reduces the added force associated with both ground motion components and the added mass to bounded values at
2.5.4 Implications of Ignoring Water Compressibility
Earthquake analysis of dams is greatly simplified if compressibility of water is ignored, because then hydrodynamic effects can be modeled by a frequency‐independent added mass (Section 2.3.4). Here, we answer the important question: can water compressibility be ignored in the earthquake analysis of concrete gravity dams?
Frequency response curves of the dam without water, when presented using normalized scales as in Figures 2.5.5 and 2.5.6, are independent of the modulus of elasticity, Es, of concrete. Similarly, the response curves including hydrodynamic effects do not vary with Es if water compressibility is ignored (Chopra 1968). However, the Ωr parameter, or correspondingly the Es value, affects the response functions when water compressibility is included.
The response of the dam is greatly influenced by the frequency ratio, Ωr. i.e. the relative frequencies of the two interacting systems, as demonstrated by Figures 2.5.1 and 2.5.3. The percentage decrease in the fundamental resonant frequency of the dam due to dam–water interaction is larger for the smaller values of Ωr, i.e. larger values of Es. The response value at resonance as well as the shape of the response curve in the neighborhood of the natural frequencies of the dam and of the impounded water also depend significantly on the frequency ratio Ωr.
With increasing Ωr, or decreasing Es, the effects of water compressibility on response become smaller and the response curve approaches the result for incompressible water. For systems with Ωr = 2.0, the effects of water compressibility are insignificant in the response to horizontal ground motion (Figures 2.5.5 and 2.5.7) but are still noticeable in the response to vertical ground motion (Figures 2.5.6 and 2.5.8). These results confirm the earlier conclusion that the effects of water compressibility become insignificant for systems with Ωr > 2 or
Figure 2.5.5 Influence of frequency ratio, Ωr, on dam response to harmonic horizontal ground motion. Results are presented (1) including water compressibility with α = 1 for Ωr = 0.67, 0.80, 1.0, and 2.0 (Es = 5.67, 3.94, 2.52, and 0.63 million psi); and (2) assuming water to be incompressible.
Figure 2.5.6 Influence of frequency ratio, Ωr, on dam response to harmonic vertical ground motion. Results are presented (1) including water compressibility with α = 1 for Ωr = 0.67, 0.80, 1.0, and 2.0 (Es = 5.67, 3.94, 2.52, and 0.63 million psi); and (2) assuming water to be incompressible.
Figure 2.5.7 Influence of frequency ratio, Ωr, on dam response to harmonic horizontal ground motion. Results are presented (1) including water compressibility with α = 0.75 for Ωr = 0.67, 0.80, 1.0, and 2.0 (Es = 5.67, 3.94, 2.52, and 0.63 million psi); and (2) assuming water to be incompressible.
Figure 2.5.8 Influence of frequency ratio, Ωr, on dam response to harmonic vertical ground motion. Results are presented (1) including water compressibility with α = 0.75 for Ωr = 0.67, 0.80, 1.0, and 2.0 (Es = 5.67, 3.94, 2.52, and 0.63 million psi); and (2) assuming water to be incompressible.
2.5.5 Comparison of Responses to Horizontal and Vertical Ground Motions
Comparing the response of the dam to horizontal and vertical ground motions (Figures 2.5.5 and 2.5.6) it is apparent – consistent with common view – that without impounded water the response to vertical ground motion is relatively small because the excitation term