Acernese, Fausto
(2005)
An interferometric seismic sensor: theoretical model and
experimental performances.
[Tesi di dottorato]
(Unpublished)
This is the latest version of this item.
| Item Type: |
Tesi di dottorato
|
| Resource language: |
English |
| Title: |
An interferometric seismic sensor: theoretical model and
experimental performances |
| Creators: |
| Creators | Email |
|---|
| Acernese, Fausto | UNSPECIFIED |
|
| Date: |
2005 |
| Date type: |
Publication |
| Number of Pages: |
112 |
| Institution: |
Università degli Studi di Napoli Federico II |
| Department: |
Scienze fisiche |
| Dottorato: |
Rischio sismico |
| Ciclo di dottorato: |
17 |
| Coordinatore del Corso di dottorato: |
| nome | email |
|---|
| Gasparini, Paolo | UNSPECIFIED |
|
| Tutor: |
| nome | email |
|---|
| Milano, Leopoldo | UNSPECIFIED | | Di Maio, Rosa | UNSPECIFIED |
|
| Date: |
2005 |
| Number of Pages: |
112 |
| Keywords: |
Interferometria, Sensori sismici, Accelerometri |
| Settori scientifico-disciplinari del MIUR: |
Area 02 - Scienze fisiche > FIS/07 - Fisica applicata (a beni culturali, ambientali, biologia e medicina) |
[error in script]
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| Date Deposited: |
01 Aug 2008 |
| Last Modified: |
01 Dec 2014 13:46 |
| URI: |
http://www.fedoa.unina.it/id/eprint/101 |
| DOI: |
10.6092/UNINA/FEDOA/101 |
Available Versions of this Item
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An interferometric seismic sensor: theoretical model and
experimental performances. (deposited 01 Aug 2008)
[Currently Displayed]
Collection description
Laser Optical Interferometry has been introduced in different fields of research for applications requiring very high precision displacement measurements. We have applied optical interferometry for the solving the problem of amplitude and direction measurement of seismic waves. In particular we propose a Michelson Interferometer as a velocimeter with optical readout.
In this work we demostrate that a simple array of two Michelson interferometer can be used as an effective seismic sensor to measure the velocity of ground motion. The sensitivity of such device should be delimited only by the enviromental parameter that can be monitored and controlled. A preliminary experimental test on this technique confirms the theoretical results: in fact there is a good agreement with a standard accelerometer for seismic application.
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