Groundwater level changes related to the ground shaking of the Noto Hanto Earthquake in 2007
The Geological Survey of Japan, AIST has been monitoring groundwater using the observation network of about 40 stations in and around the Kinki and Tokai districts for earthquake prediction research. The Noto Hanto Earthquake in 2007 (M JMA 6.9) occurred in the northwestern part of the Noto Hanto Pe...
Gespeichert in:
| Veröffentlicht in: | Earth, planets, and space planets, and space, 2008-01, Vol.60 (12), p.1153-1159 |
|---|---|
| Hauptverfasser: | , , , , , , , , , |
| Format: | Artikel |
| Sprache: | eng |
| Schlagworte: | |
| Online-Zugang: | Volltext |
| Tags: |
Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
|
| container_end_page | 1159 |
|---|---|
| container_issue | 12 |
| container_start_page | 1153 |
| container_title | Earth, planets, and space |
| container_volume | 60 |
| creator | Itaba, Satoshi Koizumi, Naoji Matsumoto, Norio Takahashi, Makoto Sato, Tsutomu Ohtani, Ryu Kitagawa, Yuichi Kuwahara, Yasuto Sato, Takashi Ozawa, Kunio |
| description | The Geological Survey of Japan, AIST has been monitoring groundwater using the observation network of about 40 stations in and around the Kinki and Tokai districts for earthquake prediction research. The Noto Hanto Earthquake in 2007 (M
JMA
6.9) occurred in the northwestern part of the Noto Hanto Peninsula, Japan on March 25, 2007. The epicentral distance to the nearest and furthest observation well is about 100 km and 400 km, respectively. Changes in groundwater level related to the Noto Hanto Earthquake were detected at many stations. Most of these were changes in the long-term trend and/or short-term oscillation; there were a few steplike changes. The coseismic static volumetric strain changes calculated from the fault model ranged between 10
−9
and 10
−10
at most of the observation stations. These changes were therefore considered to be groundwater changes caused by the ground shaking because groundwater level sensitivity to crustal volumetric strain is a few centimeters to 10
−8
strain at the most. We compared the coseismic groundwater level changes for the Noto Hanto Earthquake with those for five recent large earthquakes and obtained rough characteristics of the effect of the ground shaking on the groundwater level at each of the observation stations. |
| doi_str_mv | 10.1186/BF03352872 |
| format | Article |
| fullrecord | <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_proquest_miscellaneous_35932737</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>35932737</sourcerecordid><originalsourceid>FETCH-LOGICAL-a478t-cfbfaa4a7df0c023f55b88c825920280369ad184251ddd6082d786618e9d2e063</originalsourceid><addsrcrecordid>eNptkMtOwzAQRSMEEqWw4Qu8gQUo4EcST5ZQ9YFUwQZ2SNHUdtq0adzaCYi_x7QVbNjMjO6cudLcKLpk9I4xyO4fR1SIlIPkR1GPAdA4zYEdh1kkIgYQ_DQ6835JqaBJJnrR-9jZrtGf2BpHavNhaqIW2MyNJ87UQdWktaRdGDLfgcQvcFU1c2LLnfpsw3qCTahDdO1i2-HKkKohnFJ5Hp2UWHtzcej96G00fB1M4unL-GnwMI0xkdDGqpyViAlKXVJFuSjTdAaggKc5pxyoyHLUDBKeMq11RoFrCVnGwOSaG5qJfnS99904u-2Mb4t15ZWpa2yM7Xwh0lxwKWQAb_agctZ7Z8pi46o1uq-C0eInwOIvwABfHVzRK6xLh42q_O8FZ0xCIvPA3e45H1YhOVcsbeea8PB_rt-0xHwU</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>35932737</pqid></control><display><type>article</type><title>Groundwater level changes related to the ground shaking of the Noto Hanto Earthquake in 2007</title><source>SpringerLink Journals</source><source>Elektronische Zeitschriftenbibliothek - Frei zugängliche E-Journals</source><source>Alma/SFX Local Collection</source><source>Springer Nature OA Free Journals</source><creator>Itaba, Satoshi ; Koizumi, Naoji ; Matsumoto, Norio ; Takahashi, Makoto ; Sato, Tsutomu ; Ohtani, Ryu ; Kitagawa, Yuichi ; Kuwahara, Yasuto ; Sato, Takashi ; Ozawa, Kunio</creator><creatorcontrib>Itaba, Satoshi ; Koizumi, Naoji ; Matsumoto, Norio ; Takahashi, Makoto ; Sato, Tsutomu ; Ohtani, Ryu ; Kitagawa, Yuichi ; Kuwahara, Yasuto ; Sato, Takashi ; Ozawa, Kunio</creatorcontrib><description>The Geological Survey of Japan, AIST has been monitoring groundwater using the observation network of about 40 stations in and around the Kinki and Tokai districts for earthquake prediction research. The Noto Hanto Earthquake in 2007 (M
