Simple formulas for the dynamic stiffness of pile groups - Laboratoire ...
Simple formulas for the dynamic stiffness of pile groups - Laboratoire ...
Simple formulas for the dynamic stiffness of pile groups - Laboratoire ...
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EARTHQUAKE ENGINEERING AND STRUCTURAL DYNAMICSEarthquake Engng Struct. Dyn. 2002; 00:1–6 Prepared using eqeauth.cls [Version: 2002/11/11 v1.00]<strong>Simple</strong> <strong><strong>for</strong>mulas</strong> <strong>for</strong> <strong>the</strong> <strong>dynamic</strong> <strong>stiffness</strong> <strong>of</strong> <strong>pile</strong> <strong>groups</strong>Reza Taherzadeh 1 , Didier Clouteau 1,∗ , Régis Cottereau 21 <strong>Laboratoire</strong> MSSMat, École Centrale Paris, CNRS UMR 8579, Grande Voie des Vignes, 92295Châtenay-Malabry, France2 International Center <strong>for</strong> Numerical Methods in Engineering (CIMNE), Universitat Politècnica deCatalunya, Jordi Girona 1-3, 08034 Barcelona, SpainSUMMARY<strong>Simple</strong> <strong><strong>for</strong>mulas</strong> are derived <strong>for</strong> <strong>the</strong> <strong>dynamic</strong> <strong>stiffness</strong> <strong>of</strong> <strong>pile</strong> group foundations subjected to horizontaland rocking <strong>dynamic</strong> loads. The <strong>for</strong>mulations are based on <strong>the</strong> construction <strong>of</strong> a general model <strong>of</strong>impedance matrices as <strong>the</strong> condensation <strong>of</strong> matrices <strong>of</strong> mass, damping and <strong>stiffness</strong>, and on <strong>the</strong>identification <strong>of</strong> <strong>the</strong> values <strong>of</strong> <strong>the</strong>se matrices on an extensive database <strong>of</strong> numerical experimentscomputed using coupled Finite Element-Boundary Element (FE-BE) models. The <strong>for</strong>mulationsobtained can be readily used <strong>for</strong> design <strong>of</strong> both floating <strong>pile</strong>s on homogeneous half-space and endbearing<strong>pile</strong>s, and are applicable <strong>for</strong> a wide range <strong>of</strong> mechanical and geometrical parameters <strong>of</strong> <strong>the</strong> soiland <strong>pile</strong>s, in particular <strong>for</strong> large <strong>pile</strong> <strong>groups</strong>. For <strong>the</strong> seismic design <strong>of</strong> a building, <strong>the</strong> use <strong>of</strong> <strong>the</strong> simple<strong><strong>for</strong>mulas</strong> ra<strong>the</strong>r than a full computational model is shown to induce little error on <strong>the</strong> evaluation <strong>of</strong><strong>the</strong> response spectra and time histories. Copyright 2002 John Wiley & Sons, Ltd.key words: Soil impedance matrix; <strong>pile</strong> group foundation; design <strong><strong>for</strong>mulas</strong>; lumped-parametermodels; hidden variables models1. INTRODUCTIONWhatever <strong>the</strong> mode <strong>of</strong> vibration, <strong>the</strong> <strong>dynamic</strong> <strong>stiffness</strong> <strong>of</strong> a <strong>pile</strong> group cannot be computedby simply adding <strong>the</strong> <strong>stiffness</strong>es <strong>of</strong> <strong>the</strong> individual <strong>pile</strong>s. Depending on <strong>the</strong> mechanical andgeometrical parameters <strong>of</strong> <strong>the</strong> soil and <strong>pile</strong>s, <strong>the</strong> <strong>dynamic</strong>al behavior <strong>of</strong> each <strong>pile</strong> can be heavilyinfluenced by that <strong>of</strong> its neighbors [1]. Among o<strong>the</strong>r phenomena, it is clear that <strong>the</strong> <strong>dynamic</strong>resonance <strong>of</strong> <strong>the</strong> soil constrained within a cluster <strong>of</strong> <strong>pile</strong>s cannot be modeled when <strong>the</strong> complex<strong>dynamic</strong> interaction between <strong>the</strong>se <strong>pile</strong>s is neglected.The main approach to solve this strongly coupled problem is <strong>the</strong> use <strong>of</strong> full numerical models,taking into account <strong>the</strong> soil and <strong>the</strong> <strong>pile</strong>s with equal rigor. This is however a computationallyvery demanding approach, in particular <strong>for</strong> large number <strong>of</strong> <strong>pile</strong>s, and has only been attemptedat, to <strong>the</strong> knowledge <strong>of</strong> <strong>the</strong> authors, by Kaynia [2], using <strong>the</strong> Boundary Element (BE) method.All o<strong>the</strong>r numerical methods in <strong>the</strong> literature seem to include some simplifying assumptions.∗ Correspondence to: didier.clouteau@ecp.frCopyright 2002 John Wiley & Sons, Ltd.
2 R. TAHERZADEH, D. CLOUTEAU & R. COTTEREAUFor example, <strong>the</strong> axisymetrical Finite Element (FE) model [3], <strong>the</strong> Ring-Pile model [4], or <strong>the</strong>closely-spaced plates model [5] can be used, when <strong>the</strong> geometrical layout <strong>of</strong> <strong>the</strong> <strong>pile</strong> group allows<strong>for</strong> it. The latter two approaches consist in grouping <strong>the</strong> <strong>pile</strong>s in concentric circles or soil-<strong>pile</strong>strippedupright plates, respectively, both allowing <strong>for</strong> an easier evaluation <strong>of</strong> <strong>the</strong> interactioneffects. Ano<strong>the</strong>r approach consists in replacing <strong>the</strong> <strong>pile</strong> group by a single equivalent uprightbeam [6]. In any case, <strong>the</strong>se approaches are not adapted to <strong>the</strong> needs <strong>of</strong> civil and structuralengineers, who need to design <strong>pile</strong> foundations with little recourse to computational tools.A more interesting approach <strong>for</strong> design purposes consists in providing analytical <strong><strong>for</strong>mulas</strong>,whose structure is usually derived from physical considerations, and with tabulized parameters,depending on <strong>the</strong> geometrical and mechanical parameters <strong>of</strong> <strong>the</strong> soil and <strong>pile</strong>s. The simplesttype <strong>of</strong> such approaches is based on Winkler’s spring model <strong>for</strong> <strong>the</strong> soil, <strong>for</strong> which radiationdamping and inertial effects are neglected [7, 8, 9]. A relatively simple method was proposed byGazetas and Dobry [18] <strong>for</strong> estimating <strong>the</strong> damping characteristics <strong>of</strong> horizontally loaded single<strong>pile</strong> in layered soil. Following Wolf’s approach [10] <strong>for</strong> <strong>the</strong> modeling <strong>of</strong> soil-structure interaction(SSI), o<strong>the</strong>r researchers [11, 12, 13, 14, 15, 16] have replaced <strong>the</strong> soil-<strong>pile</strong> system by a onedegree-<strong>of</strong>-freedom (DOF) mass, with a damper and a spring. Inertial effects and radiationdamping are <strong>the</strong>re<strong>for</strong>e taken into account to some extent but <strong>the</strong> general <strong>dynamic</strong>al behavior,and in particular <strong>the</strong> interaction between <strong>the</strong> different <strong>pile</strong>s, is heavily simplified. To improve<strong>the</strong>se models, Dobry and Gazetas [17] proposed an approximate <strong>for</strong>mulation accounting <strong>for</strong><strong>the</strong> interaction between <strong>the</strong> <strong>pile</strong>s, by modeling <strong>the</strong> waves emanating from each excited <strong>pile</strong>.The additional term is <strong>the</strong>re<strong>for</strong>e based on <strong>the</strong> computation <strong>of</strong> <strong>the</strong> propagation <strong>of</strong> a wave,supposed to be cylindrical, emanating from a single excited <strong>pile</strong> in a homogeneous domain.The method was fur<strong>the</strong>r refined by Gazetas and co-workers [19, 20, 21] to attempt to modelmultiple reflections within <strong>the</strong> <strong>pile</strong> group in layered soil. However, a few attempts have beenmade at accurately modeling <strong>the</strong> large <strong>pile</strong> group foundation, in particular <strong>for</strong> <strong>the</strong> complexfrequency-dependance <strong>of</strong> end-bearing <strong>pile</strong> foundations. (Konagai [6] provides <strong><strong>for</strong>mulas</strong> validonly <strong>for</strong> sway, Mylonakis and Gazetas [21] provide <strong><strong>for</strong>mulas</strong> valid <strong>for</strong> all movements but only<strong>for</strong> a group <strong>of</strong> nine <strong>pile</strong>s and Nikolaou et al. [40] provide <strong>for</strong> kinematic <strong>pile</strong> bending <strong>for</strong> a group<strong>of</strong> twenty <strong>pile</strong>s).Despite <strong>the</strong> significant progress in <strong>pile</strong> <strong>dynamic</strong>s [22], <strong>the</strong>re is <strong>the</strong>re<strong>for</strong>e still a need <strong>for</strong> simpleengineering procedures <strong>for</strong> <strong>the</strong>ir design, following <strong>the</strong> example <strong>of</strong> <strong>the</strong> code provisions developed<strong>for</strong> <strong>the</strong> seismic design on spread footings [23, 