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Preloading with a surcharge is today commonly used together with prefabricated vertical drains for embankment construction on clayey soil to accelerate primary consolidation and increase strength. Because of considerable uncertainty related mainly to the rate of consolidation, there is a need to account for this in the vertical drain and surcharge design to ensure quality in the embankment construction. Addressing this issue, the paper presents a novel probabilistic design methodology that is compatible with the observational method. The procedure evaluates the suitable surcharge load to be used in combination with a vertical drain design in order to ensure that the established design criteria are satisfied with acceptable probability.

Preloading with a surcharge is today commonly used together with prefabricated vertical drains (PVDs) for embankment construction on clayey soil to accelerate primary consolidation and increase strength. In essence, by installing a pattern of PVDs in a loaded clay stratum consolidation will occur both vertically and horizontally (radially) towards the drains such that the spatially averaged degree of consolidation can be expressed as a function of time, t (Carrillo, 1942)

1

where the average degree of vertical consolidation is given by Terzaghi's consolidation theory

2

and the average degree of horizontal consolidation can be expressed as

3

where cv and ch are the vertical and horizontal coefficients of consolidation; hdr is the maximum vertical drain path; re is the radius of the influence zone of a PVD; and F describes the effect of drain spacing, soil disturbance and well resistance.

The theoretical aspects of soil improvement with vertical drains have been studied exhaustively. Starting with pioneering work by Porter (1936), Barron (1948) and Kjellman (1948), considerable insight into the effect of vertical drains on the consolidation process has been gained over the years. Hansbo (1979, 1981) developed the design procedure, while the smear effect in particular has since been extensively investigated (e.g. Atkinson & Eldred, 1981; Bergado et al., 1991; Indraratna & Redana, 1997, 1998; Hird & Moseley, 2000; Sharma & Xiao, 2000; Hird & Sangtian, 2002; Walker & Indraratna, 2007; Rujikiatkamjorn et al., 2013; Zhou & Chai, 2017). Many recent studies focus on development of analytical and numerical solutions to various design situations for PVDs (e.g. Lei et al., 2015; Indraratna et al., 2016; Geng & Yu, 2017; Indraratna et al., 2017; Nguyen & Kim, 2019). Settlement prediction and verification from measurements have also gained attention lately (Chung et al., 2014; Stark et al., 2017; Abdullah et al., 2018; Guo et al., 2018). A comprehensive benchmarking exercise for settlement prediction (Indraratna et al., 2018a), two studies on vacuum-surcharge preloading (Ni et al., 2019; Wang et al., 2019) and a case study (Wang et al., 2018) were also published recently.

As a consequence of the considerable amount of research on vertical drains, there exist today many alternative analytical models of F (in equation (3)) for geotechnical design of PVDs; see for example Abuel-Naga et al. (2015). From a design perspective, however, the effect of aleatory and epistemic uncertainties also needs to be considered. In fact, Müller & Larsson (2013) found that uncertainties in the relevant geotechnical parameters – mainly in ch – will likely affect the design substantially more than the choice of model for F. Nonetheless, the effect of uncertainty is much less studied, although Hong & Shang (1998) and Zhou et al. (1999) studied the effect of uncertainty on drain spacing. Bari et al. (2013, 2016) and Bari & Shahin (2014) later developed these concepts, also taking into account spatial variation in ch. Huang et al. (2010), Bong et al. (2014) and Bong & Stuedlein (2018) also investigated consolidation behaviour with spatially variable soil properties, while Müller et al. (2016) analysed probabilistically the effect of PVDs on the increase in undrained shear strength during the staged construction of an embankment.

However, no established reliability-based procedure exists today for design of surcharge loads in combination with PVDs for accelerated consolidation under embankments. Taking on this challenge, this paper presents a novel probabilistic design procedure based on the observational method (Peck, 1969). The procedure is compatible with the general reliability framework for the observational method outlined by Spross & Johansson (2017). Considering that the presented design procedure agrees with the definition of the observational method (CEN, 2004), this paper also addresses the request for studies on applications and proper use of the observational method that was expressed at the Institution of Civil Engineers (ICE) symposium held in 1995 on the Géotechnique special issue on the observational method (Nicholson, 1996).

Introduced by Peck (1969), the observational method offers an alternative to conventional design. The method is often put forward for its potential for savings when it is difficult to predict geotechnical behaviour. Although the term ‘observational method’ is sometimes used to refer to all kinds of design based on observations, it is used here in strict accordance with section 2.7 in Eurocode 7 (CEN, 2004), cited in full in Table 1. Studies discussing applications of the observational method include Wu (2011), Prästings et al. (2014), Spross & Larsson (2014), Spross et al. (2016), Spross & Johansson (2017), Bjureland et al. (2017), Fuentes et al. (2018) and Spross & Gasch (2019).

Table 1.

