๐”– Bobbio Scriptorium
โœฆ   LIBER   โœฆ

Vibrational characteristics of soil deposits with variable wave velocity

โœ Scribed by Professor George Gazetas


Publisher
John Wiley and Sons
Year
1982
Tongue
English
Weight
922 KB
Volume
6
Category
Article
ISSN
0363-9061

No coin nor oath required. For personal study only.


๐Ÿ“œ SIMILAR VOLUMES


In-plane vibrations of soil deposits wit
โœ Ch. Vrettos ๐Ÿ“‚ Article ๐Ÿ“… 1990 ๐Ÿ› John Wiley and Sons ๐ŸŒ English โš– 614 KB

The dynamic response of an inhomogeneous, linearelastic half-space to a time-harmonic vertical line load on its surface is studied. The mass density and the Poisson's ratio are assumed to be constant and the shear modulus to increase continuously with depth according to a function which is bounded a

Velocity distribution characteristics of
โœ Hiroshi Onihashi; Yasushi Nishida ๐Ÿ“‚ Article ๐Ÿ“… 2001 ๐Ÿ› John Wiley and Sons ๐ŸŒ English โš– 442 KB ๐Ÿ‘ 2 views

This paper describes the velocity distribution characteristics of a spent beam in a traveling-wave tube equipped with a velocity taper at the output section of a slow-wave circuit. It is shown that the spent beam contains both electrons not synchronized with the velocity taper and electrons synchron

Variability of shallow overland flow vel
โœ A. Sidorchuk; J. Schmidt; G. Cooper ๐Ÿ“‚ Article ๐Ÿ“… 2008 ๐Ÿ› John Wiley and Sons ๐ŸŒ English โš– 618 KB

## Abstract Field experiments at Tiramoana station 30 km north of Christchurch, New Zealand using an erosion plot 16ยท5 m long, 0ยท6 m wide, and with a slope of 14โ€“14ยท5ยฐ on rendzina soil aimed to measure the variability of flow velocity and of soil aggregates transport rate in shallow overland flow.

The importance of surface waves in vibra
โœ D. Jongmans; D. Demanet ๐Ÿ“‚ Article ๐Ÿ“… 1993 ๐Ÿ› Elsevier Science ๐ŸŒ English โš– 532 KB

Vibrations generated during civil engineering work are often dominated by prominent surface waves, the propagation of which is strongly influenced by site conditions. The effects of soil properties on the shape, amplitude and duration of Rayleigh waves are shown from synthetic seismograms. Surface