1. Introduction
Dams still present an intrinsic risk to development, with accidents remaining a significant concern today [
1]. Therefore, given the potential of material and human losses associated with dam failure, it is mandatory to adopt a framework that has the capacity to anticipate and prevent failures. The current approaches based on simplified limit equilibrium techniques [
2,
3] are not able to characterize the complex dam–foundation behavior. The ability to evaluate the safety of dam–foundation systems in an integrated manner requires further enhancement, particularly by incorporating coupled models that capture the significant interdependence between the mechanical and hydraulic behaviors [
4,
5]. Additionally, the use of appropriate constitutive laws is essential [
6,
7,
8,
9,
10].
For the analysis of gravity dams, fully coupled two-dimensional (2D) and three-dimensional discontinuum hydromechanical models have been used [
11] following sequential coupling. The interpretation of the observed behavior during the first filling of the reservoir [
11] should also consider the hydromechanical coupling in both the 2D and 3D models. Similar hydromechanical models to those adopted in dam analysis, based on the combined finite–discrete element method (FDEM), have been proposed in 2D [
12] and 3D [
13] models for hydraulic rock fracturing. The latter 2D and 3D models have also been extended to include thermal coupling [
14,
15]. The 3D thermal–hydromechanical coupling model (THM) considers the FDEM fracture mechanic calculation model, fracture–pore mixed seepage model and heat transfer model (heat conduction in solids and fluids, heat advection and heat exchange between solids and fluids) [
15]. A 2D FDEM-based THM model that follows the software Geomechanica [
16] has also been adopted for hydraulic fracturing in deep reservoirs [
17]. More recently, a hydromechanical model has also been established for poroelastic media saturated with compressible fluids, which adopts a strong coupling between the mechanical and hydraulic based on the extended finite element method (XFEM) and the Newton–Raphson method [
18]. A 2D hydromechanical coupling model has also been proposed within the framework of discontinuous deformation analysis (DDA) and was applied to evaluate the sliding stability of a gravity dam foundation in China [
19]. A hydromechanical continuum model based on the finite element method (FEM) was adopted to analyze the seepage and stress field characteristics of a roller-compacted concrete dam in China [
20].
Regarding the simulation of the behavior of the different materials, the discontinuities and the hydromechanical coupling during shear displacement, various constitutive models/relationships have been established over time. The tensile and compressive strength of dam concrete, along with its long-term behavior, have been well characterized through both in situ and laboratory tests, which are typically conducted whenever a new dam is constructed [
21,
22]. However, the mechanical behavior of the concrete–rock interface—often one of the weakest structural points, prone to crack initiation and propagation under hydrostatic loading—has been less thoroughly studied.
Direct tensile strength tests have been performed on cored concrete–rock specimens [
23]. More recently, an experimental program was carried out to investigate the mechanics and fracture properties of the concrete–rock interface, leading to the development of a tension-softening constitutive law for this interface [
24]. This experimental program was further extended to examine the fracture process at rock–concrete interfaces under the three-point bending and four-point shearing of rock–concrete composite beams with various pre-crack positions using digital image correlation techniques [
25]. More recently, the concrete–granite composite materials were numerically assessed following a mesoscopic approach under compression loads and different interface inclination angles [
26].
Concrete gravity and buttress dams are usually assumed to fail along a sliding plane, acting as a rigid body. The stability criteria are commonly assessed for two different failure modes: sliding and overturning failure. The limits for stability are given in national or regional codes and regulations [
27]. In most cases, interface cohesion is neglected.
Regarding stability analysis, there are two primary approaches to simulate concrete dam structural failure: (i) strength reduction and (ii) overload. In the strength reduction approach, the structure is subjected to normal loads, and its strength is gradually decreased until failure happens. In the overload approach, normal loads are applied to the structure, and these loads are progressively increased until the structure fails [
28]. At the design stage, concrete gravity dam safety assessments are usually based on simplified analytical stability methods [
27,
29] performed in 2D with a simplified rock surface. The European Working Group on the sliding safety of existing gravity dams addressed in its final report [
30] guidelines, site data information, experimental programs, safety assessment techniques and three-dimensional effects.
