For engineering purposes, the density of soil is often expressed in terms of void ratio. Void ratio is a key parameter in critical state soil mechanics and governs our understanding of soil compressibility, permeability, and shear strength. Typically, in-situ void ratio is evaluated based on laboratory measurements on high-quality, "undisturbed" samples of soil. While undisturbed sampling of clayey soils is commonplace in geotechnical practice, high-quality samples of granular soils are difficult and expensive to obtain. Hence, void ratio of granular soils is typically estimated using empirical relationships to in-situ measurements from penetration testing. Even for clean sands there is significant variability in these estimates, and for mixed-grain soils the applicability and performance of the empirical relationships is quite uncertain. Therefore, a more reliable way of measuring in-situ void ratio is needed. This paper examines the feasibility of evaluating in-situ soil void ratio based on the theory of linear poroelasticity and the propagation velocity of compression and shear waves (i.e., vp and vs, respectively) through fluid-saturated porous materials. Specifically, soil void ratio is evaluated via a porosity relationship that is a function of vp, vs, and four additional parameters describing the physical properties of the soil (i.e., the Poisson's ratio of the soil skeleton, the bulk modulus and mass density of water, and the mass density of the solid soil particles). In this study, the effectiveness of using high-resolution vp and vs measurements from direct-push crosshole testing to estimate in-situ void ratios is investigated at ten, predominantly clean-sand case history sites in Christchurch, New Zealand, via a comparison with void ratio estimates developed from penetration testing measurements. The seismic-based void ratio estimates are shown to be particularly sensitive to vp, requiring a measurement error of less than 2%. Given the need to make such precise in-situ measurements of vp, the DPCH method is believed to show particular promise for enabling accurate, seismic-based estimates of void ratio in the future.
Citation: Andrew C. Stolte, Brady R. Cox. Feasibility of in-situ evaluation of soil void ratio in clean sands using high resolution measurements of Vp and Vs from DPCH testing[J]. AIMS Geosciences, 2019, 5(4): 723-749. doi: 10.3934/geosci.2019.4.723
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Abstract
For engineering purposes, the density of soil is often expressed in terms of void ratio. Void ratio is a key parameter in critical state soil mechanics and governs our understanding of soil compressibility, permeability, and shear strength. Typically, in-situ void ratio is evaluated based on laboratory measurements on high-quality, "undisturbed" samples of soil. While undisturbed sampling of clayey soils is commonplace in geotechnical practice, high-quality samples of granular soils are difficult and expensive to obtain. Hence, void ratio of granular soils is typically estimated using empirical relationships to in-situ measurements from penetration testing. Even for clean sands there is significant variability in these estimates, and for mixed-grain soils the applicability and performance of the empirical relationships is quite uncertain. Therefore, a more reliable way of measuring in-situ void ratio is needed. This paper examines the feasibility of evaluating in-situ soil void ratio based on the theory of linear poroelasticity and the propagation velocity of compression and shear waves (i.e., vp and vs, respectively) through fluid-saturated porous materials. Specifically, soil void ratio is evaluated via a porosity relationship that is a function of vp, vs, and four additional parameters describing the physical properties of the soil (i.e., the Poisson's ratio of the soil skeleton, the bulk modulus and mass density of water, and the mass density of the solid soil particles). In this study, the effectiveness of using high-resolution vp and vs measurements from direct-push crosshole testing to estimate in-situ void ratios is investigated at ten, predominantly clean-sand case history sites in Christchurch, New Zealand, via a comparison with void ratio estimates developed from penetration testing measurements. The seismic-based void ratio estimates are shown to be particularly sensitive to vp, requiring a measurement error of less than 2%. Given the need to make such precise in-situ measurements of vp, the DPCH method is believed to show particular promise for enabling accurate, seismic-based estimates of void ratio in the future.
1.
Introduction
One of interactions between three types of populations is known as non-transitive, cyclic competition or a rock-paper-scissors relationship, that is, type A is stronger than type B, and type B is superior to type C, which in turn is better than A. We can find several examples of this kind of interaction in nature; the most well-known are bacteria (e.g., [1,2,3,4]) and lizards (e.g., [5,6,7]).
