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Showing posts with label earthquake. Show all posts
Showing posts with label earthquake. Show all posts

Friday, July 12, 2013

Examples in Leadership: Masao Yoshida


山は動かない [武田 信玄]。
Last Tuesday, Jul. 9, 2013, Masao Yoshida passed away. He was 58. He had esophageal cancer.

Until his illness forced him to relinquish his post late in 2011, Masao Yoshida was superintendent of Tokyo Electric Power Company's (TEPCO) Fukushima Dai-ichi Nuclear Power Station on Japan's northeast coast less than 100 miles north of Tokyo. Yoshida led the power station through the most severe nuclear reactor crisis since the Chernobyl disaster of 1986. Four of six reactors lost all power as a result of the Great Tōhoku Earthquake and Tsunami on Mar. 11, 2011; three were operating. The other was shutdown for inspection, and the fuel had been moved to an adjacent storage pool.

Despite heroic efforts of Yoshida and his crew, the three operating reactors lost cooling, and their fuel melted down. Vast quantities of hydrogen were released into the reactor buildings. Three were devastated by violent explosions. The fourth was spared, because Yoshida's men managed to open a blow out panel. Large quantities of radioactivity spewed into the air for days, contaminating a wide swath of Fukushima Prefecture and adjoining areas. The Government of Japan declared an exclusion zone around the power station. Roughly 160,000 residents had to be evacuated. At present, about half are still not permitted to return home permanently.

Confronted with the earthquake, flooding, aftershocks and the reactors spinning out of control, Yoshida sent most workers home, but convinced a crew of 50 essential operators to stay with him behind in a quake-resistent command center. The men attempted desperately to keep the nuclear fuel in the reactors and in adjacent storage pools cool and covered with water. After fresh water was exhausted, he ordered to use salt water for cooling against the wishes of TEPCO headquarters. The salt would render the reactors irreparable. TEPCO management had clung to the vain hope of being able to operate them again one day.

In a rare interview months later published online Nov. 13, 2011, by The Asahi Shimbun under the headline "Nuke plant director: 'I thought several times that I would die'", Yoshida admitted that he at times believed during the first days of the crisis that he and his men were about to die. He added that he felt that the worst was over only after three months. Despite, Yoshida ascertained that abandoning his post never crossed his mind. The fuel in the two remaining reactors could be cooled with jury-rigged electric pumps, because one emergency diesel generator had survived. Yoshida pointed out that the fuel in these reactors would have inevitably melted as well had the crew retreated from the site.

A power company is no military organization. Operators cannot be ordered to stay on their posts in the face of adversity. They could have walked away anytime. Without doubt, Masao Yoshida's exemplary leadership during the crisis and his sense of duty encouraged the crew to stay with him and fight a dangerously deteriorating situation, risking life and limb, if not cancer years down the road. Their motives were pure. They wanted to prevent the worst. Yoshida mentioned to a reporter that the families of most operators who stayed with him lived in the area.

At the time he had to take sick leave, Yoshida remarked that cleaning up and decommissioning the stricken power station was only at the beginning. The path ahead would lead through uncharted territory strewn with unprecedented challenges. He felt that the task before the operators would be colossal. One nation alone would not be able to cope with it. Rather, a concerted effort of the international community was needed to accomplish the job.

Against Yoshida's advice, little international collaboration has come forth to date. TEPCO, a company versed in selling electric power, has been struggling with containing radioactive effluent and removing radioactive debris. Sprawling tank farms have been erected to store the water contaminated by its use for keeping the reactors cool. Long rows of heavy-clad storage bins contain the collected debris. A decontamination facility has been set up for the stored water, but is not quite operational yet, while radioactivity is increasing in the groundwater near the reactors and is consistently detected in the ocean. Removal of the fuel elements from the storage pools has not even started. Nobody knows precisely where the melted fuel in the reactors resides and how to extract it.