Li et al. [
31] evaluated the stability of a large gravity dam using both the overload and strength reduction methods, but the pressures followed simplified analytical distributions. These authors highlight that the overload method, which includes more complex geometries, can be adopted to define the weak structural interfaces/zones that may require reinforcement measures. The strength reduction may also be more complex by reducing both the cohesion and friction angle. In [
32], a reduction model based on a plastic strain energy-based criterion is proposed for the bed rock and weak foundation zones. Note that the latter does not include seepage water pressures. Stability analysis has also been addressed through probabilistic analysis, usually adopting simple models or analytical expressions due to computational issues but considering uncertainties in the structural analysis and their influence on the safety factors [
33,
34,
35]. Within this methodology, it is still computationally demanding to consider the hydromechanical coupling.
Although numerical modeling techniques have been widely used to simulate the failure of concrete dams, mostly the FEM [
36] and the discrete element method (DEM), testing programs are still devised to confirm the reliability of the application of the numerical models to the study of failure mechanisms that involve sliding in jointed rock masses by comparing numerical results with experimental data, in both static and dynamic conditions. Most of the tests are carried out under overloading conditions [
37,
38]. Enzell et al. [
37] developed a 25 m long prototype of a concrete buttress dam. The testing involved gradually increasing the water pressure until the model failed. Initially, a watertight steel sheet wall was placed upstream of the dam to allow the water level to rise above the dam’s crest, transmitting water pressures to both the dam and its foundation without causing overtopping. In the numerical study presented here, this setup was precisely simulated. The steel sheet was subsequently removed to permit overtopping.
In this study, the Parmac2D-Fflow algorithm, which uses a time-stepping small-displacement hydromechanical coupled approach, including the discrete representation of the foundation discontinuities, was employed to assess the safety of gravity dams [
39,
40]. Compared with the strength reduction approach or the overtopping approach without hydromechanical coupling, the proposed innovative methodology has the advantage of allowing the consideration, in an integrated way, of (i) softening-based constitutive laws that are closer to the real behavior identified experimentally in concrete–concrete and concrete–rock interfaces; (ii) the influence of the water height increase on both the hydraulic and mechanical models; and (iii) fracture propagation along the dam–foundation interface, only allowing seepage to occur when the interface is cracked, which is closer to the expected behavior given the way that this interface is constructed. As shown, the proposed innovative methodology for the safety assessment of concrete dams allows for the definition of more reliable safety factors and the identification of more realistic failure modes that may be strengthened following retrofitting interventions. Within dam engineering, more realistic numerical constitutive models have been adopted mainly for concrete [
41].
Parametric studies were conducted to assess the impact of the mechanical properties, namely, the concrete–rock strength parameters, on the global safety factors of three gravity dams with different heights, foundation behaviors and geometries. The results obtained using a coupled/fracture propagation model, including those for which the water height increase had an influence on the water pressures, are compared with those from the strength reduction method and the overtopping scenario not considering the hydromechanical coupling as the water height is increased.
The results show that the safety assessment should be conducted using a coupled hydromechanical model that incorporates accurate material properties, namely, for the concrete–rock interface, and that considers the foundation geometry and behavior close to the in situ conditions and follows a load amplification approach that can identify weak structural zones. It is shown that the concrete–rock interface should preferably have a high value of fracture energy or, ideally, higher tensile and cohesion strengths and high associated fracture energy. The results also indicate that with a brittle concrete–rock model, the predicted safety factors are always conservative when compared with those that consider the fracture energy.
2. Numerical Approach
2.1. Mechanical Model
The adopted hydromechanical model, Parmac2D-Fflow, allows for the coupling between the hydraulic behavior and the mechanical behavior [
42] and is part of the computational model Parmac2D [
43]. The Parmac2D-Fflow implementation was chosen for the safety assessment of concrete gravity dams because it represents the foundation discontinuities, which are a key parameter in the safety assessment, and by including joint finite elements, it allows for faster and more accurate modeling when compared with discrete element approaches [
42]. The adopted hydromechanical approach [
42] and similar hydromechanical models [
12,
13] have been validated and compared with benchmark tests and with the real behavior of a Portuguese gravity dam. More recently, a similar DEM-based model [
44] was used to study the uplift pressure distribution at a dam–foundation interface, showing that the limit equilibrium approach may underestimate the stress magnitude at both the dam heel and toe [
45].
The mechanical model follows an explicit solution algorithm based on the centered difference method [
43] that calculates the velocities at the mid-intervals (
), while the generalized positions and accelerations are defined at the primary intervals (
). The deformability of each block is considered by discretizing its interior with a finite element triangular mesh. Newton’s second law of motion is integrated twice to define the nodal point displacements, leading to the following expressions for the nodal point velocities at time
:
where
is the total applied force at instant t,
is the damping force at instant
,
is the nodal point mass,
represents the velocity vector at time
, and
represents the velocity vector at time
. The total applied forces are due to (i) the external forces applied at the nodal point; (ii) the interactions with neighboring blocks, which only occur at nodal points located at the block boundaries; and (iii) the deformation of the inner block triangular finite elements.