Barreto et al. [8] proposed phenotypic and genotypic cyclic competition models to clarify the fact that three throat morphs in male lizards, known as orange, blue, and yellow, are maintained with a rock-paper-scissors relationship. Both models have the same equilibrium, but the latter gives a wider stability region than the former. Barreto et al. [8] analyzed their model by fixing all payoffs except two elements, which are given by variable parameters. However, such a case is difficult to manage because an internal equilibrium depends on these parameters. Then we consider an alternative setting as an internal equilibrium with equal frequencies for all phenotypes independent of parameters, namely, we use symmetric conditions of parameters to obtain global insights into the dynamics in this simplified system for the convenience of analysis.
In this paper, we re-examine stability conditions under the following situations: symmetric parameters for the phenotypic model, cyclic allele dominance rule, and spatial structure. We obtain the following results: (ⅰ) Cyclic allele dominance rule in a genotypic model gives a wider stable region of internal equilibrium than the allele dominance rule observed in lizards. (ⅱ) Spatial structure drastically changes the dynamical behavior, especially when all three phenotypes coexist in almost all the parameter spaces when both competition and dispersal occur locally.
In the next section, we review the phenotypic model and its corresponding genotypic model proposed by [8] and then restrict these models with two parameters to generate an internal equilibrium independent of the parameters. In section 3, we derive local stability conditions for each model. We consider cyclic allele dominance rule in section 4. In section 5, we investigate the effects of spatial structure on the stability of the internal equilibrium.
2.
The phenotypic model and its corresponding genotypic model
First, we consider a phenotypic model of cyclic competition, or a rock-paper-scissors game, following [8]. There are three phenotypes O,B, and Y. O has a better strategy than B, and B is superior to Y, which is, in turn, surpasses O. When we use a payoff matrix in Table 1, this relation can be expressed by MOY<MOO<MOB,MBO<MBB<MBY, and MYB<MYY<MYO, where MIJ is a payoff of focal individual I∈{O,B,Y} against an opponent J∈{O,B,Y}.
Table 1.
Payoff matrix of rock-paper-scissors game. MIJ is a payoff of focal individual I∈{O,B,Y} against an opponent J∈{O,B,Y}. The following magnitude relations hold: MOY<MOO<MOB,MBO<MBB<MBY,MYB<MYY<MYO.
Using these payoffs obtained by the competition between two phenotypes, the dynamics of phenotypic model are defined as
pO,n+1=WOWpO,n,
(2.1)
pB,n+1=WBWpB,n,
(2.2)
pY,n+1=WYWpY,n,
(2.3)
with pO,n,pB,n, and pY,n as the fractions of phenotypes O,B, and Y, respectively, at generation n. Here WO,WB, and WY are the fitnesses of phenotypes O,B, and Y, respectively, and W is the average fitness of the population:
WO=MOOpO,n+MOBpB,n+MOYpY,n,
(2.4)
WB=MBOpO,n+MBBpB,n+MBYpY,n,
(2.5)
WY=MYOpO,n+MYBpB,n+MYYpY,n,
(2.6)
W=WOpO,n+WBpB,n+WBpY,n.
(2.7)
This is a standard model of the rock-paper-scissors game (e.g., [9,10]).
At equilibrium we have
W=WO=WB=WY
(2.8)
by eqs.(2.1)–(2.3). A unique internal equilibrium solution for the above simultaneous equations (2.8) with pO+pB+pY=1 is
pO=M1M1+M2+M3,
(2.9)
pB=M2M1+M2+M3,
(2.10)
pY=M3M1+M2+M3,
(2.11)
where
M1=MOB(MBY−MYY)+MBB(MYY−MOY)+MYB(MOY−MBY),
(2.12)
M2=MOY(MBO−MYO)+MBY(MYO−MOO)+MYY(MOO−MBO),
(2.13)
M3=MOO(MBB−MYB)+MBO(MYB−MOB)+MYO(MOB−MBB).
(2.14)
We have another three equilibria (1,0,0),(0,1,0), and (0,0,1) as the boundary equilibria (ˆpO,ˆpB,ˆpY).
Next we move to a genotypic model corresponding to the above phenotypic model by the genotypic allele dominance rule in which an allele o dominates over two others, y and b, and an allele y dominates b. In other words, genotypes oo,oy, and ob are phenotype O, genotypes yy and yb are phenotype Y, and genotype bb is phenotype B (Table 2).
