THE THEORY AND DESIGN OF TWO TYPES OF PORTABLE SEISMOGRAPH
Summary The sensitivity of optical recorders is derived by considering the power required to maintain a critically damped, suspended mirror in angular oscillations of sufficient amplitude to displace the reflected beam through an angle comparable with the width of the diffraction maximum. For a thin...
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Veröffentlicht in: | Geophysical journal international 1950-10, Vol.6, p.129-137 |
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creator | Willmore, P. L. |
description | Summary
The sensitivity of optical recorders is derived by considering the power required to maintain a critically damped, suspended mirror in angular oscillations of sufficient amplitude to displace the reflected beam through an angle comparable with the width of the diffraction maximum. For a thin mirror, this power is simply related to its dimensions, and to the natural frequency of the suspension. The power which a seismometer can develop from ground motion of given amplitude is related to the suspended mass and its natural frequency. Combining these results, it is found that a seismometer mass of a few hundred grams is sufficient to detect ground motion of 10‐7 cm. without using an excessively small mirror in the recorder. Modern movingcoil galvanometers have sensitivities approaching the limit imposed by the inertia of the mirror, so that small electromagnetic seismographs are theoretically capable of providing the highest sensitivity required in the field.
Moving‐coil seismometers are compared with variable‐reluctance instruments, and it is decided that the former type would be more convenient in the field. Descriptions are included of seismometers having natural periods of 0. 5 sec. and of I sec. respectively. Both instruments can be adapted for horizontal or vertical operation, and are fitted into watertight cases. Tolerance to changes of level is sufficient to enable the seismometers to be left buried in soft ground, and a method of calibrating the buried instruments is described. |
doi_str_mv | 10.1111/j.1365-246X.1950.tb02987.x |
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The sensitivity of optical recorders is derived by considering the power required to maintain a critically damped, suspended mirror in angular oscillations of sufficient amplitude to displace the reflected beam through an angle comparable with the width of the diffraction maximum. For a thin mirror, this power is simply related to its dimensions, and to the natural frequency of the suspension. The power which a seismometer can develop from ground motion of given amplitude is related to the suspended mass and its natural frequency. Combining these results, it is found that a seismometer mass of a few hundred grams is sufficient to detect ground motion of 10‐7 cm. without using an excessively small mirror in the recorder. Modern movingcoil galvanometers have sensitivities approaching the limit imposed by the inertia of the mirror, so that small electromagnetic seismographs are theoretically capable of providing the highest sensitivity required in the field.
Moving‐coil seismometers are compared with variable‐reluctance instruments, and it is decided that the former type would be more convenient in the field. Descriptions are included of seismometers having natural periods of 0. 5 sec. and of I sec. respectively. Both instruments can be adapted for horizontal or vertical operation, and are fitted into watertight cases. Tolerance to changes of level is sufficient to enable the seismometers to be left buried in soft ground, and a method of calibrating the buried instruments is described.</description><identifier>ISSN: 0956-540X</identifier><identifier>EISSN: 1365-246X</identifier><identifier>DOI: 10.1111/j.1365-246X.1950.tb02987.x</identifier><language>eng</language><publisher>Oxford, UK: Blackwell Publishing Ltd</publisher><subject>Amplitudes ; Beams (radiation) ; Calibration ; Earthquake dampers ; Ground motion ; Oscillations ; Recorders ; Resonant frequency ; Seismic phenomena</subject><ispartof>Geophysical journal international, 1950-10, Vol.6, p.129-137</ispartof><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c3329-3366eb619d003b472d99ad32d47376e60984d295336eaa31c5d99bc0578309ef3</citedby><cites>FETCH-LOGICAL-c3329-3366eb619d003b472d99ad32d47376e60984d295336eaa31c5d99bc0578309ef3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://onlinelibrary.wiley.com/doi/pdf/10.1111%2Fj.1365-246X.1950.tb02987.x$$EPDF$$P50$$Gwiley$$H</linktopdf><linktohtml>$$Uhttps://onlinelibrary.wiley.com/doi/full/10.1111%2Fj.1365-246X.1950.tb02987.x$$EHTML$$P50$$Gwiley$$H</linktohtml><link.rule.ids>314,780,784,1417,27924,27925,45574,45575</link.rule.ids></links><search><creatorcontrib>Willmore, P. L.</creatorcontrib><title>THE THEORY AND DESIGN OF TWO TYPES OF PORTABLE SEISMOGRAPH</title><title>Geophysical journal international</title><description>Summary
The sensitivity of optical recorders is derived by considering the power required to maintain a critically damped, suspended mirror in angular oscillations of sufficient amplitude to displace the reflected beam through an angle comparable with the width of the diffraction maximum. For a thin mirror, this power is simply related to its dimensions, and to the natural frequency of the suspension. The power which a seismometer can develop from ground motion of given amplitude is related to the suspended mass and its natural frequency. Combining these results, it is found that a seismometer mass of a few hundred grams is sufficient to detect ground motion of 10‐7 cm. without using an excessively small mirror in the recorder. Modern movingcoil galvanometers have sensitivities approaching the limit imposed by the inertia of the mirror, so that small electromagnetic seismographs are theoretically capable of providing the highest sensitivity required in the field.