24]. This paper aims at providing such <strong><strong>for</strong>mulas</strong>,to be used <strong>for</strong> both small and large <strong>pile</strong> <strong>groups</strong>, as well as <strong>for</strong> both floating <strong>pile</strong> <strong>groups</strong> onhomogeneous half-space and end-bearing <strong>pile</strong> <strong>groups</strong>. The main novelty <strong>of</strong> this paper is that<strong>the</strong> <strong><strong>for</strong>mulas</strong> are valid over a range <strong>of</strong> parameters larger than <strong><strong>for</strong>mulas</strong> previously availablein <strong>the</strong> literature (see above references). They can be used <strong>for</strong> large numbers <strong>of</strong> <strong>pile</strong>s. This ismade possible by <strong>the</strong> use <strong>of</strong> a very general <strong>dynamic</strong> model <strong>for</strong> <strong>the</strong> representation <strong>of</strong> <strong>stiffness</strong>impedance matrices, <strong>the</strong> hidden state variable model (Sec. 3.1). The parameters appearing inthis model are <strong>the</strong>n fitted using an extensive database <strong>of</strong> full coupled FE-BE computations<strong>of</strong> soil-<strong>pile</strong> systems (Sec. 3.2). The sway and rocking <strong>of</strong> <strong>the</strong> foundation are accounted <strong>for</strong>, ina large range <strong>of</strong> parameters <strong>of</strong> <strong>the</strong> soil and <strong>pile</strong>s, and <strong>the</strong> <strong><strong>for</strong>mulas</strong> are given independently<strong>for</strong> floating (Sec. 4.1) and end-bearing <strong>pile</strong>s (Sec. 4.2). Fur<strong>the</strong>r, <strong>for</strong> <strong>the</strong> seismic design <strong>of</strong> abuilding, <strong>the</strong> use <strong>of</strong> <strong>the</strong> simple <strong><strong>for</strong>mulas</strong> ra<strong>the</strong>r than a full computational model is shown toinduce little error on <strong>the</strong> evaluation <strong>of</strong> <strong>the</strong> response spectra and time histories (Sec. 5).The reader interested in a fast use <strong>of</strong> <strong>the</strong> <strong><strong>for</strong>mulas</strong> can refer directly, <strong>for</strong> a floating <strong>pile</strong>group on homogeneous half-space (respectively, an end-bearing <strong>pile</strong> group) to Table II (resp.,Copyright¡2002 John Wiley & Sons, Ltd. Earthquake Engng Struct. Dyn. 2002; 00:1–6Prepared using eqeauth.cls
SIMPLE FORMULAS FOR THE DYNAMIC STIFFNESS OF PILE GROUPS 3Figure 1. Definition <strong>of</strong> <strong>pile</strong> group foundation.Table IV), <strong>the</strong> coefficients <strong>of</strong> which are to be used in Eq. (9) and (8) (resp., Eq. (14) and (10)).In <strong>the</strong>se equations, both <strong>the</strong> <strong>dynamic</strong> <strong>stiffness</strong> and <strong>the</strong> frequency are normalized, as describedin Sec. 2.2.2. THE IMPEDANCE MATRIX OF A PILE GROUP: DEFINITION AND NOTATIONSIn this section, we introduce <strong>the</strong> main notations and define <strong>the</strong> impedance matrix <strong>of</strong> a <strong>pile</strong>group. The normalizations, that will be used throughout <strong>the</strong> paper, <strong>of</strong> both <strong>the</strong> impedanceand <strong>the</strong> frequency, are also introduced.2.1. NotationsIn all <strong><strong>for</strong>mulas</strong>, <strong>the</strong> indices “s” and “p” will refer to <strong>the</strong> soil and <strong>the</strong> <strong>pile</strong>s, respectively. Whenconsidering two layers <strong>of</strong> soil, <strong>the</strong> top layer will still be denoted “s” while <strong>the</strong> bedrock willbe denoted “b”. E s , ν s , G s , and ρ s (respectively, E p , ν p , G p , ρ p , and E b , ν b , G b , ρ b ) hencedenote Young’s modulus, Poisson’s ratio, <strong>the</strong> shear modulus, and <strong>the</strong> unit mass <strong>of</strong> <strong>the</strong> soil(respectively, <strong>of</strong> <strong>the</strong> <strong>pile</strong>s, and <strong>of</strong> <strong>the</strong> bedrock). V s and β s (resp., V b and β b ) denote <strong>the</strong> shearwave velocity and <strong>the</strong> hysteretic damping <strong>of</strong> <strong>the</strong> soil (resp., <strong>of</strong> <strong>the</strong> bedrock). All <strong>the</strong> <strong>pile</strong>s ina group are supposed identical, with a diameter d, a length l p , an inertial moment I p , and<strong>the</strong>y are separated from each o<strong>the</strong>r by a distance s (see Fig. 1). They are rigidly attached toa mass-less square cap with a half-width B f , which is supposed to have no contact with <strong>the</strong>soil. Fur<strong>the</strong>r we define L 0 = (E p I p /E s ) 0.25 , closely related to <strong>the</strong> critical <strong>pile</strong> length definedby several authors [25, 26] and an equivalent radius <strong>for</strong> <strong>the</strong> cap R f = 2B f / √ π.Two cases will be considered in this paper: (1) floating <strong>pile</strong> <strong>groups</strong> on homogeneous halfspace,and (2) end-bearing <strong>pile</strong> <strong>groups</strong>. In <strong>the</strong> <strong>for</strong>mer case, <strong>the</strong> soil is a homogeneous half-space,while, in <strong>the</strong> latter case, <strong>the</strong> soil is composed <strong>of</strong> a layer <strong>of</strong> thickness H, resting over a bedrock,in which <strong>the</strong> tips <strong>of</strong> <strong>the</strong> <strong>pile</strong>s are embedded (l p > H).2.2. Impedance matrixThe impedance matrix or <strong>dynamic</strong> <strong>stiffness</strong> matrix Z(ω) <strong>of</strong> a <strong>pile</strong> group relates <strong>the</strong> vector <strong>of</strong><strong>for</strong>ces and moments applied on <strong>the</strong> rigid cap at <strong>the</strong> top <strong>of</strong> <strong>the</strong> <strong>pile</strong>s to <strong>the</strong> resulting vector <strong>of</strong>Copyright¡2002 John Wiley & Sons, Ltd. Earthquake Engng Struct. Dyn. 2002; 00:1–6Prepared using eqeauth.cls
4 R. TAHERZADEH, D. CLOUTEAU & R. COTTEREAUdisplacements and rotations at <strong>the</strong> same point. Since <strong>the</strong> rigid cap is supposed to be square,symmetry considerations ensure that <strong>the</strong> impedance matrix, in <strong>the</strong> basis <strong>of</strong> <strong>the</strong> rigid bodymovements <strong>of</strong> <strong>the</strong> <strong>pile</strong> cap, is not full. More precisely, only <strong>the</strong> diagonal terms, and <strong>the</strong> couplingterms between <strong>the</strong> sway along one <strong>of</strong> <strong>the</strong> axes <strong>of</strong> symmetry and <strong>the</strong> rotation around <strong>the</strong> o<strong>the</strong>rone, are non-null. Besides, <strong>the</strong> two horizontal axes <strong>of</strong> symmetry are equivalent, so that <strong>the</strong>corresponding terms in <strong>the</strong> impedance matrix are equal. Hence, only five elements should beconsidered: horizontal, rocking, pumping, torsion, and horizontal-rocking coupling. Finally, asis usually done in earthquake engineering, we disregard <strong>the</strong> pumping and torsion terms as lesssignificant, and <strong>the</strong>re<strong>for</strong>e write <strong>the</strong> impedance as[ ]Zh (ω) ZZ(ω) = hr (ω), (1)Z hr (ω) Z r (ω)where Z h (ω), Z r (ω) and Z hr (ω) are, respectively, <strong>the</strong> horizontal, rocking, and coupling elements.To simplify <strong>the</strong> comparisons between different soils and/or foundation sizes, it is customaryin foundation design [27, 29] to normalize <strong>the</strong> impedance matrix by a constant static <strong>stiffness</strong>matrix K 0 , given here by[ ]Gs RK 0 = f 00 G s Rf3 . (2)It is also classical to use a dimensionless frequency a 0 = ωR f /V s , where ω is <strong>the</strong> circularfrequency. The impedance matrix is finally writtenZ(a 0 ) = K 1/20¯Z(a 0 )K 1/20 , (3)where <strong>the</strong> tilde symbol¯refers to normalised quantities.Note that <strong>the</strong> imaginary part <strong>of</strong> <strong>the</strong> impedance matrix is sometimes plotted in <strong>the</strong> literatureafter a division by ω. While this is interesting in <strong>the</strong> simple cases where that imaginary partremains more or less linear, such as <strong>for</strong> circular rigid foundations over homogeneous soils, it isnot relevant here, so that that custom will not be followed in <strong>the</strong> plots <strong>of</strong> this paper.3. PRINCIPLE OF THE COMPUTATION OF SIMPLE FORMULASAs described in <strong>the</strong> introduction, <strong>the</strong>re is an engineering need <strong>for</strong> simple <strong>for</strong>mulations <strong>of</strong> <strong>the</strong>impedance matrix <strong>of</strong> large <strong>pile</strong> <strong>groups</strong>. The goal is to avoid using complicated and timeconsumingcomputational models, while retaining <strong>the</strong>ir accuracy. The usual approach to <strong>the</strong>derivation <strong>of</strong> <strong>the</strong>se simple <strong>for</strong>mulations consists in two steps:1. choose a structure <strong>for</strong> <strong>the</strong> <strong>for</strong>mulation, usually based on physical considerations andsimplifying assumptions2. set <strong>the</strong> values <strong>of</strong> <strong>the</strong> parameters <strong>for</strong> a range <strong>of</strong> soil and <strong>pile</strong> group characteristics, usuallyprovided in a tabulized <strong>for</strong>m.In <strong>the</strong> literature (see <strong>the</strong> introduction <strong>for</strong> references), <strong>the</strong> first step is basically a decision <strong>of</strong> <strong>the</strong>designer, which, however, conditions in a large part <strong>the</strong> quality <strong>of</strong> <strong>the</strong> <strong>for</strong>mulation. We <strong>the</strong>re<strong>for</strong>echoose here a more rational approach, in which no specific structure is chosen a priori, andmake use <strong>of</strong> <strong>the</strong> so-called ”hidden variables model” <strong>of</strong> <strong>the</strong> impedance matrix [35, 36]. Theidentification <strong>of</strong> <strong>the</strong> parameters <strong>of</strong> <strong>the</strong> final <strong><strong>for</strong>mulas</strong> is <strong>the</strong>n per<strong>for</strong>med by regression from aCopyright¡2002 John Wiley & Sons, Ltd. Earthquake Engng Struct. Dyn. 2002; 00:1–6Prepared using eqeauth.cls
