retired
Entry: seismic sensor
URI: https://terra-vocabulary.org/ncl/DataTerraRepositoryFairIncubator/motsClefs/c_4126fda4
There are two basic types of seismic sensors: (1) inertial seismometers which measure ground motion relative to an inertial reference (a suspended mass), and (2) strainmeters or extensometers which measure the motion of one point of the ground relative to another. Inertial seismometers are generally more sensitive to earthquake signals, whereas strainmeters may outperform inertial seismometers when observing very longperiod free oscillations of the Earth, tidal motions, and quasistatic deformations when it becomes increasingly difficult to maintain an inertial reference
Core metadata
is a | Concept | Sensor |
changed on | 17 Nov 2023 08:31:48.081 |
submitted by | Hélène Bressan |
accepted on | 20 May 2022 09:42:08.260 |
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date accepted |
20 May 2022 09:42:08.260
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date submitted |
20 May 2022 09:41:39.008
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definition |
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description |
There are two basic types of seismic sensors: (1) inertial seismometers which measure ground motion relative to an inertial reference (a suspended mass), and (2) strainmeters or extensometers which measure the motion of one point of the ground relative to another. Inertial seismometers are generally more sensitive to earthquake signals, whereas strainmeters may outperform inertial seismometers when observing very longperiod free oscillations of the Earth, tidal motions, and quasistatic deformations when it becomes increasingly difficult to maintain an inertial reference
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item class |
Concept
| Sensor
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label |
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modified |
17 Nov 2023 08:31:48.081
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notation |
c_4126fda4
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register |
mots clefs
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status |
status retired
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submitter |
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type |
register item
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version info |
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Definition
change note |
Invalidé par les thématiciens en juillet 2022
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deprecated |
true
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description |
There are two basic types of seismic sensors: (1) inertial seismometers which measure ground motion relative to an inertial reference (a suspended mass), and (2) strainmeters or extensometers which measure the motion of one point of the ground relative to another. Inertial seismometers are generally more sensitive to earthquake signals, whereas strainmeters may outperform inertial seismometers when observing very longperiod free oscillations of the Earth, tidal motions, and quasistatic deformations when it becomes increasingly difficult to maintain an inertial reference
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in scheme |
Vocabulaire des mots clefs
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label |
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pref label |
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source |
epos
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status |
submitted
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top concept of |
Vocabulaire des mots clefs
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type |
Concept
| Sensor
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was attributed to |
Pôle FormaTerre
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