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Introduction

The fundamental role of the foundation is to securely transfer the structure’s load to the ground below with a minimal possible permissible settlement. Structures such as elevated water towers, chimneys, TV towers, and silos are typically built on annular rafts. The annular foundation is preferred because it suits the above structures and economics. In order to fulfill the requirements of full utilization of the bearing capacity of soil and for limited settlement, the annular raft is frequently the sole option in addition to being cost-effective. A rigorous analytical model for predicting the deformation of vertically loaded piles in granular soils using the elastic continuum approach was introduced [1]. Later, pile foundation analysis and design, including the elastic continuum approach for granular piles, were introduced [2]. The behavior of pile groups and piled rafts using the elastic continuum approach, focusing on the interaction between the piles and the surrounding soil, were investigated [3]. Adding piles underneath the raft provides additional strength to the foundation and reduces the settlement of the foundation. Granular piles are used extensively for ground improvement due to their low cost and better performance [4,5,6,7,8,9,10,11]. Comparing the combined piled raft foundation (CPRF) system with the pile foundation, it is possible to obtain the appropriate level of serviceability without compromising safety and performance [12]. Due to its affordability and better performance, various researchers have analyzed the performance and behavior of CPRF under the action of static as well as dynamic loading [13,14,15,16,17,18]. The different design approaches for CPRF were proposed in various studies [19,20,21]. The interaction analysis of two granular piled raft units was studied, and the influence of each GPR on another GPR was evaluated [22].

The elastic continuum approach is a fundamental framework used in geotechnical engineering to analyze the behavior of soils and rocks. It considers these materials continuous and elastic, allowing for applying solid mechanics principles to study their response to various loading conditions. The elastic continuum approach can be used to analyze and predict the deformation, settlement, stress distribution, and stability of soil and rock structures, such as foundations, retaining walls, slopes, and tunnels. The elastic continuum approach assumes soils and rocks as homogeneous and isotropic materials. This simplification assumes that they exhibit linear elastic behavior within specific stress and strain ranges. The approach considers the fundamental concepts of stress, strain, and deformation, considering material properties, boundary conditions, and external loads.

The approach facilitates the design and assessment of geotechnical systems, considering factors such as load-bearing capacity, settlement limitations, and the prevention of failure mechanisms. The elastic continuum analysis considers the pile and the surrounding soil as a continuous medium, allowing for the evaluation of stress distribution, settlement, and pile–soil interaction. The elastic continuum approach helps to understand the load transfer mechanisms in granular piles, including the mobilization of skin friction.

The analysis of granular piles and combined granular piled raft systems using the elastic continuum approach offer a comprehensive understanding of their behavior under various loading conditions. This approach considers the interaction between the structure, piles, raft, and the surrounding soil, allowing for the assessment of performance and the optimization of design parameters. The performance of annular raft is analyzed by various researchers who found that it depends on various factors such as type of loading, type of soil, and size of annular raft and soil [23,24,25,26,27,28,29,30,31,32]. The inner and outer diameters play a vital role in the design of an annular raft which ultimately affects the settlement of the annular raft [33,34,35,36,37,38,39,40]. Some experimental studies were also carried out in order to analyze the settlement behavior of ring footing [41].

This study explicitly considers the presence of granular piles as the supporting medium for the annular raft. Previous research studies focused on other types of pile foundations or alternative support systems. Granular piles in this analysis recognize their relevance and address the specific challenges associated with this type of foundation system. This research utilizes an elastic continuum approach to analyze the behavior of the annular raft. Unlike discrete element methods or other numerical techniques that may have been employed in previous studies, the elastic continuum approach treats the raft and the supporting medium as continuous bodies. This approach allows for considering the soil–structure interaction and evaluating stresses, displacements, and settlements within the system. The present analysis reveals previously unexplored phenomena, such as load distribution patterns, settlement mechanisms, or the influence of different parameters on the raft’s performance.

Advantages of choosing granular piles over conventional piles include cost-effectiveness, as granular piles can often be more economical than steel or concrete piles due to their simpler and quicker installation. Additionally, the ease of installation is a notable benefit, especially in loose or sandy soils, as granular piles do not require heavy machinery or specialized equipment. Another advantage is settlement control, where granular piles contribute to managing settlement by improving the load-bearing capacity of the soil, particularly in loose or compressible soils. However, it is essential to acknowledge certain limitations in the study, such as the nonlinear nature of the soil considered as isotropic in the present analysis. Furthermore, the validity of the analysis is restricted to a circular raft.

The present investigation brings a new perspective to analyze the annular rafts with granular piles by employing a thorough assessment that subtracts the granular pile area from the annular raft. The findings of this research are showcased in the form of design charts, which are readily accessible to engineers. In order to ensure the applicability of the results across different raft sizes, the outcomes are presented in the form of nondimensional parameters.

This study aims to evaluate the following parameters governing the performance of annular raft with granular piles.

Settlement Influence Factor (SIF), Iagpr: The settlement influence factor is a dimensionless parameter that expresses the ratio of the settlement of a foundation to the settlement of the surrounding soil. It is often denoted by the symbol SIF and is used to characterize the relative settlement behavior of a foundation system.

Normalized shear stresses, τ1, along the GP–soil interface

Load shared (percentage) by GPs – Pgp

The ratio of settlements of an annular raft with GPs to the annular raft without GPs – Sr

Problem Definition and Analysis

GPs are compressible with a deformation modulus of Egp. The soft soil is characterized by its deformation modulus, Es, and Poisson’s ratio, νs. The modular ratio, Kgp=Egp/Es, i.e., the ratio of modulus of deformation of GP to that of the soil, is used to define the relative stiffness of the granular piles.

Figure 1 depicts an annual raft with an outer diameter, ‘dro,’ and inner diameter, ‘dri,’ supported by granular piles each of length ‘L’ and diameter d’. Granular piles are installed around the centroidal axis of the annular raft. The load applied to the annular raft pile system is P. Granular piles are characterized by deformation modulus, ‘Ep,’ and Poisson’s ratio, ‘νp.’ The annular raft rests on soil having Poisson’s ratio, ‘νs,’ and deformation modulus. ‘Es.’ The problem is not strictly axisymmetric due to the presence of a finite number of piles. The interaction stresses between the soil and the raft vary both in the radial and tangential directions. In order to simplify the analysis, the raft is subdivided into sectors, ‘A’ and ‘B,’ as depicted in Figure 2. The variations of raft stresses in the tangential direction, i.e., with ‘θ,’ in each sector are ignored. The annular raft is discretized into the ‘kr’ number of equal area annular rings (Figure 3), and the annular raft is subdivided into ‘kt’ angular subdivisions. Nodes for satisfying compatibility of settlements in sector ‘A’ are taken along the center line except in the region of GP, where they are taken a minimal distance away (0.01 times the diameter of the granular pile) from the periphery of GP to avoid problems of singularity, as shown in Figure 3 (a). The nodes for calculating settlements in sector ‘B’ are taken along the center line. Figure 3 (a) and (b) shows the stresses acting on the annular raft foundation and the global and local coordinate systems used for the purpose of numerical integration.

Figure 1:

Schematic diagram of the annular raft over GPs.

Figure 2:

Annular raft subdivisions into sectors

Figure 3:

Discretization of (a) annular raft and (b) granular pile.

GP is discretized into n cylindrical elements (Figure 3b), each of which is subject to a shear (τ) at the GP–soil interface and uniform normal stress on the base, pb. By integrating Mindlin’s equation [42, 43] for vertical displacement due to vertical force, the soil displacements are calculated at the mid-point of the periphery of each element.

In the present study, the annular raft on granular piles is analyzed by using the elastic continuum approach.

The present study is based on the following assumptions:

Isotropic, homogeneous, and linearly elastic soil: The surrounding soil is assumed to possess isotropic, homogeneous, and linearly elastic properties. This simplifying assumption allows for easier analysis by considering uniform behavior in all directions.

Perfectly rough sides of granular pile: The sides of the granular pile are assumed to have perfect roughness.

Smooth and rigid granular pile base: The base of the granular pile is assumed to be smooth and rigid, enabling simplified calculations and analysis [4344].

Disregard of installation effects and consolidation: The effects of pile installation on the surrounding soil and the consolidation effects over time are neglected in this study.

No slip or yield condition at the pile–soil interface: The pile–soil interface is assumed to have no slip or yield condition, simplifying the analysis of their interaction.

Linear stress–strain relationship: The stress–strain pattern within the soil is assumed to be linear, following Hooke’s law.

Rigid raft and uniform settlement: The raft is assumed to be rigid, and the surface beneath the raft is assumed to be smooth. Additionally, settlement is assumed to occur uniformly across the surface.

These assumptions provide a simplified framework for the analysis of the granular pile under specific conditions. However, it is essential to recognize that real-world conditions may deviate from these assumptions, and the results should be interpreted within the context of these simplifications.