SIMPLE FORMULAS FOR THE DYNAMIC STIFFNESS OF PILE GROUPS 5database <strong>of</strong> FE-BE computations. Note that <strong>the</strong> hidden state variable model that is chosenhere might appear more ma<strong>the</strong>matically than previous <strong>for</strong>mulations found in <strong>the</strong> literature.However, remember that this structure is just an intermediate state that allows to find <strong>the</strong>final <strong><strong>for</strong>mulas</strong> that will eventually be used by <strong>the</strong> engineers. In section 4, we will see someanalogies between <strong>the</strong> <strong><strong>for</strong>mulas</strong> proposed, and mechanical systems created as sets <strong>of</strong> spring,dampers and masses. The differences with lumped parameters is that with <strong>the</strong> hidden statevariables model, <strong>the</strong> equivalent mechanical model comes out naturally as a consequence <strong>of</strong> <strong>the</strong>regression, ra<strong>the</strong>r than being chosen a priori.3.1. The hidden variables modelThe construction <strong>of</strong> <strong>the</strong> hidden variables model <strong>of</strong> an impedance matrix is based on <strong>the</strong>supposition that, besides <strong>the</strong> n Γ physical DOFs on which <strong>the</strong> impedance is defined (typically<strong>the</strong> rigid-body modes <strong>of</strong> <strong>the</strong> cap <strong>of</strong> <strong>the</strong> <strong>pile</strong> group), <strong>the</strong>re exists n I additional DOFs thatrepresent some internal resonance phenomena inside <strong>the</strong> soil and <strong>the</strong> <strong>pile</strong> group. The resonancemodes corresponding to <strong>the</strong>se DOFs cannot be physically identified, as only <strong>the</strong>ir influence on<strong>the</strong> impedance matrix is observable, so <strong>the</strong> DOFs are referred to as “hidden”, or ”inner”.With respect to <strong>the</strong> n = n Γ + n I DOFs, matrices <strong>of</strong> mass M, damping D, and <strong>stiffness</strong> Kcan <strong>the</strong>n be identified, and <strong>the</strong> <strong>dynamic</strong> <strong>stiffness</strong> matrix S(a 0 ) is defined asS(a 0 ) = (K − a 2 0M) + ia 0 C. (4)The impedance matrix corresponding to <strong>the</strong> hidden variables model is <strong>the</strong>n <strong>the</strong> condensationon <strong>the</strong> n Γ physical DOFs <strong>of</strong> <strong>the</strong> <strong>stiffness</strong> matrix S(a 0 ). More specifically, introducing <strong>the</strong> blockdecomposition <strong>of</strong> Eq. (4),[SΓ (a 0 ) S c (a 0 )S T c (a 0 ) S I (a 0 )]=<strong>the</strong> impedance matrix is defined as([ ] [ ]) [ ]KΓ K cK T − a 2 MΓ M c CΓ Cc K0 I M T + ia cc M 0I C T , (5)c C IZ(a 0 ) = S Γ (a 0 ) − S c (a 0 )S −1I(a 0 )S T c (a 0 ). (6)As <strong>the</strong> hidden variables are not necessarily physical DOFs, but ra<strong>the</strong>r state variables in<strong>the</strong> background <strong>of</strong> <strong>the</strong> physical model, <strong>the</strong> matrices M, D, and K are really generalized mass,damping and <strong>stiffness</strong> matrices and do not correspond a priori with <strong>the</strong> classical mass, dampingand <strong>stiffness</strong> matrices, or to those obtained through <strong>the</strong> application <strong>of</strong> some modal reductiontechnique. Ano<strong>the</strong>r equivalent <strong>for</strong>m <strong>of</strong> <strong>the</strong> hidden variables model can be derived [35], where<strong>the</strong> hidden parts <strong>of</strong> <strong>the</strong> matrices are diagonal, and with no coupling in mass. In that case, <strong>the</strong>impedance can be written∑n hZ(a 0 ) = (K Γ − a 2 (ia 0 C l c + K l0M Γ ) + ia 0 C Γ −c)(ia 0 C l c + K l c) T(kI l − a2 0 ml I ) + ia 0c l Iwhere C l c and K l c are <strong>the</strong> l th columns <strong>of</strong> C c and K c , and m l I , cl I and kl I are <strong>the</strong> diagonalelements <strong>of</strong> M I , C I and K I .The main interest <strong>of</strong> this hidden variables model is its generality. Its structure makes itsuitable <strong>for</strong> <strong>the</strong> representation <strong>of</strong> any type <strong>of</strong> impedance matrix, provided that an appropriatenumber <strong>of</strong> hidden variables is used. Note that <strong>the</strong> numerical identification <strong>of</strong> <strong>the</strong> matrices M,l=1(7)Copyright¡2002 John Wiley & Sons, Ltd. Earthquake Engng Struct. Dyn. 2002; 00:1–6Prepared using eqeauth.cls
6 R. TAHERZADEH, D. CLOUTEAU & R. COTTEREAUC, and K is entirely per<strong>for</strong>med from <strong>the</strong> knowledge only <strong>of</strong> <strong>the</strong> impedance matrix, and that<strong>the</strong> number <strong>of</strong> hidden variables can be automatically chosen based on a precision criteria <strong>for</strong><strong>the</strong> approximation <strong>of</strong> <strong>the</strong> impedance matrix [39, 35, 36].Contrary to <strong>the</strong> lumped-parameter models <strong>of</strong> <strong>the</strong> impedance matrix [28], in which <strong>the</strong>identification <strong>of</strong> <strong>the</strong> mechanical elements yields negative values <strong>of</strong> <strong>the</strong> springs, dashpots, and/ormasses, in <strong>the</strong> hidden state variable model, <strong>the</strong> causality and stability <strong>of</strong> <strong>the</strong> soil impedancematrix are directly related to <strong>the</strong> positivity <strong>of</strong> M, K and C. In o<strong>the</strong>r words, in comparisonwith lumped parameter models, <strong>the</strong> diagnosis <strong>of</strong> unphysical models is very natural .In <strong>the</strong> next section, <strong>the</strong> numerical method that is used to derive <strong>the</strong> reference impedancematrices, and to identify <strong>the</strong> parameters <strong>of</strong> <strong>the</strong> <strong><strong>for</strong>mulas</strong>, is described. The methodology <strong>for</strong><strong>the</strong> identification <strong>of</strong> <strong>the</strong> hidden variables model <strong>of</strong> a given impedance matrix is also describedin App. 6.3.2. The reference FE-BE modelWe suppose, <strong>for</strong> <strong>the</strong> reference computations, that both <strong>the</strong> soil and <strong>the</strong> <strong>pile</strong>s behave linearlyand that <strong>the</strong> contact between <strong>the</strong> <strong>pile</strong>s and <strong>the</strong> soil is continuous in all directions, without anyslippage or gap. The elasto<strong>dynamic</strong> equations are <strong>the</strong>re<strong>for</strong>e linear. The numerical approachused to derive <strong>the</strong> reference results <strong>for</strong> <strong>the</strong> calibration <strong>of</strong> <strong>the</strong> simple <strong>for</strong>mulations is basedon an efficient FE-BE coupling technique that is described in detail in [30, 31] and is brieflyrecalled below.The soil is separated into two blocks: one, bounded and containing <strong>the</strong> <strong>pile</strong>s, which is modeledby <strong>the</strong> FE method, and <strong>the</strong> o<strong>the</strong>r, surrounding <strong>the</strong> previous one, which is modeled by <strong>the</strong> BEmethod (see Fig. 2). Within <strong>the</strong> FE block, <strong>the</strong> <strong>pile</strong>s are modeled as Bernouilli beam elements.The two blocks are <strong>the</strong>n assembled using <strong>the</strong> Craig-Bampton coupling technique [32], so as tolower <strong>the</strong> computational cost, which may reach high levels <strong>for</strong> large <strong>pile</strong> <strong>groups</strong>. This numericalmodel was already validated <strong>for</strong> <strong>stiffness</strong> problems taken from <strong>the</strong> literature (in particular [2])and <strong>the</strong> results are given in [31]. However, <strong>the</strong>se validation results only concerned