JMA
6.9) occurred in the northwestern part of the Noto Hanto Peninsula, Japan on March 25, 2007. The epicentral distance to the nearest and furthest observation well is about 100 km and 400 km, respectively. Changes in groundwater level related to the Noto Hanto Earthquake were detected at many stations. Most of these were changes in the long-term trend and/or short-term oscillation; there were a few steplike changes. The coseismic static volumetric strain changes calculated from the fault model ranged between 10
−9
and 10
−10
at most of the observation stations. These changes were therefore considered to be groundwater changes caused by the ground shaking because groundwater level sensitivity to crustal volumetric strain is a few centimeters to 10
−8
strain at the most. We compared the coseismic groundwater level changes for the Noto Hanto Earthquake with those for five recent large earthquakes and obtained rough characteristics of the effect of the ground shaking on the groundwater level at each of the observation stations.</description><identifier>ISSN: 1343-8832</identifier><identifier>ISSN: 1880-5981</identifier><identifier>EISSN: 1880-5981</identifier><identifier>DOI: 10.1186/BF03352872</identifier><language>eng</language><publisher>Berlin/Heidelberg: Springer Berlin Heidelberg</publisher><subject>Cosmochemistry. Extraterrestrial geology ; Earth and Environmental Science ; Earth Sciences ; Earth, ocean, space ; Exact sciences and technology ; Geology ; Geophysics/Geodesy</subject><ispartof>Earth, planets, and space, 2008-01, Vol.60 (12), p.1153-1159</ispartof><rights>The Society of Geomagnetism and Earth, Planetary and Space Sciences (SGEPSS); The Seismological Society of Japan; The Volcanological Society of Japan; The Geodetic Society of Japan; The Japanese Society for Planetary Sciences. 2005</rights><rights>2009 INIST-CNRS</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a478t-cfbfaa4a7df0c023f55b88c825920280369ad184251ddd6082d786618e9d2e063</citedby><cites>FETCH-LOGICAL-a478t-cfbfaa4a7df0c023f55b88c825920280369ad184251ddd6082d786618e9d2e063</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1186/BF03352872$$EPDF$$P50$$Gspringer$$Hfree_for_read</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1186/BF03352872$$EHTML$$P50$$Gspringer$$Hfree_for_read</linktohtml><link.rule.ids>314,776,780,27901,27902,41096,41464,42165,42533,51294,51551</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=21178479$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>Itaba, Satoshi</creatorcontrib><creatorcontrib>Koizumi, Naoji</creatorcontrib><creatorcontrib>Matsumoto, Norio</creatorcontrib><creatorcontrib>Takahashi, Makoto</creatorcontrib><creatorcontrib>Sato, Tsutomu</creatorcontrib><creatorcontrib>Ohtani, Ryu</creatorcontrib><creatorcontrib>Kitagawa, Yuichi</creatorcontrib><creatorcontrib>Kuwahara, Yasuto</creatorcontrib><creatorcontrib>Sato, Takashi</creatorcontrib><creatorcontrib>Ozawa, Kunio</creatorcontrib><title>Groundwater level changes related to the ground shaking of the Noto Hanto Earthquake in 2007</title><title>Earth, planets, and space</title><addtitle>Earth Planet Sp</addtitle><description>The Geological Survey of Japan, AIST has been monitoring groundwater using the observation network of about 40 stations in and around the Kinki and Tokai districts for earthquake prediction research. The Noto Hanto Earthquake in 2007 (M
JMA