The interaction between deformable blocks is carried out using joint finite elements (FEs) [
46,
47] that require (i) a small-displacement hypothesis; (ii) that each block’s finite element boundary discretization is compatible with the boundary finite element discretization of the neighboring blocks. When compared with the DEM, which handles large displacements [
42], the FEM-based joint element approach makes it easier to incorporate nonlinear elastoplastic and damage models. The discrete block foundation geometry was defined using UDEC [
44,
48]. A pre-processing stage is applied to obtain a perfectly compatible final block assembly with joint elements (see [
42] for more details).
The FE-based joint element allows for discontinuity in the displacement field using a direct relation between the stresses and displacements. At each joint element integration point, the normal
and shear
stresses in the local axis are given as follows:
where
and
are the normal and shear stresses at timestep
;
and
are the displacement increments in both the normal and tangential joint directions; and
and
are the normal and shear contact stiffnesses.
To represent the concrete–concrete and concrete–rock discontinuity behavior, a bilinear vectorial softening contact model (BL) was adopted, which has been applied in particle modeling fracture studies [
43] (
Figure 1). As presented in
Figure 1, once the maximum strength values (tensile and cohesion strengths) are reached, the corresponding maximum tensile strength and/or maximum cohesion stress are updated based on the updated damage value. The damage value ranges from 0 (no damage) to 1 (the integration point is cracked and only transfers normal and shear stresses through pure friction under normal compression stress).
The damage value at each integration point is defined by the greater of the maximum tensile and shear damage values, which are defined given the maximum recorded normal and shear joint displacement values. The constitutive law requires the definition of five material properties: (i) the ultimate tensile stress (); (ii) the maximum cohesion stress (); (iii) the coefficient of friction (); (iv) the fracture energy in mode I (); and (v) the fracture energy in mode II ().
2.2. Hydraulic Model
The hydraulic model is proposed in [
42] and is based on the principles defined in [
44] for a large-displacement formulation based on the DEM. A similar hydraulic model has been proposed in 2D and applies hydraulic fracture propagation [
12]. The hydraulic model has been extensively validated in simple benchmark examples [
12,
42,
44].
Figure 2 shows both the mechanical and hydraulic models.
Figure 2a shows the mechanical model, in which four different blocks are represented, discretized with triangular finite elements, along with the corresponding joint elements (JEs). The hydraulic model (
Figure 2b) is perfectly superimposed on the mechanical model (
Figure 2a) in a straightforward way, given that a perfectly compatible boundary mesh of plane triangular elements was defined during pre-processing [
42]. The seepage channels (SCs) of the hydraulic model, shown in
Figure 2b, align with the midplane of the joint elements, shown in
Figure 2a [
42]. For each JE, there is a corresponding seepage channel (SC). The hydraulic nodes (HNs) are the result of the superimposition of the various adjacent mechanical nodes that shared the same coordinates at the beginning of the numerical analysis.
The volume of each SC is obtained considering the mechanical apertures measured on the nodal points of the JE associated with the SC. It is assumed that flow takes place only through the set of interconnecting discontinuities (rock blocks are impervious).
Water pressures are defined on the HNs, and flow rates are calculated in the SCs (
Figure 2c). The discharge rate of each SC is calculated based on the simplified assumption of laminar seepage between parallel plates [
49,
50,
51]. This discharge rate ((m
3/s)/m) is given as follows [
52]:
where
is the theoretical value of a joint permeability factor (also called the joint permeability constant), where
is the dynamic viscosity of the fluid;
is the hydraulic aperture of the seepage channel;
is the water density;
is the acceleration of gravity;
is the difference in the piezometric head between both ends of the seepage channel; and
is the length of the
.
In each
, the discharges are summed from all the seepage channels that converge to a given
, according to the following:
If only steady-state conditions are considered, the volume variation between two consecutive timesteps may be neglected. The HN water pressure at the following timestep (
) is given as follows:
where
is the water bulk modulus (N/m
2),
is the volume variation (m
3) associated with the
between two consecutive steps and
is the timestep used in the hydraulic domain.