floating<strong>pile</strong> <strong>groups</strong> on homogeneous half-spaces so that we present here a comparison, on a particularexample, <strong>of</strong> <strong>the</strong> FE-BE model with <strong>the</strong> BE approach described in [34].We <strong>the</strong>re<strong>for</strong>e consider a 4 × 9 <strong>pile</strong> group embedded in a soil with two layers (see Fig. 2).The <strong>pile</strong>s have a Young’s modulus <strong>of</strong> 25 GPa, a diameter <strong>of</strong> d = 1.3 m and are separated bys = 2.6 m. The first layer <strong>of</strong> soil is H = 9.5 m-thick, and is <strong>for</strong>med <strong>of</strong> a very s<strong>of</strong>t saturatedorganic clay with S-wave velocity V s = 80 m/s, unit mass ρ s = 1.5 Mg/m 3 and Poisson’s ratioν s = 0.49. The lower layer <strong>of</strong> soil is a stiff sand with S-wave velocity V d = 300 m/s, unit massρ d = 2 Mg/m 3 and Poisson’s ratio ν d = 0.4, in which <strong>the</strong> <strong>pile</strong>s penetrate 6 m. In both layers<strong>the</strong> hysteretic damping is taken as β s = β d = 0.05. As seen on Fig. 2, <strong>the</strong> agreement between<strong>the</strong> results in <strong>the</strong> two numerical approaches is very good.It should be noted that <strong>the</strong> frequency-dependance <strong>of</strong> <strong>pile</strong> <strong>groups</strong> is particularly sensitive to<strong>the</strong> number <strong>of</strong> <strong>pile</strong>s and to its character <strong>of</strong> floating or end-bearing. The <strong>dynamic</strong> <strong>stiffness</strong> <strong>of</strong>single <strong>pile</strong>s and <strong>pile</strong> <strong>groups</strong> with a small number <strong>of</strong> <strong>pile</strong>s is nearly independent <strong>of</strong> frequency [33],while that <strong>of</strong> larger <strong>pile</strong> <strong>groups</strong> may show large variations with frequency. Likewise, <strong>the</strong> behavior<strong>of</strong> end-bearing <strong>pile</strong> <strong>groups</strong> is much more erratic with frequency than that <strong>of</strong> floating <strong>pile</strong> <strong>groups</strong>on homogeneous half-space. These physical results are retrieved with <strong>the</strong> FE-BE approach andan example <strong>of</strong> such comparison is shown in Fig. 3. These results were obtained considering <strong>the</strong>sample number 4 in Tables I and III.Copyright¡2002 John Wiley & Sons, Ltd. Earthquake Engng Struct. Dyn. 2002; 00:1–6Prepared using eqeauth.cls
SIMPLE FORMULAS FOR THE DYNAMIC STIFFNESS OF PILE GROUPS 7Dynamic <strong>stiffness</strong> [N/m]0−2−4−60 2 4 6 8 102 x Frequency [Hz]Damping [N/m]64200 2 4 6 8 108 x Frequency [Hz]Figure 2. FE model (left) <strong>of</strong> <strong>the</strong> 4 × 9 <strong>pile</strong> group within a block <strong>of</strong> soil andcomparison <strong>of</strong> <strong>the</strong> real (right, up) and imaginary (right, down) parts <strong>of</strong> <strong>the</strong>horizontal impedance computed using <strong>the</strong> FE-BE model (solid line) and <strong>the</strong> BEmodel (dashed line) [34].3060Normalized Real Part [−]20100−10−20Normalized Imaginary Part [−]5040302010−300 1 2 3 4 5 6Dimensionless Frequency [−]00 1 2 3 4 5 6Dimensionless Frequency [−]Figure 3. Real (left) and imaginary (right) parts <strong>of</strong> <strong>the</strong> normalized horizontalimpedance matrix, <strong>for</strong> floating (solid line) and end-bearing (dashed line) <strong>pile</strong><strong>groups</strong>.It is also interesting to note, on Fig. 3, <strong>for</strong> <strong>the</strong> end-bearing <strong>pile</strong> group, that <strong>the</strong> imaginarypart <strong>of</strong> <strong>the</strong> impedance (it is also true <strong>for</strong> <strong>the</strong> rocking term, not shown here) present a small andalmost constant value below some cut-<strong>of</strong>f frequency, which is <strong>the</strong> resonance frequency <strong>of</strong> <strong>the</strong>top layer <strong>of</strong> soil. Indeed, <strong>for</strong> very low frequencies, surface waves cannot build up in that toplayer and take energy away from <strong>the</strong> foundation, so that <strong>the</strong> radiation damping is very low.Above that cut-<strong>of</strong>f frequency, a large peak can be observed on <strong>the</strong> imaginary part (with <strong>the</strong>real part almost cancelling), indicating a resonance within <strong>the</strong> soil, that tends to soak energyaway from <strong>the</strong> foundation.4. COMPUTATION OF SIMPLE FORMULAS FOR PILE GROUPSIn this section, we present <strong>the</strong> derivation <strong>of</strong> <strong>the</strong> simple <strong><strong>for</strong>mulas</strong> in <strong>the</strong> cases <strong>of</strong> <strong>the</strong> floating<strong>pile</strong> <strong>groups</strong> on homogeneous half-space and end-bearing <strong>pile</strong> <strong>groups</strong>, and using <strong>the</strong> ideasCopyright¡2002 John Wiley & Sons, Ltd. Earthquake Engng Struct. Dyn. 2002; 00:1–6Prepared using eqeauth.cls
8 R. TAHERZADEH, D. CLOUTEAU & R. COTTEREAU1050Normalized Real Part [−]50−5−10Normalized Imaginary Part [−]40302010−150 1 2 3 4 5 6Dimensionless Frequency [−]00 1 2 3 4 5 6Dimensionless Frequency [−]Figure 4. Real (left) and imaginary (right) parts <strong>of</strong> <strong>the</strong> horizontal impedancematrix <strong>for</strong> different <strong>pile</strong> separations: s/d = 2 (solid line), s/d = 2.5 (dashed line)and s/d = 3.5 (solid-dashed line). The figures correspond to a 15 × 15 <strong>pile</strong> groupwith E p/E s = 300 and R f /l p = 1.1.2060Normalized Real Part [−]100−10−20−30Normalized Imaginary Part [−]5040302010−400 1 2 3 4 5 6Dimensionless Frequency [−]00 1 2 3 4 5 6Dimensionless Frequency [−]Figure 5. Real (left) and imaginary (right) parts <strong>of</strong> <strong>the</strong> rocking term <strong>of</strong> <strong>the</strong><strong>dynamic</strong> <strong>stiffness</strong> matrix <strong>for</strong> different <strong>pile</strong> separations: R f /l p = 0.7 (solid line),R f /l p = 0.65 (dashed line) and R f /l p = 0.55 (solid-dashed line). The figurescorrespond to a 14 × 14 <strong>pile</strong> group with E p/E s = 375 and s/d = 2.discussed above. Depending on <strong>the</strong> type <strong>of</strong> <strong>pile</strong> group, and on <strong>the</strong> type <strong>of</strong> element <strong>of</strong> <strong>the</strong>impedance matrix, more or less hidden variables are necessary to describe its behavior, and,correspondingly, more or less parameters are needed in <strong>the</strong> <strong><strong>for</strong>mulas</strong>.4.1. Floating <strong>pile</strong> <strong>groups</strong>We first consider floating <strong>pile</strong> <strong>groups</strong> embedded in a homogeneous half-space. In that case,<strong>the</strong> variation <strong>of</strong> <strong>the</strong> <strong>dynamic</strong> <strong>stiffness</strong> with <strong>the</strong> frequency is ra<strong>the</strong>r smooth, as seen in Fig. 4and 5. More precisely, <strong>the</strong> <strong>dynamic</strong> <strong>stiffness</strong> always has a parabolic variation while <strong>the</strong> dampingcoefficient is approximately linear. The parabolic decrease <strong>of</strong> <strong>the</strong> real part seems to indicatethat a mass remains entrapped between <strong>the</strong> <strong>pile</strong>s and vibrates in-phase with <strong>the</strong> cap.The hidden variables model predicts in all cases in <strong>the</strong> database (described in Table I) atwo-DOFs system, one <strong>for</strong> <strong>the</strong> sway and one <strong>for</strong> <strong>the</strong> rocking, and with no hidden variables. NoteCopyright¡2002 John Wiley & Sons, Ltd. Earthquake Engng Struct. Dyn. 2002; 00:1–6Prepared using eqeauth.cls
SIMPLE FORMULAS FOR THE DYNAMIC STIFFNESS OF PILE GROUPS 9Table I. The database <strong>of</strong> soil-<strong>pile</strong> group systems used to derive <strong>the</strong> simple<strong>for</strong>mulations <strong>for</strong> floating <strong>pile</strong> <strong>groups</strong> on homogeneous half-space. The range <strong>of</strong>parameters is 250 ≤ E p/E s ≤ 1500, 2 ≤ s/d p ≤ 3.6 and 0.55 ≤ R f /l p ≤ 2 andconstant hysteric damping β s = 0.05.Sample Piles E p d E s B f l p s V s[-] [GPa] [m] [GPa] [m] [m] [m] [m/s]1 8 × 8 30 1 0.1 15 18 3.3 1402 11 × 11 30 1 0.1 20 18 3.3 1403 16 × 16 30 1 0.1 30 18 3.3 1404 13 × 13 40 1 0.08 20 24 2.8 1305 13 × 13 30 1 0.08 20 24 2.8 1306 13 × 13 20 1 0.08 20 24 2.8 1307 15 × 15 25 1.3 0.08 20 18 2.5 1308 15 × 15 25 1 0.08 20 18 2.5 1309 15 × 15 25 0.7 0.08 20 18 2.5 13010 18 × 18 30 1 0.02 25 14 2.6 6011 18 × 18 30 1 0.08 25 14 2.6 13012 18 × 18 30 1 0.1 25 14 2.6 14013 16 × 16 30 1 0.08 15 28 2.0 13014 16 × 16 30 1 0.08 15 20 2.0 13015 16 × 16 30 1 0.08 15 14 2.0 130that <strong>the</strong> coupling term is negligible. On Fig. 6, a schematic drawing <strong>of</strong> a system correspondingto such impedance is presented. The superstructure is subjected to <strong>the</strong> seismic horizontal <strong>for</strong>cef s . The elements <strong>of</strong> <strong>the</strong> normalized impedance can <strong>the</strong>re<strong>for</strong>e be written⎧⎪⎨˜Z h (a 0 ) = (˜k h − a 2 0 ˜m