Rotary actuated seismic source and methods for continuous direct-push downhole seismic testing

Remotely operated rotary actuated shear wave generating apparatus and methods that generate horizontally polarized vertically propagating shear waves for use in down-hole shear wave velocity measurements. Seismic signals are generated by an offset mass rotating in a plane perpendicular to the surfac...

Ausführliche Beschreibung

Gespeichert in:
Bibliographische Detailangaben
Hauptverfasser: Quinn, Mark K, McGillivray, Alexander V, Mayne, Paul W
Format: Patent
Sprache:eng
Online-Zugang:Volltext bestellen
Tags: Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
container_end_page
container_issue
container_start_page
container_title
container_volume
creator Quinn, Mark K
McGillivray, Alexander V
Mayne, Paul W
description Remotely operated rotary actuated shear wave generating apparatus and methods that generate horizontally polarized vertically propagating shear waves for use in down-hole shear wave velocity measurements. Seismic signals are generated by an offset mass rotating in a plane perpendicular to the surface of the ground, which impacts an impact member coupled to the ground. The energy of impact is transmitted to the ground parallel to the surface of the ground. The apparatus uses a spring-loaded rotating mass that has a rotary motion. Because acceleration of the mass is not horizontal, reaction forces caused by acceleration of the mass create less horizontal shear stress in the ground prior to the desired time (impact). Reaction forces of the accelerated rotating mass does not generate undesirable waves that obscure the desirable waves caused by impact with the impact member. The source generates transient shear waves repeatedly at constant intervals. Wave motions are recorded by a probe as it is advanced into the ground, without pause.
format Patent
fullrecord <record><control><sourceid>uspatents_EFH</sourceid><recordid>TN_cdi_uspatents_grants_07650962</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>07650962</sourcerecordid><originalsourceid>FETCH-uspatents_grants_076509623</originalsourceid><addsrcrecordid>eNqNjTEKwkAQAK-xEPUP-4FAUIxYB8VarJXlbpM7SG7D7S7i740g1lbTzDBLd7-yYnkBejVUCiCUZEwehK14AswBRtLIQaDjAp6zpmxsAiEV8lpNJhECP3PkgX65ksxev3aLDgehzZcrB-fTrb1UJtO8yyqPvuAH9aHZ18dmu_tDeQNYKz5b</addsrcrecordid><sourcetype>Open Access Repository</sourcetype><iscdi>true</iscdi><recordtype>patent</recordtype></control><display><type>patent</type><title>Rotary actuated seismic source and methods for continuous direct-push downhole seismic testing</title><source>USPTO Issued Patents</source><creator>Quinn, Mark K ; McGillivray, Alexander V ; Mayne, Paul W</creator><creatorcontrib>Quinn, Mark K ; McGillivray, Alexander V ; Mayne, Paul W ; Georgia Tech Research Corporation</creatorcontrib><description>Remotely operated rotary actuated shear wave generating apparatus and methods that generate horizontally polarized vertically propagating shear waves for use in down-hole shear wave velocity measurements. Seismic signals are generated by an offset mass rotating in a plane perpendicular to the surface of the ground, which impacts an impact member coupled to the ground. The energy of impact is transmitted to the ground parallel to the surface of the ground. The apparatus uses a spring-loaded rotating mass that has a rotary motion. Because acceleration of the mass is not horizontal, reaction forces caused by acceleration of the mass create less horizontal shear stress in the ground prior to the desired time (impact). Reaction forces of the accelerated rotating mass does not generate undesirable waves that obscure the desirable waves caused by impact with the impact member. The source generates transient shear waves repeatedly at constant intervals. Wave motions are recorded by a probe as it is advanced into the ground, without pause.</description><language>eng</language><creationdate>2010</creationdate><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://image-ppubs.uspto.gov/dirsearch-public/print/downloadPdf/7650962$$EPDF$$P50$$Guspatents$$Hfree_for_read</linktopdf><link.rule.ids>230,308,780,802,885,64039</link.rule.ids><linktorsrc>$$Uhttps://image-ppubs.uspto.gov/dirsearch-public/print/downloadPdf/7650962$$EView_record_in_USPTO$$FView_record_in_$$GUSPTO$$Hfree_for_read</linktorsrc></links><search><creatorcontrib>Quinn, Mark K</creatorcontrib><creatorcontrib>McGillivray, Alexander V</creatorcontrib><creatorcontrib>Mayne, Paul W</creatorcontrib><creatorcontrib>Georgia Tech Research Corporation</creatorcontrib><title>Rotary actuated seismic source and methods