In honor of Masao Yoshida and in memory of his advice, an international not-for-profit foundation should be created bearing his name. The foundation should provide expert advice facilitating the succinct and expeditious cleanup of Fukushima Dai-ichi Nuclear Power Station, using novel methods and best practices, with the aim that the residents of the villages and towns around the stricken power station can soon return home for good. The world owes this effort to Masao Yoshida and the Fukushima Fifty whose families used to live there.

Reference

Acknowledgement
I thank simplyinfo.org for keeping me up to date with recent developments at Fukushima Dai-ichi Nuclear Power Station.

Addenda

Friday, February 22, 2013

Fukushima Radiophobia & The Mind


The disastrous nuclear reactor accident at Fukushima Dai-ichi (number one) Nuclear Power Station on the Pacific coast 120 miles north of Tokyo is nearing its second anniversary. As a consequence of the loss of all electric power after the Tohoku-Chihou-Taiheiyou-Oki Earthquake and Tsunami on March 11, 2011, nuclear fuel melted down in three of the station's six reactors.

Aerial view of Fukushima Daiichi Nuclear Power Station on March 24, 2011, after hydrogen explosions devastated the upper floors of the reactor buildings of Units 1 (background), 3 and 4 (foreground) in the wake of the March 11 earthquake and tsunami. Unit 4 was offline for inspection. TEPCO believes that hydrogen seeped into its building from Unit 3 via standby gas treatment system piping. The building of Unit 2 lost a blowout panel on the eastern side and was spared (courtesy cryptome.org).

Destructive hydrogen explosions severely damaged the facilities. The amounts of radioactivity released into the environment has been surpassed only by the Chernobyl reactor accident of 1986. Residents near the plant were exposed to radioactive fallout while evacuating the area. The immediate surroundings of the power station and the region affected by the plume of airborne radioactivity remain highly contaminated today. Roughly 80,000 residents living in the government-declared exclusion zones are not permitted to return home permanently. Only daytime visits are allowed on occasion (see Chris Meyers' report with the title "A year on, only brief home visits for Japan nuclear evacuees" published online by Reuters Feb. 13, 2012). The International Medical Corps aptly summarizes the challenges the evacuees have faced on its Fukushima Prefecture Fact Sheet.

Gamma radiation-based contamination map (high: orange; low: blue; dose rates can be obtained from the IMC Fukushima Prefecture fact sheet) showing the plume area, radii of the 12- and 15-mile evacuation zones as well as of the 50-mile ingestion zone US citizens were advised to avoid (source: NNSA).
In the meantime, the devastated power station's operator Tokyo Electric Power Company (TEPCO) has been arduously cleaning up the ruins, while keeping the stricken reactors cooled. Progress has been pain-staking slow. The molten fuel in the reactors has remained inaccessible because of forbiddingly high levels of radiation. Thousands of tons of nuclear fuel stored in water pools in and around the reactor buildings remain yet to be removed. Tank farms with contaminated cooling water have grown to vast proportions. Hisashi Hattori reports in his article with the title "High radiation bars decommissioning of Fukushima plant" published online Feb. 21, 2013, by The Asahi Shimbun: “Currently, there are nearly 500 storage tanks on the plant premises, many as tall as three-story buildings. TEPCO plans to add more by 2015 when it expects to have to store 700,000 tons of radioactive water.”

Birdseye view of Fukushima Dai-ichi Nuclear Power Station in February, 2013. Unit 1 (top, left) has been enshrouded in a tent-like structure to control gassous radioactive effluents. The refueling floor of Unit 4 (top; right) has been cleared in preparation for a new roof structure. TEPCO is in the process of clearing debris off the refueling floor of Unit 3 (left of Unit 4). Note the sprawling tank farm for the storage of contaminated cooling water (source: House of Japan).
Despite TEPCO's strenuous efforts, significant amounts of radioactivity are still released into the environment every day (TEPCO press release with the title "Progress Status of the Long-and-mid Term Roadmap towards the Decommissioning of Units1-4 of TEPCO Fukushima Daiichi Nuclear Power Station" dated Oct. 22, 2012). Not a single nuclear fuel rod, spent or still in use at the time of the accident, has been removed from the damaged reactors, and the company has been unable to determine the precise location of the molten fuel in the ruined reactors.