h ) + ia 0˜c h˜Z r (a 0 ) = (˜k r − a⎪⎩2 0 ˜m r ) + ia 0˜c r˜Z sr (a 0 ) = 0, (8)where <strong>the</strong> values <strong>of</strong> ˜k h , ˜c h , ˜m h , ˜k r , ˜c r and ˜m r depend on <strong>the</strong> case considered. Remember that<strong>the</strong> definition <strong>of</strong> <strong>the</strong> normalized frequency a 0 is given in Sec. 2.2 and that <strong>the</strong> normalizedvalues in <strong>the</strong>se <strong><strong>for</strong>mulas</strong> (8) must be scaled by <strong>the</strong> static <strong>stiffness</strong> to yield <strong>the</strong> actual value <strong>of</strong><strong>the</strong> impedance matrix, as described in Sec. 2.2.In previous works, <strong>the</strong> leading parameters <strong>for</strong> this type <strong>of</strong> <strong>pile</strong> <strong>groups</strong> were identified to be<strong>the</strong> ratio <strong>of</strong> Young’s moduli E p /E s and <strong>the</strong> normalized separation <strong>of</strong> <strong>the</strong> <strong>pile</strong>s s/d [2, 37], or <strong>the</strong>factor L 0 = (E p I p /E s ) 0.25 related to <strong>the</strong> active <strong>pile</strong> length [38, 25, 26]. We decide here to use asleading parameters <strong>the</strong> normalized radius <strong>of</strong> <strong>the</strong> foundation R f /l p and a normalized active <strong>pile</strong>length ratio L 0 /s. We <strong>the</strong>re<strong>for</strong>e provide equations <strong>of</strong> <strong>the</strong> parameters χ ∈ {˜k h , ˜c h , ˜m h , ˜k r , ˜c r , ˜m r }Copyright¡2002 John Wiley & Sons, Ltd. Earthquake Engng Struct. Dyn. 2002; 00:1–6Prepared using eqeauth.cls
10 R. TAHERZADEH, D. CLOUTEAU & R. COTTEREAUFigure 6. A schematic drawing <strong>of</strong> a simple model <strong>for</strong> floating <strong>pile</strong> group.in <strong>the</strong> <strong>for</strong>m( ) λ1( ) λ2 Rf L0χ = λ 0 , (9)l p swith <strong>the</strong> values <strong>of</strong> λ 0 , λ 1 and λ 2 being provided <strong>for</strong> each <strong>of</strong> <strong>the</strong> parameters. A multiple regressionanalysis was <strong>the</strong>n conducted with respect to <strong>the</strong> two quantities R f /l p and L 0 /s, and lead to<strong>the</strong> values described in Table II. The regression coefficient R is also indicated in <strong>the</strong> same tableto provide an indicator <strong>of</strong> <strong>the</strong> accuracy <strong>of</strong> <strong>the</strong> regression analysis.In general terms, <strong>the</strong> <strong><strong>for</strong>mulas</strong> in Table II corroborate <strong>the</strong> observed results that, <strong>for</strong> shortseparations between <strong>the</strong> <strong>pile</strong>s, and <strong>for</strong> weak soils, both normalized <strong>dynamic</strong> <strong>stiffness</strong> anddamping increase. Note that, as indicated by <strong>the</strong> zeros in Table II, <strong>the</strong> influence <strong>of</strong> <strong>the</strong> ratioR f /l p on <strong>the</strong> horizontal impedance is negligible, while it is ra<strong>the</strong>r important <strong>for</strong> <strong>the</strong> rockingterm. Besides <strong>the</strong> uni<strong>for</strong>m presentation in Table II, <strong>the</strong> reader may also find an expanded,non-normalized, version <strong>of</strong> <strong>the</strong> same <strong><strong>for</strong>mulas</strong> in App. 6, <strong>for</strong> easier reading.4.2. End-bearing <strong>pile</strong> <strong>groups</strong>We <strong>the</strong>n consider end-bearing <strong>pile</strong> <strong>groups</strong>. As stated earlier, <strong>the</strong>ir <strong>dynamic</strong>al behavior is muchmore complicated than that <strong>of</strong> floating <strong>pile</strong> <strong>groups</strong> on homogeneous half-space. The structure<strong>of</strong> <strong>the</strong> approximation <strong>for</strong> <strong>the</strong> impedance matrix is <strong>the</strong>re<strong>for</strong>e difficult to guess a priori and weuse <strong>the</strong> hidden variables model in a very general setting. Note that, as <strong>the</strong> coupling term isnegligible in <strong>the</strong> cases considered, <strong>the</strong> hidden variables model was identified independently on<strong>the</strong> horizontal and rocking terms <strong>of</strong> <strong>the</strong> impedance matrix.The identification <strong>of</strong> <strong>the</strong> hidden variables model <strong>for</strong> all <strong>the</strong> cases in <strong>the</strong> database describedin Table IV suggest <strong>the</strong> consideration <strong>of</strong> three hidden variables <strong>for</strong> <strong>the</strong> sway and none <strong>for</strong> <strong>the</strong>rocking. Besides, no coupling in <strong>the</strong> <strong>stiffness</strong> <strong>for</strong> <strong>the</strong> first hidden variable and no coupling in <strong>the</strong>damping <strong>for</strong> <strong>the</strong> two o<strong>the</strong>rs seemed to be necessary. The chosen structure <strong>for</strong> <strong>the</strong> end-bearingCopyright¡2002 John Wiley & Sons, Ltd. Earthquake Engng Struct. Dyn. 2002; 00:1–6Prepared using eqeauth.cls
SIMPLE FORMULAS FOR THE DYNAMIC STIFFNESS OF PILE GROUPS 11Table II. Coefficients <strong>for</strong> <strong>the</strong> horizontal and rocking elements <strong>of</strong> <strong>the</strong> impedance <strong>of</strong>a floating <strong>pile</strong> <strong>groups</strong> on homogeneous half-space.( ) λ1 Rf(χ = λL0) λ20 l p s λ0 λ 1 λ 2 R [%]˜k h 6.8 0 0.3 80˜c h 5 0 0.5 90˜m h 0.4 0 1.6 86˜k r 8 -0.6 0.4 83˜c r 5 -0.5 0.2 72˜m r = ˜m h leq/4 2 0.7 -1 0.4 96<strong>pile</strong> <strong>groups</strong> is <strong>the</strong>re<strong>for</strong>e written, as a special case <strong>of</strong> Eq. (7) <strong>for</strong> <strong>the</strong> hidden variables model,⎧⎪⎨˜Z h (a 0 ) = (˜k h − a 2 a0 ˜m h ) + ia 0˜c h +2 0˜c2 1˜k−2 2˜k−2 3(˜k 1−a 2 0 ˜m1)+ia0˜c1 (˜k 2−a 2 0 ˜m2)+ia0˜c2 (˜k 3−a 2 0˜Z ˜m3)+ia0˜c3r (a 0 ) = (˜k r − a 2 0 ˜m r ) + ia 0˜c r,⎪⎩ ˜Z sr (a 0 ) = 0(10)and represented as a set <strong>of</strong> mass, springs, and dampers in Fig. 7. The previous observation <strong>for</strong><strong>the</strong> coupling with <strong>the</strong> hidden variables can be translated in Fig. 7 by <strong>the</strong> fact <strong>the</strong> mass m 1 islinked to <strong>the</strong> foundation by a dashpot while <strong>the</strong> masses m 2 and m 3 are linked to it throughsprings. This fact arises from <strong>the</strong> presence <strong>of</strong> <strong>the</strong> cut-<strong>of</strong>f frequency <strong>of</strong> <strong>the</strong> top layer <strong>of</strong> soil thatwas discussed in Sec. 3.2.More physical remarks can be made in <strong>the</strong> different frequency ranges defined by <strong>the</strong>resonance frequencies a 0α <strong>of</strong> <strong>the</strong> masses m α representing <strong>the</strong> hidden variables. In <strong>the</strong> lowfrequency range (a 0 ≪ a 01 ), a first-order expansion gives˜Z h (a 0 ) = ˜k 0 + ia 0 (˜c h + ˜c 2 + ˜c 3 ). (11)It is worth noticing that <strong>the</strong> slope <strong>of</strong> <strong>the</strong> imaginary part ˜c 0 + ˜c 1 + ˜c 2 + ˜c 3 is not small sinceit allows to quickly reach <strong>the</strong> level <strong>of</strong> <strong>the</strong> hysteretical damping. In <strong>the</strong> range <strong>of</strong> resonance <strong>of</strong>mass m 1 (a 0 − a 01 ≪ 2ζ 1 a 01 , with ζ α = c α /(2 √ k α m α )), and supposing that all <strong>the</strong> resonancefrequencies are far enough from each o<strong>the</strong>r (a 0 − a 02 ≫ 2ζ 2 a 02 and a 0 − a 03 ≫ 2ζ 3 a 03 ), onehas[˜Z h (a 0 ) = ˜k h + ˜k 1 − ˜k a 2 022a 2 02 − − ˜k a 2 ]033 a2 0 a 2 03 − a2 0[ ( ) a2 2 ( )+ ia 0 ˜c h − ˜c 1 + ˜c 02a2 2]2a 2 02 − + ˜c 033 a2 0 a 2 03 − (12)a2 0which means that around a 01 , <strong>the</strong> mass m 1 has <strong>the</strong> same displacement as <strong>the</strong> foundation, sothat <strong>the</strong>re is no damping contribution from ˜c 1 . For a 0 ≪ a 02 , masses m 2 and m 3 are also linkedto <strong>the</strong> foundation but <strong>the</strong> dashpots ˜c 2 and ˜c 3 introduce some damping. The equivalent slopeCopyright¡2002 John Wiley & Sons, Ltd. Earthquake Engng Struct. Dyn. 2002; 00:1–6Prepared using eqeauth.cls