Principles of the observational method cited from section 2.7 in Eurocode 7 (CEN, 2004)

ClausePrinciple*
1‘When prediction of geotechnical behaviour is difficult, it can be appropriate to apply the approach known as ‘the observational method’, in which the design is reviewed during construction.
2P The following requirements shall be met before construction is started.
 (a) Acceptable limits of behaviour shall be established.
 (b) The range of possible behaviour shall be assessed and it shall be shown that there is an acceptable probability that the actual behaviour will be within the acceptable limits.
 (c) A plan of monitoring shall be devised, which will reveal whether the actual behaviour lies within the acceptable limits. The monitoring shall make this clear at a sufficiently early stage, and with sufficiently short intervals to allow contingency actions to be undertaken successfully.
 (d) The response time of the instruments and the procedures for analysing the results shall be sufficiently rapid in relation to the possible evolution of the system.
 (e) A plan of contingency actions shall be devised, which may be adopted if the monitoring reveals behaviour outside acceptable limits.
3P During construction, the monitoring shall be carried out as planned.
4P The results of the monitoring shall be assessed at appropriate stages and the planned contingency actions shall be put into operation if the limits of behaviour are exceeded.
5P Monitoring equipment shall either be replaced or extended if it fails to supply reliable data of appropriate type or in sufficient quantity.’
*

‘P’ indicates a principle, which must not be violated.

When loading soft clay, significant settlement can be expected. From a serviceability point of view, the relevant limit state to analyse for an embankment concerns the occurrence of residual settlements after completion of the embankment and the superstructure

4

where Δsallow is the allowable residual settlement and ΔS is the occurring residual settlement. The conceptual idea of the proposed design procedure is to ensure that this serviceability limit state is only violated with an acceptable target failure probability – that is, P(G < 0) = pFT.

Considering that compression of clay consists of primary compression (consolidation) and secondary compression (mainly creep), the design concept needs to manage both aspects. However, secondary compression can be limited by ensuring that the preloading causes sufficient overconsolidation (Jamiolkowski & Lancellotta, 1981; Alonso et al., 2000; Han, 2015; Indraratna et al., 2018b), which is useful in the practical design situation. This permits the considerable simplification of taking only primary consolidation settlement into account in the design analysis, as is done in this paper. To ensure only limited compression after completion, sufficient primary compression settlement, starget, thus needs to develop during the preloading. Making starget a prescribed settlement target to be met during the preloading phase to satisfy P(G < 0) = pFT, equation (4) can be reformulated into

5

where S is the predicted long-term primary compression settlement caused by the embankment load. The establishment of the starget value is conceptually visualised in Fig. 1. In the authors’ opinion, Δsallow can in practice be set to 0 to reserve a margin for any occurrence of secondary compression after completion or any creep possibly occurring during primary consolidation (Leroueil, 1996; Hawlader et al., 2003; Feng & Yin, 2018). This implies that the starget value can be determined as the percentile of the distribution of S that corresponds to the predetermined pFT.

The limit state G is a function of the random variables affecting primary consolidation settlements, which are collected in a vector X= [X1, Xi, …, Xm]. In this paper, these correspond to the vertical and horizontal coefficients of consolidation, the unit weight and natural water content of the clay, the unit weight of the embankment material and four settlement parameters evaluated from constant-rate-of-strain (CRS) oedometer tests, as detailed in the illustrative design example.

Fig. 1.

Conceptual idea of the design procedure. Top: embankment height plotted against time. Bottom: developed settlement plotted against time. The S is used to determine the starget value. To ensure that ΔSallow is only exceeded with pFT, a surcharge height hsur is selected so that the starget value and OCR = 1·10 are attained within tmax with acceptable probability

Fig. 1.

Conceptual idea of the design procedure. Top: embankment height plotted against time. Bottom: developed settlement plotted against time. The S is used to determine the starget value. To ensure that ΔSallow is only exceeded with pFT, a surcharge height hsur is selected so that the starget value and OCR = 1·10 are attained within tmax with acceptable probability

Close modal

By preloading with a surcharge that is placed on top of the embankment for some time, the consolidation process can be sped up, allowing starget to be reached before a predefined maximum allowable preloading time, tmax. When starget is reached, the surcharge is unloaded and the superstructure completed, after which the embankment is taken into service. Designing the embankment with the observational method, the designing engineer's task is to select a PVD design (e.g. drain type and spacing) and a surcharge load that in combination satisfy two criteria: (a) that the predicted but uncertain settlement Ssurtmax that is caused by the preloading until t = tmax will reach starget with acceptable probability, pacc

6

and (b) that the overconsolidation ratio, OCR, after unloading the surcharge at tmax will exceed OCRtarget = 1·10 with acceptable probability in the middle of the clay stratum

7

The first criterion ensures that a sufficiently large surcharge load is applied initially, to allow the probabilistically determined starget value to be reached with the probability pacc within the available timeframe (t < tmax). Fig. 1 illustrates the probability P(Ssurtmax ≥ starget) for some selected initial surcharge heights, hsur. Since the observational method allows changes (‘contingency actions’) to the preliminary design during construction – that is increase of the surcharge height during the preloading – the main embankment design requirement P(G < 0) = pFT can in principle be satisfied regardless of applied initial surcharge height. This implies that the pacc will depend on the risk appetite of the decision maker in the project at hand, who will face the cost of contingency actions or project delay with the probability 1 − pacc at most (see details in the later section entitled ‘Discussion’).