6.9) occurred in the northwestern part of the Noto Hanto Peninsula, Japan on March 25, 2007. The epicentral distance to the nearest and furthest observation well is about 100 km and 400 km, respectively. Changes in groundwater level related to the Noto Hanto Earthquake were detected at many stations. Most of these were changes in the long-term trend and/or short-term oscillation; there were a few steplike changes. The coseismic static volumetric strain changes calculated from the fault model ranged between 10
−9
and 10
−10
at most of the observation stations. These changes were therefore considered to be groundwater changes caused by the ground shaking because groundwater level sensitivity to crustal volumetric strain is a few centimeters to 10
−8
strain at the most. We compared the coseismic groundwater level changes for the Noto Hanto Earthquake with those for five recent large earthquakes and obtained rough characteristics of the effect of the ground shaking on the groundwater level at each of the observation stations.</description><subject>Cosmochemistry. Extraterrestrial geology</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Earth, ocean, space</subject><subject>Exact sciences and technology</subject><subject>Geology</subject><subject>Geophysics/Geodesy</subject><issn>1343-8832</issn><issn>1880-5981</issn><issn>1880-5981</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2008</creationdate><recordtype>article</recordtype><sourceid>C6C</sourceid><recordid>eNptkMtOwzAQRSMEEqWw4Qu8gQUo4EcST5ZQ9YFUwQZ2SNHUdtq0adzaCYi_x7QVbNjMjO6cudLcKLpk9I4xyO4fR1SIlIPkR1GPAdA4zYEdh1kkIgYQ_DQ6835JqaBJJnrR-9jZrtGf2BpHavNhaqIW2MyNJ87UQdWktaRdGDLfgcQvcFU1c2LLnfpsw3qCTahDdO1i2-HKkKohnFJ5Hp2UWHtzcej96G00fB1M4unL-GnwMI0xkdDGqpyViAlKXVJFuSjTdAaggKc5pxyoyHLUDBKeMq11RoFrCVnGwOSaG5qJfnS99904u-2Mb4t15ZWpa2yM7Xwh0lxwKWQAb_agctZ7Z8pi46o1uq-C0eInwOIvwABfHVzRK6xLh42q_O8FZ0xCIvPA3e45H1YhOVcsbeea8PB_rt-0xHwU</recordid><startdate>20080101</startdate><enddate>20080101</enddate><creator>Itaba, Satoshi</creator><creator>Koizumi, Naoji</creator><creator>Matsumoto, Norio</creator><creator>Takahashi, Makoto</creator><creator>Sato, Tsutomu</creator><creator>Ohtani, Ryu</creator><creator>Kitagawa, Yuichi</creator><creator>Kuwahara, Yasuto</creator><creator>Sato, Takashi</creator><creator>Ozawa, Kunio</creator><general>Springer Berlin Heidelberg</general><general>Terra</general><scope>C6C</scope><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7SM</scope><scope>8FD</scope><scope>FR3</scope><scope>H8D</scope><scope>KR7</scope><scope>L7M</scope></search><sort><creationdate>20080101</creationdate><title>Groundwater level changes related to the ground shaking of the Noto Hanto Earthquake in 2007</title><author>Itaba, Satoshi ; Koizumi, Naoji ; Matsumoto, Norio ; Takahashi, Makoto ; Sato, Tsutomu ; Ohtani, Ryu ; Kitagawa, Yuichi ; Kuwahara, Yasuto ; Sato, Takashi ; Ozawa, Kunio</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a478t-cfbfaa4a7df0c023f55b88c825920280369ad184251ddd6082d786618e9d2e063</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2008</creationdate><topic>Cosmochemistry. Extraterrestrial geology</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Earth, ocean, space</topic><topic>Exact sciences and technology</topic><topic>Geology</topic><topic>Geophysics/Geodesy</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Itaba, Satoshi</creatorcontrib><creatorcontrib>Koizumi, Naoji</creatorcontrib><creatorcontrib>Matsumoto, Norio</creatorcontrib><creatorcontrib>Takahashi, Makoto</creatorcontrib><creatorcontrib>Sato, Tsutomu</creatorcontrib><creatorcontrib>Ohtani, Ryu</creatorcontrib><creatorcontrib>Kitagawa, Yuichi</creatorcontrib><creatorcontrib>Kuwahara, Yasuto</creatorcontrib><creatorcontrib>Sato, Takashi</creatorcontrib><creatorcontrib>Ozawa, Kunio</creatorcontrib><collection>Springer Nature OA Free Journals</collection><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>Earthquake Engineering Abstracts</collection><collection>Technology