12 R. TAHERZADEH, D. CLOUTEAU & R. COTTEREAUFigure 7. A schematic drawing <strong>of</strong> a simple model <strong>for</strong> end bearing <strong>pile</strong> group.around a 01 tends to ˜c 0 + ˜c 2 + ˜c 3 = β eq /a 01 which is actually small as expected to model <strong>the</strong>sole hysteretical damping β eq . Usually ˜c 1 ≫ a 01 β eq . In <strong>the</strong> range <strong>of</strong> resonance <strong>of</strong> <strong>the</strong> mass m 2(an equivalent <strong>for</strong>mula can be derived <strong>for</strong> mass m 3 ), a large imaginary part is brought on byk α2ζ α, which corresponds to <strong>the</strong> peaks observed in Fig. 3. Finally, at high frequency (a 0 ≫ a 03 ),one has()˜Z h (a 0 ) = ˜k h − ˜c2 1− a 2 0 ˜m h + ia 0˜c h (13)˜m 1which classically corresponds to all <strong>the</strong> masses m 1 , m 2 and m 3 being fixed. One can see ˜c 1as <strong>the</strong> radiative damping which occurs only above a 01 since <strong>for</strong> this frequency we have shownthat <strong>the</strong> damping is only β eq /a 01 . Thus this model reproduces <strong>the</strong> cut-<strong>of</strong>f frequency at <strong>the</strong>resonance frequency <strong>of</strong> <strong>the</strong> layer.Once <strong>the</strong> structure <strong>of</strong> <strong>the</strong> approximation has been decided, a multiple regression analysisis per<strong>for</strong>med on <strong>the</strong> same leading parameters as be<strong>for</strong>e, plus <strong>the</strong> ratio (ρ b V b )/(ρ s V s ) to yield<strong>the</strong> <strong><strong>for</strong>mulas</strong> presented in Table IV. Note that several coefficients appear as zeros in <strong>the</strong> table,which means that <strong>the</strong> parameters modeled do not have any influence on <strong>the</strong> <strong>for</strong>mula. Note alsothat, as be<strong>for</strong>e, <strong>the</strong> <strong><strong>for</strong>mulas</strong> are presented in a non-normalized manner in App. 6 <strong>for</strong> easierreading. The general <strong><strong>for</strong>mulas</strong> <strong>for</strong> <strong>the</strong> parameters areχ = λ 0(RfH) λ1( ) λ2( ) λ3 L0 ρb V b. (14)s ρ s V sIt is particularly interesting to note that, although <strong>the</strong> <strong><strong>for</strong>mulas</strong> were derived from ra<strong>the</strong>rma<strong>the</strong>matical considerations (<strong>the</strong> hidden variables model and a regression analysis), <strong>the</strong>yyield a very good evaluation <strong>of</strong> <strong>the</strong> resonance frequencies <strong>of</strong> <strong>the</strong> soil layer. Indeed, <strong>the</strong> firstfundamental frequency <strong>of</strong> <strong>the</strong> soil layer ω s 01 = 2πV s /(4H) and √ k 1 /m 1 = 1.4V s /H (see App. 6<strong>for</strong> non-normalized <strong><strong>for</strong>mulas</strong>) coincide. Likewise, <strong>the</strong> second fundamental frequency <strong>of</strong> <strong>the</strong> soilCopyright¡2002 John Wiley & Sons, Ltd. Earthquake Engng Struct. Dyn. 2002; 00:1–6Prepared using eqeauth.cls
SIMPLE FORMULAS FOR THE DYNAMIC STIFFNESS OF PILE GROUPS 13Table III. The database <strong>of</strong> soil-<strong>pile</strong> group systems used to derive <strong>the</strong> simple<strong>for</strong>mulations <strong>for</strong> end-bearing <strong>pile</strong> <strong>groups</strong>. The range <strong>of</strong> parameters is 125 ≤E p/E s ≤ 750, 2.8 ≤ s/d p ≤ 4.4, 1 ≤ R f /H ≤ 2.1 and 3 ≤ V b /V s ≤ 8 andconstant hysteretic damping β s = 0.05.Samples Piles E p d E s B f l p H V s V b s[-] [GPa] [m] [GPa] [m] [m] [m] [m/s] [m/s] [m]1 8 × 8 30 1 0.1 15 16 14 140 830 3.32 11 × 11 30 1 0.1 20 16 14 140 830 3.33 16 × 16 30 1 0.1 30 16 14 140 830 3.34 13 × 13 40 1 0.08 20 22 20 130 620 2.85 13 × 13 30 1 0.08 20 22 20 130 620 2.86 13 × 13 20 1 0.08 20 22 20 130 620 2.87 15 × 15 25 1.3 0.2 37 20 18 200 780 4.38 18 × 18 30 1 0.04 32 20 18 90 440 3.19 18 × 18 30 1 0.1 32 20 18 140 700 3.110 14 × 14 30 1 0.08 26 26 24 130 1000 3.311 14 × 14 30 1 0.08 26 20 18 130 1000 3.312 14 × 14 30 1 0.08 26 16 14 130 1000 3.313 13 × 13 30 1 0.06 26 18 16 110 620 3.614 13 × 13 30 1 0.06 26 18 16 110 620 3.615 13 × 13 30 1 0.06 26 18 16 110 620 3.6layer ω s 02 = 6πV s /(4H) is very well approximated by <strong>the</strong> third resonance <strong>of</strong> <strong>the</strong> simple model√k3 /m 3 = 5.1V s /H.5. IMPACT OF THE FORMULAS ON THE EVALUATION OF DESIGN QUANTITIESIn this last section, we discuss <strong>the</strong> accuracy <strong>of</strong> <strong>the</strong> proposed <strong><strong>for</strong>mulas</strong> on two practical cases.More particularly, <strong>the</strong> accuracy <strong>of</strong> <strong>the</strong> predicted transfer functions, spectral acceleration ontop <strong>of</strong> a building and relative displacement between top and bottom <strong>of</strong> <strong>the</strong> building, using<strong>the</strong> proposed <strong><strong>for</strong>mulas</strong>, is demonstrated. In a second test, we compare <strong>the</strong> accuracy <strong>of</strong> ourproposed <strong>for</strong>mula with ano<strong>the</strong>r one from <strong>the</strong> literature.5.1. Case 1For this validation, a 10 ×10 end-bearing <strong>pile</strong> group is used, with <strong>pile</strong>s with d p = 1 m, l p = 22m, s = 5 m, and connected by a 1.1 m-thick, rigid, cap with B f = 25 m. The mechanicalproperties <strong>of</strong> <strong>the</strong> <strong>pile</strong>s are E p = 30 GPa, ν p = 0.25, and ρ p = 2500 kg/m 3 . This <strong>pile</strong> <strong>groups</strong>tands in H = 20 m-thick soil layer, with properties E s = 60 MPa, ν s = 0.4 and ρ s = 1750Copyright¡2002 John Wiley & Sons, Ltd. Earthquake Engng Struct. Dyn. 2002; 00:1–6Prepared using eqeauth.cls
14 R. TAHERZADEH, D. CLOUTEAU & R. COTTEREAUTable IV. Coefficients <strong>for</strong> <strong>the</strong> horizontal and rocking elements <strong>of</strong> <strong>the</strong> impedance<strong>of</strong> an end-bearing <strong>pile</strong> group.( ) λ1 Rf(χ = λL0) λ2( ) λ3ρb V b0 H s ρ sV sλ 0 λ 1 λ 2 λ 3 R [%]˜k 0 = ˜k h − ˜k 2 − ˜k 3 10 0.5 0.35 0 93˜c h = ˜c 0 + ˜c 1 1 -0.5 0.5 0.5 60˜m h = ˜m 0 0.5 -1 0 0 82˜k 1 2.6 1 0 0 65˜c 1 1.9 -1.5 0 0 75˜m 1 1.4 -1 0 0 80˜k 2 1.25 0.35 -1 0.5 60˜c 2 0.04 0 -1 1 62˜m 2 0.08 -1 -1 0.5 80˜k 3 16.1 3 3 -0.5 75˜c 3 3 2 3 -1.5 70˜m 3 0.6 1 3 -0.5 75˜k r 15 0.5 1 1 98˜c r 17 0.5 2 -0.5 95˜m r = ˜m 0 leq/4 2 1.6 -1.5 1 -0.5 90kg/m 3 . The mechanical properties <strong>of</strong> <strong>the</strong> underlying half-space are E b = 1.5 GPa and ν b = 0.3and ρ b = 2000 kg/m 3 . The real and imaginary parts <strong>of</strong> <strong>the</strong> impedance are shown on Fig. 8, bothas computed using <strong>the</strong> numerical FE-BE model, and using <strong>the</strong> simple <strong><strong>for</strong>mulas</strong> <strong>of</strong> Eq. (10). Theagreement between <strong>the</strong> two approaches is good, in particular <strong>for</strong> <strong>the</strong> shaking term, considering<strong>the</strong> important variability in frequency. Note that <strong>the</strong> <strong>pile</strong> group considered here was not used<strong>for</strong> <strong>the</strong> regression analysis that determined <strong>the</strong> parameters in Table IVWe now turn to <strong>the</strong> observation <strong>of</strong> <strong>the</strong> accuracy <strong>of</strong> <strong>the</strong> proposed <strong>for</strong>mulations <strong>for</strong> <strong>the</strong>estimation <strong>of</strong> engineering quantities <strong>of</strong> interest. We <strong>the</strong>re<strong>for</strong>e consider a 60 m high-building(20 floors), with floors <strong>of</strong> 22.5 m ×22.5 m, and 6 columns ×6 columns. The slab weight perunit area is 500 kg/m 2 and <strong>the</strong> characteristics <strong>of</strong> <strong>the</strong> beams and columns are, respectively,EI = 5.1 MN.m 2 and EI = 1 MN.m 2 .We first consider <strong>the</strong> estimation <strong>of</strong> transfer functions in two different cases: (1) using <strong>the</strong>entire, 6 × 6, impedance matrix computed from <strong>the</strong> FE-BE model, and considering both <strong>the</strong>kinematic and inertial interaction, and (2) using only <strong>the</strong> horizontal and rocking elements <strong>of</strong><strong>the</strong> impedance matrix computed with <strong>the</strong> proposed <strong>for</strong>mula (10) and neglecting <strong>the</strong> kinematicinteraction. For both cases, <strong>the</strong> displacement field is decomposed on a basis that contains <strong>the</strong>rigid body modes <strong>of</strong> <strong>the</strong> building (l m ), which coincide with those <strong>of</strong> <strong>the</strong> foundation, and <strong>the</strong>flexible modes <strong>of</strong> <strong>the</strong> building on a rigid basis (φ n ):u(ω,x) = ∑ mc m (ω)l m (x) + ∑ nα n (ω)φ n (x) = [ c α ] { LΦ}(15)Copyright¡2002 John Wiley & Sons, Ltd. Earthquake Engng Struct. Dyn. 2002; 00:1–6Prepared using eqeauth.cls