The second criterion ensures that significant secondary compression is avoided. The requirement for OCRsurtmax ≥ 1·10 follows the general technical requirements and guidance for geotechnical works issued by the Swedish Transport Administration (STA, 2013a, 2013b). Other target values than OCRsurtmax ≥ 1·10 can be applied in a straightforward way based on local regulations. ‘Acceptable probability’ in this context refers to requirement 2(b) in the observational method (Table 1); because of the significant uncertainties of the geotechnical conditions in the ground, the surcharge height can only be selected based on the probability that the corresponding load will be sufficient to meet the two design criteria (equations (6) and (7)).

During the preloading, monitoring of settlements (requirement 2c) and use of contingency actions (requirement 2e) ensure that the two criteria are actually met, so that the serviceability limit state (equation (5)) is violated – that is, post-completion primary compression occurs – only with the probability pFT at most. A suitable contingency action if the monitoring indicates too slow a rate of settlement may be to increase the surcharge load; if the rate is faster than required, unloading the surcharge is required when both criteria are satisfied (for details see the Illustrative design example). An overview of the conceptual idea is provided in Fig. 1 and a flowchart of the procedure in Fig. 2.

Fig. 2.

Flowchart for probabilistic design of surcharges on vertical drains in accordance with the observational method

Fig. 2.

Flowchart for probabilistic design of surcharges on vertical drains in accordance with the observational method

Close modal

To be able to assess the design criteria (equations (6) and (7)), the random variables in X need to be evaluated. In this paper, a Bayesian approach to statistics is taken, since this is the most reasonable approach to interpret structural failure probabilities. This implies that probabilities are interpreted as a degree of belief in an event (rather than as the observable relative frequency of the event after many repeated trials, which the classical frequentist approach requires). With a Bayesian approach, the calculated failure probabilities will be correct on average for a large number of structures; Vrouwenvelder (2002), Baecher & Christian (2003) and other textbooks on structural reliability analysis provide more detailed discussions on this matter.

As consolidation settlement is an averaging process, the mean value of each geotechnical parameter in X= [X1, Xi, …, Xm] is modelled as a random variable (where subscript i henceforth in this chapter is dropped for convenience)

8

where X¯m is the uncertain mean value of the measured geotechnical property with expected value x¯m; ε is an error factor that describes the inherent variability and any statistical uncertainty and measurement errors in the evaluation of X¯m; and T represents a transformation model (in case of indirect measurements) that also may contain a random error, which accounts for any uncertainty in the transformation model between the measured property and the sought geotechnical parameter. In this paper, the respective ε of the investigated geotechnical parameters is assumed to be log-normally distributed, as is common practice (e.g. Lacasse & Nadim, 1996; Baecher & Christian, 2003; Fenton & Griffiths, 2008; Huang et al., 2010), while transformation errors are assumed either normally or log-normally distributed. Transformation models T are therefore treated separately (see equation (20)). Similar statistical models have been described and used by, for example, Phoon & Kulhawy (1999), Ching & Phoon (2012), Bergman et al. (2013) and Müller et al. (2014, 2016).

To evaluate the uncertainty of the mean value of each measured geotechnical property, X¯m=x¯mε, based on the available geotechnical investigations, all data can be transformed with the natural logarithm to allow working with normal distributions. The X¯m can thus be rewritten to

9

where lnx¯m denotes the expected value based on n data points that have been transformed with the natural logarithm and ε{ln} is the associated zero-mean normally distributed error.

If there is no trend with depth, z, the evaluation of lnx¯m is straightforward, but when a trend exists, which may be for geological reasons, the trend can be considered by evaluating the variability around a regression line. Several models are possible, but in this paper a simple normal regression is used with variance estimated from the n available data points that have already been transformed with the natural logarithm, such that

10

where a^ and b^ are regression parameters evaluated from the log-transformed data points.

The error ε can be divided into three multiplied log-normally distributed error components

11

where εinh represents the inherent variability of the measured property after averaging it over the failure domain; εst represents the statistical uncertainty in the estimation of the mean value; and εme represents the measurement error related to the estimation of the mean value. Each log-normally distributed component has a zero mean of the corresponding normal distribution and corresponding variances бinh{ln}2,бst{ln}2 and бme{ln}2 as parameters. With this model, the X¯m can be characterised by the log-normal distribution LNlnx¯m,бεln2, where бεln2=бinhln2+бstln2+бmeln2, after having applied the rule for multiplication of log-normally distributed variables. The variance of each error component is derived in the following subsections.

The variability of the measured data points may include both an inherent variability and a measurement error – that is, εdata{ln}=εinh{ln}εme,m{ln}, where ε{ln}me,m is the measurement error related to each log-transformed measured data point. Applying the rule for multiplied log-normally distributed variables and rearranging the terms, the variance of the natural logarithm of the inherent variability is

12

where бme,mln2=ln[COV(εme,m)2+1] in which the error εme,m is the reported error of the applied measurement method (see e.g. the compilation by Phoon & Kulhawy (1999) and Müller et al. (2016)).