Soil Displacements at the Nodes of Annular Raft

Soil displacements along annular raft are determined at the prescribed nodes of sectors ‘A’ and ‘B.’ For sectors ‘A,’ ‘B,’ and GP, the soil displacements are obtained due to the influence of stresses of sectors ‘A,’ ‘B,’ and GPs. Solutions for a point load in the interior and surface of a semi-infinite elastic continuum were provided in [45,46,47]. In order to obtain soil displacements due to the influence of stresses on sector ‘A,’ the influence area of the granular pile, which covers part of sector ‘A,’ is deducted. The geometric considerations for the deduction of GPs areas are explained in Fig. 4.

Figure 4:

Geometrical consideration in integration scheme.

The condition for any annulus ‘j’ of an annular raft passing through the region of GP, as depicted in Figure 4, is OgV<roj<OgUorOgV<roj-1<OgU {{\rm{O}}_{\rm{g}}}{\rm{V}} < {{\rm{r}}_{\rm{o}}}\left({\rm{j}} \right) < {{\rm{O}}_{\rm{g}}}{\rm{U}}\;{\rm{or}}\;{{\rm{O}}_{\rm{g}}}{\rm{V}} < {{\rm{r}}_{\rm{o}}}\left({{\rm{j -}}1} \right) < {{\rm{O}}_{\rm{g}}}{\rm{U}} where ro(j) and ro(j-1) are the outer radii of annuli ‘j’ and ‘j-l,’ respectively. If any annulus ‘j’ is passing through the area of GPs, the condition for element ‘kt’ of annulus ‘j’ falling in the area of GP is to be investigated further. The central angle of any GP ‘l’ from the global axis, Xg, is θpl=2πNpl1 {\theta _p}\left(l \right) = {{2\pi} \over {{N_p}}}\left({l - 1} \right) where ‘l’ varies from 1 to Np. The angle ‘ϕ’ defined as the angle between the center line of any GP to its tangent, as shown in Fig. 4, is expressed as Sinϕ=d/2OgOp {{Sin}}\left(\phi \right) = {{\left({d/2} \right)} \over {{O_g}{O_p}}} where Og Op is the distance of the centroidal axis of the annular raft given as 2×OgOp=dro2+dri221/2 2 \times {{\rm{O}}_{\rm{g}}}{{\rm{O}}_{\rm{p}}} = {\left[ {{{{\rm{d}}_{{\rm{ro}}}^2 + {\rm{d}}_{{\rm{ri}}}^2} \over 2}} \right]^{1/2}}

Angles of tangential lines of any GP ‘l’ are θ1l=θplϕθ2l=θpl+ϕ \matrix{{{\theta _1}\left(l \right) = {\theta _p}\left(l \right) - \phi} \cr {{\theta _2}\left(l \right) = {\theta _p}\left(l \right) + \phi} \cr}

The condition for element ‘kt’ of annulus ‘j’ falling in the granular pile region is θ1(l) < θj(kt) < θ2(l), where θj(kt) is the angle element ‘kt’ of annulus ‘j’ that makes with global axis, Xg. The elements near the GP periphery are further to be checked for their overlap. The essential condition of any element which fulfills the above condition and has its elemental angle θj (kt) = ψ with its centroidal distance r(j) is OgN < ro(j) < OgM.

OgN and OgM can be obtained from the property of triangle (ΔOgOpN or ΔOgOpM) as OgN=d/2Sinβ2ψSinψ {O_g}N = {{\left({d/2} \right){\mathop{Sin}\nolimits} \left({{\beta _2} - \psi} \right)} \over {{\mathop{Sin}\nolimits} \psi}} OgM=d/2Sinβ2ψSinψ {O_g}M = {{\left({d/2} \right){\mathop{Sin}\nolimits} \left({{\beta _2} - \psi} \right)} \over {{\mathop{Sin}\nolimits} \psi}} where β2=sin12OgOpdsinψ {\beta _2} = {sin ^{- 1}}\left({{{2{O_g}{O_p}} \over d}sin \psi} \right) . The soil displacement equations for sector ‘A’ of the annular raft are ρAsa=SAsad=l=1l=NpIAsapτES++IAsaAprAES+IAsaBprBES \matrix{{\left\{{\rho _A^{sa}} \right\} = \left\{{{{S_A^{sa}} \over d}} \right\} = \left[ {\sum _{l = 1}^{l = Np}\left[ {I_A^{sap}} \right]} \right]\left\{{{\tau \over {{E_S}}}} \right\} +} \cr {+ \;\left[ {I_A^{saA}} \right]\left\{{{{{p_{rA}}} \over {{E_S}}}} \right\} + \left[ {I_A^{saB}} \right]\left\{{{{{p_{rB}}} \over {{E_S}}}} \right\}} \cr} where {SAsa} and {ρAsa} are the soil displacement vector and normalized soil displacement vectors of size ‘kr’ each. [IAsap] is the influence coefficient matrix of soil displacement of size, kr×(n+l), for the influences of interface shear stresses and base pressure of any GP on nodes of sector ‘A’; [IBsaA] is the influence coefficient matrix of soil displacement of size, kr×kr, for nodes of sector ‘A’ and evaluated for the effect of contact stresses on sector ‘A.’ [IBsaB] is the influence coefficient matrix of soil displacement of size, kr×kr, for nodes of sector ‘A’ and evaluated for the effect of contact stresses on sector ‘B.’ {PrA}and {PrB} are the normal pressure column vectors of size, kr, each for sectors ‘A’ and ‘B,’ respectively, and {τ} is a column vector having size (n+l) for the shaft stresses and the normal stresses on the base of the pile.

For sector ‘B’ of the annular raft, the soil displacement equations are ρBsa=SBsad=l=1l=NpIBsapτES++IBsaAprAES+IBsaBprBES \matrix{{\left\{{\rho _B^{sa}} \right\} = \left\{{{{S_B^{sa}} \over d}} \right\} = \left[ {\sum _{l = 1}^{l = Np}\left[ {I_B^{sap}} \right]} \right]\left\{{{\tau \over {{E_S}}}} \right\} +} \cr {+ \;\left[ {I_B^{saA}} \right]\left\{{{{{p_{rA}}} \over {{E_S}}}} \right\} + \left[ {I_B^{saB}} \right]\left\{{{{{p_{rB}}} \over {{E_S}}}} \right\}} \cr} where {SBsa} and {ρBsa} are the vectors of soil displacement and normalized soil displacement of sizes ‘kr’ each for sector ‘B.’ [IBsap] is the influence coefficient matrix of soil displacement of size kr×(n+l) for the influences of interface shear stresses and base pressure of any GP on nodes of sector ‘B’; [IBsaA] is the soil displacement influence coefficient matrix of size, kr×kr, for nodes of sector ‘B’ and evaluated for the effect of contact stresses on sector ‘A’; [IBsaB] is the soil displacement influence coefficient matrix of size, kr×kr, for nodes of sector ‘B’ and evaluated for the effect of contact stresses on sector ‘B.’

Granular Pile

In addition to the load, a granular pile’s settlement is typically influenced by its geometry and deformation modulus. The magnitude of applied stress influences the granular material’s deformation modulus. As a result, depending on the average principal stress at each level and the depth of the granular pile under loading, the deformation modulus may vary.

Granular pile displacement:

Displacement of the granular pile is evaluated by a generalized stress–strain relationship as εGP=σGPEGP {\varepsilon _{GP}} = {{{\sigma _{GP}}} \over {{E_{GP}}}} where εGP is the axial strain of the element of granular pile and σGP is the axial stress on the element of granular pile.

Relationship between axial and shear stresses of GP:

In order to consider the equilibrium condition from Fig. 4, the base pressure pb and the shear stresses, τ, are correlated with total load P, as P=j=1j=nτjπdLn+pbπd24 P = \sum\nolimits _{j = 1}^{j = n}{{{\tau _j}\pi dL} \over n} + {p_b}{{\pi {d^2}} \over 4} where n is the total number of elements of the granular pile.