SIMPLE FORMULAS FOR THE DYNAMIC STIFFNESS OF PILE GROUPS 15Real part [N/m]0−10 1 2 3 4 51 x Frequency [Hz]Real part [N/m]100 1 2 3 4 52 x Frequency [Hz]Imaginary part [N.m]100 1 2 3 4 52 x Frequency [Hz]Imaginary part [N.m]100 1 2 3 4 52 x Frequency [Hz]Figure 8. Comparison between <strong>the</strong> real (up) and imaginary (down) parts <strong>of</strong> <strong>the</strong>horizontal (left) and rocking (right) elements <strong>of</strong> <strong>the</strong> impedance matrix <strong>for</strong> a 10×10end-bearing <strong>pile</strong> group computed using <strong>the</strong> simplified <strong><strong>for</strong>mulas</strong> (10) (dashed line)and <strong>the</strong> FE-BE model (solid line).where L is <strong>the</strong> matrix <strong>of</strong> <strong>the</strong> rigid body modes <strong>of</strong> <strong>the</strong> structure and Φ is <strong>the</strong> matrix <strong>of</strong> <strong>the</strong>eigenmodes <strong>of</strong> <strong>the</strong> structure clamped at its base. The response <strong>of</strong> <strong>the</strong> structure, taking intoaccount soil-structure interaction, is <strong>the</strong>n computed using <strong>the</strong> following <strong>for</strong>mula([ Z(ω) 00 0]+ (1 + 2iβ)[ 0 00 Λ] [− ω 2 MΓM ΩΓM ΓΩI]) { c(ω)α(ω)} { } Z(ω)c0 (ω)=0where <strong>the</strong> diagonal matrix Λ contains <strong>the</strong> squares <strong>of</strong> <strong>the</strong> lowest circular frequencies <strong>of</strong> <strong>the</strong>structure on fixed base and I is <strong>the</strong> identity matrix arising from <strong>the</strong> orthogonality <strong>of</strong> <strong>the</strong>eigenmodes with respect to <strong>the</strong> mass matrix. Γ stands <strong>for</strong> <strong>the</strong> rigid body modes and Ω <strong>for</strong> <strong>the</strong>eigenmodes on fixed base, while c 0 is <strong>the</strong> kinematic interaction. The differences between <strong>the</strong>two models with respect to this <strong>for</strong>mulation are <strong>the</strong> impedance matrix Z(ω) and <strong>the</strong> kinematicinteraction factor takes equal to ∆u i (ω) with ∆ having null components but a unitary <strong>for</strong><strong>the</strong> sway term. Besides, it is worth noticing that <strong>the</strong> simplified model does not correspond to<strong>the</strong> physical model sketched on Fig. 7 subjected to an uni<strong>for</strong>m acceleration a i . Indeed, inertial<strong>for</strong>ces are not applied on mass m 1 , m 2 and m 3 since <strong>the</strong>se masses are in <strong>the</strong> soil and have <strong>the</strong>irinertial <strong>for</strong>ces already balanced in <strong>the</strong> soil.The resonance frequencies <strong>of</strong> <strong>the</strong> soil are computed at f s 01 = 1.55 Hz and f s 02 = 4.6 Hz.Assuming a horizontal harmonic base motion at <strong>the</strong> bedrock, <strong>the</strong> horizontal transfer functionat <strong>the</strong> free surface and at <strong>the</strong> top <strong>of</strong> <strong>the</strong> building are represented on Fig. 9. It clearly shows <strong>the</strong>effect <strong>of</strong> <strong>the</strong> soil-structure interaction, as well as <strong>the</strong> ability <strong>of</strong> <strong>the</strong> <strong><strong>for</strong>mulas</strong> (10) to compute<strong>the</strong> resonance frequency <strong>of</strong> <strong>the</strong> coupled system (<strong>the</strong> peaks <strong>of</strong> <strong>the</strong> dotted and dash-dotted lineson Fig. 9 coincide almost exactly).We <strong>the</strong>n consider two real recordings <strong>of</strong> earthquakes, with different frequency contents (seeFig. 10) and peak ground accelerations (PGA) at about 0.3 g. On Fig. 11 a comparison is given<strong>of</strong> <strong>the</strong> spectral acceleration on top <strong>of</strong> <strong>the</strong> building computed in <strong>the</strong> two cases considered earlier<strong>of</strong> <strong>the</strong> FE-BE model supposing inertial and kinematic interaction and <strong>the</strong> simple <strong><strong>for</strong>mulas</strong> (10)neglecting <strong>the</strong> kinematic interaction. On Fig. (12), a comparison is given <strong>of</strong> <strong>the</strong> time histories<strong>of</strong> <strong>the</strong> relative displacements between <strong>the</strong> top and <strong>the</strong> base <strong>of</strong> <strong>the</strong> building. On both figures,<strong>the</strong> agreement between <strong>the</strong> two approaches is very good.(16)Copyright¡2002 John Wiley & Sons, Ltd. Earthquake Engng Struct. Dyn. 2002; 00:1–6Prepared using eqeauth.cls
16 R. TAHERZADEH, D. CLOUTEAU & R. COTTEREAU1412Transfer Function [−]10864200 1 2 3 4 5Frequency [Hz]Figure 9. Transfer function at ground surface free field (solid line), <strong>of</strong> <strong>the</strong> structurewithout SSI (dashed line), and <strong>of</strong> <strong>the</strong> structure with SSI (dashed-dotted line), allcomputed with <strong>the</strong> FE-BE approach, and transfer function <strong>of</strong> <strong>the</strong> structure withSSI computed with <strong>the</strong> proposed <strong><strong>for</strong>mulas</strong> (dotted line). The figures correspondsto a structure resting on a 10 × 10 end-bearing <strong>pile</strong> group.Acceleration [m/s 2 ]Acceleration [m/s 2 ]30−30 4 8 12 16Time [s]30−30 4 8 12 16Time [s]Spectral acceleration [m/s 2 ]10864200 4 8 12 16Frequncy [Hz]Figure 10. Ground acceleration (left) and 5%-damped response spectra (right)recorded in Aegion (Greece) in 1995 (top and solid line), and in Friuli (Italy) in1976 (bottom and dashed line).5.2. Case 2In this example, we compare our simplified <strong>for</strong>mulations 10 <strong>for</strong> <strong>the</strong> impedance <strong>of</strong> <strong>the</strong> endbearing<strong>pile</strong> group introduced in Sec. 3.2 with <strong>the</strong> simplified <strong><strong>for</strong>mulas</strong> proposed in [34, 21]. Weuse an equivalent with <strong>of</strong> R f = 8 m, because <strong>the</strong> <strong><strong>for</strong>mulas</strong> in Table IV are proposed <strong>for</strong> circularor square foundation. Fig. 13 shows this comparison, along with <strong>the</strong> value <strong>of</strong> <strong>the</strong> BE solution.Our <strong><strong>for</strong>mulas</strong> seems to behave at least as well as <strong>the</strong> previously available one. Remember thatits range <strong>of</strong> application, in in particular in terms <strong>of</strong> <strong>the</strong> numbers <strong>of</strong> <strong>pile</strong>s is much larger.Copyright¡2002 John Wiley & Sons, Ltd. Earthquake Engng Struct. Dyn. 2002; 00:1–6Prepared using eqeauth.cls
SIMPLE FORMULAS FOR THE DYNAMIC STIFFNESS OF PILE GROUPS 17108Spectral acceleration [m/s 2 ]7.552.5Spectral acceleration [m/s 2 ]64200 2 4 6 8 10Frequency [Hz]00 2 4 6 8 10Frequency [Hz]Figure 11. Comparison <strong>of</strong> <strong>the</strong> acceleration response spectra at <strong>the</strong> top <strong>of</strong> <strong>the</strong>building <strong>for</strong> <strong>the</strong> Friuli earthquake (left) and <strong>the</strong> Aegion earthquake (right), using<strong>the</strong> complete FE-BE model (solid line) and <strong>the</strong> simple <strong>for</strong>mulation (dashed line).The figures corresponds to a structure resting on a 10×10 end-bearing <strong>pile</strong> group.0.120.03Relative displacement [m]0.080.040−0.04−0.08Relative displacement [m]0.020.010−0.01−0.02−0.120 6 12 18 24 30Time [s]−0.030 6 12 18 24 30Time [s]Figure 12. Comparison <strong>of</strong> <strong>the</strong> relative displacements between <strong>the</strong> top and <strong>the</strong> base<strong>of</strong> <strong>the</strong> building <strong>for</strong> <strong>the</strong> Friuli earthquake (left) and <strong>the</strong> Aegion earthquake (right),using <strong>the</strong> complete FE-BE model (solid line) and <strong>the</strong> simple <strong>for</strong>mulation (dashedline). The figures corresponds to a structure resting on a 10 × 10 end-bearing <strong>pile</strong>group.6. CONCLUSION<strong>Simple</strong> <strong>for</strong>mulations have been derived <strong>for</strong> <strong>the</strong> <strong>dynamic</strong> <strong>stiffness</strong> matrices <strong>of</strong> <strong>pile</strong> groupfoundations subjected to horizontal and rocking <strong>dynamic</strong> loads. These <strong>for</strong>mulations were foundusing a large database <strong>of</strong> impedance matrices computed using a FE-BE model. They can bereadily employed <strong>for</strong> design <strong>of</strong> large foundations on <strong>pile</strong>s and are shown to yield very accuratevalues <strong>of</strong> <strong>the</strong> estimated quantities <strong>of</strong> interest <strong>for</strong> building design. The <strong>for</strong>mulations have beenderived both <strong>for</strong> floating <strong>pile</strong> <strong>groups</strong> on homogeneous half-space and end-bearing <strong>pile</strong> <strong>groups</strong>in a homogenous stratum. They can be used <strong>for</strong> large <strong>pile</strong> <strong>groups</strong> (n ≥ 50), as well as <strong>for</strong> alarge range <strong>of</strong> mechanical and geometrical parameters <strong>of</strong> <strong>the</strong> soil and <strong>the</strong> <strong>pile</strong>s. They providea first step towards code provisions specifically focused on <strong>pile</strong> footings.Copyright¡2002 John Wiley & Sons, Ltd. Earthquake Engng Struct. Dyn. 2002; 00:1–6Prepared using eqeauth.cls