In principle, however, the effect of ε{ln}inh on lnX¯m is partially affected by the scale of the structural failure, which requires the evaluation of the variance function Γ2 to assess the variance reduction. However, in this paper it is for simplicity assumed that the clay layer is sufficiently thick to make the settlement a fully averaging process; consequently, Γ2=0, which eradicates the effect of local zones in the clay that deviate from the mean value. If there is a less thick clay layer, the reader is referred to, for example, Fenton & Griffiths (2008) or Vanmarcke (2010) for details on the evaluation of Γ2.

With a linear trend line with depth, the uncertainty of ε{ln}st at a certain depth z is calculated from the general normal regression process with unknown variance (Raiffa & Schlaifer, 1961; Tang, 1980; Ang & Tang, 2007)

13

where z=[1zz2zr]; I is the identity matrix; υ denotes the number of degrees of freedom, which in this case is equal to n − 1, and

14

where the rows represent the n depths at which independent measurements were taken. Assuming a linear trend, r = 1, which according to Tang (1980) simplifies equation (13) into

15

where the factor ψz is a function of z (henceforth in this section denoted by subscript z)

16

in which z¯ is the sample mean of the depths where the measurements were taken and бz2 is the sample variance of the respective depths zi. (If no linear trend exists, ψ = 1/n, which gives the straightforward result бst{ln}2=бinh{ln}2/n.)

Lastly, the uncertainty of ε{ln}me (see equation (12)), in the evaluation of the uncertainty related to the mean value lnX¯m, decreases with the number of independent measurements of the property

17

Combining equations (12)–(17) and assuming a fully averaging process such that бinh{ln}2Γ2=0, the total variance of ε{ln} becomes a function of z and evaluates to

18

The mean value and the variance of X¯m as functions of z (equations (9), (10) and (18)) can be found by transforming the parameters of the lognormal distribution through

19a
19b

At this point, the effect of transformation uncertainty related to the normally distributed T (in equation (8)) with parameters μT and бT2 can be taken into account if needed. Assuming no correlation between the transformation uncertainty and the other error components

20a
20b

As equation (20) combines log-normally and normally distributed variables, numerical simulation of the corresponding probability distribution of X¯ is favourable, as discussed in the illustrative example.

To determine starget as the percentile corresponding to the probability P(G < 0) = pFT (equation (5)), the distribution of S needs to be evaluated (Fig. 1). In general terms

21

where Δe(z) is the change in void ratio at depth z because of the change in effective stress Δσ′(z) at depth z; e0(z) is the initial void ratio at depth z; and hclay is the total thickness of the saturated clay layer. For most clays, Δe can be described by the compression index, Cc, evaluated as the slope of the e–log(σ′) plot, such that

22

where σ0 is the initial vertical stress. However, for soft clays, the assumption that this slope is a straight line is not valid; its application would greatly overestimate the settlement (Larsson, 1986). This paper therefore applies the more detailed approach for the evaluation of the distribution of S that is the standard practice for the soft Swedish clays. (The presented design procedure can, however, be used in a straightforward way also with the Cc.) The approach is based on CRS oedometer tests and allows straightforward prediction of primary consolidation settlements for practical engineering purposes from the shape of stress–strain curves (Larsson & Sällfors, 1986; SIS, 1991). Reformulating equation (21)

23

where Δϵ(z) is the change in strain at depth z because of Δσ′(z). The shape of the stress–strain curves is described with the parameters preconsolidation pressure σc, limit pressure σL towards increasing soil modulus, two soil moduli M0 and ML, a modulus number M′ = ΔMσ′ for the part where the modulus increases linearly with the effective stress, and a baseline intersection parameter a (Fig. 3). In essence, the method implies that the stress–strain curve is divided into three parts with different inclination (soil moduli). To find the Δϵ(z) corresponding to some Δσ′(z), one can in principle enter the range of Δσ′(z) – that is [σ0(z), σ0(z) + Δσ′(z)] – on the horizontal axis in Fig. 3 and read the corresponding strain range off the vertical axis. This procedure can be mathematically described by the following set of equations, which are used depending on what part of the curve the range of Δσ′(z) covers (Larsson & Sällfors, 1986)

24a
24b
24c

where a = σL − ML/M′. Evaluation details regarding the settlement parameters from CRS tests are presented in the Appendix.

Fig. 3.

Definition of settlement parameters based on CRS tests (Larsson & Sällfors, 1986). The strain corresponding to an applied load can be read off the vertical axis, as shown with dotted lines. The settlement parameters describe this relationship mathematically. Details of their evaluation are summarised in the Appendix

Fig. 3.