The hydraulic aperture to be used in Equation (4) (
) is given as follows:
where
is the hydraulic aperture at nominal zero normal stress, and
is the joint normal displacement taken as positive in the opening. As shown in
Figure 3, a maximum aperture value,
, is adopted for numerical convergence issues. A minimum aperture value,
, is also adopted, below which mechanical closure does not affect the contact permeability (
Figure 3) [
12,
13,
42,
44].
Regarding the hydraulic boundary conditions, the HNs may be assumed to have zero permeability, usually adopted at the bottom and lateral faces of the foundation rock mass. The HNs may also have imposed pressure values, which are usually used to set the pressures at the top of the foundation, upstream and downstream from the dam and at the HNs intersected by the drainage system.
A 3D extension that also adopts seepage channels has been proposed for dam foundation hydromechanical analysis [
11], and a 3D model that follows a similar methodology but adopts seepage surfaces has been proposed [
13] for hydraulic fracture propagation.
2.3. Coupled Hydromechanical Model
A sequential coupling scheme is adopted between the mechanical model and the hydraulic model, which evolves over time through the interaction between both domains. At each timestep, the seepage channel hydraulic apertures are calculated considering the normal displacements of the associated joint elements calculated with the mechanical model. Following this, the water pressures calculated using the hydraulic model are then transferred to the mechanical model and are considered in the calculation of the internal forces of the associated joint elements (effective stresses). Additional details can be found in [
42]. Regarding stability issues, the hydraulic volumes associated with the HNs and the masses associated with the mechanical nodal points are scaled assuming a unitary timestep in order to ensure numerical stability [
42].
The adopted discontinuum hydromechanical model allows for two different approaches for the seepage flow:
(i) Seepage occurs in all interfaces independently of their damage, and the corresponding water pressures are installed from the beginning of the simulation on all interfaces, including the dam–foundation interface;
(ii) At the dam–foundation interface, seepage only occurs after the joint element integration points are found to be cracked, making it possible to model a coupled propagation failure along the dam–foundation interface due to a hypothetical dam overtopping scenario (CP-FP). An initially impervious dam–foundation interface is a more realistic scenario given the way that the concrete dam is built, as special foundation treatment is carried out to ensure cohesion between the concrete and foundation rock, which significantly reduces the permeability in the absence of fracture.
2.4. Model Geometry
Three gravity dams of different heights, (15 m, 30 m and 60 m) were assessed adopting two foundation fracture geometries.
Figure 4 shows the schematic geometry of the adopted dam–foundation system.
Table 1 presents all the required geometric parameters to generate the models. The adopted dam cross-section geometry is within the usual dimensions given the dam height. The grout curtain geometry, close to the heel of the dam, and the location of the seepage curtain also follow the guidelines usually adopted for Portuguese dams. The consideration of the rock wedge downstream of the dam is based on the existing conditions of the Pedrogão dam [
42].
The foundation rock masses were represented with two families of discontinuities:
- (i)
One model, called “reg”, was considered with the following:
- a.
A family of continuous horizontal discontinuities with spacings of 2.5 m in the 15 m high dam models, 5.0 m in the 30 m high dam models, and 10.0 m in the 60 m high dam models;
- b.
A family formed by vertical discontinuities with an average spacing of 2.5 m and a standard deviation of 1.0 m in the 15 m high dam models, an average spacing of 5.0 m and a standard deviation of 2.0 m in the 30 m high dam models, and an average spacing of 10.0 m and a standard deviation of 4.0 m in the 30 m high dam models;
- (ii)
Another model was considered, called “dip”, with families of continuous orthogonal discontinuities that make angles of 15° and 105° with the horizontal.
In the latter case, the orientation and the fact that the families of discontinuities are continuous and flat favor the formation of failure mechanisms, with the formation of wedges that can slide under the dam.
To increase the complexity of the failure mode associated with the dam–foundation stability scenario (strength reduction or load amplification), it was considered that the foundation downstream from the dam is at a higher level, contributing to the dam stability. An additional discontinuity was imposed downstream from the toe of the dam, creating a wedge that allowed sliding to occur even if elastic foundation behavior was assumed.
In the concrete dam, a set of horizontal continuous discontinuities were assumed. These discontinuities were located 3.0 m apart in the model with the dam 15 m in height (5 dam blocks), 2.0 m apart in the 30 m high dam model (15 blocks) and 4.0 m apart in the 60 m high dam model (15 blocks). The objective was not only to simulate dam lift joints but also to allow the mechanism failure to include the dam body.