The axial forces on the top and bottom face of an element ‘i’ are Pit=Pj=1j=(i1)τjπdLn {P_{it}} = P - \sum\nolimits _{j = 1}^{j = (i - 1)}{{{\tau _j}\pi dL} \over n} Pib=Pj=1j=iτjπdLn {P_{ib}} = P - \sum\nolimits _{j = 1}^{j = i}{{{\tau _j}\pi dL} \over n}

Combining equations (10) and (11) Pit=j=ij=nτjπdLn+pbπd24 {P_{it}} = \sum\nolimits _{j = i}^{j = n}{{{\tau _j}\pi dL} \over n} + {p_b}{{\pi {d^2}} \over 4} Pib=j=i+1j=nτjπdLn+pbπd24 {P_{ib}} = \sum\nolimits _{j = \left({i + 1} \right)}^{j = n}{{{\tau _j}\pi dL} \over n} + {p_b}{{\pi {d^2}} \over 4}

The axial stresses for the element ‘i’ on its top and bottom faces are σit=pb+j=ij=n4L/dτjn {\sigma _{it}} = {p_b} + \sum\nolimits _{j = i}^{j = n}{{4\left({L/d} \right){\tau _j}} \over n} σib=pb+j=i+1j=n4L/dτjn {\sigma _{ib}} = {p_b} + \sum\nolimits _{j = \left({i + 1} \right)}^{j = n}{{4\left({L/d} \right){\tau _j}} \over n}

The average axial stress on the element, ‘i’ σvi=σit+σib2=pb+j=i+1j=n4L/dτjn+2L/dτjn {\sigma _{vi}} = {{{\sigma _{it}} + {\sigma _{ib}}} \over 2} = {p_b} + \sum\nolimits _{j = \left({i + 1} \right)}^{j = n}{{4\left({L/d} \right){\tau _j}} \over n} + {{2\left({L/d} \right){\tau _j}} \over n}

The relation between shear stresses and axial stresses of the element shown in the above equation can be expressed in the matrix form as σv=A3τ \left\{{{\sigma _v}} \right\} = \left[ {{A_3}} \right]\left\{\tau \right\} where {τ} is the shear stress column vector of size (n+1) for the granular pile, including normalized stresses on the base, and {σv} is the axial stress column vector of size (n+1).

Matrix [A3] relates the shear and axial stresses as per equation (17), and it is an upper triangular matrix of size (n+1). A3=2L/dn4L/dn4L/dn102L/dn4L/dn1002L/dn12L/dn4L/dn102L/dn1001 \left[ {{A_3}} \right] = \left[ {\matrix{{{{2\left({L/d} \right)} \over n}} & {{{4\left({L/d} \right)} \over n}} & {{{4\left({L/d} \right)} \over n}} & - & - & - & - & - & 1 \cr 0 & {{{2\left({L/d} \right)} \over n}} & {{{4\left({L/d} \right)} \over n}} & - & - & - & - & - & 1 \cr 0 & 0 & {{{2\left({L/d} \right)} \over n}} & - & - & - & - & - & 1 \cr - & - & - & - & - & - & - & - & - \cr - & - & - & - & - & - & - & - & - \cr - & - & - & - & - & - & - & - & - \cr - & - & - & - & - & - & {{{2\left({L/d} \right)} \over n}} & {{{4\left({L/d} \right)} \over n}} & 1 \cr - & - & - & - & - & - & 0 & {{{2\left({L/d} \right)} \over n}} & 1 \cr - & - & - & - & - & - & 0 & 0 & 1 \cr}} \right]

Granular pile displacements:

The displacement of GP is determined from displacement of the top of the GP ρt. The settlement of the first element of the granular pile is ρ1ppv=S1ppvd=ρτεv1Δz2d \rho _1^{ppv} = {{S_1^{ppv}} \over d} = {\rho _\tau} - {\varepsilon _{v 1}}{{\Delta z} \over {2d}} where

ΔZ=L/n = the length of the element, εv1 = the axial strain of GP’s first element,

S1ppv = the displacement of the first node, and ρ1ppv = the normalized displacement of the first node.

Thus, the displacement of any element ‘i’ is written as ρippv=ρtj=1j=i1εvjΔzdεviΔz2d \rho _i^{ppv} = {\rho _{\rm{t}}} - \sum\nolimits _{{\rm{j}} = 1}^{{\rm{j}} = \left({{\rm{i}} - 1} \right)}{\varepsilon _{{\rm{vj}}}}{{\Delta {\rm{z}}} \over {\rm{d}}} - {\varepsilon _{{\rm{vi}}}}{{\Delta {\rm{z}}} \over {2{\rm{d}}}} where εvi is the axial strain of ith element of GP and εvj is the axial strain of jth element of GP.

In order to determine the settlement of the base of GP, the strain at the base is εb=dSppvdz=pbEgp {\varepsilon _{\rm{b}}} = - {{{\rm{d}}{{\rm{S}}^{{\rm{ppv}}}}} \over {{\rm{dz}}}} = {{{{\rm{p}}_{\rm{b}}}} \over {{{\rm{E}}_{{\rm{gp}}}}}}

The above equation can be rewritten by using a finite difference scheme with unequal spacing intervals as 4Sn1ppv36Snppv+32Sn+1ppv12Δz/d=pbEgp {{4{\rm{S}}_{{\rm{n}} - 1}^{{\rm{ppv}}} - 36{\rm{S}}_{\rm{n}}^{{\rm{ppv}}} + 32{\rm{S}}_{{\rm{n}} + 1}^{{\rm{ppv}}}} \over {12\left({\Delta {\rm{z}}/{\rm{d}}} \right)}} = - {{{{\rm{p}}_{\rm{b}}}} \over {{{\rm{E}}_{{\rm{gp}}}}}} where Sn-1ppv = displacement of element ‘n-1’, Snppv = displacement of element ‘n’, and Sn+1ppv = displacements of elements n+1.

The normalized form of the above equation is 4ρn1ppv36ρnppv+32ρn+1ppv=pbEgp12L/dn 4\rho _{{\rm{n}} - 1}^{{\rm{ppv}}} - 36\rho _{\rm{n}}^{{\rm{ppv}}} + 32\rho _{{\rm{n}} + 1}^{{\rm{ppv}}} = - {{{{\rm{p}}_{\rm{b}}}} \over {{{\rm{E}}_{{\rm{gp}}}}}}{{12\left({{\rm{L}}/{\rm{d}}} \right)} \over {\rm{n}}}

Substituting the values of ρn-1ppv and ρnppv from Eq. (19) and rearranging the terms ρn+1ppv=ρtj=1j=n2εvjΔzd3432εvn1Δzd1832εvnΔzd632L/dpbnKgpES \matrix{{\rho _{{\rm{n}} + 1}^{{\rm{ppv}}} = {\rho _{\rm{t}}} - \sum\nolimits _{{\rm{j}} = 1}^{{\rm{j}} = \left({{\rm{n}} - 2} \right)}{\varepsilon _{{\rm{vj}}}}{{\Delta {\rm{z}}} \over {\rm{d}}} -} \cr {- {{34} \over {32}}{\varepsilon _{{\rm{v}}\left({{\rm{n}} - 1} \right)}}{{\Delta {\rm{z}}} \over {\rm{d}}} - {{18} \over {32}}{\varepsilon _{{\rm{vn}}}}{{\Delta {\rm{z}}} \over {\rm{d}}} - {6 \over {32}}{{\left({{\rm{L}}/{\rm{d}}} \right){{\rm{p}}_{\rm{b}}}} \over {{\rm{n}}{{\rm{K}}_{{\rm{gp}}}}{{\rm{E}}_{\rm{S}}}}}} \cr}

Combining equations (20) and (24) to get the vertical displacements of GP, one gets ρppv=ρt1+B3σvES \left\{{{\rho ^{{\rm{ppv}}}}} \right\} = {\rho _{\rm{t}}}\left\{1 \right\} + \left[ {{{\rm{B}}_3}} \right]\left\{{{{{\sigma _{\rm{v}}}} \over {{{\rm{E}}_{\rm{S}}}}}} \right\} where B3=L/dnKgp0.500010.500110.5110.501134321832632n+1×n+1 \left[ {{{\rm{B}}_3}} \right] = {{\left({{\rm{L}}/{\rm{d}}} \right)} \over {{\rm{n}}{{\rm{K}}_{{\rm{gp}}}}}}{\left[ {\matrix{{- 0.5} & 0 & 0 & - & - & - & - & - & 0 \cr {- 1} & {- 0.5} & 0 & - & - & - & - & - & 0 \cr {- 1} & {- 1} & {- 0.5} & - & - & - & - & - & - \cr - & - & - & - & - & - & - & - & - \cr - & - & - & - & - & - & - & - & - \cr - & - & - & - & - & - & - & - & - \cr - & - & - & - & - & - & - & - & - \cr {- 1} & {- 1} & - & - & - & - & - & {- 0.5} & 0 \cr {- 1} & {- 1} & - & - & - & - & {- {{34} \over {32}}} & {- {{18} \over {32}}} & {- {6 \over {32}}} \cr}} \right]_{\left({{\rm{n}} + 1} \right) \times \left({{\rm{n}} + 1} \right)}}

Using the relationship between shear stresses and axial stresses (Eq. 17), the displacement of GP nodes in the vertical direction can be expressed in terms of shear stresses as ρppv=ρt1+D3τES \left\{{{\rho ^{{\rm{ppv}}}}} \right\} = {\rho _{\rm{t}}}\left\{1 \right\} + \left[ {{{\rm{D}}_3}} \right]\left\{{{\tau \over {{{\rm{E}}_{\rm{S}}}}}} \right\} where [D3] = [B3] [A3], and the size of square matrix [D3] is (n+1).