Definition of settlement parameters based on CRS tests (Larsson & Sällfors, 1986). The strain corresponding to an applied load can be read off the vertical axis, as shown with dotted lines. The settlement parameters describe this relationship mathematically. Details of their evaluation are summarised in the Appendix

Close modal

To simplify, the clay stratum can be divided into l separate layers, where each layer is thick enough to allow the assumption of negligible spatial correlation (made in equation (18)). This gives

25

where hj is the thickness of each layer. All parameters required for the calculation of Δϵj are evaluated for the centre of the respective layer based on the CRS oedometer tests and the corresponding uncertainty is taken into account using equations (8)–(20). Having evaluated equation (20) for all relevant geotechnical parameters, a probability distribution of S (equations (24) and (25)) is simulated to obtain a first guess of starget from equation (5). Since the embankment height needs to be compensated with a height hs,comp = starget for the occurring consolidation, Δσ′ needs to be iteratively adjusted with respect to both the obtained starget and the volume of dry crust and embankment material submerged under the groundwater level. Fig. 4 shows this principle: to end up at the intended embankment height hemb above the ground level after unloading of the surcharge, the initial total embankment height at the beginning of the preloading needs to be hemb + hs,comp + hsur (cf. top of Fig. 1), since the embankment will settle in accordance with the predetermined starget (i.e. hs,comp).

In the evaluation of U (equations (1)–(3)), the well resistance is here disregarded for simplicity, such that (cf. Hansbo, 1979, 1981; Hong & Shang, 1998)

26

where rw is the equivalent drain radius; kh is the horizontal hydraulic conductivity of the undisturbed soil; kh is the horizontal hydraulic conductivity of the disturbed soil; and rs is the radius of the remoulded or disturbed soil (the smear zone). Considering Müller & Larsson's (2013) findings that, in practice, uncertainties as regards the relevant geotechnical parameters – mainly in ch – will affect the design more than the choice of model for F, the authors find the simplification of disregarding the well resistance reasonable for practical applications.

Fig. 4.

Schematic illustration of embankment preloading and the situation after unloading. To end up with an embankment height of hemb after unloading the surcharge, the initial embankment height needs to be compensated with a height hs,comp = starget, because of the occurring settlement (GW, groundwater level)

Fig. 4.

Schematic illustration of embankment preloading and the situation after unloading. To end up with an embankment height of hemb after unloading the surcharge, the initial embankment height needs to be compensated with a height hs,comp = starget, because of the occurring settlement (GW, groundwater level)

Close modal

To ensure that the design criteria (equations (6) and (7)) are satisfied with acceptable probability, a sufficiently large surcharge load needs to be selected (Fig. 1). The higher the surcharge, the higher the probability that sufficient settlement (equation (6)) and overconsolidation (equation (7)) will develop during the preloading. To analyse the effect of the surcharge load on this probability, a set of probability distributions of the predicted settlement and OCR after tmax are simulated by computing the following equations for different surcharge loads (i.e. surcharge heights hsur)

27a
27b

where Ssur is the predicted settlement after infinite time for some selected hsur evaluated with the same principle as shown in equations (24) and (25); Utmax is the degree of consolidation after tmax (equations (1)–(3)); γemb is the unit weight of the embankment; hemb is the final height of the embankment above ground level (see Fig. 4); hcrust is the thickness of the dry crust; γemb is the effective unit weight taking into account any submersion of embankment material under the groundwater table; and γw is the unit weight of water taking into account the uplift effect on the submerged dry crust. In equation (27b), σ0 is evaluated for the middle of the clay stratum (cf. equation (7)) and complete submersion of the dry crust is assumed; reformulation to take only partial submersion into account is straightforward. Moreover, because of the more rapid consolidation at the PVDs, increased horizontal load distribution area with depth is assumed negligible.

Having established the probability distributions for Ssurtmax and OCRsurtmax for a range of hsur, the respective probabilities of meeting the design criteria (Ssurtmax ≥ starget and OCRsurtmax ≥ 1·10 in the middle of the clay stratum) can be calculated for this range of hsur. The designing engineer then selects a suitable hsur that with acceptable probability satisfies the design criteria; this decision–theoretical consideration is further elaborated upon in the ‘Discussion’ section.

To illustrate the proposed design procedure, a practical example is presented, using real case data for the soil characterisation and embankment geometry. A 1·2 m high road embankment is to be constructed on 15·5 m of very soft clay (after unloading of 0·3 m of the dry crust). The embankment is located in the south of the county of Stockholm, Sweden, and has a width of 23 m. A critical cross-section is presented in Fig. 5, for which the design is made. PVDs are to be installed to increase the rate of consolidation; this example considers only the specific PVD design described in Table 2 to make it possible to focus on the surcharge design. The available preloading time (tmax) is 15 months. Soil samples have been collected at the critical section and the results of this investigation are presented in Table 3, Figs 6 and 7. The deformation properties were evaluated with the CRS oedometer test (see Appendix), in accordance with the Swedish standard (SIS, 1991). Any settlement of the dry crust and underlying till layer is disregarded.

Fig. 5.

Cross-section of analysed case

Fig. 5.

Cross-section of analysed case

Close modal
Fig. 6.

Result of geotechnical investigation of water content, wN, and unit weight of the clay, γcl with assessment of variability of the exponential mean value trendlines presented as ±1 standard deviation (SD)

Fig. 6.

Result of geotechnical investigation of water content, wN, and unit weight of the clay, γcl with assessment of variability of the exponential mean value trendlines presented as ±1 standard deviation (SD)

Close modal
Fig. 7.

