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Technical Note

Discussion/comments of «Wave-induced uplift pressure on berm revetment with Seabee slope” by Zijun Zhou, Yongping Chen, Yi Pan, Yusheng Zhen & Min Gan

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Pages 372-375 | Received 28 Sep 2021, Accepted 08 Nov 2021, Published online: 23 Nov 2021

ABSTRACT

The purpose of these comments and discussion has been to demonstrate how wave statistics can be incorporated into future applications of the proposed empirical equations to estimate the maximum relative uplift pressure under positive and negative freeboards on berm revetment with Seabee slope. This is demonstrated by using a joint distribution of significant wave height and surf parameter as well as by giving examples of the results.

1. Discussion

First, the discussers wish to compliment the authors, Zhou et al. (Citation2020) (hereafter referred to as Z20), on their results proposing empirical equations to estimate the maximum relative uplift pressure under positive and negative freeboards on berm revetment with Seabee slope. The empirical equations were obtained as best fit to data from laboratory tests in model scale 1:14 representing irregular wave conditions. Overall, the uneven distribution of the uplift pressure on this revetment structure would affect its stability and cause damage. These comments and discussion have been written to demonstrate how wave statistics can be incorporated into future applications of the authors’ empirical equations.

Z20 defined the dimensionless parameter

(1) p1%=p1%ρgHs(1)

representing the 1% relative uplift pressure, where p1% is the uplift pressure level exceeded by 1% of the measured time series, ρ is the fluid density, g is the acceleration due to gravity, and Hs is the significant wave height. The following empirical equations to estimate the maximum relative freeboard on berm revetment with Seabee slope were proposed:

(2) p1%=γaξpbexp(cξp)(2)

For negative freeboard:

(3) γ=1.172(3.623RbHs+0.6836)2;0.36RbHs0.06(3)
(4) (a,b,c)=(0.5214,1.1,0.2027);1.38ξp2.78(4)

For positive freeboard:

(5) γ=0.97+0.009RbHs1;0.09RbHs0.56(5)
(6) (a,b,c)=(0.76,0.78,0.31);1.3ξp2.8(6)

where γ is the influence parameter of the elevation of the berm expressed in terms of the relative freeboard Rb/Hs, and Rb is the freeboard of the berm. Moreover, ξp is the surf parameter defined as ξp=tanθ/Hs/λp where tanθ is the slope with an angle θ to the horizontal, λp=(g/2π)Tp2 is the deep water spectral wave length, Tp is the spectral period, and Hs is the deep water significant wave height. EquationEquations (1) to (Equation6) were obtained as best fit to data obtained in physical model tests performed in a wave flume using irregular waves in model scale 1:14 (see Z20 for more details).

The statistical features of p1% (and thus of p1%) will be exemplified based on wave statistics obtained from the joint probability density function (pdf) of Hs and ξp provided in the Appendix, which is based on data from wave measurements made in the Northern North Sea during a 29 years period. Here, the conditional expected value of p1% given Hs,Ep1%|Hs and the conditional variance of p1% given Hs, Varp1%|Hs are considered.

Based on EquationEquations (4) and (Equation6), p1% is valid within a finite interval, and thus, the conditional pdf of ξp given Hs, f(ξp|Hs) in EquationEquation (A2) in the Appendix follows the truncated lognormal pdf

(7) ft(ξp|Hs)=1Nf(ξp|Hs);ξP1=1.3ξpξP2=2.8(7)
(8) N=Φlnξp2μσΦlnξP1μσ(8)

where Φ is the standard Gaussian cumulative distribution function (cdf) (where μ and σ2 are the mean value and the variance, respectively, of lnξp) given by

(9) Φ(x)=12πxet2/2dt(9)

It should be noted that the interval limits ξP1 and ξP2 in EquationEquation (7) are based on the results depicted in Fig. 13 of Z20 (i.e. slightly extending the interval in EquationEquation (4)). Further details of f(ξp|Hs) are given in EquationEquations (A2) to (EquationA6) in the Appendix.

First, define

(10) P(ξp|Hs)p1%γ=aξpbexp(cξp)(10)

Then, the conditional expected value of P given Hs, EP|Hs and the conditional variance of P given Hs, VarP|Hs are calculated from the truncated pdf of ξp given Hs in EquationEquations (7) and (Equation8) as (Bury Citation1975)

(11) EP|Hs=ξP1ξP2Pξp|Hsftξp|Hsdξp(11)
(12) VarP|Hs=E(P(ξp|Hs))2EP|Hs2(12)

where

(13) E(P(ξp|Hs))2=ξP1ξP2P(ξp|Hs)2ftξp|Hsdξp(13)

The conditional coefficient of variation is

(14) RP|Hs=(VarP|Hs)1/2EP|Hs(14)

depict EP|Hs () and RP|Hs () for the negative and positive freeboards versus Hs in the range 2– 3 m. This interval of Hs includes the full scale values Hs= 2.1 m, 2.5 m, 2.8 m corresponding to the model scale (1:14) values Hs= 0.15 m, 0.18 m, 0.20 m, respectively (see Z20). Here and in the following examples, the slope tanθ is taken as 1:3 (as in Z20).

