dc.contributor.author |
MAKRIS, N |
en |
dc.contributor.author |
GAZETAS, G |
en |
dc.date.accessioned |
2014-03-01T01:09:22Z |
|
dc.date.available |
2014-03-01T01:09:22Z |
|
dc.date.issued |
1993 |
en |
dc.identifier.issn |
0016-8505 |
en |
dc.identifier.uri |
https://dspace.lib.ntua.gr/xmlui/handle/123456789/10932 |
|
dc.subject |
DEFORMATION |
en |
dc.subject |
DYNAMICS |
en |
dc.subject |
PILES |
en |
dc.subject |
VIBRATION |
en |
dc.subject |
WAVES |
en |
dc.subject.classification |
Engineering, Geological |
en |
dc.subject.classification |
Geosciences, Multidisciplinary |
en |
dc.subject.other |
DEFORMATION |
en |
dc.subject.other |
STIFFNESS |
en |
dc.subject.other |
VIBRATION |
en |
dc.title |
DISPLACEMENT PHASE DIFFERENCES IN A HARMONICALLY OSCILLATING PILE |
en |
heal.type |
journalArticle |
en |
heal.identifier.primary |
10.1680/geot.1993.43.1.135 |
en |
heal.identifier.secondary |
http://dx.doi.org/10.1680/geot.1993.43.1.135 |
en |
heal.language |
English |
en |
heal.publicationDate |
1993 |
en |
heal.abstract |
Analytical solutions are developed for harmonic wave propagation in an axially or laterally oscillating pile embedded in homogeneous soil and excited at the top. Pile-soil interaction is realistically represented through a dynamic Winkler model, the springs and dashpots of which are given values based on results of finite element analyses with the soil treated as a linear hysteretic continuum. Closed form expressions are derived for the phase velocities of the generated waves; these are compared with characteristic phase. velocities in rods and beams subjected to compression-extension (axial) and flexural (lateral) vibrations. The role of radiation and material damping is elucidated; it is shown that the presence of such damping radically changes the nature of wave propagation, especially in lateral oscillations where an upward propagating (reflected) wave is generated even in a semi-infinite head-loaded pile. Solutions are then developed for the phase differences between pile displacements at various depths. For most piles such differences are not significant and waves emanate nearly simultaneously from the periphery of an oscillating pile. This conclusion is useful in analysing dynamic pile to pile interaction, the consequences of which are shown in this Paper. |
en |
heal.publisher |
THOMAS TELFORD SERVICES LTD |
en |
heal.journalName |
GEOTECHNIQUE |
en |
dc.identifier.doi |
10.1680/geot.1993.43.1.135 |
en |
dc.identifier.isi |
ISI:A1993KR72700009 |
en |
dc.identifier.volume |
43 |
en |
dc.identifier.issue |
1 |
en |
dc.identifier.spage |
135 |
en |
dc.identifier.epage |
150 |
en |