18 R. TAHERZADEH, D. CLOUTEAU & R. COTTEREAU22Dynamic <strong>stiffness</strong> [N/m]3 x 109 Frequency [Hz]10Damping [N/m]2.5 x 109 Frequency [Hz]1.51−10.5−20 1 2 3 4 5 600 1 2 3 4 5 6Figure 13. Real (left) and imaginary (right) parts <strong>of</strong> <strong>the</strong> horizontal impedancematrix, <strong>for</strong> a 36 end-bearing <strong>pile</strong> group computed using <strong>the</strong> simplified<strong><strong>for</strong>mulas</strong> (10) (solid line) and BE solution (dashed line) and simplified analyticalsolution <strong>of</strong> [8] (dotted line).REFERENCES1. Wolf JP. Foundation analysis using simple physical model. Prentice-Hall: Englewood Cliffs, New-Jersey,1994.2. Kaynia AM. Dynamic <strong>stiffness</strong> and seismic response <strong>of</strong> <strong>pile</strong> <strong>groups</strong>. Research Report R82-03,Masshachussetts Institute <strong>of</strong> Technology, ; 1982.3. Waas G, Hartmann HG. Seismic analysis <strong>of</strong> <strong>pile</strong> foundations including soil-<strong>pile</strong>-soil interaction. Proceedings<strong>of</strong> <strong>the</strong> 8th World Conference on Earthquake Engineering San Francisco, July 1984; 555–62.4. Takemiya H. Ring-Pile analysis <strong>for</strong> a grouped <strong>pile</strong> foundation subjected to base motion. StructuralEngineering/Earthquake Engineering 1986; 3(1):195–202.5. Ohira A, Tazoh T, Dewa T, Shimizu K, Shimada M. Observation <strong>of</strong> earthquake response behaviours <strong>of</strong>foundations <strong>pile</strong>s <strong>for</strong> road bridge. Proceedings <strong>of</strong> <strong>the</strong> 8th World Conference on Earthquake Engineering,San Francisco, July 1984; 3:577–584.6. Konagai K, Ahsan R, Maruyama D. <strong>Simple</strong> expression <strong>of</strong> <strong>the</strong> <strong>dynamic</strong> <strong>stiffness</strong> <strong>of</strong> grouped <strong>pile</strong>s in swaymotion. Journal <strong>of</strong> Earthquake Engineering 2000; 4(3):355–376.7. Crouse CB, Cheang L. Dynamic testing and analysis <strong>of</strong> <strong>pile</strong> group foundation. In Dynamic Response <strong>of</strong>Pile Foundations-Experiment, Analysis and Observation, Nogami T. (ed). ASCE: New-York, 1987; 79–98.8. Mylonakis G, Nikolaou A, Gazetas G. Soil-Pile-Bridge seismic interaction: kinematic and inertial effects.Part I: s<strong>of</strong>t soil. Earthquake Engineering and Structural Dynamics 1997; 26(3):337–359.9. Hutchinson TC, Chai YH, Boulanger RW, Idriss IM. Inelastic seismic response <strong>of</strong> extended <strong>pile</strong>-shaftsupportedbridge structures. Earthquake Spectra 2004; 20(4):1057–1080.10. Wolf JP. Soil-structure-interaction analysis in time domain. Prentice-Hall: Englewood Cliffs, New-Jersey,1988.11. Levine MB, Scott RF. Dynamic response verification <strong>of</strong> simplified bridge-foundation model. Journal <strong>of</strong>Geotechnical Engineering 1989; 115(2):1246–1260.12. Spyrakos CC. Assessment <strong>of</strong> SSI on <strong>the</strong> longitudinal seismic response <strong>of</strong> short span bridges. EngineeringStructures 1990; 12(1):60–66.13. Harada T, Yamashita N, Sakanashi K. Theoretical study on fundamental period and damping ratio <strong>of</strong> bridgepier-foubdation system. In Proceedings <strong>of</strong> <strong>the</strong> Japan Society <strong>of</strong> Civil Engineers 1994; 489(1-27):227–234.14. Chaudhary MS, Parakash S. Dynamic soil structure interaction <strong>for</strong> bridge abutment on <strong>pile</strong>s. InGeotechnical Special Publication 1998;2:1247–1258.15. Spyrakos CC, Loannidis G. Seismic behavior <strong>of</strong> a post-tensioned integral bridge including soil-structureinteraction (SSI). Soil Dynamics and Earthquake Engineering 2003; 23(1):53–63.16. Tongaonkar NP, Jangid RS. Seismic response <strong>of</strong> isolated bridges with soil-structure interaction. SoilDynamics and Earthquake Engineering 2003; 23(4):287–302.17. Dobry R, Gazetas G. <strong>Simple</strong> method <strong>for</strong> <strong>dynamic</strong> <strong>stiffness</strong> and damping <strong>of</strong> floating <strong>pile</strong> <strong>groups</strong>. Geotechnique1988; 38(4):557–574.Copyright¡2002 John Wiley & Sons, Ltd. Earthquake Engng Struct. Dyn. 2002; 00:1–6Prepared using eqeauth.cls
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Identification <strong>of</strong> <strong>the</strong> essential parameters <strong>for</strong> <strong>the</strong> lateral impedance<strong>of</strong> large <strong>pile</strong> <strong>groups</strong>. In Proceedings <strong>of</strong> <strong>the</strong> 4th International Conference on Geotechnical EarthquakeEngineering, Thessaloniki, Greece, June 2007, in CDROM.32. Craig RJ, Bampton M. Coupling <strong>of</strong> substructures <strong>for</strong> <strong>dynamic</strong> analyses. AIAA Journal 1968; 6(7):1313–1319.33. Miura K, Kaynia AM, Masuda K, Kitamura E, Seto Y. Dynamic behaviour <strong>of</strong> <strong>pile</strong> foundations inhomogeneous and non-homogeneous media. Earthquake Engineering and Structural Dynamics 1994;23(2):183–192.34. Gazetas G, Hess P, Zinn R, Mylonakis G, Nikolaou A. Seismic response <strong>of</strong> a large <strong>pile</strong> group. In Proceedings<strong>of</strong> <strong>the</strong> 11th European Conference on Earthquake Engineering, Paris, September 1998, in CDROM.35. Cottereau R, Clouteau D, Soize C. Construction <strong>of</strong> a probabilistic model <strong>for</strong> impedance matrices. ComputerMethods in Applied Mechanics and Engineering 2007; 196(17-20):2252–2268.36. Cottereau R, Clouteau D, Soize C. Probabilistic impedance <strong>of</strong> foundation: Impact <strong>of</strong> <strong>the</strong> seismic design onuncertain soils. Earthquake Engineering and Structural Dynamics 2008; 37(6):899-918.37. Gazetas G. Seismic response <strong>of</strong> end-bearing single <strong>pile</strong>s. International Journal <strong>of</strong> Soil Dynamics andEarthquake Engineering 1984; 3(2):82–93.38. Poulos HG. Behavior <strong>of</strong> laterally loaded <strong>pile</strong>s: PART II - group <strong>pile</strong>s. Journal <strong>of</strong> <strong>the</strong> Soil Mechanics andFoundations Division, ASCE, 1971;733–751.39. Cottereau R. Probabilistic models <strong>of</strong> impedance matrices. PhD <strong>the</strong>sis, Ecole Centrale Paris, France,(http://tel.archives-ouvertes.fr/tel-00132950/en/); 2006.40. Nikolaou S., Mylonakis G., Gazetas G. and Tazoh T. Kinematic <strong>pile</strong> bending during earthquake: analysisand field measurement. Geotechnique 2001; 51(5):425-440.APPENDIX AIn this appendix, <strong>the</strong> practical methodology <strong>for</strong> <strong>the</strong> construction <strong>of</strong> <strong>the</strong> reduced matrixS(a 0 ) = K − a 2 0M + ia 0 C is introduced. Three main steps are identified:¢The impedance <strong>of</strong> <strong>the</strong> FE-BE model is computed. More specially a set <strong>of</strong> values {Z(a 0l )}<strong>of</strong> <strong>the</strong> impedance matrix at a finite number <strong>of</strong> frequencies (a 0l ) 1≤l≤L is computed.¢The set <strong>of</strong> values {Z(a 0l )} is interpolated to yield a matrix-valued rational function in<strong>the</strong> <strong>for</strong>m a 0 → N(a 0 )/q(a 0 ), which approximates <strong>the</strong> behavior <strong>of</strong> <strong>the</strong> impedance matrix{Z(a 0 )} <strong>of</strong> <strong>the</strong> model. The function a 0 → N(a 0 ) is a matrix-valued polynomial in (ia 0 ),Copyright¡2002 John Wiley & Sons, Ltd. Earthquake Engng Struct. Dyn. 2002; 00:1–6Prepared using eqeauth.cls
20 R. TAHERZADEH, D. CLOUTEAU & R. COTTEREAUand <strong>the</strong> function a 0 → q(a 0 ) is a scalar polynomial in (ia 0 ). Many methods can be usedto achieve that goal.¢The identification <strong>of</strong> <strong>the</strong> matrices K, C and M from <strong>the</strong> polynomials a 0 → N(a 0 ) anda 0 → q(a 0 ) is <strong>the</strong>n per<strong>for</strong>med. This step does not involve any approximation and isfur<strong>the</strong>r detailed in [39].APPENDIX BIn this appendix, we present an extended version <strong>of</strong> <strong>the</strong> <strong><strong>for</strong>mulas</strong> presented in Tables IIand IV, in a non-normalized <strong>for</strong>m. For <strong>the</strong> case <strong>of</strong> <strong>the</strong> floating <strong>pile</strong> <strong>groups</strong> on homogeneoushalf-space <strong>the</strong> coefficients appearing in <strong>the</strong> non-normalized version <strong>of</strong> Eq. (8) are⎧ (⎪⎨k h = 6.8G s RL0) 0.3√ f sc h = 5 GsR2 f L 0V s s(17)⎪⎩ (m h = 0.4ρ s Rf3 L0) 1.6sand( ) 0.6 ⎧⎪ ⎨ k r = 8G s Rf3 lp (L0) 0.4R f s√ (c⎪ r = 5 GsR3 fV Rf⎩slL0) 0.2(18)p sm r = 0.7G s Rf 4l ( L0) 0.4p sThe range <strong>of</strong> parameters is 250 ≤ E p /E s ≤ 1500, 2 ≤ s/d p ≤ 3.6 and 0.55 ≤ R f /l p ≤ 2 andconstant hysteric damping β s = 0.05.For <strong>the</strong> case <strong>of</strong> end-bearing <strong>pile</strong> <strong>groups</strong>, <strong>the</strong> coefficients appearing in <strong>the</strong> non-normalizedversion <strong>of</strong> Eq. (10) are⎧( ) 0.5 Rf (⎪⎨k 0 = k h − k 2 − k 3 = 10G s RL0) 0.35f H√ sc h = c 0 + c 1 = GsR2 f H L 0 ρ b V bV s R f s ρ sV s⎪⎩m h = 1 2 ρ sHRf2 , (19)⎧R⎪⎨ k 1 = 2.6G 2 f s Hc 1 = 1.9 GsR2 fV s(HR f ) 1.5 , (20)⎪⎩m 1 = 1.4ρ s Rf 2H ⎧) 0.35 s)sL 0( √Rfk ⎪⎨ 2 = 1.25G s Rρb V bf H(L 0 ρ sV sc 2 = 0.04G s Rf2 ρ b V b, (21)ρ sVs2√⎪⎩ m 2 = 0.08ρ s Rf 2H s ρb V bL 0 ρ sV s⎧Rk 3 = 16.1G 4 (f L0) 3√ρsV ss H ⎪⎨3 s ρ b V bc 3 = 3 Gs R 4 (f L0) 3( ) 1.5 ρsV sV s H 2 s, (22)ρ b V b⎪⎩Rm 3 = 0.6ρ 4 (f L0) 3√ρsV ss H 1 s ρ b V bCopyright¡2002 John Wiley & Sons, Ltd. Earthquake Engng Struct. Dyn. 2002; 00:1–6Prepared using eqeauth.cls
SIMPLE FORMULAS FOR THE DYNAMIC STIFFNESS OF PILE GROUPS 21and ⎧⎪ ⎨⎪ ⎩k r = 15G s R 3 f√R fc r = 17 GsR4 fV sH(L0m r = 1.6ρ s R 4 f L0sL 0sρ b V bρ sV sρ sV sρ b V b) √ 2 Rfs√H. (23)R f H ρsVsρ b V bThe range <strong>of</strong> parameters is 125 ≤ E p /E s ≤ 750, 2.8 ≤ s/d p ≤ 4.4, 1 ≤ R f /H ≤ 2.1 and3 ≤ V b /V s ≤ 8 and constant hysteretic damping β s = 0.05.Copyright¡2002 John Wiley & Sons, Ltd. Earthquake Engng Struct. Dyn. 2002; 00:1–6Prepared using eqeauth.cls