{
"USGS Publications Warehouse": {
"@context": "https://schema.org",
"@type": "Article",
"additionalType": "Journal Article",
"name": "Multi-component ground motion response spectra for coupled horizontal, vertical, angular accelerations, and tilt",
"identifier": [
{
"@type": "PropertyValue",
"propertyID": "USGS Publications Warehouse IndexID",
"value": "70033217",
"url": "https://pubs.usgs.gov/publication/70033217"
},
{
"@type": "PropertyValue",
"propertyID": "USGS Publications Warehouse Internal ID",
"value": 70033217
},
{
"@type": "PropertyValue",
"propertyID": "ISSN",
"value": "09720405"
}
],
"journal": {
"@type": "Periodical",
"name": "ISET Journal of Earthquake Technology",
"volumeNumber": "44",
"issueNumber": "1"
},
"inLanguage": "en",
"isPartOf": [
{
"@type": "CreativeWorkSeries",
"name": "ISET Journal of Earthquake Technology"
}
],
"datePublished": "2007",
"dateModified": "2012-03-12",
"abstract": "Rotational and vertical components of ground motion are almost always ignored in design or in the assessment of structures despite the fact that vertical motion can be twice as much as the horizontal motion and may exceed 2g level, and rotational excitation may reach few degrees in the proximity of fault rupture. Coupling of different components of ground excitation may significantly amplify the seismic demand by introducing additional lateral forces and enhanced P-?? effects. In this paper, a governing equation of motion is postulated to compute the response of a SDOF oscillator under a multi-component excitation. The expanded equation includes secondary P-?? components associated with the combined impacts of tilt and vertical excitations in addition to the inertial forcing terms due to the angular and translational accelerations. The elastic and inelastic spectral ordinates traditionally generated considering the uniaxial input motion are compared at the end with the multi-component response spectra of coupled horizontal, vertical and tilting motions. The proposed multi-component response spectrum reflects kinematic characteristics of the ground motion that are not identifiable by the conventional spectrum itself, at least for the near-fault region where high intensity vertical shaking and rotational excitation are likely to occur.",
"publisher": {
"@type": "Organization",
"name": "U.S. Geological Survey"
},
"author": [
{
"@type": "Person",
"name": "Kalkan, E.",
"givenName": "E.",
"familyName": "Kalkan",
"identifier": {
"@type": "PropertyValue",
"propertyID": "ORCID",
"value": "0000-0002-9138-9407",
"url": "https://orcid.org/0000-0002-9138-9407"
}
},
{
"@type": "Person",
"name": "Graizer, V.",
"givenName": "V.",
"familyName": "Graizer"
}
]
}
}