Soil displacement at the nodes of granular pile with annular raft

Soil displacement equations for a granular pile are represented by Eq. 28, ρsp=Sspd=l=1l=NpIspvvτES++IspAprAES+IspBprBES \matrix{{\left\{{{\rho ^{sp}}} \right\} = \left\{{{{{S^{sp}}} \over d}} \right\} = \left[ {\sum\nolimits _{l = 1}^{l = Np}\left[ {{I^{sp{\rm{vv}}}}} \right]} \right]\left\{{{\tau \over {{E_S}}}} \right\} +} \cr {+ \left[ {{I^{spA}}} \right]\left\{{{{{p_{rA}}} \over {{E_S}}}} \right\} + \left[ {{I^{spB}}} \right]\left\{{{{{p_{rB}}} \over {{E_S}}}} \right\}} \cr} where {Ssp} is the vector of soil displacements of size (n+1) and {ρsp} is the vector of normalized soil displacements of size (n+1) each for GP nodes.

[Ispvv] is a square matrix of size (n+l) with the coefficients evaluated for the effect of elemental shear stresses and base pressure of the GP; the influence of stresses of all adjacent GPs is taken at the central nodes of GP as shown in Fig. 3 in order to achieve an average influence; [IspA] is a matrix of size, (n+l) × kr with the coefficients evaluated for the effect of the contact stresses on sector ‘A’ on the GP node. [IspB] is a matrix of size (n+1) ×kr for the influence of contact stresses on sector ‘B’ on GP nodes.

Granular Pile and Annular Raft Displacements

The granular pile displacement equations are similar to equation (27) ρppv=ρt1+D3τES \left\{{{\rho ^{{\rm{ppv}}}}} \right\} = {\rho _{\rm{t}}}\left\{1 \right\} + \left[ {{{\rm{D}}_3}} \right]\left\{{{\tau \over {{{\rm{E}}_{\rm{S}}}}}} \right\} where [D3] is a square matrix of size, (n+1) =[A][B], {ρppv} is the normalized displacement vector of GP of size, (n+1). ρt is the normalized top displacement of GP. The annular raft is considered rigid. Hence, the displacements of nodes of sectors ‘A’ and ‘B’ are all equal to the top displacement of GP, ρt. For sectors ‘A’ and ‘B,’ annular raft displacement equations are ρApa=ρt1 \left\{{\rho _A^{pa}} \right\} = {\rho _t}\left\{1 \right\} ρBpa=ρt1 \left\{{\rho _B^{pa}} \right\} = {\rho _t}\left\{1 \right\}

Compatibility of Displacements

Solutions are obtained in terms of contact pressures for sectors ‘A’ and ‘B’ and shear stresses through the compatibility of displacements. Applying the compatibility condition for displacements of nodes in sector ‘A’ (Eqs (6) and (30)) ρAsa=ρApal=1l=NpIAsapvτES+IAsaAprAES+IAsaBprBES=ρt1 \matrix{{\left\{{\rho _A^{sa}} \right\} = \left\{{\rho _A^{pa}} \right\}} \cr {\left[ {\sum\nolimits _{l = 1}^{l = Np}\left[ {I_A^{sapv}} \right]} \right]\left\{{{\tau \over {{E_S}}}} \right\} + \left[ {I_A^{saA}} \right]\left\{{{{{p_{rA}}} \over {{E_S}}}} \right\} + \left[ {I_A^{saB}} \right]\left\{{{{{p_{rB}}} \over {{E_S}}}} \right\} = {\rho _t}\left\{1 \right\}} \cr}

Similarly, for nodes in Sector ‘B,’ from Eqs. (7) and (31) ρBsa=ρBpal=1l=NpIBsapvτES+IBsaAprAES+IBsaBprBES=ρt1 \matrix{{\left\{{\rho _B^{sa}} \right\} = \left\{{\rho _B^{pa}} \right\}} \cr {\left[ {\sum\nolimits _{l = 1}^{l = Np}\left[ {I_B^{sapv}} \right]} \right]\left\{{{\tau \over {{E_S}}}} \right\} + \left[ {I_B^{saA}} \right]\left\{{{{{p_{rA}}} \over {{E_S}}}} \right\} + \left[ {I_B^{saB}} \right]\left\{{{{{p_{rB}}} \over {{E_S}}}} \right\} = {\rho _t}\left\{1 \right\}} \cr}

For nodes along the granular pile, the compatibility condition from (Eqs (28) and (29)) is ρsp=ρppvEτES+IspAPrAES+IspBPrBES=ρt1 \matrix{{\left\{{{\rho ^{sp}}} \right\} = \left\{{{\rho ^{ppv}}} \right\}} \cr {\left[ E \right]\left\{{{\tau \over {{E_S}}}} \right\} + \left[ {{I^{spA}}} \right]\left\{{{{{P_{rA}}} \over {{E_S}}}} \right\} + \left[ {{I^{spB}}} \right]\left\{{{{{P_{rB}}} \over {{E_S}}}} \right\} = {\rho _t}\left\{1 \right\}} \cr} where E=l=1l=NpIspvvD3 \left[ E \right] = \left[ {\sum\nolimits _{l = 1}^{l = Np}\left[ {{I^{sp{\rm{vv}}}}} \right]} \right] - \left[ {{D_3}} \right] of size (n+1) × (n +1)

Equations (32), (33), and (34) are solved simultaneously to obtain the contact pressures for sectors ‘A’ and ‘B’ and interfacial shear stresses along GP with the base pressure. The displacement of the annular raft is obtained from the evaluated stresses.

The settlement of the GP–annular raft foundation is expressed as Sagpr=PE3dlagpr {S_{agpr}} = {P \over {{E_3}d}}{l_{agpr}} Sar=PESdoIar {\rm S_{{\rm{ar}}}} = {{\rm{P}} \over {{{\rm{E}}_{\rm{S}}}{{\rm{d}}_{\rm{o}}}}}{{\rm{I}}_{{\rm{ar}}}} where Iagpr is the settlement influence factor for the annular raft on granular piles, which depends on the geometric and stiffness parameters related to GP and annular raft. The geometric parameters – annular ratio, Dr, and normalized annular width, Dg, related to annular raft dimensions – are defined as Dr=dridro,where0<Dr<1and {D_r} = {{{d_{ri}}} \over {{d_{ro}}}},\;\;\;where\;0 < {D_r} < 1\;\;\;and Dg=drodri2d {D_g} = {{{d_{ro}} - {d_{ri}}} \over {2d}} where dro and dri are the outer and inner diameters of the annular raft and ‘d’ is the diameter of the granular pile. Sar is the normalized settlement of an annular raft only (without GPs), and Iar is the SIF of an annular raft without GPs.

Spacing of Gps in Terms of Dr and Dg

The spacing of a group of four granular piles is calculated in terms of Dr and Dg as follows. The granular piles are installed in such a way that the center of the GP lies on the equal area axis of the annular raft (r). From Fig. (5), equal area of the annular raft can be written as πr2ri2=πro2r2 \pi \left({{r^2} - r_i^2} \right) = \pi \left({r_o^2 - {r^2}} \right) 2r2=ro2+ri2r=ro2+ri22 \matrix{2{r^2} = r_o^2 + r_i^2 \cr r = \sqrt {{{r_o^2 + r_i^2} \over 2}}} 2S=2r \sqrt 2 S = 2r

By substituting the value of r from equation (37), spacing S can be written as S=2.ro2+ri22 s = \sqrt 2 .\sqrt {{{r_o^2 + r_i^2} \over 2}}

By normalizing spacing with dia. of the pile (d), the above equation can be written as Sd=dro2+dri24 {S \over d} = \sqrt {{{d_{ro}^2 + d_{ri}^2} \over 4}}

Annular ratio (Dr) and normalized annular width (Dg) are defined as Dr=dridro&Dg=drodri2ddri=droDr \matrix{{{D_r} = {{{d_{ri}}} \over {{d_{ro}}}}\;\& \;{D_g} = {{{d_{ro}} - {d_{ri}}} \over {2d}}} \cr {{d_{ri}} = {d_{ro}} \cdot {D_r}} \cr}

By substituting the value of dri Dg=dro1Dr2d {D_g} = {{{d_{ro}}\left({1 - {D_r}} \right)} \over {2d}}

Now, dro and dri can be written as dro=2dDg1Dr {d_{ro}} = {{2d{D_g}} \over {1 - {D_r}}} dri=2dDg1DrDr {d_{ri}} = {{2d{D_g}} \over {1 - {D_r}}}{D_r}

By substituting the values of dro and dri from equations (46) and (47) in equation (43), normalized spacing can be written as Sd=4d2Dg21Dr2+4d2Dg21Dr2Dr24Sd=d2Dg2+d2Dg2Dr21Dr2 \matrix{{S \over d} = \sqrt {{{{{4{d^2}D_g^2} \over {{{\left({1 - {D_r}} \right)}^2}}} + {{4{d^2}D_g^2} \over {{{\left({1 - {D_r}} \right)}^2}}}D_r^2} \over 4}}\cr{S \over d} = \sqrt {{{{d^2}D_g^2 + {d^2}D_g^2D_r^2} \over {{{\left({1 - {D_r}} \right)}^2}}}}}

The overall response of the GP–annular raft foundation is evaluated in terms of the settlement influence factor, the normalized GP–soil interfacial shear stresses, the percentage load carried by GP, and normal contact pressure distributions for sectors ‘A’ and ‘B’ of the annular raft. The parameters which affect the overall response of annular raft with GPs are (i) the geometric ones – the annular ratio, Dr, and normalized annular width, Dg, and length to diameter ratio of GP, L/d; (ii) the number of granular piles, Np; and (iii) the relative GP–soil stiffness, Kgp = (Ep/Es).