Now, that we are nearing the two-year milestone, the international media have begun to gauge the current state of affairs in Fukushima. In her article with the title "Unexpected Post-Fukushima Health Woes: Depression, Obesity" posted on CommonHealth Reform and Reality Feb. 15, 2013, guest contributor Judy Foreman writes that no noticeable direct effects on public health could be attributed to the exposure to ionizing radiation. She tells us furthermore that an international panel of experts concluded that the estimated effective absorbed doses were too small to warrant any concerns for public health. Rather, the experts warned that radiophobia is deeply affecting people, developing into the preeminent medical condition threatening public health. Ms. Foreman notes depression and obesity are on the rise in Fukushima Prefecture, while Geoff Brumfiel reported in his news feature with the title "Fukushima: Fallout of fear" published online by the journal Nature Jan. 16, 2013, that depression, anger and anxieties were prevalent among the displaced.

Phobia is defined as irrational, disproportional fear. Radiophobia represents the irrational, disproportional fear of ionizing radiation. This diagnosis does not seem to pertain to the evacuees from Fukushima who must face fears of the actual consequences of the radiological catastrophe every day. Their fears seem neither irrational nor disproportional.

Absorbed radiation dose estimates available to date for the people of Fukushima must be met with caution. No resident around the Fukushima Dai-ichi Nuclear Power Station wore a dosimeter when the fallout rained down. In their preliminary Dose Assessment Report published last summer, radiation experts convened by the World Health Organization had to resort to computational models to estimate effective absorbed dose averages for the examined population. The averages were extrapolated from recordings of a handful of functional monitoring stations scattered across the prefecture. The recordings were incomplete. The available data did not cover the earliest hours of the accident (see The Mainichi article with the title "Fukushima radiation spread to residential areas hours before venting" published online Feb. 22, 2013). Moreover, it does not account for local variations and the contribution of human activity to individual effective absorbed doses.

Individual absorbed doses may depend profoundly on whether the person was indoors or outdoors at the time of the radioactive fallout, whether residents who stayed indoors were well insulated from the outside air, what produce a person consumed in the days and weeks after the releases, i.e. fresh home-grown groceries harvested in the garden and freshly-caught fish or prepackaged food bought in stores, as well as the source of water consumed. Moreover, medical predisposition, gender and age may have influenced how much radioactivity was incorporated and remains in the body.

Personal whole body counts were not performed early enough after the accident to directly capture the internal exposure to ionizing radiation emitted by incorporated short-lived radionuclides. By contrast, cesium-137 with a comparatively long half-life of 30 years is still concentrating in crops, vegetables, mushrooms and life stock and will persist to threaten the human food chain. A quarter century after the Chernobyl reactor accident, Bavarian wild boar stew must remain off the dinner table because the meat's radioactive cesium content is deemed unsafe for human consumption (see Charles Hawley's report with the title "A Quarter Century after Chernobyl: Radioactive Boar on the Rise in Germany" published by Spiegel International Online Jul. 30, 2010). In Japan, continuously emerging hot spots of cesium contamination may pose ever new local health risks for decades to come, requiring unrelenting, meticulous clean-up as well as persistent, diligent crop and life stock controls.

Thyroid cancer rates in Belarus after the Chernobyl reactor accident (source: S. Yamashita).
The health effects of the unleashed ionizing radiation may take more time to manifest themselves than two years. Demidchik and others (2007) showed that thyroid cancer rates in children began to increase noticeably three years after the Chernobyl reactor accident, though the cancers were attributable to iodine-131 from the accident with a half-life of only eight days.

Furthermore, yet unrecognized long-latency effects may progressively attain prevalence. Pets abandoned in the exclusion zone of Fukushima are frequently found ravaged by viral infections. Though the infections might have mainly been the result of the harsh living conditions in the zone (see Jenny Marder's post with the title "What's the Fallout for Dogs Near Fukushima?" published online by PBS Newshour's Rundown Nov. 10, 2011), high infection rates may suggest that immune responses have been compromised, possibly because of the protracted exposure to low-level ionizing radiation (Manda and others, 2012).