Figure 1. EP|Hs versus Hs for negative and positive freeboards with slope 1:3.

The positive and negative freeboard ranges represent the Z20 data.
Figure 1. EP|Hs versus Hs for negative and positive freeboards with slope 1:3.

Figure 2. RP|Hs versus Hs for negative and positive freeboards with slope 1:3.

Figure 2. RP|Hs versus Hs for negative and positive freeboards with slope 1:3.

From , it appears, as Hs increases from 2 m to 3 m, that: EP|Hs increases from about 0.84 to about 0.88 for positive freeboard; and decreases from about 0.71 to about 0.62 for negative freeboard. The Z20 data representing the full scale values Hs= 2.1 m, 2.5 m, 2.8 m corresponding to ξp = 2.04, 1.86, 1.77, respectively, using Tp=1.914s=7.1s, are also shown for the positive and negative freeboard ranges taken from Fig. 13 in Z20. It appears that the two curves are within the ranges of the corresponding data.

From , it appears, as Hs increases from 2 m to 3 m, that: RP|Hs varies slightly from about 0.038 to about 0.035 with a maximum of about 0.039 for Hs = 2.3 m for positive freeboard; and decreases from about 0.133 to about 0.105 for negative freeboard.

Furthermore, examples of physical results are provided for negative and positive freeboards using the results in . Combination of EquationEquations (1), (Equation10) and (Equation11) yields

(15) Ep1%|Hs=ρgHsγEP|Hs(15)

First, for negative freeboard:

Taking Rb/Hs=0.25 in EquationEquation (3) gives γ=1.12 which substituted in EquationEquation (15) for Hs= 2.5 m, ρ= 1025 kg/m3 and EP|Hs=2.5m=0.656 (see ) yields

(16) Ep1%|Hs=2.5m=1025×9.81×2.5×1.12×0.656=1.85×104Nm2(16)

Furthermore, now Rp1%|Hs=2.5m=RP|Hs=2.5m=0.124 (see ), and thus Ep1%|Hs=2.5m plus and minus one standard deviation of 12.4% become 2.08×104N/m2 and 1.62×104N/m2, respectively.

Second, for positive freeboard:

Taking Rb/Hs=0.25 in EquationEquation (5) gives γ=1.01 which substituted in EquationEquation (15) for EP|Hs=2.5m=0.862 (see ) yields

(17) Ep1%|Hs=2.5m=1025×9.81×2.5×1.01×0.862=2.19×104Nm2(17)

Furthermore, now Rp1%|Hs=2.5m=RP|Hs=2.5m=0.039 (see ), and thus Ep1%|Hs=2.5m plus and minus one standard deviation of 3.9% become 2.28×104N/m2 and 2.10×104N/m2, respectively.

Thus, as expected, these examples demonstrate that the wave-induced uplift pressure on berm revetment with Seabee slope is larger under positive freeboard than under negative freeboard.

In future applications of the empirical equations to estimate the maximum relative uplift pressure under positive and negative freeboards on berm revetment with Seabee slope proposed by Zhou et al. (Citation2020), it should be considered to implement the statistical properties of waves as demonstrated in this discussion, although the proposed equations and parameters may be subject to regional limitations. The utilization of these empirical equations jointly with wave statistics should represent an important component in, for instance, risk analysis used as part of revetment structure design. It should be noted, however, that implementation of wave statistics is not limited to the joint distribution of significant wave height and surf parameter applied here.

Disclosure statement

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

References

Appendix.

Joint pdf of Hs and ξP

Here, the joint pdf of Hs and ξP provided by Myrhaug and Fouques (Citation2010) (hereafter referred to as MF10) is used as an example. This (Hs,ξp) distribution was deduced based on a joint pdf of Hs and Tp obtained as a best fit to data from wave measurements made in the Northern North Sea during a 29-year period. The joint pdf of Hs and ξp is given as

(A1) f(Hs,ξp)=f(ξp|Hs)p(Hs)(A1)

where f(Hs) is the marginal pdf of Hs given by the combined lognormal and Weibull distribution given in EquationEquations (2Equation4) in MF10. The conditional pdf of ξp given Hs is given by the following lognormal distribution

(A2) f(ξp|Hs)=12πσξpexp(lnξpμ)22σ2(A2)

where μ and σ2 are the mean value and the variance, respectively, of lnξp, given by

(A3) μ=lntanθ(Hs/(g/2π))1/2+a1+a2Hsa3(A3)
(A4) σ2=b1+b2eb3Hs(A4)

with

(A5) (a1,a2,a3)=(1.780,0.288,0.474)(A5)
(A6) (b1,b2,b3)=(0.001,0.097,0.255)(A6)

where Hs is in meters in EquationEquations (A3) and (EquationA4) (see MF10 for more details).