GEO600

In the 1970s, two groups in Europe, one led by Heinz Billing in Germany and one led by Ronald Drever in UK, initiated investigations into laser-interferometric gravitational wave detection. In 1975 the Max Planck Institute for Astrophysics in Munich started with a prototype of armlength, which led to a prototype with armlength at the Max Planck Institute of Quantum Optics (MPQ) in Garching in 1983. In 1977 the Department of Physics and Astronomy of the University of Glasgow began similar investigations, and in 1980 started operation of a prototype. In 1985 the Garching group proposed the construction of a large detector with armlength, the British group an equivalent project in 1986. The two groups combined their efforts in 1989the project GEO was born, with the Harz mountains in northern Germany considered an ideal site. The project was, however, not funded, because of financial problems. Thus in 1994 a smaller detector was proposed: GEO600, to be built in the lowlands near Hannover, with arms of in length. The construction of this British-German gravitational wave detector started in September 1995. In 2001 the Max Planck Institute for Gravitational Physics (Albert Einstein Institute, AEI) in Potsdam took over the Hannover branch of the MPQ, and since 2002 the detector is operated by a joint Center of Gravitational Physics of AEI and Leibniz Universität Hannover, together with the universities of Glasgow and Cardiff. Since 2002 GEO600 participated in several data runs in coincidence with the LIGO detectors. ==Hardware==

GEO600 is a Michelson interferometer. It consists of two arms, which the laser beam passes twice, so that the effective optical arm length is . The major optical components are located in an ultra-high vacuum system, with a pressure of less than 10−8 mbar. Furthermore, the whole suspension cage sits on piezo crystals. The crystals are used for an 'active seismic isolation system'. It moves the whole suspension in the opposite direction of the ground motion, so that ground motion is cancelled. Optics The main mirrors of GEO600 are cylinders of fused silica with a diameter of and a height of . The beam splitter, with dimensions of diameter and thickness, is the only transmissive piece of optics in the high power path, therefore it was made from special grade fused silica. Its absorption has been measured to be smaller than 0.25 ppm per . Advanced GEO600 uses many advanced techniques and hardware that are planned to be used in the next generation of ground based gravitational wave detectors: • Monolithic suspensions: The mirrors are suspended as pendulums. While steel wires are used for secondary mirrors, GEO's main mirrors are hanging from so-called 'monolithic' suspensions. This means that the wires are made from the same material as the mirror: fused silica. The reason is that fused silica has less mechanical losses, and losses lead to noise. • Electrostatic drives: Actuators are needed to keep the mirrors in their position and to align them. Secondary mirrors of GEO600 have magnets glued to them for this purpose. They can then be moved by coils. Since gluing magnets to mirrors will increase mechanical losses, the main mirrors of GEO600 use electrostatic drives (ESDs). The ESDs are a comb-like structure of electrodes at the back side of the mirror. If a voltage is applied to the electrodes, they produce an inhomogeneous electric field. The mirror will feel a force in this field. • Thermal mirror actuation system: A system of heaters is sitting at the far east mirror. When heated, a thermal gradient will appear in the mirror, and the radius of curvature of the mirror changes due to thermal expansion. The heaters allow thermal tuning of the mirror's radius of curvature. • Signal recycling: An additional mirror at the output of the interferometer forms a resonant cavity together with the end mirrors and thus increases a potential signal. • Homodyne detection (also called 'DC readout') • Output Mode Cleaner (OMC): An additional cavity at the output of the interferometer in front of the photodiode. Its purpose is to filter out light that does not potentially carry a gravitational wave signal. • Squeezing: Squeezed vacuum is injected into the dark port of the beam splitter. The use of squeezing can improve the sensitivity of GEO600 above 700 Hz by a factor of 1.5. A further difference to other projects is that GEO600 has no arm cavities. ==Sensitivity and measurements==

The sensitivity for gravitational wave strain is usually measured in amplitude spectral density (ASD). The peak sensitivity of GEO600 in this unit is 2×10−22 1/ at 600 Hz. At high frequencies the sensitivity is limited by the available laser power. At the low frequency end, the sensitivity of GEO600 is limited by seismic ground motion. ==Joint science run with LIGO==

In November 2005, it was announced that the LIGO and GEO instruments began an extended joint science run. The three instruments (LIGO's instruments are located near Livingston, Louisiana and on the Hanford Site, Washington in the US) collected data for more than a year, with breaks for tuning and updates. This was the fifth science run of GEO600. No signals were detected on previous runs. The first observation of gravitational waves on 14 September 2015 was announced by the LIGO and Virgo interferometer collaborations on 11 February 2016. However, the Virgo interferometer in Italy was not operating at the time, and the GEO600 was in engineering mode and is not sensitive enough, and so could not confirm the signal. The GEO600 began taking data simultaneously with Advanced LIGO on 18 September 2015. ==Claims on holographic properties of spacetime==

On 15 January 2009 it was reported in New Scientist that some yet unidentified noise that was present in the GEO600 detector measurements might be because the instrument is sensitive to extremely small quantum fluctuations of space-time affecting the positions of parts of the detector. This claim was made by Craig Hogan, a scientist from Fermilab, on the basis of his own theory of how such fluctuations should occur motivated by the holographic principle. The New Scientist story states that Hogan sent his prediction of "holographic noise" to the GEO600 collaboration in June 2008, and subsequently received a plot of the excess noise which "looked exactly the same as my prediction". However, Hogan knew before that time that the experiment was finding excess noise. Hogan's article published in Physical Review D in May 2008 states: Hogan cites a 2007 talk from the GEO600 collaboration which already mentions "mid-band 'mystery' noise", and where the noise spectra are plotted. A similar remark was made in a GEO600 paper submitted in October 2007 and published in May 2008: It is a very common occurrence for gravitational wave detectors to find excess noise that is subsequently eliminated. According to Karsten Danzmann, the GEO600 principal investigator, ==Data and Einstein@home==

Not only the output of the main photodiode is registered, but also the output of a number of secondary sensors, for example photodiodes that measure auxiliary laser beams, microphones, seismometers, accelerometers, magnetometers and the performance of all the control circuits. These secondary sensors are important for diagnosis and to detect environmental influences on the interferometer output. The data stream is partly analyzed by the distributed computing project 'Einstein@home', software that volunteers can run on their computers. From September 2011, both VIRGO and the LIGO detectors were shut down for upgrades, leaving GEO600 as the only operating large scale laser interferometer searching for gravitational waves. Subsequently, in September 2015, the advanced LIGO detectors came online and were used in the first Observing Run 'O1' at a sensitivity roughly 4 times greater than Initial LIGO for some classes of sources (e.g., neutron-star binaries), and a much greater sensitivity for larger systems with their peak radiation at lower audio frequencies. These advanced LIGO detectors were developed under the LIGO Scientific Collaboration with Gabriela González as the spokesperson. ==See also==