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Research Article

Pseudo-static Winkler springs for longitudinal underground structures subjected to shear waves

ORCID Icon, ORCID Icon & ORCID Icon
Received 15 Feb 2024, Accepted 10 Apr 2024, Published online: 25 Apr 2024
 

ABSTRACT

Shear waves in underground longitudinal structures impose deformations that need to be accounted for in structural design. Simplified approaches for such structures typically consider the Winkler foundation model, assuming Euler-Bernoulli beam theory, which neglects shearing-induced distortions, especially significant when shear waves are a dominant component of the seismic motion. In order to overcome these limitations, Timoshenko beam models have been proposed in the literature. These approaches however depend on an appropriate determination of the ground springs. Existing analytical formulations often assume plane-strain conditions, inadequate for representing low frequencies and thus are not directly applicable for pseudo-static interaction analyses. The present paper develops analytical solutions to determine transverse and rotation Winkler springs for structures subjected shear waves. The proposed springs overcome the drawbacks of plane-strain models and can be construed as a generalisation of them. The springs are obtained as a function of the seismic wavelength and the ground-structure stiffness contrast. Results obtained are validated against solutions from the literature and numerical results from a full 3D finite-element model. A non-dimensional parametric study is also presented, that allow an expedited evaluation of ground springs for practical applications.

List of symbols

As=

cross-sectional area

E=

elastic modulus of the soil

G=

shear modulus of the soil

Es=

elastic modulus of the structure

Gs=

shear modulus of the structure

Is=

cross-sectional moment of inertia

kS=

transverse spring under S-waves

=

rotation spring

L=

length of the structure

R=

soil reaction factor

r0=

cross-sectional radii of structure

u=

radial displacement

us=

structural displacement

uff=

free-field motion

uff0=

amplitude of free-field motion

v=

tangential displacement

VP=

compressional wave velocity of the medium

VS=

shear wave velocity of the medium

w=

longitudinal displacements

η=

compressibility factor

θ=

polar coordinate

λS=

seismic shear wavelength

ν=

Poisson’s coefficient of the soil

νs=

Poisson’s coefficient of the structure

σr=

radial normal stress

τrθ=

tangential shear stress

ω=

frequency of harmonic oscillation

ωS=

equivalent frequency for S-waves

φs=

sectional rotation

φs0=

amplitude of structural response in rotation

Disclosure statement

No potential conflict of interest was reported by the author(s).

Correction Statement

This article has been corrected with minor changes. These changes do not impact the academic content of the article.

Additional information

Funding

This work was supported by the Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET) and by the Secretaria de Ciencia y Tecnologia (SECyT) of the Universidad Nacional de Cordoba.

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