locations. This made it possible to localize the source of the signal to
a relatively compact region of space. While these characteristics were
incorporated into the Vela system to improve the detection of nuclear
weapons, these same characteristics were what made the satellites
capable of detecting gamma-ray bursts.
On July 2, 1967, at 14:19 UTC, the Vela 4 and Vela 3 satellites detected a flash of gamma radiation that were unlike any known nuclear weapons signatures.
Nuclear bombs produce a very brief, intense burst of gamma rays less
than one millionth of a second. The radiation then steadily fades as the
unstable nuclei decay.
The signal detected by the Vela satellites had neither the intense
initial flash nor the gradual fading, but instead there were two
distinct peaks in the light curve. Solar flares and new supernovas were the two other possible explanations for the event, but neither had occurred on that day. Unclear on what had happened, but not considering the matter particularly urgent, the team at the Los Alamos Scientific Laboratory, led by Ray Klebesadel, filed the data away for later investigation.
Vela 5 was launched on May 23, 1969. Because the sensitivity and
time resolution on these satellites were significantly more accurate
than the instruments on Vela 4, the Los Alamos team expected these new
satellites to detect more gamma-ray bursts. Despite an enormous amount
of background signals
picked up by the new detectors, the research team found twelve events
which had not coincided with any solar flares or supernovas. Some of the
new detections also showed the same double-peak pattern that had been
observed by Vela 4.
Although their instrumentation offered no improvement over those
on Vela 5, the Vela 6 satellites were launched on April 8, 1970, with
the intention of determining the direction from which the gamma rays
were arriving. The orbits for the Vela 6 satellites were chosen to be as
far away from Vela 5 as possible, generally on the order of
10000 kilometers apart. This separation meant that, despite gamma rays
traveling at the speed of light,
a signal would be detected at slightly different times by different
satellites. By analyzing the arrival times, Klebesadel and his team
successfully traced sixteen gamma-ray bursts. The random distribution of
bursts across the sky made it clear that the bursts were not coming
from the sun, moon, or other planets in our solar system.
In 1973, Ray Klebesadel, Roy Olson, and Ian Strong of the University of California Los Alamos Scientific Laboratory published Observations of Gamma-Ray Bursts of Cosmic Origin, identifying a cosmic source for the previously unexplained observations of gamma-rays.
Shortly thereafter, Klebesadel presented his findings at the 140th
meeting of the American Astronomical Society. Although he was
interviewed only by The National Enquirer, news of the discovery quickly spread through the scientific community. Between 1973 and 2001 more than 5300 papers were published on GRBs.
Early research missions
Shortly
after the discovery of gamma-ray bursts, a general consensus arose
within the astronomical community that in order to determine what caused
them, they would have to be identified with astronomical objects at
other wavelengths, particularly visible light, as this approach had been
successfully applied to the fields of radio X-ray astronomy. This method would require far more accurate positions of several gamma-ray bursts than the Vela system could provide.
Greater accuracy required the detectors to be spaced farther apart.
Instead of launching satellites only into Earth's orbit, it was deemed
necessary to spread the detectors throughout the solar system.
By the end of 1978, the first Inter-Planetary Network (IPN) had been completed. In addition to the Vela satellites, the IPN included 5 new space probes: the Russian Prognoz 7, in orbit around the earth, the German Helios 2, in elliptical orbit around the Sun, and NASA's Pioneer Venus Orbiter, Venera 11, and Venera 12, each of which orbited Venus. The research team at the Russian Institute for Space Research
in Moscow, led by Kevin Hurley, was able to use the data collected by
the IPN to accurately determine the position of gamma-ray bursts with an
accuracy of a few minutes of arc.
However, even when using the most powerful telescopes available,
nothing of interest could be found within the determined regions.
To explain the existence of gamma-ray bursts, many speculative theories were advanced, most of which posited nearby galactic sources. Little progress was made, however, until the 1991 launch of the Compton Gamma Ray Observatory and its Burst and Transient Source Explorer (BATSE) instrument, an extremely sensitive gamma-ray detector. This instrument provided crucial data indicating that GRBs are isotropic (not biased towards any particular direction in space, such as toward the galactic plane or the Galactic Center).
Because the Milky Way galaxy has a very flat structure, if gamma-ray
bursts were to originate from within the Milky Way, they would not be
distributed isotropically across the sky, but instead concentrated in
the plane of the Milky Way. Although the luminosity of the bursts
suggested that they had to be originating within the Milky Way, the
distribution provided very strong evidence to the contrary.
BATSE data also showed that GRBs fall into two distinct
categories: short-duration, hard-spectrum bursts ("short bursts"), and
long-duration, soft-spectrum bursts ("long bursts"). Short bursts are typically less than two seconds in duration and are dominated by higher-energy photons;
long bursts are typically more than two seconds in duration and
dominated by lower-energy photons. The separation is not absolute and
the populations overlap observationally, but the distinction suggests
two different classes of progenitors. However, some believe there is a
third type of GRBs.
The three kinds of GRBs are hypothesized to reflect three different
origins: mergers of neutron star systems, mergers between white dwarfs
and neutron stars, and the collapse of massive stars.
