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dc.contributor.author이현규-
dc.date.accessioned2016-09-29T02:51:02Z-
dc.date.available2016-09-29T02:51:02Z-
dc.date.issued2015-04-
dc.identifier.citationCLASSICAL AND QUANTUM GRAVITY, v. 32, NO 7, Page. 1-2en_US
dc.identifier.issn0264-9381-
dc.identifier.issn1361-6382-
dc.identifier.urihttp://hdl.handle.net/20.500.11754/23518-
dc.identifier.urihttp://iopscience.iop.org/article/10.1088/0264-9381/32/7/074001-
dc.description.abstractThe Advanced LIGO gravitational wave detectors are second-generation instruments designed and built for the two LIGO observatories in Hanford, WA and Livingston, LA, USA. The two instruments are identical in design, and are specialized versions of a Michelson interferometer with 4 km long arms. As in Initial LIGO, Fabry–Perot cavities are used in the arms to increase the interaction time with a gravitational wave, and power recycling is used to increase the effective laser power. Signal recycling has been added in Advanced LIGO to improve the frequency response. In the most sensitive frequency region around 100 Hz, the design strain sensitivity is a factor of 10 better than Initial LIGO. In addition, the low frequency end of the sensitivity band is moved from 40 Hz down to 10 Hz. All interferometer components have been replaced with improved technologies to achieve this sensitivity gain. Much better seismic isolation and test mass suspensions are responsible for the gains at lower frequencies. Higher laser power, larger test masses and improved mirror coatings lead to the improved sensitivity at mid and high frequencies. Data collecting runs with these new instruments are planned to begin in mid-2015.-
dc.description.sponsorshipThe authors gratefully acknowledge the support of the United States National Science Foundation for the construction and operation of the LIGO Laboratory and the Science and Technology Facilities Council of the United Kingdom, the Max-Planck-Society, and the State of Niedersachsen/Germany for support of the construction and operation of the GEO600 detector. The authors also gratefully acknowledge the support of the research by these agencies and by the Australian Research Council, the International Science Linkages programme of the Commonwealth of Australia, the Council of Scientific and Industrial Research of India, the Istituto Nazionale di Fisica Nucleare of Italy, the Spanish Ministerio de Economia y Competitividad, the Conselleria d'Economia, Hisenda i Innovacio of the Govern de les Illes Balears, the Royal Society, the Scottish Funding Council, the Scottish Universities Physics Alliance, The National Aeronautics and Space Administration, OTKA of Hungary, the National Research Foundation of Korea, Industry Canada and the Province of Ontario through the Ministry of Economic Development and Innovation, the National Science and Engineering Research Council Canada, the Carnegie Trust, the Leverhulme Trust, the David and Lucile Packard Foundation, the Research Corporation, and the Alfred P. Sloan Foundation. This article has LIGO document number LIGO-P1400177.-
dc.publisherIOP PUBLISHING LTDen_US
dc.subjectgravitational waves-
dc.subjectinterferometers-
dc.subjectseismic isolation-
dc.subjectoptics-
dc.titleAdvanced LIGOen_US
dc.typeArticleen_US
dc.relation.no7-
dc.relation.volume32-
dc.identifier.doi10.1088/0264-9381/32/7/074001-
dc.relation.page1-2-
dc.relation.journalCLASSICAL AND QUANTUM GRAVITY-
dc.contributor.googleauthorAasi, J.-
dc.contributor.googleauthorAbbott, B. P.-
dc.contributor.googleauthorAbbott, R.-
dc.contributor.googleauthorAbbott, T.-
dc.contributor.googleauthorAbernathy, M. R.-
dc.contributor.googleauthorAckley, K.-
dc.contributor.googleauthorAdams, C.-
dc.contributor.googleauthorAdams, T.-
dc.contributor.googleauthorAddesso, P.-
dc.contributor.googleauthorLee, H. K.-
dc.relation.code2015000505-
dc.sector.campusS-
dc.sector.daehakCOLLEGE OF NATURAL SCIENCES[S]-
dc.sector.departmentDEPARTMENT OF PHYSICS-
dc.identifier.pidhyunkyu-
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COLLEGE OF NATURAL SCIENCES[S](자연과학대학) > PHYSICS(물리학과) > Articles
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