Table 2.
Allele dominance rule (Ⅰ). An allele o is dominant to other alleles y and b, then three genotypes oo, oy, and ob correspond to a phenotype O. An allele y is dominant to an allele b, then two genotypes yy and yb correspond to a phenotype Y. An allele b is recessive to other alleles, then only one genotype bb corresponds to a phenotype B.
Therefore, because we also have the same relationships (2.8) for genetypic model, we have the same phenotypic equilibrium (2.9)–(2.11) with eqs.(2.12)–(2.14) as the corresponding phenotypic model.
3.
Stability condition for equilibrium (1/3,1/3,1/3)
The payoff matrix includes nine payoffs and is a little complicated. Following [8], we reduce it to two values. We fix the values of the payoffs at 1 for the competitions between the same phenotypes, but we also adopt the symmetric cases --- namely, we give a larger payoff α>1 to a stronger competitor and a smaller one β<1 to a weaker competitor (Table 3), which results in the same equilibrium fractions of 1/3 for all three phenotypes [9].
Table 3.
Payoff matrix with only two parameters. We obtain the same equilibrium fractions of 1/3 for all three phenotypes. Parameter ranges are given by 0<β<1<α.
Then the characteristic equation of the linearized system becomes
λ(λ2+a1λ+a2)=0,
where
a1=−4+α+β1+α+β,
(3.5)
a2=4+2(α+β)+α2+β2(1+α+β)2.
(3.6)
Jury conditions or Schur-Cohn criteria (e.g., [11]) for second-degree characteristic equations λ2+a1λ+a2=0 are known as
|a1|<1+a2<2.
(3.7)
Because a1<0 from eq.(3.5), the left inequality of eq.(3.7) becomes −a1<1+a2, that is, a1+a2+1>0, which holds by the calculation using eqs.(3.5)–(3.6):
a1+a2+1=(1−α)2+(1−β)2+(α−β)22(1+α+β)2>0.
The right inequality of eq.(3.7) 1+a2<2, that is, a2−1<0, gives
αβ>1.
(3.8)
Notice that it is symmetric with respect to α and β; namely, eq.(3.8) does not change when α and β are exchanged.
Indeed, it is known that eq.(3.8) becomes a globally asymptotic stable condition, which can be checked using the Lyapunov function [9]. If eq.(3.8) does not hold, then we can observe the trajectory of the heteroclinic cycle between three vertices in the triangular space for three phenotypic frequencies [9] similar to the three-species Lotka-Volterra cyclic competition model [12] (See Figure 1(a) and (b)).
Figure 1.
Trajectories of phenotypic frequencies. (a)-(c) for eqs.(3.1)-(3.3), (d)-(f) for eqs.(2.27)-(2.36) with Table 3. β is fixed to 0.3. α=2 for (a) and (d), α=3 for (b) and (e), α=4 for (c) and (f). Figure 2(a) tells us that internal equilibrium is unstable for (a), (b) and (d), but stable for (c), (e) and (f). Colorbars indicate the time steps of the dynamics.
Figure 2.
Stable and unstable region on parameter spaces of the equilibrium point (3.4) for (a) allele dominance rule (Ⅰ) and (b) allele dominance rule (Ⅱ). α and β indicate payoffs for strong and weak competitors, respectively. Green, red and yellow regions indicate stable for both phenotypic and genotypic models, stable for genotypic model but unstable for phenotypic one and unstable for both phenotypic and genotypic models, respectively. Allele dominance rule (Ⅱ) has larger stability region than (Ⅰ).
which is a quadratic inequation on α or β and is also symmetric with respect to α and β.
Figure 2(a) shows the local stability region obtained by eq.(3.8) and eq.(3.17). We can observe their dynamics by numerical simulations (Figure 1).
4.
Cyclic allele dominance rule expands the stability region of the internal equilibrium
Common side-blotched lizards have an allele dominance rule (Ⅰ), that is, an allele o for an orange throat is the most dominant over others, an allele y for a yellow one is intermediate, and an allele b for a blue one is the most recessive (Table 2). In other words, this allele dominance rule has three kinds of alleles: most dominant, intermediate, and most recessive. We refer to these as o, y, and b, respectively.
