There is no seismic rating for the nuclear waste thin storage canisters that may already be cracking at San Onofre and other nuclear plants, especially in the corrosive coastal environment. Each of the canisters contains more radiation (Cesium-137) than that released from Chernobyl.
Nelson Mar, PhD (former Senior Engineer for the original design of San Onofre Units 2 & 3), said San Onofre is not designed for current earthquake or tsunami risks. See 3/27/12 Irvine City Council meeting video.
They do not know how and they do not expect to know how any time in the foreseeable future. Major earthquakes can occur on what are predicted to be minor faults. Based on scientific data, only probabilities can be calculated for potential future earthquakes. U.S. Geological Survey (USGS)
- “Information about how big an earthquake’s going to be may not be in the earth’s crust BEFORE the earthquake begins” says USGS seismologist Dr. Lucy Jones.
- Although it is known that most global earthquakes will concentrate at the plate boundaries, there is no reliable method of accurately predicting the time, place and magnitude of an earthquake…
Many seismic countries, however, have research programs based on identifying possible precursors to major earthquakes. This includes the study of dilatancy, how rocks crack and expand under the increased stress associated with the earthquake. Some major earthquakes, but not all, are heralded by the occurrence of foreshocks. which can be detected by dense local monitoring networks. Other instruments can measure changes in the levels of radon gas, electrical and magnetic properties, velocity changes of seismic waves and changes in topography. Long term monitoring and examination by these sensors is required as some or all of these factors may change due to the opening of cracks PRIOR to the earthquake. All attempts to predict earthquakes have, however, been generally considered as failures and it is unlikely that accurate prediction will occur in the near future. Efforts will, instead, be channelled into hazard mitigation. Earthquakes are difficult or impossible to predict because of their inherent random element and their near-chaotic behaviour. British Geology Survey FAQS
- “The Earth’s natural systems are not static… This is why I personally feel we need to regularly update the scientific data we use to inform our regulatory approach so that our nuclear facilities are adequately protected against unanticipated events”, said NRC Chairman Macfarlane at the November 6, 2012 INPO CEO conference, in reference to the Fukushima nuclear disaster.
Building design limitations due to ground motion unpredictibility
Professor Thomas Heaton of Caltech’s Earthquake Engineering Research Lab, reveals limitations in designing structures to protect against large earthquakes. Every earthquake has different dynamics and affects different types of construction differently. “All tall buildings are designed to be flexible, but here’s the rub,” Heaton said. “People talk about a building designed for an 8 [magnitude], as if anybody has a good idea of what the actual ground motion would be in an 8. There’s tremendous variation from one place to another.” If you “put a really large quake under downtown L.A., 7-plus, it could be a true nightmare.” L.A. Times, Earthquakes on the brain, April 1, 2014.
Disconnected faults can jump nine feet, according to new 2015 USGS data
Southern California 8+ earthquake 30-year probability increased from 3% to 7% due to new understanding about how disconnected faults can jump up to nine feet.
Estimates of the chance of a magnitude 8.0 or greater earthquake hitting California in the next three decades have been raised from about 4.7% to 7%, the U.S. Geological Survey said Tuesday [March 9, 2015]. Scientists said the reason for the increased estimate was because of the growing understanding that earthquakes aren’t limited to separate faults, but can start on one fault and jump to others. The result could be multiple faults rupturing in a simultaneous mega-quake… LA Times, March 9, 2015
Fracking on the Newport-Inglewood Fault
- Fracking for oil is currently being done in Baldwin Hills by the Plains Exploration and Production Co (PXP), a Texas based company, on the Newport-Inglewood fault. Earthquakes have been triggered by fracking.
- The Newport-Inglewood fault runs by the San Onofre nuclear power plant. Even though San Onofre is shutdown, the over 1600 tons of highly radioactive waste could be damaged by an earthquake from this fault, resulting in a nuclear disaster greater than the one currently happening in Japan. See also SCEC Final Technical Report, Integration of Fault Information, November 2009, p. 15 & 22.
- The California Conservation Division of Oil, Gas and Geothermal Resources has authority to regulate fracking, but refuses to do so. The last Division Chief lost her job after supporting stronger regulations.
- See The ‘F’ Word: Unregulated Fracking at Oil Wells Raising Concerns – KCET SoCal Connected 3/23/2012.
- “Governor Jerry Brown…”fired two officials who had sharply slowed down the process for issuing new drilling permits. He followed that with the year-end appointment of Tim Kustic as the chief drilling regulator —“a geologist who knows the industry,” says Rock Zierman, head of the California Independent Petroleum Association. Occidental Petroleum CEO Steve Chazen gave Brown a nod at the company’s fourth-quarter conference call in January: “We are pretty encouraged by the way things are going now. . . . The governor is very pro-jobs.” City Journal Summer 2012.
- In the Los Angeles Basin (Figure 4.4-9), disposal wells are concentrated mainly in oilfields located along the Holocene Newport-Inglewood fault zone (slip rate 1.5 mm/yr), a segment of which was the source of the destructive 1933 Mw6.4 Long Beach earthquake, and in the Wilmington oilfield.
