Jump to content

Seismic hazard

From Wikipedia, the free encyclopedia

This is an old revision of this page, as edited by CasualObserver'48 (talk | contribs) at 07:15, 6 October 2011 (Attempt to make differences less 'confusing', and indicate example uses for the topic). The present address (URL) is a permanent link to this revision, which may differ significantly from the current revision.

Seismic hazard refers to the study of expected earthquake ground motions at the earth's surface, and its likely effects on existing natural conditions and man-made structures for public safety considerations; the results of such studies are published as seismic hazard maps, which identify the relative motion of different areas on a local, regional or national basis.[1] With hazards thus determined, their risks are assessed and included in such areas as building codes for standard buildings, designing larger buildings and infrastructure projects, land use planning and determining insurance rates.

Surface motion map for a hypothetical earthquake on the northern portion of the Hayward Fault Zone and its presumed northern extension, the Rodgers Creek Fault Zone

The calculations for seismic hazard, first formulated by C. Allin Cornell in 1968,[2] can be quite complex.[3] First, the regional geology and seismology is examined for patterns (using seismometers and earthquake location). Zones of similar potential for seismicity are drawn. For example, the famous San Andreas Fault might be drawn as a long narrow zone. Zones in the continental interior (the site for intraplate earthquakes) would be drawn as broad areas, since causative faults are generally not identified.

Each zone is given properties associated with source potential: how many earthquakes per year, the maximum size of earthquakes (maximum magnitude), etc. Finally, the calculations require formulae that give the required hazard indicators for a given earthquake size and distance. For example, some districts prefer to use peak acceleration, others use peak velocity, and more sophisticated uses require response spectral ordinates.

The computer program then integrates over all the zones and produces probability curves for the key ground motion parameter. The final result gives you a 'chance' of exceeding a given value over a specified amount of time. Standard building codes for homeowners might be concerned with a 1 in 500 years chance, while nuclear plants look at the 10,000 year time frame. A longer-term seismic history can be obtained through paleoseismology. The results may be in the form of a ground response spectrum for use in seismic analysis.

More elaborate variations on the theme also look at the soil conditions.[4] If you build on a soft swamp, you are likely to experience many times the ground motions than your neighbour on solid rock. The standard seismic hazard calculations become adjusted upwards if you are postulating characteristic earthquakes.

Areas with high ground motion due to soil conditions are also often subject to soil failure due to liquefaction. Soil failure can also occur due to earthquake-induced landslides in steep terrain. Large area landsliding can also occur on rather gentle slopes as was seen in the "Good Friday Earthquake" in Anchorage, Alaska, March 28, 1964.

Maximum considered earthquake

In most seismic hazard analyses, the "maximum considered earthquake", or "maximum considered event" (MCE) for an area is an earthquake that is expected to occur once in approximately 2,500 years; that is, has a 2-percent probability of exceedance in 50 years. Many building codes will require non-essential buildings to be designed for "collapse prevention" in an MCE, so that the building remains standing - allowing for safety and escape of occupants - rather than full structural survival of the building.

US seismic hazard maps

Some maps released by the USGS are shown with peak ground acceleration with a 10% probability of exceedance in 50 years, measured in Metre per second squared. For parts of the US, the National Seismic Hazard Mapping Project in 2008 resulted in seismic hazard maps showing peak acceleration (as a percentage of gravity) with a 2% probability of exceedance in 50 years.

See also

References

  1. ^ Natural Resources Canada page on Seismic Hazard Calculations
  2. ^ Cornell, C.A. 1968, Engineering seismic risk analysis, Bulletin of the Seismological Society of America, 58, 1583-1606
  3. ^ McGuire, R. 2008, Probabilistic seismic hazard analysis: Early history, Earthquake Engng Struct. Dyn., 37, 329–338
  4. ^ Wang, Z. 2008. A technical note on seismic microzonation in the central United States, J. Earth Syst. Sci. 117, S2, pp. 749–756

U.S. Geological Survey National Seismic Hazard Maps: http://earthquake.usgs.gov/research/hazmaps/

The Global Seismic Hazard map: http://www.seismo.ethz.ch/GSHAP/

Retrieved from "https://en.wikipedia.org/enwiki/w/index.php?title=Seismic_hazard&oldid=454196547"