Although perhaps we have not yet discovered it in realistic genetic systems, we can theoretically consider another allele dominance rule (Ⅱ), that is, all alleles having intermediate dominance: o dominant over y, y over b, and b over o (Table 4). This rule could be called as a "cyclic allele dominance rule." Similarly, in this rule, we name these alleles o, y, and b, and any allele can be replaced by another one.
Table 4.
Allele dominance rule (Ⅱ). An allele o is dominant to an allele y, then two genotypes oo and oy correspond to a phenotype O. An allele y is dominant to an allele b, then two genotypes yy and yb correspond to a phenotype Y. An allele b is dominant to an allele o, then two genotypes bb and ob correspond to a phenotype B.
A calculation for allele dominance rule (Ⅱ) similar to that for allele dominance rule (Ⅰ) reveals that the boundary of local stability obtained from the Jury condition (3.7) is determined by
8(αβ−1)+α(α−1)+β(β−1)=0,
(4.1)
which only differs from the first calculation in the smaller coefficient of αβ−1 compared to eq.(3.17). Figure 2(b) shows the local stability region by allele dominance rule (Ⅱ) using eq.(4.1), which clearly has a larger stability region than rule (Ⅰ).
From a theoretical point of view, we should also consider the cases with the same allele dominance rules but with different cyclic competitive strengths. Then another possible combination exists, that is, Table 2 with α<1 and β>1. However, this combination gives the same stability regions as Figure 2(a) by the symmetry of the boundary equation (3.17) on the parameters α and β; eq.(3.17) does not change when α and β are exchanged. On the other hand, it is trivial that no qualitative difference exists between the two cases: Table 4 with α>1 and β<1 and Table 4 with α<1 and β>1.
5.
Spatial simulation
Barreto et al. [8] showed the same stabilizing effect in a genetic system of lizards as the previous section of this paper. Here we introduce a spatial structure into a phenotypic model and consider its effects on population dynamics.
The phenotypic model includes two processes: competition and reproduction. When we add a spatial structure into this model, we restrict the spatial range, both for the opponents against a focal individual and for the dispersion of offspring by reproduction. When we set such a spatial restriction as a whole or as a neighborhood, we consider four distinct cases: (a) global competition and global dispersion, (b) global competition and local dispersion, (c) local competition and global dispersion, and (d) local competition and local dispersion.
The Monte Carlo simulation procedures for the above four cases use the following algorithm (See the C program code in the Electronic Supplementary Materials):
(ⅰ) We prepare a two-dimensional square lattice space, each-side with a size of 100, so that the total number of sites on a whole lattice becomes N=100×100=10000. We use a periodic boundary condition. The states O, Y, and B are randomly distributed according to the initial fractions: (pO,pY,pB)=(0.3,0.3,0.4), respectively.
(ⅱ) The first process is competition, which determines the payoffs after games against randomly chosen opponents. All individuals experience this process. The payoffs for all the sites i(=1,…,N) in a whole population with size N are determined in order; the site (ℓ,m) with x-coordinate ℓ(ℓ=1,…,100) and y-coordinate m(m=1,…,100) on the two-dimensional square lattice is numbered (ℓ−1)×100+m. An individual I∈{O,B,Y} is included on the site i. Another site j is randomly chosen in a whole population in the cases of (a) and (b) or, in the cases of (c) and (d), in the nearest neighboring four individuals. An individual J∈{O,B,Y} is included on the site j. Two individuals I and J compete and an individual I gets a payoff by a payoff matrix (Table 3). All the payoffs are transferred to their offspring, and they are gathered in one offspring pool in the cases of (a) and (c) or, in the cases of (b) and (d), in local offspring pools. Here, we use lower cases for the sites and corresponding upper cases for the states of the individuals on those sites.
(ⅲ) The second process is dispersion, which gives positions of offspring selected from the offspring pool. The model is discrete-generation: all individuals die, and the states at the next time steps for all the sites i(=1,…,N) in a whole population with size N are replaced in order. For each site, an individual is randomly chosen from a whole pool for (a) and (c) or from each local pool for (b) and (d); this choice is made in proportion to the relative payoff against total payoffs in a whole population in the cases of (a) and (c) or in the nearest neighboring four individuals in the cases of (b) and (d). In other words, this random selection depends on WOW,WYW, and WBW. After the previous process (ⅱ), all the individuals have their own payoffs. In the cases of (a) and (c), we can then calculate W,WO,WY, and WB as the total payoffs for, respectively, a whole population, phenotype O, phenotype Y, and phenotype B. In the cases of (b) and (d), we can obtain W,WO,WY, and WB as the total payoffs for, respectively, a local population, phenotype O in the local population, phenotype Y in the local population, and phenotype B in the local population. Here a local population is restricted to individuals on five sites: the focal site and its nearest neighboring four sites.