for continuous direct-push downhole seismic testing</title><description>Remotely operated rotary actuated shear wave generating apparatus and methods that generate horizontally polarized vertically propagating shear waves for use in down-hole shear wave velocity measurements. Seismic signals are generated by an offset mass rotating in a plane perpendicular to the surface of the ground, which impacts an impact member coupled to the ground. The energy of impact is transmitted to the ground parallel to the surface of the ground. The apparatus uses a spring-loaded rotating mass that has a rotary motion. Because acceleration of the mass is not horizontal, reaction forces caused by acceleration of the mass create less horizontal shear stress in the ground prior to the desired time (impact). Reaction forces of the accelerated rotating mass does not generate undesirable waves that obscure the desirable waves caused by impact with the impact member. The source generates transient shear waves repeatedly at constant intervals. Wave motions are recorded by a probe as it is advanced into the ground, without pause.</description><fulltext>true</fulltext><rsrctype>patent</rsrctype><creationdate>2010</creationdate><recordtype>patent</recordtype><sourceid>EFH</sourceid><recordid>eNqNjTEKwkAQAK-xEPUP-4FAUIxYB8VarJXlbpM7SG7D7S7i740g1lbTzDBLd7-yYnkBejVUCiCUZEwehK14AswBRtLIQaDjAp6zpmxsAiEV8lpNJhECP3PkgX65ksxev3aLDgehzZcrB-fTrb1UJtO8yyqPvuAH9aHZ18dmu_tDeQNYKz5b</recordid><startdate>20100126</startdate><enddate>20100126</enddate><creator>Quinn, Mark K</creator><creator>McGillivray, Alexander V</creator><creator>Mayne, Paul W</creator><scope>EFH</scope></search><sort><creationdate>20100126</creationdate><title>Rotary actuated seismic source and methods for continuous direct-push downhole seismic testing</title><author>Quinn, Mark K ; McGillivray, Alexander V ; Mayne, Paul W</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-uspatents_grants_076509623</frbrgroupid><rsrctype>patents</rsrctype><prefilter>patents</prefilter><language>eng</language><creationdate>2010</creationdate><toplevel>online_resources</toplevel><creatorcontrib>Quinn, Mark K</creatorcontrib><creatorcontrib>McGillivray, Alexander V</creatorcontrib><creatorcontrib>Mayne, Paul W</creatorcontrib><creatorcontrib>Georgia Tech Research Corporation</creatorcontrib><collection>USPTO Issued Patents</collection></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext_linktorsrc</fulltext></delivery><addata><au>Quinn, Mark K</au><au>McGillivray, Alexander V</au><au>Mayne, Paul W</au><aucorp>Georgia Tech Research Corporation</aucorp><format>patent</format><genre>patent</genre><ristype>GEN</ristype><title>Rotary actuated seismic source and methods for continuous direct-push downhole seismic testing</title><date>2010-01-26</date><risdate>2010</risdate><abstract>Remotely operated rotary actuated shear wave generating apparatus and methods that generate horizontally polarized vertically propagating shear waves for use in down-hole shear wave velocity measurements. Seismic signals are generated by an offset mass rotating in a plane perpendicular to the surface of the ground, which impacts an impact member coupled to the ground. The energy of impact is transmitted to the ground parallel to the surface of the ground. The apparatus uses a spring-loaded rotating mass that has a rotary motion. Because acceleration of the mass is not horizontal, reaction forces caused by acceleration of the mass create less horizontal shear stress in the ground prior to the desired time (impact). Reaction forces of the accelerated rotating mass does not generate undesirable waves that obscure the desirable waves caused by impact with the impact member. The source generates transient shear waves repeatedly at constant intervals. Wave motions are recorded by a probe as it is advanced into the ground, without pause.</abstract><oa>free_for_read</oa></addata></record>
fulltext fulltext_linktorsrc
identifier
ispartof
issn
language eng
recordid cdi_uspatents_grants_07650962
source USPTO Issued Patents
title Rotary actuated seismic source and methods for continuous direct-push downhole seismic testing
url https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2024-12-28T10%3A31%3A28IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-uspatents_EFH&rft_val_fmt=info:ofi/fmt:kev:mtx:patent&rft.genre=patent&rft.au=Quinn,%20Mark%20K&rft.aucorp=Georgia%20Tech%20Research%20Corporation&rft.date=2010-01-26&rft_id=info:doi/&rft_dat=%3Cuspatents_EFH%3E07650962%3C/uspatents_EFH%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_id=info:pmid/&rfr_iscdi=true