词条 | Arias Intensity |
释义 |
The Arias Intensity (IA) is a measure of the strength of a ground motion.[1] It determines the intensity of shaking by measuring the acceleration of transient seismic waves. It has been found to be a fairly reliable parameter to describe earthquake shaking necessary to trigger landslides.[2] It was proposed by Chilean engineer Arturo Arias in 1970. It is defined as the time-integral of the square of the ground acceleration: (m/s) where g is the acceleration due to gravity and Td is the duration of signal above threshold. Theoretically the integral should be infinite.[3] The Arias Intensity could also alternatively be defined as the sum of all the squared acceleration values from seismic strong motion records.[2] References1. ^{{cite journal|title=New predictive equations for Arias intensity from crustal earthquakes in New Zea |journal=Journal of Seismology| volume =13| issue= 1|pages=31–52 |date= |bibcode=2009JSeis..13...31S |doi=10.1007/s10950-008-9114-2}} {{Seismology-stub}}2. ^1 {{cite web|url=http://www.itc.nl/ilwis/applications/application07.asp |title=7. Seismic landslide hazard zonation |publisher=Faculty of Geo-Information Science and Earth Observation of the University of Twente |date=2006-09-29 |accessdate=2010-12-12}} 3. ^{{cite web|url=http://www.geologie.ac.at/filestore/download/JB1471_193_A.pdf |archive-url=https://web.archive.org/web/20110531193712/http://www.geologie.ac.at/filestore/download/JB1471_193_A.pdf |dead-url=yes |archive-date=2011-05-31 |title=Earthquake-Triggered Landslides in Austria – Dobratsch Revisited |author=Wolfgang A. Lenhardt |publisher=Jahrbuch der Geologischen Bundesanstalt |date=2007 }} 1 : Seismology |
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