Figure 5:

Spacing of group of four GPs in terms of Dr and Dg.

Results and Discussion
Comparison of the present work

The results from the present study are validated with the previous one by [48] for a group of four GPs for spacings 2 and 3. Using the above expression of spacing, the spacing of four GPs is calculated in terms of Dr and Dg. The spacing achieved for Dr=0.2 and Dg=2 is 2.55, which lies in between the spacings 2 and 3.

As a result, a plot of SIF v/s Kgp is depicted in order to validate and compare the results, and with the spacing of 2.55, the SIF results are projected to fall between the spacings 2 and 3. The comparison of the present study is depicted in Fig. 6.

Figure 6:

Comparison of variation of SIF with Kgp for different spacing [45].

Validation of the present work

The SIF values of the present work are compared with the experimental work [41] that is shown in Table 2. The SIF values show good agreement with the experimental analysis of the annular raft conducted by [4950].

Figure 7 can be referred to as a design chart to calculate the settlement of the annular raft. According to the results, increasing the annular ratio (Dr) increases the value of the settlement influence factor (Ir). The corresponding values of Ir for Dr =0.2 and Dr=0.8 are 0.8024 and 0.8010, respectively. It is observed that there is no significant change in the value of Iar for Dr up to 0.6, and for Dr>0.6, the Iar values significantly increased. As per the results, as the inner diameter of the annular raft increases, the value of settlement of the annular raft also increases. The settlement of the annular raft increases as the inner diameter of the raft becomes larger. This is because, with a larger inner diameter, the annular raft behaves more like a strip, resulting in a reduced area of the raft. Consequently, the reduced area contributes to an increase in the settlement of the annular raft.

Figure 7:

Variation of SIF (only annular raft without GPs) with Dr.

Parametric study:

The outcomes of a parametric investigation utilizing the continuum approach are disclosed, showcasing the solutions acquired across the specified parameter ranges detailed in Table 1.

Parameters used in the study.

S. No. Parameters Corresponding values
1. Kgp 10–400
2. Dr 0.2, 0.4, 0.6, 0.8
3. Dg 2, 3, 4, 5
4. L/d 5–40
5. Np 2–12

Validation of the SIF values.

S.No. Variable verified (Dr) 0.2 0.4 0.6 0.8
1. Al Sanad (1993) [49] 0.814 0.709 0.532 0.345
2. Egorov (1965) [50] 0.79 0.80 0.82 0.90
3. Present analysis 0.80 0.80 0.81 0.85

The results of the above analysis are presented in the form of design charts for ready use. The effect of an annular raft resting on a group of GPs is evaluated by comparing the results of a group of four GPs with and without the annular raft. In the case of four GPs without the annular raft, the total load is equally distributed to the GPs, and the spacing of GPs is calculated in terms of Dr and Dg in order to keep the spacing of GPs same as GPs with the annular raft.

The variation of SIF (Iagpr) with relative stiffness of GPs (Kgp) is depicted in Figure 8 for normalized annular width (Dg) range of 2–5, L/d=10, and annular ratio (Dr) of 0.2. SIF for an annular raft with GPs is very less in comparison to SIF for GPs without a raft. It shows that the annular raft participates in the load transfer and significantly decreases the value of SIF. With the increase of the annular width, the area of the annular raft increases resulting in smaller values of SIF. SIF for the annular raft with GPs decreases marginally with the increase of relative stiffness of GPs as expected.

Figure 8:

Variation of Iagpr with Kgp for a group of four GPs having Dr=0.2 and L/d=10 (a) without the annular raft and (b) with the annular raft.

The rate of decrease of SIF with Kgp decreases with the increase of Dg. A higher annular ratio, Dr, represents the higher internal diameter of the annular raft, i.e., a large area of the annular raft for the same value of annular width. Thus, the effect of granular piles in reducing the settlement influence factor of annular raft decreases with the increase of Dr.

SIF value for Dr = 0.2 and Dg = 2 decreased from 0.128 to 0.085 for Kgp, increasing from 10 to 400. Corresponding values for Dr = 0.2 and Dg = 5 are 0.061 and 0.054 for Kgp = 10 and 400, respectively. The values of SIF are very high comparatively for four GPs without raft for the same spacing. It shows that the annular raft participates in load transfer and reduces the settlement.

For the parameters used in Figure 8, SIF is evaluated for Dr =0.4 and depicted in Figure 9. These results are very similar to those given in Figure 8.

Figure 9:

Variation of Iagpr with Kgp of the group of four GPs with and without raft for Dr=0.4 and L/d=10: (a) without annular raft and (b) with annular raft.

SIF values for Dr=0.4 and Dg=2 are 0.104 and 0.074 for Kgp =10 and 400, respectively. Corresponding values for Dr = 0.4 and Dg = 5 are 0.046 and 0.043 for Kgp = 10 and 400, respectively. SIF values decrease as expected with an increase in the annular ratio.

SIF values are evaluated for the same parameters as before, for Dr =0.6, it is depicted in Figure 10. The results are very similar once again to those shown in Figures 8 and 9. SIF values for Dr=0.6 and Dg=2 are 0.075 and 0.060 for Kgp =10 and 400, respectively. Corresponding values for Dr = 0.6 and Dg = 5 are 0.031 and 0.030 for Kgp = 10 and 400, respectively. As the annular ratio increased from Dr=0.4 to Dr=0.6, the SIF values decreased as expected, and the rate of decrease of SIF continuously decreased as the annular ratio increased.

Figure 10:

Variation of Iagpr with Kgp of a group of four GPs with and without raft for Dr=0.6 and L/d=10: (a) without annular raft and (b) with annular raft.

Using the same parameters, SIF is evaluated for Dr =0.8, as depicted in Figure 11, and the results are very similar to those in Figures 8, 9, and 10. SIF values of Dr = 0.8 and Dg = 2 are 0.039 and 0.037 for Kgp =10 and 400, respectively. Corresponding values for Dr = 0.8 and Dg = 5 are 0.017 and 0.016 for Kgp = 10 and 400, respectively. For a higher annular ratio, the spacing of GPs also increased, which results in lower values of SIF when only GPs are provided. The minimum rate of decrease of the SIF value is recorded for the highest annular ratio, i.e., Dr=0.8. It shows that the annular raft significantly reduces the settlement when it is rested over a group of four granular piles.

Figure 11:

Variation of Iagpr with Kgp of a group of four GPs with and without raft for Dr=0.8 and L/d=10.

For Dg values of 3 and 4, the Iagpr remains relatively constant. This can be attributed to the increased annular width of the annular raft. With a wider annular width, the raft area increases, leading to a scenario where the majority of the load is borne by the annular raft rather than being shared by the granular piles (GPs). Consequently, the load on the GPs is reduced in these cases.

The variation of SIF with Kgp for different numbers of GPs for L/d = 10, Dr=0.4, and Dg=3 is depicted in Figure 12. It is observed that by increasing the number of GPs, the SIF decreased as expected. The minimum value of SIF is recorded for 12 GPs. It is also observed that as the Kgp of GPs increases, the SIF also decreases. The significant change in the rate of change of SIF is up to the value of Kgp=100; after that, the rate of decrease of SIF decreased.

Figure 12:

Variation of Iagpr with Kgp - Effect of number of granular piles (Np).

In order to evaluate the effect of parameter L/d on SIF, the SIF variation with Kgp is depicted in Figure 13 (a) for Dg=2, Dr=0.2 and 0.4, and L/d=5-40. The comparison of SIF between Dr=0.2 and 0.4 for a range of L/d is also shown in Figure 13 (a). The value of SIF for Dr=0.4 is less than that of Dr=0.2 for a particular L/d that shows the SIF decreases as the annular ratio increases. It is also observed from the above results that for larger L/d, the value of SIF decreases significantly up to the Kgp=100; after that, the rate of decrease of SIF decreases. The rate of decrease of SIF is high up to Kgp=100 due to the low-bearing capacity of the GPs, and the rate of decrease of SIF decreases after the value of Kgp=100 because as Kgp increases, the load-bearing capacity of the GPs also increases.

