1989
DOI: 10.1016/s0267-7261(89)80019-3
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Recursive evaluation of interaction forces of unbounded soil in frequency domain

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Cited by 9 publications
(3 citation statements)
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“…While it is a major simplification of the actual seismic wave field, at the present time, it seems to be the only pragmatic choice . Afterwards, the free‐field motion of the nodes representing the boundary of excavated region ( Vtrue¯b0) is used to determine their motion following the excavation (Figure B), using Equation , where Strue¯bbf is the dynamically condensed impedance matrix of the soil‐structure interface for the excavated region and Strue¯bb represents the counterpart matrix of the same nodes for soil medium prior to excavation (Figure B). Utrue¯b0=Strue¯bbf1Strue¯bbVtrue¯b0 …”
Section: Numerical Modelingmentioning
confidence: 99%
“…While it is a major simplification of the actual seismic wave field, at the present time, it seems to be the only pragmatic choice . Afterwards, the free‐field motion of the nodes representing the boundary of excavated region ( Vtrue¯b0) is used to determine their motion following the excavation (Figure B), using Equation , where Strue¯bbf is the dynamically condensed impedance matrix of the soil‐structure interface for the excavated region and Strue¯bb represents the counterpart matrix of the same nodes for soil medium prior to excavation (Figure B). Utrue¯b0=Strue¯bbf1Strue¯bbVtrue¯b0 …”
Section: Numerical Modelingmentioning
confidence: 99%
“…Specifically, in a first iteration the pseudo-forces are taken as zero and equation (4) is integrated in the usual fashion. The time history of the SOIL-STRUCTURE INTERACTION PROBLEM displacements at the soil-structure interface are then used to evaluate the pseudo-forces from equation (5). Using the computed pseudo-forces one solves equation (4) again and so on until some appropriately selected norm becomes equal to or smaller than a certain prescribed tolerance.…”
Section: The Htfd Methodsmentioning
confidence: 99%
“…By examining historical earthquakes and studying recorded earthquakes, it is clear that the study area has a high potential from a tectonic seismic point of view and is highly seismic [2]. Meanwhile, the whole province of Tehran is located in an area with a relative earthquake risk of "very high" (In this case, the Peak Ground Acceleration, PGA, is 0.35 g (according to the third edition of the 2800 standard) [Ref.…”
Section: Seismicity and Geotechnical Specifications Of The Areamentioning
confidence: 99%