Settlement parameters from CRS oedometer tests with assessment of variability of the exponential mean value trendlines presented as ±1 standard deviation

Fig. 7.

Settlement parameters from CRS oedometer tests with assessment of variability of the exponential mean value trendlines presented as ±1 standard deviation

Close modal
Table 2.

PVD design in the illustrative design example

ParameterSymbolValue
Influence radius of drains*re0·37 m
Drain radiusrw0·033 m
Smear zone radiusrs = 2rw0·066 m
Conductivity ratio of smeared zonekh/kh4
Horizontal/vertical conductivity ratiokh/kv2·5
Longest drain pathhdr7·75 m
*

Equivalent to a triangular pattern with 0·7 m centre-to-centre drain spacing.

Two-way drainage assumed.

Table 3.

Geotechnical parameters with probability distributions considered in the illustrative design example

ParameterSymbolComment
Unit weight of clayγclSeven samples (Fig. 6)
Natural water contentwNSeven samples (Fig. 6)
Preconsolidation pressureσcNine samples (Fig. 7)*
Limit pressure towards increasing modulusσLNine samples (Fig. 7)*
Modulus for σ′ ≤ σcM0Nine samples (Fig. 7)
Modulus for σc < σ′ ≤ σLMLNine samples (Fig. 7)
Unit weight of the embankmentγembAssumed log-normally distributed with mean 20·8 kN/m3 and COV of 5%
Vertical consolidation coefficientcvEvaluated deterministically (0·2 m2/year); 50% COV assumed for all layers
Horizontal consolidation coefficientchCalculated as 2·5cv with assumed 50% COV for a log-normal Ti
*

σc and σL were assumed perfectly correlated to avoid the impossible situation of having σc > σL.

COV in line with data presented by Lumb (1974).

Since trend lines with depth are present for the investigated soil properties, the procedure for probabilistic soil characterisation outlined by equations (8)–(20) was applied on the random parameters (Figs 6 and 7). The clay stratum was divided into four layers (equation (25)).

For simplicity, measurement errors were not considered. Moreover, ch was assumed to be 2·5cv, which the Swedish Road Administration (SRA, 1989) suggests for Swedish clays and to which an unbiased log-normally distributed transformation error equivalent to 50% coefficient of variation (COV) was added (equation (20)). The value of M′ was calculated by applying the established empirical relationship between M′ and wN (Larsson & Sällfors, 1986) as a transformation model, T

28

to which an unbiased normally distributed transformation error of 15% COV was assigned, based on the data that were used to derive the relationship. All geotechnical parameters were assumed mutually independent for simplicity, except for the parameters σc and σL, which were assumed fully correlated to avoid the impossible case of having σL < σc (cf. Fig. 3). Transformation errors and correlation were taken into account using numerical simulation of the probability distributions in Matlab.

In this design example, the pFT was set to 5%, in line with Akbas & Kulhawy (2009); see also Fenton et al. (2016). This implies a 5% probability of having post-completion settlements beyond Δsallow. Reserving such allowable settlements for any remaining secondary compression settlement that still occurs despite the OCR requirement (equation (7)), the post-completion primary compression settlement was strictly limited in the design calculations – that is, Δsallow = 0.

Crude Monte Carlo simulation was used to generate 10 000 samples for each parameter at each of the four layer centres from the evaluated random variables. To establish starget + Δsallow as the 5% upper percentile of S, samples of S (equation (25)) were iteratively generated for increasing Δσ′ until the equality Δσ′ = γemb(hemb + hcrust) + γemb(starget − hcrust) − γwhcrust was satisfied, thereby compensating the embankment height for occurring settlements (see Fig. 4). This gave starget = 1·34 m to be satisfied during the preloading phase (Fig. 8(a)). Samples of Utmax were generated from a distribution (equations (1)–(3) and (26)) based on the deterministic parameters in Table 2 and the random cv (Fig. 8(b)).

Fig. 8.

Histograms of (a) total predicted settlement after infinite time, where starget was determined as the upper percentile corresponding to pFT; (b) distribution of Utmax

Fig. 8.

Histograms of (a) total predicted settlement after infinite time, where starget was determined as the upper percentile corresponding to pFT; (b) distribution of Utmax

Close modal

To analyse the effect of different surcharge loads on the two design criteria, Ssurtmax and OCRsurtmax (equation (27)) were evaluated for a range of surcharge loads: 0 ≤ hsur ≤ 4 m. The probabilities of them meeting their respective design criteria are shown in Fig. 9. For example, the OCR requirement is satisfied with 97% probability at hsur = 1·25 m; however, it is only 75% probable that starget will be attained before tmax for this load. A correlation analysis of the two design criteria provides additional valuable insights (Fig. 10): by analysing the underlying simulations of the probabilities in Fig. 9 for the considered hsur, the initial surcharge load can also be selected with the unloading strategy in mind. For example, by applying hsur = 1·25 m, the settlement monitoring can be used not only to verify attainment of starget, but also to ensure fulfilment of the OCR requirement, because Fig. 10(a) indicates that if the measured settlement will exceed starget within tmax, the OCRtarget will also be satisfied. Conversely, for hsur = 0·75 m, exceedance of starget does not guarantee attainment of OCRtarget (Fig. 10(b)).