The variation and comparison of SIF for Dr=0.6 and 0.8 for different L/d are depicted in Figure 13 (b). It is observed from the results that for the same annular width (Dg=2) by increasing the annular ratio, the SIF decreases significantly, and the SIF values are also decreasing for GPs having a larger L/d ratio. As the relative stiffness of GPs (Kgp) increases, the capacity of GPs increases; hence, SIF decreases. By increasing the annular ratio from 0.2 to 0.8 for Dg=2 and L/d=5, the SIF value significantly decreased from 0.135 to 0.042 (i.e., 68.90% decrement). By increasing the L/d up to 40, for Dg=2, and Kgp=10, the SIF value for Dr=0.2 and 0.8 decreased 67.54%, which shows that increasing the L/d of the GPs can reduce the settlement.

Figure 13:

Variation of Iagpr with Kgp for Dg=2, with the effect of Dr and L/d: (a) Dr=0.2 and 0.4 (b) Dr=0.6 and Dr=0.8.

Similar results are obtained for Dg=3, for a range of Dr=0.2–0.4 and L/d=5–40 depicted in Figure 14 (a). The SIF value for Dg=3, L/d=5, and Kgp decreases from 0.099 to 0.028 by increasing the Dr from 0.2 to 0.8.

The SIF values for Dg=3 and L/d =5–40 for greater Dr=0.6 and 0.8 are evaluated and depicted in Figure 14 (b). It is observed from the results that the difference in SIF values in Dr=0.2 to 0.4 is less in comparison to greater annular ratios, i.e., Dr=0.6 and 0.8. It is also observed that the SIF values are decreasing by increasing the annular width and L/d. For the same annular ratio and the annular width, increasing the L/d of GPs also significantly decreases the SIF values.

Figure 14:

Variation of Iagpr with Kgp for Dg=3 and with variation of Dr and L/d: (a) Dr=0.2 and Dr=0.4; (b) Dr=0.6 and Dr=0.8.

Similar results are obtained for Dg=4, Dr=0.2–0.4, and Dr=0.6–0.8 in Figure 15 (a) and (b), respectively. Similar trends and results are observed for the given range of parameters.

Figure 15:

Variation of Iagpr with Kgp for Dg=4 and with variation of Dr and L/d: (a) Dr=0.2 and Dr=0.4; (b) Dr=0.6 and Dr=0.8.

The SIF variation with Kgp is depicted in Figure 16 (a) for Dg=5, Dr=0.2 and 0.4, and different values of L/d. It is observed that there is a significant decrement in SIF values for Dg=5 in comparison to Dg=2. By increasing the Dg=2 to Dg=5, by keeping Dr =0.2, and L/d=5, the SIF values for Kgp=10 decreased up to 54.07%.

Figure 16:

Variation of Iagpr with Kgp for Dg=5 and with variation of Dr and L/d: (a) Dr=0.2 and Dr=0.4; (b) Dr=0.6 and Dr=0.8.

Similarly, the variation of SIF with Kgp for Dg =5, Dr=0.6–0.8, and L/d=5–40 is depicted in Figure 16 (b). For Dg=5, the comparison in SIF values between Dr=0.6 and 0.8 for a range of L/d=5–40 is comparatively more significant as compared to lower values of Dg. It is observed from the results that the rate of decrement of SIF values decreases by increasing Dr=0.6 to 0.8. The minimum SIF value is recorded for Dg=5, Dr=0.8, and L/d=40.

In order to assess the effect of annular ratio and annular width simultaneously, the variation of SIF with Kgp is evaluated by keeping L/d=10 for the group of four GPs.

The variation of SIF with Kgp is depicted in Figure 17 for Dr=0.2 and 0.4 for the range of Dg=2–5. The results show that the SIF decreases significantly by increasing the annular ratio, Dr, and the annular width, Dg. As the relative stiffness of GPs (Kgp) increases, the strength of the GPs increases; hence, the rate of decrease of SIF reduces. For the same annular ratio (Dr=0.2), by increasing the annular width (Dg) from 2 to 5, the SIF decreased 52.27%. Similarly, for the same annular ratio, Dr=0.4, by increasing the annular width (Dg) from 2 to 5, the SIF decreased 55.24%. By providing an annular raft having Dr=0.4, Dg=5, the SIF value decreased up to 63.63% as compared to an annular raft having Dr=0.2, Dg=2. The results clearly show that the higher annular width has a comparatively larger area to distribute the load resulting in reduced values of SIF.

Figure 17:

Variation of Iagpr with Kgp, effect of Dr and Dg for L/d=10.

Similarly, the results are evaluated and depicted in Figure 18 for Dr=0.6 and 0.8 and Dg=2–5 for each Dr. The SIF decreased for larger annular ratios, such as 0.6 and 0.8, and for the same annular ratio, and the SIF decreased by increasing the annular width due to the large size of the raft and the space between the GPs. For the same annular ratio (Dr=0.6), by increasing the annular width (Dg) from 2 to 5, the SIF decreased 58.29%. Similarly, for the same annular ratio, Dr=0.8, by increasing the annular width (Dg) from 2 to 5, the SIF decreased 59.11%. By providing an annular raft having Dr=0.4, Dg=5, the SIF value decreased up to 77.70% as compared to an annular raft having Dr=0.2, Dg=2.

Figure 18:

Variation of Iagpr with Kgp, effect of Dr and Dg.

The variation of the ratio of settlements of the annular granular piled raft to the annular raft, Sagpr/Sar, with Kgp is shown in Figure 19, along with the influence of Dg. The ratio of settlements decreases with the increase in the relative stiffness of GPs. The ratio, Sagpr/Sar, is more for larger values of Dg due to an increase in the area of the annular raft resulting in a reduction of the influence of GPs on settlement. Sagpr/Sar values for L/d=10, Dr=0.2, and Dg=2 are 0.814 and 0.542 for Kgp=10 and 400, respectively. Corresponding values for Dr=0.2 and Dg=5 are 0.972 and 0.854, respectively. Similar effects are observed with the increase of annular ratio, Dr.

Figure 19:

Variation of the ratio of settlement of annular granular piled raft to the settlement of annular raft, Sr with Kgp – effect of Dg for L/d=10.

The influence of the relative length of GPs is critically analyzed and depicted in the form of variation of the ratio Sagpr/Sar with Kgp in Figure 20. The ratio of settlements decreases with the increase of L/d. The reductions are more for L/d, increasing from 10 to 20 in comparison to those for L/d, increasing from 20 to 40. The values of Sagpr/Sar for Kgp=100 is 0.817, 0.708, and 0.652 for L/d=10, 20, and 40, respectively. There is a 20.14% reduction in the value of the ratio Sagpr/Sar by increasing the L/d =10 to 40.

Figure 20:

Variation of the ratio of settlement of annular granular piled raft to the settlement of annular raft, Sr with Kgp – effect of L/d for Dr=0.4, Dg=3.

The variation of the ratio of the settlement of the annular granular piled raft to the settlement of the annular raft with Np is depicted in Figure 21 for the evaluation of the effect of number of GPs. It is observed from the results that the value of Sr decreases by increasing the number of the pile (Np). It is also observed that by increasing the L/d of the GPs, the settlement ratio decreases by further increasing the number of GPs. By increasing the L/d of the GPs, the load-bearing capacity of the GPs increases, resulting reduction in the settlement ratio of the GPs. There is a significant reduction in the Sr by increasing L/d, and the rate of decrease increases as the L/d increases.

Figure 21:

Variation of the ratio of settlement of the annular granular piled raft to the settlement of annular raft, Sr with Np – effect of L/d for Dr=0.4, Dg=3, Kgp=100.

The normalized contact pressure distributions at the raft–soil interface β2=sin12OgOpdsinψ \left({\beta _2} = {sin ^{- 1}}\left({{{2{O_g}{O_p}} \over d}sin \psi} \right)\right) with normalized radial distance (R1 = r/d) are depicted in Figure 22. For sectors ‘A’ and ‘B’ along with the influence of granular piles, the stresses for the sectors of the annular raft with GP, i.e., sector ‘A,’ are less particularly in the region close to the granular pile as compared to those for the sector without the granular pile, i.e., sector ‘B.’ The annular raft stresses at the inner and outer edges of the annular raft are almost identical for both sectors ‘A’ and ‘B’ of the annular raft. The raft stresses decrease with the increase of number of GPs. The value of Praft at a radial distance of 4d from the center of the annular raft without GP is 1.09 and decreased to 0.52, 0.45, and 0.40 for sector ‘B’ of the annular raft with number of GPs 4, 6, and 8, respectively.