(ⅳ) The above procedures (ⅱ) and (ⅲ) are repeated for 10000(=100×100) time steps for each parameter combination of α=1,1.05,1.10,…,5 and β=0,0.05,0.10,…,1. The repetition of the simulations is 100 for each parameter combination, and we record the fraction of the coexistence of the three phenotypes.
We show the results of the Monte Carlo simulation by the above algorithm in Figure 3. Case (a) completely coincides with Figure 2(a). Case (b) gives a wider coexistence region due to local dispersion. Case (c) has the same result as case (a) because the global dispersal produces the same effect with random choices of opponents from the population. Case (d) shows coexistence in almost all the simulations for the entire parameter space. Therefore, we can conclude that locally limited interactions between individuals strongly promote the coexistence of all phenotypes.
Figure 3.
Phase diagram for coexistence and non-coexistence. Each parameter α or β is set for every 0.05 increment. Initial values are given as (pO,pB,pY)=(0.3,0.3,0.4). Simulation runs are repeated for 100 times for each parameter set and their fractions are shown by continuous gradation between green and yellow. Green indicates coexistence until the end of simulations. Yellow corresponds to non-coexistence in which one phenotype goes extinct, and then an inferior phenotype disappears and ultimately only one phenotype survives, due to finite size of the system. (Upper left panel) global competition and global dispersion; (Upper right panel) global competition and local dispersion; (Lower left panel) local competition and global dispersion; (Lower right panel) local competition and local dispersion.
In case (d), individuals with the same phenotypes tend to cluster and adopt collective behavior, so changes of state occur only on the boundaries between these clusters, causing a slower change of total population and stabilization (See Figure 4). Indeed [13] already reached such a conclusion from a continuous-time cyclic competition model that also calculated the average domain size or boundary length at a steady state. This spatial structure in the population is gradually produced by both local competition and local dispersion, and, in turn, also gives different results in competition and dispersion, either globally or locally.
Figure 4.
Snapshot of spatial pattern by Monte Carlo simulation of phenotypic model on two-dimensional square lattice space after some time. Both competition and dispersion occur locally. We can observe that several dozens of same phenotypic individuals are clustering. (Right panel) The whole spatial pattern with 1000×1000 lattice sites. (Left panel) The upper left part of spatial pattern with 100×100 lattice sites. Colors indicate O,B,Y as orange, blue, yellow, respectively. α=2.0 and β=0.3.
Similar to [8], we show the difference between the phenotypic model and its corresponding genotypic model, but we can also give an explicit condition using a simplified system. In addition, we investigate other allele dominance rules to clarify their effects on the stability of internal equilibrium compared to the allele dominance rule observed in lizards. Unfortunately, however, we cannot specify the mechanism by which the genotypic model stabilizes the system more than the phenotypic model. To discover it, we need to find models other than cyclic competition in which the genotypic models give different dynamic behaviors than the corresponding phenotypic models.
A recent proposal by [14] may have important implications for future work in this area. As they point out, the present three-strategy payoff matrix can be built up as the sum of nine independent Fourier components, g(1),…,g(9), with orthogonality and normalization:
where we have g(1),g(8), and g(9) as irrelevant constant terms, a coordination (Potts) component that equally favors the formation of one of the homogeneous states, and a cyclic (rock-paper-scissors) component, respectively. This formulation may offer more detailed insights into dynamical behaviors if we examine cases with various combinations of coefficients corresponding to the strengths of these components.