Table 2 shows the numbers of mechanical and hydraulic elements used in the six dam–foundation models. The average edge lengths of the triangular elements were set as follows:
A length of 0.5 m in the 15 m high concrete dam models (Dam 15-reg and Dam 15-dip);
A length of 1.0 m in the 30 m high concrete dam (Dam 30-reg and Dam 30-dip);
A length of 2.0 m in the 60 m high concrete dam (Dam 60-reg and Dam 60-dip).
2.5. Hydromechanical Model Parameters
Both the dam concrete and rock mass blocks were assumed to follow elastic linear behavior, with the properties shown in
Table 3, which match the experimental properties of the granite and concrete adopted in [
24].
Table 3b presents the adopted interface elastic and strength contact model parameters. The concrete–concrete and concrete–rock interfaces followed a bilinear softening model (see
Section 2.1). Also presented are the rock–rock interface strength properties when a nonlinear foundation model was adopted, where zero tensile and cohesion stress and a friction coefficient of 1.0 were assumed. The normal and shear stiffness values should be as high as required to ensure that the deformation occurs mainly within the blocks; but, to ensure numerical robustness, the maximum values need to be limited. The normal stiffness values were defined as if the joint had a fictitious thickness of 0.50 m, and a ratio of 0.4 was assumed between the normal and shear stiffnesses, which are within the usual values adopted for discrete media [
42,
44].
The tensile strength (
) and the fracture energy (
) adopted for the concrete–concrete interface correspond to the experimental values obtained for concrete [
24]. The tensile strength (
) and the fracture energy in mode I (
) adopted for the concrete–rock interface correspond to the properties presented in [
24] for specimen TPB 5-5, which correspond to the best-fit bilinear softening model that predicted an excellent agreement with the experimental results. The cohesive stress (
) and the fracture energy in mode II (
) were defined for both contact interfaces adopting the following relationships of
and
. The adopted values were within the range of values usually adopted for BL contact models representing concrete and rock material [
40,
43]. In [
53,
54], a factor of 1.75 was adopted for the cohesive stress and a factor of 2.0 was adopted for the fracture energy in mode II. A friction angle of 1.0 was also adopted for both interfaces, which is also within the usually adopted values.
The following hydraulic apertures were considered:
= 0.1668 mm,
and
[
42]. It was assumed that the permeability of the dam–foundation interface was half of the foundation discontinuity permeability. In the grout curtain vicinity, a permeability 2.5 times lower than that adopted for the rock mass was considered. The dam construction joints were impervious.
The hydraulic parameters were within the range of the parameters adopted in [
42], which have been shown to predict the observed hydraulic behavior of a Portuguese gravity dam. In [
42,
55], a grout curtain with a permeability 10.0 times lower than that of the rock mass was adopted, whereas a lower value of 2.5 was adopted in this work. Note that the grout curtain permeability has a noticeable influence on the quantity of water that flows through the foundation: a lower permeability value is associated with a lower water flow but has little influence on the pressure distribution, which is the main parameter that affected the stability studies that are presented here [
55].
2.6. Hydromechanical Model Boundary Conditions and Analysis Sequence
Concerning the mechanical boundary conditions, the base of the model was fixed, and horizontal displacements perpendicular to the lateral boundaries were prevented. As for the hydraulic boundary conditions, zero permeability was assumed at the base and lateral boundaries of the model, and the drainage system was simulated by assigning water pressures along the drain axis equivalent to one-third of the hydraulic head upstream from the dam.
The models developed were used to assess the sliding safety of the dam–foundation system. The analysis was carried out in two phases: First, a hydromechanical calculation was carried out, considering the weight of the dam, assuming that the water table was at ground level and that the ratio between the horizontal and vertical effective stresses in situ was equal to 0.5. In the second phase, with the reservoir assumed to be at the dam crest level, the hydrostatic pressure was applied at the upstream face of the dam and at the base of the reservoir, assuming that all the discontinuities had linear elastic behavior. In this phase, a coupled hydromechanical analysis was carried out. In cases where the nonlinear behavior of the discontinuities was assumed, this was only considered after equilibrium had been reached, assuming linear elastic behavior.
Subsequently, for each gravity dam, an overtopping scenario was assessed by gradually increasing the reservoir water level using 1 m height increments.