Fig. 9.

Probability of satisfying the two design criteria for a range of hsur

Fig. 9.

Probability of satisfying the two design criteria for a range of hsur

Close modal
Fig. 10.

Visualisation of the respective probabilities of satisfying the two design criteria for (a) hsur = 1·25 m and (b) hsur = 0·75 m

Fig. 10.

Visualisation of the respective probabilities of satisfying the two design criteria for (a) hsur = 1·25 m and (b) hsur = 0·75 m

Close modal

A suitable hsur for the preliminary design of the surcharge is selected considering the correlation analysis and the appetite for client's risk; the authors recommend selecting hsur such that the OCRtarget is attained before starget. The monitoring during preloading and the unloading strategy (discussed below) thereby both become straightforward, as one can rely on the observed vertical deformation for both targets.

If the surcharge has a considerable height, the stability may be unsatisfactory. This is normally managed by designing berms to the embankment slopes. It may also be favourable to install vertical drains under the berms, as consolidation improves the shear strength of the soil. For very high surcharges, a staged construction sequence may be required (see e.g. Müller et al., 2016). Installing vertical drains under the berms also considerably limits the horizontal deformation, which otherwise may impair the evaluation of the settlement monitoring during construction.

Following the framework of the observational method (Table 1), a monitoring plan to observe the settlements is prepared, along with alarm thresholds and a contingency action plan that describes how the surcharge shall be raised if an alarm threshold is violated.

If the settlement and pore pressure measurements during the preloading indicate that the consolidation is taking longer than expected, the contingency action to raise the surcharge is applied to increase the rate of deformation so that the targets can be attained within tmax. For a detailed discussion on monitoring of the consolidation process for embankments on clay, the authors refer the reader to Prästings et al. (2014).

If hsur has been selected as recommended above, it is crucial to unload the surcharge when starget is attained. If unloading is delayed, the continuing consolidation will decrease the volume of fill that is removed down to the final embankment crest level. This may leave the OCR requirement not fulfilled (equations (7) and (27b)), making significant secondary compression more likely to occur after completion of the embankment and the superstructure.

As established in the earlier section entitled ‘Overview of the design procedure’, the engineer who designs the surcharge load and the vertical drains has to take significant uncertainties regarding the ground conditions into account. By designing the surcharge with the observational method, these uncertainties can be managed cost-effectively. As shown in Fig. 9, the larger the surcharge load, the higher is the probability of satisfying the two design criteria. However, the engineer fortunately does not need to satisfy the design criteria with high probability, as the observational method offers the possibility to adjust the design to the actual conditions with a contingency action if the initial design should prove to be inadequate. Alternatively, the engineer may choose to apply a higher surcharge from the outset, at a higher initial cost but with the advantage of avoiding a cumbersome and potentially costly contingency action. The design challenge lies in comparing the cost and probability of having to raise the surcharge considerably after some time, with the certain cost associated with a higher initial surcharge.

What probability, pacc, of successful initial surcharge height is acceptable then (see requirement 2(b) in Table 1)? In the authors’ opinion, there is no specific value that can be used in all projects, but pacc needs to be established for each individual project by the appropriate risk owner – that is, the person responsible for achieving satisfactory quality in the project and who has the mandate to make decisions about risks. This follows from the general principles of geotechnical risk management (ISO, 2009; Spross et al., 2018).

The selection of pacc is not critical for the structural design; it is, in fact, only a matter of economic risk, as the prepared contingency action to raise the surcharge ensures that the design criteria, in principle, can be met during the available preloading time in all situations. The pacc will therefore depend on the risk owner's risk appetite. For reference, a risk-neutral decision maker (who finds the solution that minimises the statistically expected total project cost to be the most favourable) can find the optimal initial hsur by making a pre-posterior decision analysis using the reliability framework for the observational method outlined by Spross & Johansson (2017). The complete decision analysis is not within the scope of this paper, but conceptually the outcome will largely depend on the cost and probability of having to raise the surcharge height as a contingency action, in relation to the certain cost of applying a higher surcharge from the outset. For example, if the contingency action is cheap because of large availability of material, it can be allowed with higher probability. Note, however, that a complete design analysis of the embankment should also consider the PVDs, as the probability of satisfying the design criteria can be increased by, for example, decreasing the drain spacing.

The proposed design procedure does not consider spatial variability of the evaluated random parameters. However, the authors find this simplification reasonable when the design is made for a critical embankment section where the geotechnical investigation has also been carried out. The available information from the geotechnical investigation and the evaluated probability distributions therefore well represent the present knowledge of the geotechnical conditions on this particular section. A procedure that considers spatial variability and applies local averaging (e.g. Vanmarcke, 2010; Bari & Shahin, 2014; Jiang et al., 2014; Mašín, 2015) would, however, be useful if an embankment section at some distance from the closest investigated soil volumes is to be analysed. This is therefore a natural future advance of the procedure. In practice, however, the authors believe that if hsur has been evaluated for a critical section of the embankment, using the same height for a longer stretch of the embankment should give sufficiently good results.