For decades after the discovery of GRBs, astronomers searched for
a counterpart: any astronomical object in positional coincidence with a
recently observed burst. Astronomers considered many distinct objects,
including white dwarfs, pulsars, supernovae, globular clusters, quasars, Seyfert galaxies, and BL Lac objects. Researchers specifically looked for objects with unusual properties which might relate to gamma-ray bursts: high proper motion, polarization, orbital brightness modulation, fast time scale flickering, extreme colors, emission lines, or an unusual shape. From the discovery of GRBs through the 1980s, GRB 790305b was the only event to have been identified with a candidate source object: nebula N49 in the Large Magellanic Cloud.
All other attempts failed due to poor resolution of the available
detectors. The best hope seemed to lie in finding a fainter, fading,
longer wavelength emission after the burst itself, the "afterglow" of a
GRB.
As early as 1980, a research group headed by Livio Scarsi at the University of Rome began working on Satellite per Astronomia X, an X-ray astronomy research satellite. The project developed into a collaboration between the Italian Space Agency and the Netherlands Agency for Aerospace Programmes. Though the satellite was originally intended to serve the sole purpose of studying X-rays, Enrico Costa of the Istituto di Astrofisica Spaziale suggested that the satellite's four protective shields could easily serve as gamma-ray burst detectors. After 10 years of delays and a final cost of approximately $350 million, the satellite, renamed BeppoSAX in honor of Giuseppe Occhialini, was launched on April 30, 1996.
In 1983, a team composed of Stan Woosley, Don Lamb, Ed Fenimore, Kevin Hurley, and George Ricker began discussing plans for a new GRB research satellite, the High Energy Transient Explorer (HETE).
Although many satellites were already providing data on GRBs, HETE
would be the first satellite devoted entirely to GRB research.
The goal was for HETE to be able to localize gamma-ray bursts with much
greater accuracy than the BATSE detectors. The team submitted a
proposal to NASA in 1986 under which the satellite would be equipped
with four gamma ray detectors, an X-ray camera, and four electronic
cameras for detecting visible and ultraviolet light. The project was to
cost $14.5 million, and the launch was originally planned for the summer of 1994. The Pegasus XL
rocket, which launched HETE on November 4, 1996, did not release its
two satellites, so the HETE and SAC-B, an Argentinian research satellite
also on board, missions were attached to the reocket and unable to
direct their solar panels towards the sun, and within one day of the
launch, all radio contact with the satellites was lost.
The eventual successor to the mission, HETE 2, was successfully
launched on 9 October 2000. It observed its first GRB on 13 February
2001.
Observations and analysis
BeppoSAX detected its first gamma-ray burst GRB960720 on July 20, 1996
from an X-ray burst in one of the two Wide Field Cameras (WFCs), but it
was only discovered in the data six weeks later, by a Dutch duty
scientist systematically checking WFC-bursts coinciding in time with
BATSE-triggers from the same direction. Follow-up radio observations
with the Very Large Array by Dale Frail
did not find an afterglow at the derived position from the deconvolved
data, but a routine procedure for finding gamma-ray bursts with BeppoSAX
could be established. This led to the detection of a gamma-ray burst on
January 11, 1997, and one of its Wide Field Cameras also detected
X-rays at the same moment coinciding with a BATSE-trigger. John Heise, Dutch project scientist for BeppoSAX's WFCs, quickly deconvolved the data from the WFCs using software by Jean in 't Zand, a Dutch former gamma-ray spectroscopist at the Goddard Space Flight Center, and in less than 24 hours, produced a sky position with an accuracy of about 10 arcminutes.
Although this level of accuracy had already been surpassed by the
interplanetary networks, they were unable to produce the data as quickly
as Heise could.
In the following days, Dale Frail, working with the Very Large Array,
detected a single fading radio source within the error box, a BL Lac object. An article was written for Nature
stating that this event proved that GRBs originated from active
galaxies. However, Jean in 't Zand rewrote the WFC deconvolution
software to produce a position with an accuracy of 3 arcminutes, and the
BL Lac object was no longer within the reduced error box. Despite
BeppoSAX having observed both X-rays and a GRB and the position being
known within that same day, the source of the burst was not identified.
Success for the BeppoSAX team came in February 1997, less than
one year after it had been launched. A BeppoSAX WFC detected a gamma-ray
burst (GRB 970228),
and when the X-ray camera onboard BeppoSAX was pointed towards the
direction from which the burst had originated, it detected a fading
X-ray emission. Ground-based telescopes later identified a fading
optical counterpart as well.
The location of this event having been identified, once the GRB faded,
deep imaging was able to identify a faint, very distant host galaxy in
the GRB's location. Within only a few weeks the long controversy about
the distance scale ended: GRBs were extragalactic events originating
inside faint galaxies at enormous distances.
By finally establishing the distance scale, characterizing the
environments in which GRBs occur, and providing a new window on GRBs
both observationally and theoretically, this discovery revolutionized
the study of GRBs.
Two major breakthroughs also occurred with the next event registered by BeppoSAX, GRB 970508.