The intuitive reason local competition and local dispersion both stabilize an internal equilibrium is that several dozens of identical phenotypic individuals gather and adopt collective behavior, restricting phenotypic changes on the boundary. To investigate their stabilization mechanisms in detail, we should further rely on other kinds of analysis, especially spatial pattern formation, which may play an important role in stabilizing the dynamics. So far, the concept of "vortex" has been proposed to characterize the spatial pattern [15,16,17], and it has also been shown that clockwise or anti-clockwise rotating spiral patterns with characteristic sizes emerge that yield finite size effects by cyclic competition models or rock-paper-scissors games in physics [18,19,20,21] and evolutionary games [22,23]. More precisely, the coexistence of three strategies transforms into one of the homogeneous states after a suitable relaxation time if the characteristic length of patterns exceeds a threshold value comparable to the system size. Here we use a small lattice space size (100×100) for Figure 3, but we should further investigate these finite size effects using a larger lattice space, such as 1000×1000, as in Figure 4.
In this paper, we only show whether three phenotypes can coexist or not in the long run using a Monte Carlo simulation. However, we can expect an internal equilibrium to be asymptotically stable for the case of coexistence in larger Monte Carlo systems than in smaller ones (Figure 5).
Figure 5.
Time series of frequencies by Monte Carlo simulation of phenotypic model on two-dimensional square lattice space. Both competition and dispersion occur locally. We can confirm that fluctuations are due to the effect of finite size of lattice sites. The numbers of lattice sites are (a) 1000×1000, (b) 100×100, (c) 10×10. All phenotypes survived after 2000 Monte Carlo steps in (a) and (b), but in (c) B went extinct around 70 generations by chance, and then O died out almost inevitably (but not definitely because of finite system size) because Y is stronger than O. Colors indicate O,B,Y as orange, blue, yellow, respectively. Initial frequencies are (pO,pB,pY)=(0.3,0.3,0.4). α=2.0 and β=0.3.
Here we can only show the condition of the locally asymptotic stability of a genotypic model. We expect that condition to be replaced by global stability, but we leave it as a future problem.
In addition, we would like to examine a genotypic model in a lattice space and clarify whether it becomes more stable than a phenotypic model and to what degree its stability can be evaluated by, for example, the return time of perturbation to an internal equilibrium.
Throughout this paper, we use only symmetric conditions of parameters to obtain global insights into the dynamics, then we should study more complicated models with symmetry-breaking interactions, including the parameter setting of [8], in future research.
Acknowledgements
I sincerely appreciate Prof. Akira Sasaki for giving me useful comments and encouraging me. I would also like to thank three anonymous reviewers whose comments were helpful in revising the manuscript.
Conflict of interest
The author declares no conflict of interest.
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Table 1.
Payoff matrix of rock-paper-scissors game. MIJ is a payoff of focal individual I∈{O,B,Y} against an opponent J∈{O,B,Y}. The following magnitude relations hold: MOY<MOO<MOB,MBO<MBB<MBY,MYB<MYY<MYO.
Table 2.
Allele dominance rule (Ⅰ). An allele o is dominant to other alleles y and b, then three genotypes oo, oy, and ob correspond to a phenotype O. An allele y is dominant to an allele b, then two genotypes yy and yb correspond to a phenotype Y. An allele b is recessive to other alleles, then only one genotype bb corresponds to a phenotype B.
Table 3.
Payoff matrix with only two parameters. We obtain the same equilibrium fractions of 1/3 for all three phenotypes. Parameter ranges are given by 0<β<1<α.
Table 4.
Allele dominance rule (Ⅱ). An allele o is dominant to an allele y, then two genotypes oo and oy correspond to a phenotype O. An allele y is dominant to an allele b, then two genotypes yy and yb correspond to a phenotype Y. An allele b is dominant to an allele o, then two genotypes bb and ob correspond to a phenotype B.