Figure 22:

Variation of normalized contact pressure distribution at raft–soil interface, Praft with normalized radial distance (R1) – effect of Np.

Furthermore, the analysis reveals that increasing the number of granular piles (GPs) results in reduced stresses within the raft. This reduction occurs due to the load-sharing mechanism facilitated by the GPs.

The variation in stress distribution highlights an interesting observation: the contact stresses in sector A (the region where the piles are present) are lower compared to sector B. This disparity is primarily due to the presence of piles in sector A, which effectively redistributes and shares the load within that specific region. As a result, the raft experiences reduced contact stresses in the vicinity of the pile region (sector A) due to the load-bearing contribution of the GPs.

This observation underscores the significance of the presence of GPs in mitigating contact stresses and optimizing stress distribution within the raft system, particularly in the sector where the piles are located.

The annular raft stresses for sectors ‘A’ and ‘B’ decrease with the increase of relative stiffness of GPs, as presented in Figure 23. The reduction in stresses with Kgp is almost uniform along the radial distance from the inner edge of the annular raft to the outer edge of the annular raft. The contact stresses of the annular raft at the raft–soil interface are significantly reduced in the region of the pile in sector ‘A.’ It is observed that the raft contact stresses (Praft) are almost identical at the inner and outer edges of the annular raft for a particular Kgp, except in the region of the pile. As expected, the lowest value of raft stresses was recorded for the GP having Kgp=400.

Figure 23:

Variation of normalized contact pressure distribution at raft–soil interface, Praft, with normalized radial distance (R1) – effect of Kgp.

The contact stresses at the interface between the annular raft and the underlying soil are significantly reduced in the region where the pile is located in sector ‘A.’ This reduction is attributed to the load-bearing contribution of the piles, which effectively redistributes and shares the load in that specific region.

The contact stresses (Praft) along the inner and outer edges of the annular raft are almost identical for a particular value of Kgp, except in the region of the pile. This observation aligns with expectations, as the presence of the pile influences the stress distribution locally.

The distribution of shear stresses along the GP–soil interface, normalized with the total load on an annular raft, i.e., [τN=τ/πdL] with a normalized depth of GP, ZN=z/L, is depicted in Figure 24 for the influence of Dg.

Figure 24:

Comparison of normalized shear stress variation with the normalized depth for a group of four GPs with and without annular raft for Dr=0.2, L/d=10, and Kgp=100.

The shear stress variation for a group of four granular piles is calculated with and without an annular raft in order to analyze the effect of the annular raft on the group of four GPs. The shear stresses decrease with the increase of Dg as the size of the raft increases. It is clear from the results that the annular raft plays a significant role in load bearing as compared to GPs. The shear stresses are significantly less in the GPs when the annular raft is provided over GPs. As the raft is placed over the GPs, the raft takes the maximum load, and the shear stresses induced at the GP–soil interface are less in the top portion of GPs and increased slightly near the base of the GPs.

For Dr=0.2 and Dg=2, the value of shear stresses for a group of four GPs is recorded at 2.324, and for a Group of four GPs with an annular raft, the value of shear stress is 0.123 at the top of the GPs. It shows that by providing the annular raft, the shear stresses of the GPs are reduced up to 94% at the top of GPs and 72% at the base of the GPs. For Dg=3, the values of shear stresses for a group of four GPs with and without raft are recorded 0.107 and 2.233, respectively; at the top of GPs and at the base of the GPs, the values are 0.329 and 1.064, respectively. For Dr=0.2 and Dg=3, the shear stresses at the top of the GPs are reduced up to 95.20%, and at the base of the GPs, they are reduced up to 69.05%. Similarly, for Dg=5, the shear stresses of GPs with and without raft at the top of GPs are 2.134 and 0.084, respectively, and at the base of the GPs, they are 0.913 and 0.208, respectively. For Dg=5, the annular raft reduced the shear stresses of GPs up to 96.06% at the top of GPs and up to 77.22% at the base of the GPs. The results show that the annular raft significantly reduces the shear stresses of the GPs at the top and base of GPs.

The interfacial shear stresses in the group of four GPs with annular raft are calculated for the ranges of Dr =0.4, 0.6, and 0.8 also and compared with the shear stresses of a group of four GPs without annular raft at the same spacing as the spacing of GPs underneath the annular raft.

The shear stresses of a group of four GPs with and without annular raft for Dr=0.4 are depicted in Figure 25. For Dr=0.4 and Dg=2, the values of shear stresses for a group of four GPs with and without annular raft are recorded 0.106 and 2.248, respectively; at the top of the GPs and at the base of the GPs, they are 0.349 and 1.079, respectively. It shows that by providing the annular raft, the shear stresses of the GPs can be reduced up to 95.26% at the top of the GPs and 67.66% at the base of the GPs. By increasing the annular ratio from 0.2 to 0.4, the shear stresses of the GPs reduced 13.77% at the top of the GPs and 13.50% at the base of the GPs.

Figure 25:

Comparison of normalized shear stress variation with the normalized depth for a group of four GPs with and without annular raft for Dr=0.4, L/d=10, and Kgp=100.

Similarly, by increasing the annular width Dg up to 5 for the same annular ratio, Dr=0.4, the shear stresses of the GPs further reduced due to the increased width of the annular raft. For Dr=0.4 and Dg=5, the shear stresses of a group of four GPs with and without raft are recorded 0.058 and 2.101, respectively; at the top of the GPs and at the base of the GPs, they are 0.145 and 0.876, respectively.

By increasing the annular width of the annular raft, the shear stresses are reduced up to 97.21% at the top of the GPs and up to 83.36% at the base of the GPs as compared to only GPs.

Similar trends are obtained for Dr=0.6 depicted in Figure 26. As the annular ratio Dr increased to 0.6, the shear stresses significantly reduced compared to smaller annular ratios, i.e., 0.2 and 0.4. For Dr=0.6 and Dg=2, the value of shear stresses for a group of four GPs with and without annular raft is recorded 0.087 and 2.147, respectively; at the top of the GPs and at the base of the GPs, they are 0.349 and 1.079, respectively. Similarly, the shear stresses reduced with the depth and slightly increased in the bottom portion of the GPs. As the annular width increased to 5 (i.e., Dg=5), the shear stresses of the GPs with and without raft decreased because of the increased size of the annular raft. The shear stresses for Dg=5 for a group of four GPs with and without annular raft are recorded 0.032 and 2.083, respectively; at the top of the GPs and at the base of the GPs, they are 0.084 and 0.908, respectively. The shear stresses were reduced up to 98.44% at the top of the GPs and 90.69% at the base of the GPs.

Figure 26:

Comparison of normalized shear stress variation with the normalized depth for a group of four GPs with and without the annular raft for Dr=0.6, L/d=10, and Kgp=100.

The shear stress variation with depth for the annular ratio (Dr) 0.8 for different annular width of the annular raft is depicted in Figure 27. The shear stresses for Dg=2, with and without a raft, are recorded 0.033 and 2.085, respectively; at the top of the GPs and at the base of the GPs, they are 0.132 and 0.895, respectively. By providing an annular raft over GPs, there is a reduction of shear stresses of GPs up to 98.39% at the top and 85.24% at the base of the GPs. By increasing the annular width up to Dg=5, the shear stresses of GPs with and without annular raft are recorded 0.014 and 2.079, respectively; at the top of the GPs and at the base of the GPs, they are 0.047 and 0.963, respectively. By increasing the annular width of the annular raft up to Dg=5, the shear stress of GPs reduced up to 99.28% at the top of the GPs and 95.03% at the base of the GPs.

Figure 27:

Comparison of normalized shear stress variation with the normalized depth for a group of four GPs with and without the annular raft for Dr=0.8, L/d=10, and Kgp=100.

It is seen from the above results that in comparison to only GPs, the annular raft over GPs can reduce the shear stresses of the GPs significantly and can transfer the maximum load. The annular raft reduces the shear stresses of GPs.

The annular ratio and the annular width play a significant role in the strength of the annular raft and its performance. As the annular ratio of the annular raft increased, the internal diameter of the annular raft increased, and the raft tended to behave like a strip, and the shear stresses of GPs got reduced. For a particular annular ratio, by increasing the annular width of the annular raft, a further significant reduction is seen in the shear stresses of GPs which proves the significance of the performance of the annular raft and cost reduction.

The shear stresses of GPs get reduced up to 13.77% at the top of the GPs and 13.35% at the base of the GPs while increasing the annular ratio from 0.2 to 0.4 for Dg=2.

The shear stresses at the top and base of the GPs for different parameters are listed in Table 3. As per the results, increasing the annular ratio and annular width reduces the shear stresses significantly at the top and base of the GPs. The reduction in shear stress results from the wider annular width, which has more raft area to distribute the load and space between the GPs.

Shear stresses and its reduction due to the presence of an annular raft.