This event was localized within 4 hours of its discovery, allowing
research teams to begin making observations much sooner than any
previous burst. By comparing photographs of the error box taken on May 8
and May 9 (the day of the event and the day after), one object was
found to have increased in brightness. Between May 10 and May, Charles Steidel recorded the spectrum of the variable object from the W. M. Keck Observatory. Mark Metzger analyzed the spectrum and determined a redshift
of z=0.835, placing the burst at a distance of roughly 6 billion light
years. This was the first accurate determination of the distance to a
GRB, and it further proved that GRBs occur in extremely distant
galaxies.
Prior to the localization of GRB 970228, opinions differed as to whether or not GRBs would emit detectable radio waves. Bohdan Paczyński and James Rhoads published an article in 1993 predicting radio afterglows, but Martin Rees and Peter Mészáros
concluded that, due to the vast distances between GRBs and the earth,
any radio waves produced would be too weak to be detected. Although GRB 970228 was accompanied by an optical afterglow, neither the Very Large Array nor the Westerbork Synthesis Radio Telescope were able to detect a radio afterglow. However, five days after GRB 970508, Dale Frail, working with the Very Large Array in New Mexico,
observed radio waves from the afterglow at wavelengths of 3.5 cm, 6 cm,
and 21 cm. The total luminosity varied widely from hour to hour, but
not simultaneously in all wavelengths. Jeremy Goodman of Princeton University explained the erratic fluctuations as being the result of scintillation
caused by vibrations in the Earth's atmosphere, which no longer occurs
when the source has an apparent size larger than 3 micro-arcseconds.
After several weeks, the luminosity fluctuations had dissipated. Using
this piece of information and the distance to the event, it was
determined that the source of radio waves had expanded almost at the speed of light. Never before had accurate information been obtained regarding the physical characteristics of a gamma-ray burst explosion.
Also, because GRB 970508 was observed at many different wavelengths, it was possible to form a very complete spectrum for the event. Ralph Wijers and Titus Galama
attempted to calculate various physical properties of the burst,
including the total amount of energy in the burst and the density of the
surrounding medium. Using an extensive system of equations, they were able to compute these values as 3×1052 ergs
and 30,000 particles per cubic meter, respectively. Although the
observation data was not accurate enough for their results to be
considered particularly reliable, Wijers and Galama did show that, in
principle, it would be possible to determine the physical characters of
GRBs based on their spectra.
The next burst to have its redshift calculated was GRB 971214
with a redshift of 3.42, a distance of roughly 12 billion lightyears
from Earth. Using the redshift and the accurate brightness measurements
made by both BATSE and BeppoSAX, Shrinivas Kulkarni,
who had recorded the redshift at the W. M. Keck Observatory, calculated
the amount of energy released by the burst in half a minute to be 3×1053 ergs,
several hundred times more energy than is released by the Sun in 10
billion years. The burst was proclaimed to be the most energetic
explosion to have ever occurred since the Big Bang, earning it the nickname Big Bang 2.
This explosion presented a dilemma for GRB theoreticians: either this
burst produced more energy than could possibly be explained by any of
the existing models, or the burst did not emit energy in all directions,
but instead in very narrow beams
which happened to have been pointing directly at Earth. While the
beaming explanation would reduce the total energy output to a very small
fraction of Kulkarni's calculation, it also implies that for every
burst observed on Earth, several hundred occur which are not observed
because their beams are not pointed towards Earth.
In November 2019, astronomers reported a notable gamma ray burst explosion, named GRB 190114C, initially detected in January 2019, that, so far, has been determined to have had the highest energy, 1 Tera electron volts (Tev), ever observed for such a cosmic event.
Current missions
Konus-Wind is flown on board Wind
spacecraft. It was launched on 1 November 1994. Experiment consists of
two identical gamma ray spectrometers mounted on opposite sites of the
spacecraft so all sky is observed.
INTEGRAL, the European Space Agency's
International Gamma-Ray Astrophysics Laboratory, was launched on
October 17, 2002. It is the first observatory capable simultaneously
observing objects at gamma ray, X-ray, and visible wavelengths.
NASA's Swift
satellite launched in November 2004. It combines a sensitive gamma-ray
detector with the ability to point on-board X-ray and optical telescopes
towards the direction of a new burst in less than one minute after the
burst is detected.
Swift's discoveries include the first observations of short burst
afterglows and vast amounts of data on the behavior of GRB afterglows at
early stages during their evolution, even before the GRB's gamma-ray
emission has stopped. The mission has also discovered large X-ray flares
appearing within minutes to days after the end of the GRB.
On June 11, 2008 NASA's Gamma-ray Large Area Space Telescope (GLAST), later renamed the Fermi Gamma-ray Space Telescope,
was launched. The mission objectives include "crack[ing] the mysteries
of the stupendously powerful explosions known as gamma-ray bursts."
Another gamma-ray burst observation mission is AGILE. Discoveries of GRBs are made as they are detected via the Gamma-ray Burst Coordinates Network so that researchers may promptly focus their instruments on the source of the burst to observe the afterglows.
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