Figure 1. Sensitivity analysis of void ratio estimates based on typical values of vs and vp for soils relative to typical ranges in: (a) Poisson’s ratio of the soil skeleton, (b) pore-water temperature, and (c) mass density of the solid soil particles. Each line and shaded area indicate the median value and bound limits, respectively, of the parameter varied in the sensitivity analysis. The void ratio is evaluated for six constant values of vp, as indicated by line type. A theoretical void ratio path for a soil with increasing vs and vp is indicated by the dashed arrow
Figure 2. Comparison of site investigation data at the Kilmore Street site: (a) CPT cone tip resistance, (b) normalized soil behavior type index, and (c) void ratio measurements from gel-push samples of varying quality (poor, average, and high) in comparison to in situ estimates obtained from three CPT-based Dr empirical relationships and representative ranges of emin and emax from laboratory testing. Each void ratio line and shaded area indicate the mean value and ±1 standard deviation bounds
Figure 3. Comparison of site investigation data at the Madras-Armagh site: (a) CPT cone tip resistance, (b) normalized soil behavior type index, and (c) void ratio measurements from gel-push samples of varying quality (poor and average) in comparison to in situ estimates obtained from three CPT-based Dr empirical relationships and representative ranges of emin and emax from laboratory testing. Each void ratio line and shaded area indicate the mean value and ±1 standard deviation bounds
Figure 4. Comparison of site investigation data at the Rawhiti Domain (NZGD VSVP 57188) site: (a) soil classification from continuous sonic borehole samples, (b) CPT cone tip resistance, (c) vs, (d) vp, and (e) in-situ estimates of void ratio. Three CPT-based Dr empirical relationships and representative ranges of emin and emax from laboratory testing were used to estimate in-situ void ratio. Each void ratio line and shaded area indicate the mean value and ±1 standard deviation bounds. Seismic-based estimates of in-situ void ratio are indicated by circular markers at two assumed values for Poisson’s ratio of the soil skeleton, with νSK = 0.15 always yielding lower void ratio estimates than νSK = 0.35
Figure 5. Comparison of site investigation data at the Charles Street (NZGD VSVP 57196) site: (a) soil classification from continuous sonic borehole samples, (b) CPT cone tip resistance, (c) vs, (d) vp, and (e) in-situ estimates of void ratio. Three CPT-based Dr empirical relationships and representative ranges of emin and emax from laboratory testing were used to estimate in-situ void ratio. Each void ratio line and shaded area indicate the mean value and ±1 standard deviation bounds. Seismic-based estimates of in situ void ratio are indicated by circular markers at two assumed values for Poisson’s ratio of the soil skeleton, with νSK = 0.15 always yielding lower void ratio estimates than νSK = 0.35
Figure 6. Comparison of site investigation data at the Palinurus Road (NZGD VSVP 57185) site: (a) soil classification from continuous sonic borehole samples, (b) CPT cone tip resistance, (c) vs, (d) vp, and (e) in-situ estimates of void ratio. Three CPT-based Dr empirical relationships and representative ranges of emin and emax from laboratory testing were used to estimate in-situ void ratio Each void ratio line and shaded area indicate the mean value and ±1 standard deviation bounds. Seismic-based estimates of in-situ void ratio are indicated by circular markers at two assumed values for Poisson’s ratio of the soil skeleton, with νSK = 0.15 always yielding lower void ratio estimates than νSK = 0.35
Figure 7. Comparison of site investigation data at the Carisbrooke Playground (NZGD VSVP 57193) site: (a) soil classification from continuous sonic borehole samples, (b) CPT cone tip resistance, (c) vs, (d) vp, and (e) in-situ estimates of void ratio. Three CPT-based Dr empirical and representative ranges of emin and emax from laboratory testing were used to estimate in-situ void ratio Each void ratio line and shaded area indicate the mean value and ±1 standard deviation bounds. Seismic-based estimates of in-situ void ratio are indicated by circular markers at two assumed values for Poisson’s ratio of the soil skeleton, with νSK = 0.15 always yielding lower void ratio estimates than νSK = 0.35. As indicated by small square markers, individual vp measurements were modified such that the corresponding νSK = 0.35 void ratio estimate (small circular markers) agrees with the mean Baldi et al.
[5] estimate at the same testing depth
Figure 8. Histograms of the percent change in vp required to adjust seismic-based in-situ void ratio estimates to match the corresponding mean estimate from each CPT-based empirical relationship: (a) Baldi et al. [5], (b) Kulhawy and Mayne [3], and (c) Jamiolkowski et al. [7]. The histograms are based on 253 void ratio estimates in clean sands across nine sites in Christchurch, New Zealand
Figure 9. Comparison of empirical cumulative distribution functions showing the percent difference between DPCH seismic-based in-situ void ratio estimates and those obtained from each of the three CPT-based estimates [3,5,7], and the percent difference between the Baldi et al. [5] and the Kulhawy and Mayne [3] CPT-based void ratio estimates