Several wells in the Wilmington field are located within 4 km (2.5 mi) of the Holocene Palos Verdes fault (slip rate 3 mm/yr). Only scattered seismicity has occurred near any these fields except Inglewood and Cheviot Hills at the northwestern end of the Newport-Inglewood trend. As in the Ventura Basin, clusters of seismicity are located close to some disposal wells but also elsewhere. The cluster at the top-center of the figure are aftershocks of the 2014 La Habra earthquake.
An Independent Scientific Assessment of Well Stimulation in California, An Examination of Hydraulic Fracturing and Acid Stimulations in the Oil and Gas Industry, Jane C. S. Long, PhD, California Council on Science and Technology, Steering Committee Chairman; Science Lead Jens T. Birkholzer, PhD, Lawrence Berkeley National Laboratory Principal Investigator; Laura C. Feinstein, PhD, California Council on Science and Technology, Project Manager
Fracking can trigger earthquakes
Earthquakes can be triggered by any significant perturbation of the hydrologic regime. In areas where potentially active faults are already close to failure, the increased pore pressure resulting from fluid injection, or, alternatively, the massive extraction of fluid or gas, can induce sufficient stress and/or strain changes that, with time, can lead to sudden catastrophic failure in a major earthquake.
- Seismologists across the globe were surprised by the magnitude of shaking that occurred in the segment of fault responsible for the Tohoku quake. Japanese scientists had not believed a quake of such intensity could occur in that area, which in turn impacted tsunami strength estimates.
- Insights gained from the Tohoku earthquake are leading scientists to re-evaluate the way they’ve assumed many other major faults are segmented. This may end up altering some hazard analyses for the West Coast, and will contribute to improved scenario modeling, building code development, and public warnings about tsunami threats.
- An unparalleled amount of strong ground motion data were recorded.
- Many cases of liquefaction were witnessed and filmed for the first time. Liquefaction occurs when soil loses strength and stiffness due to an applied stress like an earthquake and behaves like a liquid, often causing damage to structures and infrastructure.
- Even though the Japanese had planned and were well-prepared for a 200- or 300-year tsunami, they were not prepared for the 1000-year tsunami (an event that’s likely to occur just once every 1,000 years) that came instead. Consequently, Japan is currently updating its tsunami disaster plans for all of its coastal areas and requiring that all plans take evidence from paleo-tsunami deposits into consideration.
- Paleo-tsunami deposits are the sand and mud that tsunamis leave behind. By studying deposits from recent events like the March 11 tsunamis, scientists are able to develop criteria for what those deposits look like and use them to examine coastal areas for records of tsunamis that struck centuries back. They can tell when tsunamis occurred and how far inland they reached by looking at the evidence left behind. USGS coastal and marine geologists Bruce Jaffe, Bruce Richmond, and Rick Wilson have worked with Japanese scientists over the past year to study these deposits in Japan. Said Jaffe, “Japan has learned from this tsunami that it’s necessary to look at the geologic evidence for tsunamis in conjunction with the current understanding of earthquake potential to accurately assess the future tsunami hazard.” He explained that “Each tsunami brings its own sand and mud. Japan recognizes the value of using the very rich record of past tsunamis to help us understand the hazard for future tsunamis.”
- The United States is also conducting its own paleo-tsunami deposit studies in California, Alaska, the Caribbean, Puerto Rico, and the Virgin Islands to better understand the tsunami risk in those areas.
Ratepayers must pay $64 million in new seismic studies.
- The California Public Utilities Commission is forcing ratepayers to pay $64 million in new seismic studies, even though existing data proves San Onofre cannot handle the current known risks and USGS says size of earthquakes is not predictable (e.g. size may change after earthquake begins). Similar $64 million dollar studies were also approved for the Diablo Canyon nuclear power plant.
- Part of the seismic studies include sonic blasts that will maim and kill large numbers of whales, dolphins, seals, sea lions, otters, and other marine life. See Coastal Commission staff recommendations approved by the Commission.
Lessons learned about strike-slip faults from 8.6 East Indian Ocean earthquake.
- On April 11, 2012, an 8.6 earthquake struck the East Indian Ocean along a strike-slip fault – the largest earthquake ever recorded on a strike slip and 10 times larger than any previously recorded strike-slip quake.
- A large earthquake in one part of the globe can trigger earthquakes elsewhere. In the 6 days after the quake, the number of earthquakes across the globe that were 5.5 or larger increased nearly five fold. “if you asked any of us if this event is possible a year ago, we would have laughed at you”, said Thomas Heaton, seismologist at California Institute of Technology. BayCitizen.org 9/28/2012, USGS 9/26/2012, Nature 2012
San Onofre and Diablo Canyon nuclear plants are located within the “Ring of Fire”.
The “Ring of Fire“, also called the Circum-Pacific belt, is the zone of earthquakes surrounding the Pacific Ocean. About 90% of the world’s earthquakes occur there.
See animation of 2011 global 6.0+ earthquakes (using USGS data) and more maps below.
Lessons learned about length of a fault.
Known length of a fault is not always a predictor of magnitude as in the 1952 Kern County 7.5 earthquake.
Seismic evaluations are not required before license renewal.
San Onofre was originally licensed to shut down in 2013, but was extended to 2022. The plant was designed in 1973 for a 40 year lifespan. In 2013 Southern California Edison plans to ask for an extension to 2042. A comprehensive seismic analysis has not been conducted on San Onofre since 1995, according to an April 2012 Government Accountability Office report.