Research Database</collection><collection>Engineering Research Database</collection><collection>Aerospace Database</collection><collection>Civil Engineering Abstracts</collection><collection>Advanced Technologies Database with Aerospace</collection><jtitle>Earth, planets, and space</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Itaba, Satoshi</au><au>Koizumi, Naoji</au><au>Matsumoto, Norio</au><au>Takahashi, Makoto</au><au>Sato, Tsutomu</au><au>Ohtani, Ryu</au><au>Kitagawa, Yuichi</au><au>Kuwahara, Yasuto</au><au>Sato, Takashi</au><au>Ozawa, Kunio</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Groundwater level changes related to the ground shaking of the Noto Hanto Earthquake in 2007</atitle><jtitle>Earth, planets, and space</jtitle><stitle>Earth Planet Sp</stitle><date>2008-01-01</date><risdate>2008</risdate><volume>60</volume><issue>12</issue><spage>1153</spage><epage>1159</epage><pages>1153-1159</pages><issn>1343-8832</issn><issn>1880-5981</issn><eissn>1880-5981</eissn><abstract>The Geological Survey of Japan, AIST has been monitoring groundwater using the observation network of about 40 stations in and around the Kinki and Tokai districts for earthquake prediction research. The Noto Hanto Earthquake in 2007 (M
JMA
6.9) occurred in the northwestern part of the Noto Hanto Peninsula, Japan on March 25, 2007. The epicentral distance to the nearest and furthest observation well is about 100 km and 400 km, respectively. Changes in groundwater level related to the Noto Hanto Earthquake were detected at many stations. Most of these were changes in the long-term trend and/or short-term oscillation; there were a few steplike changes. The coseismic static volumetric strain changes calculated from the fault model ranged between 10
−9
and 10
−10
at most of the observation stations. These changes were therefore considered to be groundwater changes caused by the ground shaking because groundwater level sensitivity to crustal volumetric strain is a few centimeters to 10
−8
strain at the most. We compared the coseismic groundwater level changes for the Noto Hanto Earthquake with those for five recent large earthquakes and obtained rough characteristics of the effect of the ground shaking on the groundwater level at each of the observation stations.</abstract><cop>Berlin/Heidelberg</cop><pub>Springer Berlin Heidelberg</pub><doi>10.1186/BF03352872</doi><tpages>7</tpages><oa>free_for_read</oa></addata></record> |
| fulltext | fulltext |
| identifier | ISSN: 1343-8832 |
| ispartof | Earth, planets, and space, 2008-01, Vol.60 (12), p.1153-1159 |
| issn | 1343-8832 1880-5981 1880-5981 |
| language | eng |
| recordid | cdi_proquest_miscellaneous_35932737 |
| source | SpringerLink Journals; Elektronische Zeitschriftenbibliothek - Frei zugängliche E-Journals; Alma/SFX Local Collection; Springer Nature OA Free Journals |
| subjects | Cosmochemistry. Extraterrestrial geology Earth and Environmental Science Earth Sciences Earth, ocean, space Exact sciences and technology Geology Geophysics/Geodesy |
| title | Groundwater level changes related to the ground shaking of the Noto Hanto Earthquake in 2007 |
| url | https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-02-08T21%3A30%3A43IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-proquest_cross&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Groundwater%20level%20changes%20related%20to%20the%20ground%20shaking%20of%20the%20Noto%20Hanto%20Earthquake%20in%202007&rft.jtitle=Earth,%20planets,%20and%20space&rft.au=Itaba,%20Satoshi&rft.date=2008-01-01&rft.volume=60&rft.issue=12&rft.spage=1153&rft.epage=1159&rft.pages=1153-1159&rft.issn=1343-8832&rft.eissn=1880-5981&rft_id=info:doi/10.1186/BF03352872&rft_dat=%3Cproquest_cross%3E35932737%3C/proquest_cross%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_pqid=35932737&rft_id=info:pmid/&rfr_iscdi=true |