Three different calculation hypotheses were considered:
The uncoupled approach (UCP)—In the UCP approach, the hydraulic model pressures are kept constant during the process of increasing the water level above the dam crest. In this approach, the uplift pressures are not influenced by the subsequent changes in the mechanical apertures or by the water level rise that just affects the mechanical model;
The coupled approach (CP)—In the CP approach, the water level rise above the dam crest influences both the mechanical model (hydrostatic pressure at the upstream face of the dam and upstream foundation surface) and the hydraulic model (applied hydraulic-imposed pressure at the reservoir bottom). In this approach, a coupled calculation is performed for each water level, so the mechanical aperture variations affect the hydraulic model and the pressure variations in the hydraulic model affect the mechanical apertures. Seepage occurs in all interfaces independently of their damage (the corresponding water pressures are installed from the beginning of the simulation on all interfaces);
The coupled approach taking into account fracture propagation at the dam–foundation interface (CP-FP)—The CP-FP approach is similar to the CP approach, with one exception: seepage is only allowed to occur at the dam–foundation interface after cracking occurs, making it possible to model the fracture propagation along the dam–foundation interface due to a hypothetical dam overtopping scenario. In all other interfaces, seepage occurs independently of their damage, as adopted in the CP approach.
For each calculation hypothesis, two different foundation behaviors were assessed: an elastic model (E) and a brittle model (B), following the properties presented in
Table 3 for rock–rock contacts. For the reference model properties, a stability analysis based on the strength reduction approach, usually adopted in dam design [
36,
56,
57], was also carried out. In this analysis, zero tensile and cohesion stresses were adopted at the concrete–rock interface, and the frictional term of the corresponding joint elements was gradually reduced up to failure.
4. Conclusions
An explicit time-stepping discontinuum hydromechanical coupled algorithm, Parmac2D-Fflow, was used to evaluate the safety of gravity dams considering various dam heights, foundation geometries and behaviors, and concrete–rock strength properties.
As shown, the strength reduction method commonly used in concrete gravity dam design is overly simplistic. The strength reduction methodology fails to account for the actual material behavior of both the concrete and dam foundation, resulting in excessively conservative safety factors. Additionally, the predicted strength reduction safety factors are not significantly influenced by the dam height, the foundation geometry and behavior or the real concrete–rock and concrete–concrete interface behavior. The strength reduction approach oversimplifies the failure modes, predicting only shear sliding failure, even in scenarios involving a downstream wedge within the rock mass.
The results presented, with the wedge and without the wedge contribution, show that the safety assessment of gravity dams should be conducted using a coupled hydromechanical model that (i) incorporates accurate material properties; (ii) considers the foundation geometry and behavior; (iii) follows a load amplification approach. An initially impervious dam–foundation interface should also be considered, as this represents a more realistic scenario. Additionally, accounting for nonlinearity within the dam body may be crucial for same cases, as neglecting it may lead to overestimated safety factors.
For the results presented with the reference model concrete–rock contact strength properties and for different fracture energy scenarios and contact strength scenarios, the following was found:
The UCP approach always leads to higher safety factors than those obtained with a coupled approach (CP and CP-FP), which is non-conservative. The UCP approach may also predict incorrect failure modes, which may affect the correct retrofitting interventions. For this reason, it is important to carry out a coupled hydromechanical analysis;
The safety factor should preferably be defined using the CP-FP approach, which considers the seepage at the dam–foundation interface from the onset of the calculation. In the CP-FP approach, cracking only started to occur at the concrete–rock interface for water levels closer to the maximum water level value for which the dam remains stable. This sudden increase and propagation led, in some cases, to safety factors slightly lower than those predicted with the CP approach.
The results show that, contrary to the expected, it is possible to obtain safety factors with a brittle foundation higher than those predicted with an elastic foundation. If the proper in situ behavior is not known in advance, the safety factors should be defined following parametric studies;
If the foundation discontinuities favor the failure mode, its influence on the predicted safety factor is noticeable. For this reason, the geologic characterization is of the upmost importance;
The parametric studies show that the concrete–rock interface should preferably have a high value of fracture energy or, ideally, higher tensile and cohesion strengths and high associated fracture energy, otherwise the differences in the CP and in the CP-FP predictions are not noticeable;
During construction, it may be sufficient to characterize the concrete–rock interface only through strength parameter definition (tensile/cohesion), as the results indicate that with a brittle concrete–rock model, the predicted safety factors are always conservative when compared with those that consider the fracture energy.
When compared with the strength reduction method or an overload approach following the UCP approach, the proposed overload approach that follows either the CP or CP-FP approach predicts more realistic failure modes and, for this reason, has the potential to be used to identify weak structural interfaces/zones that may require reinforcement measures.