Engineering and Construction

INTRODUCTION
As discussed previously, the actual rupture of the ground due to fault movement could damage a structure. Secondary effects, such as the liquefaction of loose granular soil and slope movement or failure could also cause structural damage. This chapter will discuss some of the other earthquake-induced effects or structural conditions that can result in damage to foundations and retaining walls.

Topics will include earthquake-induced settlement and foundation alternatives to mitigate earth-quake effects.

Earthquakes throughout the world cause a considerable amount of death and destruction.

Earthquake damage can be classified as being either structural or nonstructural. For example, the Federal Emergency Management Agency (1994) states:

Damage to buildings is commonly classified as either structural or non-structural. Structural damage means the building’s structural support has been impaired. Structural support includes any vertical and lateral force resisting systems, such as the building frames, walls, and columns. Non-structural damage does not affect the integrity of the structural support system. Examples of non-structural damage include broken windows, collapsed or rotated chimneys, and fallen ceilings. During an earthquake, buildings get thrown from side to side, and up and down. Heavier buildings are subjected to higher forces than light-weight buildings, given the same acceleration. Damage occurs when structural members are overloaded, or differential movements between different parts of the structure strain the structural components. Larger earthquakes and longer shaking durations tend to damage structures more. The level of damage resulting from a major earthquake can be predicted only in general terms, since no two buildings undergo the exact same motions during a seismic event. Past earthquakes have shown us, however, that some buildings are likely to perform more poorly than others.

There are four main factors that cause structural damage during an earthquake, as follows:

1. Strength of shaking. For small earthquakes (magnitude less than 6), the strength of shaking decreases rapidly with distance from the epicenter of the earthquake. According to the United States Geological Survey (2000b), the strong shaking along the fault segment that slips during a earthquake becomes about half as strong at a distance of 8 mi, a quarter as strong at a distance of 17 mi, an eighth as strong at a distance of 30 mi, and a sixteenth as strong at a distance of 50 mi.

In the case of a small earthquake, the center of energy release and the point where slip begins is not far apart. But in the case of large earthquakes, which have a significant length of fault rup- ture, these two points may be hundreds of miles apart. Thus for big earthquakes, the strength of shaking decreases in a direction away from the fault rupture.

2. Length of shaking. The length of shaking depends on how the fault breaks during the earthquake. For example, the maximum shaking during the Loma Prieta earthquake lasted only 10 to 15 sec But during other magnitude earthquakes in the San Francisco bay area, the shaking may last 30 to 40 sec. The longer the ground shakes, the greater the potential for structural damage. In general, the higher the magnitude of an earthquake,  the longer the duration of the shaking ground (see Table 13.2).



3. Type of subsurface conditions. Ground shaking can be increased if the site has a thick deposit of soil that is soft and submerged. Many other subsurface conditions can cause or contribute to structural damage. For example, as discussed in Sec. 13.4, there could be structural damage due to liquefaction of loose submerged sands.

4. Type of building. Certain types of buildings and other structures are especially susceptible to the side-to-side shaking common during earthquakes. For example, sites located within approxi- mately 10 mi (16 km) of the epicenter or location of fault rupture are generally subjected to rough, jerky, and high frequency seismic waves that are often more capable of causing short buildings to vibrate vigorously. For sites located at greater distance, the seismic waves often develop into longer period waves that are more capable of causing high-rise buildings and buildings with large floor areas to vibrate vigorously (Federal Emergency Management Agency, 1994).

Much like diseases will attack the weak and infirm, earthquakes damage those structures that have inherent weaknesses or age-related deterioration. Those buildings that are nonreinforced, poorly constructed, weakened from age or rot, or underlain by soft or unstable soil are most susceptible to damage. The next section will discuss some of these susceptible structures.