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dc.contributor.authorLandrø, Martin
dc.contributor.authorNi, Yuan
dc.contributor.authorAmundsen, Lasse
dc.date.accessioned2018-01-19T09:02:17Z
dc.date.available2018-01-19T09:02:17Z
dc.date.created2016-08-03T13:57:07Z
dc.date.issued2016
dc.identifier.citationGeophysics. 2016, 81 (3), P33-P46.nb_NO
dc.identifier.issn0016-8033
dc.identifier.urihttp://hdl.handle.net/11250/2478295
dc.description.abstractGhost cavitation, which is a term describing that cavitation bubbles are generated acoustically, has been hypothesized to occur when the ghost reflected signals from many individual air guns beneath the sea surface produce a pressure that is close to zero in the water above the source array. Ghost cavitation is typically observed some milliseconds after the ghost reflection, and it may last for 5–15 ms, depending on the configuration of the source array. The cavitation process subsequently generates a weak high-frequency signal. To investigate this potential signal model and mechanism, we have performed a dedicated source experiment. We found that the distance between the source strings in a source array is a major factor that influences the amount and strength of the high-frequency signal. By increasing the separation distance from 6.5 to 8 m, we have observed a significant decrease in the high-frequency signal. Further, the amount of ghost cavitation can be reduced by increasing the distance between the guns. Also single sub-arrays may create ghost cavitation sound, of course weaker in signal strength compared with full arrays, in agreement with the model. Conventional air-gun modeling can be used to predict where ghost cavitation can occur. Therefore, in principle, a workflow could be developed to quantify grossly if and how much high-frequency signals could be generated by this mechanism, given the source array configuration, and further change the configuration to reduce to a very minimum the high-frequency signals, if deemed necessary. For an air-gun array consisting of two subarrays separated by 6 m and fired at 9 m depth, we found that the high-frequency signals emitted between 1 and 10 kHz were of similar strength to the noise from conventional cargo ships, depending on their size and the vessels’ speed.nb_NO
dc.language.isoengnb_NO
dc.publisherSociety of Exploration Geophysicistsnb_NO
dc.titleReducing high-frequency ghost cavitation signals from marine air-gun arraysnb_NO
dc.typeJournal articlenb_NO
dc.typePeer reviewednb_NO
dc.description.versionpublishedVersionnb_NO
dc.source.pagenumberP33-P46nb_NO
dc.source.volume81nb_NO
dc.source.journalGeophysicsnb_NO
dc.source.issue3nb_NO
dc.identifier.doi10.1190/geo2015-0305.1
dc.identifier.cristin1370308
dc.description.localcode© 2016 Society of Exploration Geophysicists. All rights reserved.nb_NO
cristin.unitcode194,64,90,0
cristin.unitnameInstitutt for geovitenskap og petroleum
cristin.ispublishedtrue
cristin.fulltextpreprint
cristin.qualitycode2


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