Don’t see the answer that you’re looking for?Comments * © 2022 Science Trends LLC. The aim of the earthquake simulation studies is to define the character of ground motion as close to the real one to reduce the damage mitigations before, during, and after an earthquake. The local site effects were mostly successfully generated on the synthetic high-frequency seismograms (Figure 5). 04 103 g. It is expected that this method can be applied to observation sites throughout the country. Pairojn and Wasinrat [4] proposed the MLR model to predict average peak informative post ground acceleration, PHAavg (Y), in Thailand by including magnitude, and distance as predictor variables.
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The MLR model has been used for probabilistic hazard analysis, risk analysis, building design analysis, and many other fields, that is, and construction of nuclear power plants, dams, bridges, and high-rise buildings. 050, 1=3. Validating site effects is inevitable to estimate earthquake ground motion and disaster mitigation. The MLR model can be generalized as follows:where M represents the magnitude and R represents the distance. PGA is equal to the amplitude of the largest absolute acceleration recorded on an accelerogram at a site during a particular earthquake.
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The RMSE measures the error between a predicted value and an observed value, defined as:where Yi is the predicted values from MLR model and Yi is the observed values from n observations.
Damage to buildings is related to both peak ground velocity (PGV) and the duration of the earthquake – the longer high-level shaking persists, the greater the likelihood of damage. Most of these effects cannot be determined easily and comprehensive studies are needed. It provides unprocessed acceleration time-series, manually processed acceleration, velocity, and displacement waveforms, acceleration and displacement response spectra, and other relevant engineering parameters. -see the history of the largest earthquake and put on every major solar system day number and year. Another of the most seismically active regions (5-6% of the total number of earthquakes) is the Alpide belt, which ranges from the Mediterranean in the west to the Himalayas in the east).
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Peak ground acceleration can be expressed in fractions of g (the standard acceleration due to Earth’s gravity, equivalent to g-force) as either a decimal or percentage; in m/s2 (1g=9. This work was led by Ozlem Karagoz from the Tokyo Institute of Technology (formerly), Çanakkale Onsekiz Mart University (currently). 2) of the ASCE/SEI 7-10 and 7-16 standards. As PhD students, we found it difficult to access the research we needed, so we decided to create a new Open Access publisher that levels the playing field for scientists across the world.
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Meanwhile, seismologists improved methods by using mathematics and physics to extract the earth structures from analyzing ground motions (seismograms). Unable to display preview. Correspondence to
Fabio Romanelli . It was found that the average peak horizontal ground acceleration by regression models was attenuated by the distance from the epicenters. It can be correlated to macroseismic intensities on the Mercalli scale3 but these correlations are associated with large uncertainty. 0 License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.
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This investigation is aimed at proposing regression models for average peak horizontal ground acceleration of earthquakes recorded by seismometers installed you can check here a station in Chiang Mai, Thailand. 1007/978-1-4615-1693-4_2
Publisher Name: Springer, Boston, MA
view publisher site Print ISBN: 978-1-4613-5681-3
Online ISBN: 978-1-4615-1693-4eBook Packages: Springer Book Archive
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