Dr Dg Shear stresses of GPs without annular raft Shear stresses of GPs with annular raft Shear stresses reduction due to annular raft (%)

Top Bottom Top Bottom Top Bottom
0.2 2 2.324458 1.079298 0.123507 0.403755 94.70 62.65
3 2.232964 1.064219 0.107169 0.328567 95.20 69.17
4 2.169796 0.974238 0.100482 0.263145 95.38 72.99
5 2.134603 0.913877 0.084327 0.208937 96.06 77.21
0.4 2 2.248837 1.079708 0.106494 0.349187 95.28 67.66
3 2.160045 0.957485 0.089982 0.261161 95.83 72.72
4 2.120533 0.892764 0.074019 0.194048 96.51 78.26
5 2.101452 0.876311 0.058483 0.145743 97.22 83.37
0.6 2 2.147183 0.935131 0.087404 0.259689 95.93 72.23
3 2.103237 0.876795 0.063182 0.171468 97.00 80.44
4 2.08833 0.886777 0.047783 0.11668 97.71 86.84
5 2.082598 0.907918 0.03232 0.08452 98.45 90.69
0.8 2 2.085437 0.895009 0.033402 0.132094 98.40 85.24
3 2.079723 0.934551 0.024073 0.080976 98.84 91.34
4 2.079205 0.954441 0.020154 0.060053 99.03 93.71
5 2.079428 0.963823 0.014868 0.047917 99.28 95.03

The effect of number of GPs on shear stress variation with normalized depth (Z1) is also evaluated and depicted in Figure 28. The shear stress variation is evaluated for Dr=0.4 and Dg=3, and the effect of number of GPs is evaluated. It is observed that shear stresses τ1 decreased with depth with the increase of no. of GPs due to a reduction in the load carried by GPs. The results indicate that as the number of granular piles increases, the shear stresses (τ1) decrease with depth. This decrease can be attributed to the fact that an increased number of granular piles leads to a reduction in the load carried by each pile. Consequently, the load is more evenly distributed among a more significant number of piles, resulting in a decrease in shear stresses with increasing depth. This behavior can be attributed to the enhanced load-sharing capacity of the granular piles, which leads to a more efficient distribution of loads within the system.

Figure 28:

Variation of τ1 with Z1 – effect of number of GPs for Dr=0.4, Dg=3, L/d=10, and Kgp=50.

The variation of shear stresses normalized with load, Pp, carried by GPs, τ1*, with the normalized depth is also evaluated and depicted in Figure 29. The normalized shear stresses τ1* decrease over the top 75% length of the GPs but increase over the rest of their length.

Figure 29:

Variation of τ1*τ1* with Z1 – effect of number of GPs for Dr=0.4, Dg=3, L/d=10, Kgp=50.

The influence of annular width is analyzed and depicted in Figure 30 in the form of variation of the percentage of applied load carried by GP (Pp/Px100) with Kgp. The percentage of load transferred to GPs increased from 10.41% for Kgp=10 to 19.35% for Kgp=400 for the annular raft with Dr=0.2 and Dg=2, i.e., comparatively smaller annular raft. By increasing the annular width of the annular raft from 2 to 5, the percentage load transferred to GPs decreased as the raft size increased, and the raft is participating more as compared to GPs in load bearing due to the increased size of the annular raft. For Dg=5, the percentage of load transferred to GPs increased from 2.78% for Kgp=10 to 10.80% for Kgp=400.

Figure 30:

Variation of percentage load shared by GP (Pgp) and Raft with Kgp – effect of annular width, Dg.

Similarly, the percentage load shared by GPs (Pgp) is evaluated for a greater annular ratio, i.e., Dr=0.4, and the effect of Dg is depicted in Figure 31. It is observed from the results that for the same annular width, i.e., Dg=2, by increasing the annular ratio, Dr=0.2 to 0.4, the percentage load shared by GPs decreased. For Dr=0.4, by increasing the annular width, the percentage load shared by GPs gets reduced, the same as seen in Figure 30. For Dr=0.4, Dg=2, the percentage of load transferred to GPs increased from 7.48% for Kgp=10 to 17.57% for Kgp=400. By increasing the annular width, i.e., Dg=5, the percentage of load transferred to GPs increased from 1.78% for Kgp=10 to 7.90% for Kgp=400.

Figure 31:

Variation of percentage load shared by GP (Pgp) and raft with Kgp – effect of the annular width, Dg.

The variation of percentage load shared by GPs (Pgp) with Kgp for GPs of different L/d is depicted in Figure 32. It is observed from the results that by increasing Kgp of the GPs, the percentage load shared by GPs increases significantly. The improvement in the load shared by GPs is higher for GPs having greater L/d. It is also observed that the rate of load shared by GPs increases as the Kgp increases. By increasing the value of Kgp from 50 to 400, the load shared by the GP of L/d=40 increased from 9.5% to 18%. The significant change in the load sharing of GPs is observed by increasing Kgp and L/d of GPs. As the parameter Kgp increases, there is a corresponding increase in the load-bearing capacity of the GP, leading to an escalation in the value of Pgp. Additionally, an observed trend indicates that Pgp increases with an augmentation in L/d, signifying that a GP having larger L/d is capable of carrying a greater load in comparison to a GP with a smaller L/d.

Figure 32:

Variation of percentage load shared by GP (Pgp) and raft with Kgp – effect of L/d.

Conclusions

Analysis of an annular raft over four granular piles based on an elastic continuum approach is presented. The effects of various geometric and relative stiffness parameters on the response of the annular raft–GP system are quantified in terms of settlement influence factor, percentage load carried by the GPs, and the GP shaft–soil interface stresses and the contact pressures beneath the raft. The following conclusions are made on the basis of the present study:

As the parameter Kgp undergoes an incremental increase, there is a noteworthy and statistically significant decrease observed in the parameter Iagpr. For a given set of conditions with Dg=2, Dr=0.2, and L/d=10, the computed values of Iagpr corresponding to Kgp values of 10 and 400 are 0.127 and 0.085, respectively. This numerical comparison reveals a substantial decrease of 33.07% in the value of Iagpr, underscoring the pronounced impact of Kgp on the observed trend.

The influence of the parameter Kgp on the values of Iagpr is discerned across varying levels of Dr. Specifically, at Kgp=10, the computed values of Iagpr for Dr=0.2, 0.4, 0.6, and 0.8 are 0.127, 0.103, 0.075, and 0.041, respectively, for a given set of conditions with L/d=10 and Dg=2. Notably, the analysis reveals that as Dr increases, there is an escalated percentage decrease in Iagpr by 18.89%, 40.94%, and 67.71% for Dr=0.4, 0.6, and 0.8, respectively, relative to the reference value of Iagpr at Dr=0.2, which is 0.127.

The parameter L/d exerts a pronounced influence on the values of Iagpr. Given a set of conditions with Dg=2, Dr=0.4, and Kgp=400, the computed values of Iagpr exhibit a noticeable trend: 0.094, 0.074, 0.056, and 0.043 for L/d ratios of 5, 10, 20, and 40, respectively. The observed pattern reveals a significant decrease in Iagpr with increasing L/d ratios, resulting in percentage reductions of 21.27%, 40.42%, and 54.25% concerning the baseline Iagpr value at L/d=5, which is 0.094. These outcomes underscore a substantial decrease in Iagpr associated with a larger granular pile, indicating a noteworthy structural response to varying length-to-diameter ratios.

The shear stresses at the top exhibit lower values in comparison to the base, primarily attributed to the induced shear stresses with increasing depth. Notably, an observation revealed a significant percentage increase of 226.9% in shear stresses from the top to the bottom for conditions characterized by Dr=0.2, Kgp=100, Dg=2, and L/d=10. However, it is noteworthy that an increase in Dg leads to a reduction in shear stresses compared to the reference case of Dg=2. This phenomenon can be attributed to the increased annular width, resulting in a larger raft area, which, in turn, diminishes the load transfer to the piles.

The percentage load carried by GP increases with the increase of its stiffness and decreases with the increase of the relative size of raft. The raft–soil interface normal stresses decrease with the increase of stiffness of GP. The influences of GP stiffness and relative length of GP are found to be more for relatively large size of raft. A significant change in the GP behavior due to the presence of the raft is to transfer the load to points at depth, i.e., the percentage of load transferred to the base of GP increases with the increase of the relative size of the raft.

The settlement influence factor for the annular raft decreases with the increase of the annular ratio, the annular width, and the stiffness of GP. For a higher annular ratio or annular width, i.e., the influence of granular piles on the settlement reduction of an annular raft is limited. The ratio of settlement of annular raft depends on the same parameters as stated above. The percentage load transferred to GP increases with the increase of stiffness of GP and/or relative length of GP, while it decreases with the increase of annular ratio and annular width.

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Geosciences, other, Materials Sciences, Composites, Porous Materials, Physics, Mechanics and Fluid Dynamics