Moving‐coil seismometers are compared with variable‐reluctance instruments, and it is decided that the former type would be more convenient in the field. Descriptions are included of seismometers having natural periods of 0. 5 sec. and of I sec. respectively. Both instruments can be adapted for horizontal or vertical operation, and are fitted into watertight cases. Tolerance to changes of level is sufficient to enable the seismometers to be left buried in soft ground, and a method of calibrating the buried instruments is described.</description><subject>Amplitudes</subject><subject>Beams (radiation)</subject><subject>Calibration</subject><subject>Earthquake dampers</subject><subject>Ground motion</subject><subject>Oscillations</subject><subject>Recorders</subject><subject>Resonant frequency</subject><subject>Seismic phenomena</subject><issn>0956-540X</issn><issn>1365-246X</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1950</creationdate><recordtype>article</recordtype><recordid>eNqVkUtrwlAQhS-lhVrb_xC66ibpfT9cFFKNMcUaMSnV1SWPKyhaba5S_fdNULqVDgzDMN-ZxTkAPCLoobqelx4inLmY8qmHFIPeLodYSeEdrkDr73QNWlAx7jIKp7fgztolhIgiKlugkw4Cp-54MnP8Uc_pBUkUjpy476SfsZPOxkHSLON4kvqvw8BJgih5j8OJPx7cg5t5trLm4Tzb4KMfpN2BO4zDqOsP3YIQrFxCODc5R6qEkORU4FKprCS4pIIIbjhUkpZYsZozWUZQwWogLyATkkBl5qQNnk5_t9Xme2_sTq8XtjCrVfZlNnurEacYSyIJvowyTCnijIjLKEVCSiWgqtHOCS2qjbWVmetttVhn1VEjqJsY9FI3XuvGa93EoM8x6EMtfjmJfxYrc_yHUodvEcKK_AJqq4eY</recordid><startdate>195010</startdate><enddate>195010</enddate><creator>Willmore, P. L.</creator><general>Blackwell Publishing Ltd</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7SM</scope><scope>8FD</scope><scope>FR3</scope><scope>H8D</scope><scope>KR7</scope><scope>L7M</scope><scope>7TN</scope><scope>F1W</scope><scope>H96</scope><scope>L.G</scope></search><sort><creationdate>195010</creationdate><title>THE THEORY AND DESIGN OF TWO TYPES OF PORTABLE SEISMOGRAPH</title><author>Willmore, P. L.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c3329-3366eb619d003b472d99ad32d47376e60984d295336eaa31c5d99bc0578309ef3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>1950</creationdate><topic>Amplitudes</topic><topic>Beams (radiation)</topic><topic>Calibration</topic><topic>Earthquake dampers</topic><topic>Ground motion</topic><topic>Oscillations</topic><topic>Recorders</topic><topic>Resonant frequency</topic><topic>Seismic phenomena</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Willmore, P. L.</creatorcontrib><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><collection>Oceanic Abstracts</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><jtitle>Geophysical journal international</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Willmore, P. L.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>THE THEORY AND DESIGN OF TWO TYPES OF PORTABLE SEISMOGRAPH</atitle><jtitle>Geophysical journal international</jtitle><date>1950-10</date><risdate>1950</risdate><volume>6</volume><spage>129</spage><epage>137</epage><pages>129-137</pages><issn>0956-540X</issn><eissn>1365-246X</eissn><abstract>Summary
The sensitivity of optical recorders is derived by considering the power required to maintain a critically damped, suspended mirror in angular oscillations of sufficient amplitude to displace the reflected beam through an angle comparable with the width of the diffraction maximum. For a thin mirror, this power is simply related to its dimensions, and to the natural frequency of the suspension. The power which a seismometer can develop from ground motion of given amplitude is related to the suspended mass and its natural frequency. Combining these results, it is found that a seismometer mass of a few hundred grams is sufficient to detect ground motion of 10‐7 cm. without using an excessively small mirror in the recorder. Modern movingcoil galvanometers have sensitivities approaching the limit imposed by the inertia of the mirror, so that small electromagnetic seismographs are theoretically capable of providing the highest sensitivity required in the field.
Moving‐coil seismometers are compared with variable‐reluctance instruments, and it is decided that the former type would be more convenient in the field. Descriptions are included of seismometers having natural periods of 0. 5 sec. and of I sec. respectively. Both instruments can be adapted for horizontal or vertical operation, and are fitted into watertight cases. Tolerance to changes of level is sufficient to enable the seismometers to be left buried in soft ground, and a method of calibrating the buried instruments is described.</abstract><cop>Oxford, UK</cop><pub>Blackwell Publishing Ltd</pub><doi>10.1111/j.1365-246X.1950.tb02987.x</doi><tpages>9</tpages></addata></record> |
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subjects | Amplitudes Beams (radiation) Calibration Earthquake dampers Ground motion Oscillations Recorders Resonant frequency Seismic phenomena |
title | THE THEORY AND DESIGN OF TWO TYPES OF PORTABLE SEISMOGRAPH |
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