This paper presents a novel probabilistic design procedure for embankments on soft clay that is compatible with the observational method. The procedure evaluates the suitable surcharge load to be used in combination with PVDs. While the procedure analyses the primary compression settlements of the clay, it also takes secondary compression into account by ensuring a sufficient degree of overconsolidation after unloading of the surcharge. The procedure highlights the considerable effect that the uncertainty regarding key geotechnical parameters – mainly the consolidation coefficients – has on the prediction of the rate of consolidation. Moreover, it is shown how the observational method can be efficiently applied to manage this uncertainty to avoid project delay. The involved analyses can also contribute considerably to managing some of the geotechnical risks in the construction of embankments.

The authors would like to acknowledge the Swedish Transport Administration for funding this project and supplying data for the illustrative design example.

Constant-rate-of-strain oedometer tests

In Swedish practice, incremental tests have mainly been replaced by CRS oedometer tests with drainage only at the top surface (SIS, 1991). The result is plotted as a stress–strain curve and a modulus–stress curve on linear scales (Fig. 3). The σc is evaluated by extending lines of the two straight parts of the stress–strain curve and inscribing an isosceles triangle between the lines and the stress–strain curve. The stress at the left angle gives the σc. For better agreement with standard incremental tests, the stress–strain curve is then moved laterally a distance c, so that it passes through σc on the curve.

In the modulus–stress plot, the initial modulus M0 is extended to σc, at which point the modulus is assumed to drop instantly to ML. To evaluate σL, the linearly increasing part of the modulus curve is moved c kPa to the left, giving σL at the intersection with ML. Lastly, M′ is the slope of the linearly increasing part of the modulus curve. Because of swelling effects and sample disturbance, M0 is regularly underpredicted in CRS tests. In practice, M0 is therefore usually estimated from empirical relationships. Further details can be found in Larsson & Sällfors (1986) and Larsson (1986).

a

intersection parameter evaluated from CRS

a^

regression parameter

b^

regression parameter

Cc

compression index

ch

coefficient of horizontal consolidation

cv

coefficient of vertical consolidation

e0

initial void ratio

F

function describing the effect of drain spacing, soil disturbance and well resistance

G

limit state function

hclay

total thickness of the saturated clay

hcrust

thickness of the dry crust

hdr

maximum vertical drain path

hemb

final height of the embankment above ground level

hj

thickness of clay layer j

hs,comp

required embankment height compensation for the occurring settlement

hsur

surcharge height

I

identity matrix

kh

horizontal hydraulic conductivity of the undisturbed soil

kh

horizontal hydraulic conductivity of the disturbed soil

l

number of layers of clay stratum

M

soil modulus number evaluated from CRS

M0

soil modulus evaluated from CRS

ML

soil modulus evaluated from CRS

n

number of data points

OCRtarget

target overconsolidation ratio

OCRsurtmax

overconsolidation ratio after unloading the surcharge at tmax

pacc

acceptable probability of satisfying a design criterion

pFT

acceptable target failure probability

re

radius of the influence zone of a PVD

rs

radius of the remoulded or disturbed soil

rw

equivalent drain radius

S

probability distribution of the predicted long-term primary compression settlement without surcharge

Ssur

probability distribution of the predicted long-term primary compression settlement with surcharge

Ssurtmax

probability distribution of the primary compression settlement caused by the surcharge at tmax

starget

target primary compression settlement

T

transformation model (that may contain a random error)

t

time

tmax

maximum allowable preloading time

U

degree of consolidation

Uh

average degree of horizontal consolidation

Utmax

degree of consolidation at tmax

Uv

average degree of vertical consolidation

wN

water content

X

vector of random variables, Xi

X¯

mean value of a geotechnical parameter including all errors

X¯m

mean value of the measured geotechnical property including random error

x¯m

expected mean value of the measured geotechnical property

Z

matrix of depths

z

vector of depths

z

depth

z¯

mean depth

Γ2

variance function

γcl

unit weight of the clay

γemb

unit weight of the embankment material

γemb

effective unit weight of the embankment material

γw

unit weight of water

Δe

change of void ratio

ΔM

change in soil modulus

ΔS

probability distribution of the occurring residual settlement

Δsallow

allowable residual settlement

Δϵ

change in strain

Δσ

change in effective stress

ε[*]

random error factor

ε{ln}

random error factor after transformation with the natural logarithm

бz2

sample variance of z

бln2

variance of the random error component described by the subscript [*] after transformation with the natural logarithm

б2

variance of the random variable described by the subscript [*]

μ[*]

mean value of the random variable described by the subscript [*]

σ0

initial vertical stress

σc

preconsolidation pressure evaluated from CRS

σL

limit pressure towards increasing soil modulus evaluated from CRS

ψz

factor for evaluation of statistical uncertainty

data

variability in available measurement data

inh

inherent variability

me

measurement error related to the estimation of the mean value

me,m

measurement error related to the measured data point

st

statistical error

z

subscript indicating a function of z

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