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Deterministic Response for a Case Study Bridge

4.2. ADINA FSI Finite Element Model

4.2.5. Deterministic Response for a Case Study Bridge

This section illustrates the deterministic response of a case study bridge from

Houston/Galveston Bay area. Figure 4-9 depicts the case study bridge geometry.

The deck width is 11m and consists of a 0.2m thick slab with six AASHTO type

III girders. The bent beam is supported by three square columns of 0.8m dimension

and 5m height. The columns are reinforced with twelve 28mm diameter rebars in

the longitudinal direction and a spiral with a pitch of 0.25m in the transverse

direction. The columns are supported by a pile foundation consisting of a 2.6m

square pile cap and eight 0.4m diameter piles of 14m length. The bridge is assumed

to be located at a soft clay site which is the typical soil type in the

Houston/Galveston region. This means a cohesive soil condition with undrained

Figure 4-9. Case study bridge geometry.

The deterministic response of the developed FSI model is provided here in

order to increase insight on the response of simply supported span bridges under

extreme wave and surge condition. Key quantities monitored include the

hydrodynamic forces on superstructure and substructure, and horizontal and

vertical displacement of the superstructure. Since there is no connection between

the super- and substructure, the bridge is susceptible to deck movement and

unseating under extreme wave and surge loads. The hazard input parameters for

the considered scenarios are presented in Table 4-1. The second and third

combinations of wave and surge values are selected to produce vertical forces that

are larger than the uplift capacity (i.e., weight of the deck for the case study

bridge) according to AASHTO (2008). The fourth row, hazard scenario 3-L,

2.6m

AASHTO Type III Girder 0.2m

0.4m 5m

0.8m

contains the same hazard parameters as the third one; however, the turbulence is

neglected in this scenario (i.e., the fluid flow is considered to be laminar).

Table 4-1. Hazard parameters for the deterministic study.

No. Hmax (m) Tp (s) ds (m) Zc (m)

1 1.8 5.0 6.0 0

2 3.2 6.0 6.0 0

3 4.2 6.0 7.5 -1.5

3-L 4.2 6.0 7.5 -1.5 (laminar flow)

Figure 4-10 depicts the vertical and horizontal displacement time history of

the top waveward node of the deck for each scenario. The deck displacements for

scenario 1 are small and are in the order of magnitude of 10-4m. However, hazard

scenarios 2 and 3 (and 3-L) lead to deck shifting and unseating. Scenarios 3 and 3-

L lead to similar responses, as expected. Nevertheless, the vertical deck

displacement for the laminar flow (case 3-L) is slightly less than the turbulent flow

model (case 3). Therefore, it is recommended to use the turbulent flow model for

higher accuracy since it is believed to provide a better representation of the

problem than laminar flow model. More discussion on the flow assumption is

provided in the sensitivity study in Section 5.2.2. The results indicate that the

deck displacement is different for scenarios 2 and 3, underscoring the impact of

consequently vertical displacements are larger for the submerged deck (scenario 3).

On the other hand, lateral forces and displacements are larger for the deck located

at the waterline since the wave crest can directly impact the deck (scenario 2).

Additionally, the submerged bridge deck undergoes larger moments as well as

larger rotation. Due to these differences in responses, greater distortion occurs in

fluid elements for scenario 3, and the simulation stops before a full wave passage.

Figure 4-11 shows the displacement of the deck during wave and surge load for

hazard scenarios 2 and 3 at time 1.7s. Differences in the displacement response and

the rotation of the leeward part of the submerged deck are evident. After the

bridge deck is shifted, the contact area between super- and substructure decreases.

Thus the bridge deck has less resistance against the next wave cycle, as can be

seen in Figure 4-10 (b) for scenario 2.

Figure 4-10. (a) Vertical and (b) horizontal deck displacements under different wave and surge load scenarios.

Figure 4-11. Deck displacement under wave and surge action at time 1.7s: (a) scenario 2; and (b) scenario 3.

Figure 4-12. (a) Vertical and (b) horizontal forces per unit length on the superstructure. The bold line in (a) represents the weight of the bridge deck per unit

length.

In addition to displacements, the total forces per unit length imposed on the

bridge deck are plotted in Figure 4-12. The deck weight is shown in a bold line.

Vertical forces on the bridge deck for scenario 1 follow a sinusoid pattern, similar

to the trend observed in the experiment (Sheppard and Marin 2009). Nonetheless,

the force pattern is not sinusoidal for scenarios that lead to the rigid body

deck movement; therefore, this phenomenon has not been observed (A preliminary

experimental result of the unrestrained deck is presented by Cox et al. (2012) in

the ATC-SEI Advances in Hurricane Engineering Conference, which supports the

results of FSI the model). The vertical forces do not increase significantly after the

deck uplift. The initial vertical forces for scenarios 3 and 3-L are greater than zero

due to the buoyancy. By comparing Figure 4-10 and Figure 4-12, it can be

concluded that the waveward face of the deck can be uplifted before vertical forces

fully overcome the deck weight. However, significant transverse displacement

occurs after the full deck uplift. Also, Figure 4-12 (b) reveals an alteration in the

direction of horizontal forces on the submerged bridge deck (3 and 3-L) after deck

uplift. The vertical forces are almost identical for turbulent and laminar flow.

However, there is a slight difference in the horizontal forces. The maximum

difference in terms of horizontal forces between turbulent and laminar flow models

is 2.1%.

As mentioned in Chapter 3, wave and surge loads on the bridge

substructure can be approximated based on the Morison equation (1950). The fluid

domain should be solved to find the acceleration and velocity of water particles

spatially varying; i.e., they are not constant along the column height. Since the

water is relatively shallow, and large wave heights are expected during coastal

storms, linear wave theory is not applicable to solve the fluid domain. Therefore,

the stream function (Dean 1965) is employed to solve the fluid domain for the

velocity and acceleration. The stream function solves the Laplace equation with a

nonlinear free surface boundary condition by computing a series solution. A

computer code, originally developed by Chaplin (2012) is modified to calculate the

stream function and the velocity and acceleration of water particles at any given

point of time and space for the given wave profile. This computer code

automatically increases the stream function order to reach an accurate water

surface that matches the input profile. After solving the fluid domain, forces are

calculated by integrating Equation (3-5) over 50 points along the column height.

Figure 4-13 (a) compares the horizontal velocity of water particles at

elevation 1.2m from the channel bottom line obtained from the stream function

and the FSI model for the first hazard scenario. Also, Figure 4-13 (b) depicts the

water velocity profile for hazard scenario 1 under the wave crest. This figure shows

a good agreement between the theoretical (stream function) and numerical model.

Figure 4-13. Horizontal water velocity at 1.2m elevation; and (b) horizontal water velocity profile at wave crest for scenario 1. Theoretical values are calculated from the

stream function, where numerical values are the results from FSI model.

Horizontal forces on the waveward column for the first hazard scenario

resulting from the numerical model and the Morison equation are shown in Figure

4-14. The Cd and Cm coefficients in the Morison equation are taken equal to 1 and

2, respectively. Although the fluid domain is in good agreement, the forces from

the Morison equation are smaller than the numerical model. This is because the

Morison equation does not consider wave diffraction, which is not an accurate

assumption for the column width in the case study bridge. Therefore, the Morison

equation does not lead to conservative results for estimation of forces on

substructure. Nevertheless, the forces on the substructure are significantly smaller

than the forces on superstructure, and they do not govern the behavior of the

5.2.2. Therefore, no modification is proposed for the substructure forces that are

calculated from the Morison equation.

Figure 4-14. Horizontal forces on waveward column for scenario 1. Theoretical values are calculated from the Morison equation (1950), where numerical values are the

results from FSI model.

4.3. Summary

This chapter introduced two different numerical models that are developed to

assess the vulnerability of coastal bridges under storm wave and surge loads. The

first model only includes the structural domain, and thus, is more computationally

efficient. The second model includes a full fluid-structure interaction model which

is verified by comparison with experimental test data from the literature. This

model is computationally intense; however, it can be used for validation of the

and surge load models applied to the structure only simulations. The two

developed numerical models are used in the following chapters for probabilistic

76

Chapter 5

Hurricane Hazard Parameters and

Uncertainty Treatment

This chapter explores the hazard intensity measures that should be adopted to

condition the fragility models for coastal bridges. Also, this chapter defines the

random variables that should be considered in the probabilistic analysis.

Appropriate probability density functions are introduced for hazard and structural

random variables. The significance of different modeling parameters are identified

5.1. Determination of the Most Influential Parameters for