Cat rescued from the Fukushima exclusion zone showing symptoms of a severe viral infection around nose and eyes (source: Touhoku inunekokyuen).
In conclusion, it is too early to ascertain that the radioactive fallout from the stricken reactors will not directly affect public health. The anxieties the Fukushima evacuees harbor seem well grounded and will not be alleviated by official assertions, proclaiming the risk to health exists only in the mind. People's fears will dissipate only when government action effects palpable, lasting improvements.

References
Acknowledgment
I thank the contributors of SimplyInfo.org without whom I could not have written this post.

Monday, July 4, 2011

A Marker to Remember

Villagers in the Alps must not fear tsunamis like the inhabitants of the east coast of Japan. But they must confront snow avalanches which may be highly destructive to home and life as well.

Unlike tsunamis in Japan, avalanches in the Alps recur with great regularity every year. Indeed, some avalanches fall with seemingly clockwork-like precision. Hamlets huddled on the slopes of deep, narrow valleys between towering mountains are particularly at risk. Over the centuries, the villagers maintained logs in which they meticulously recorded the time and date a particular avalanche descended, the precise area affected, the depth of the snow and its composition.


Topographic map of the surroundings of the village of Obergoms, Vs, Switzerland, showing the extent of avalanches (hatched) recorded in February, 1951, plus the paths of avalanches (arrows) noted between 1700 and 1999 (courtesy http://www.obergommer.ch).  
With the help of this knowledge, the villagers grew protective forests on the slopes above and erected barriers to hold back the snow masses on summits and ridges. They were able to designate uninhabitable zones that were indefensible. This tradition of prudence rooted in generation-old experience represents a powerful example telling us that our survival depends in no small way on our awareness of history and our willingness to learn from it.

Report of Japanese Government to the IAEA Ministerial Conference on Nuclear Safety, Fig. III-1-17.
Similarly, based on age-old experience with tsunamis, villagers in the Aneyoshi neighborhood of the modern-day city and fishing port of Miyako, Iwate Prefecture, on the northeast coast of Japan aptly erected a roadside marker, warning future generations that if they built their homes downhills from this point, their lives would be in peril (for review see Hideo Takagi's remarkable opinion piece with the title "Preserving the Remains in Areas Struck by the Tsunami-Applying the Aftermath of the Tragedy to Disaster Education and Enlightenment" posted on the Daily Yomiuri online). The humble stone monument can be seen in the left photograph above. The debris besides the road visible in the right photograph documents that the Tohoku-Oki Earthquake and Tsunami on Mar. 11, 2011, starkly proved the stone's inscription true (photograph below).

The marker's warning (photo by Dr. Masayuki Oishi).
The catastrophe exacted the greatest loss of lives in Japan's post-war history. Moreover, quake and tsunami devastated the Fukushima Dai-ichi Nuclear Power Station on the shores of the Pacific Ocean outside Fukushima City, precipitating the third nuclear reactor accident with fuel melt-downs in the history of the commercial use of nuclear power only rivaled by Three Mile Island in 1979 and Chernobyl in 1986. Four reactors suffered destructive explosions, radioactively contaminating air, land, and sea with yet unfathomable consequences. Mitigation is ongoing. The health of hundreds of thousands of people is at stake.


Radiation dose meter at Fukushima Medical University 35 miles from the stricken nuclear power station. The readings are continuously updated. In the week after the quake, dosemeter readings in Fukushima City spiked above 20 μSv/h. At this dose, we are exposed to an effective absorbed dose of 0.175 Sv in a year which corresponds to 17.5 rem; a dose that nuclear industry professionals perhaps accumulate over their entire career.

Perhaps, one day monuments similar to that on the road near Miyako will be erected in Fukushima at a safe distance from the ruins of the Fukushima Dai-ichi Nuclear Power Station, reminding future generations on their quest for ever more energy not to proceed beyond this point, because the price exacted is too high.

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Saturday, May 21, 2011

The Enigma of 1 Fukushima 4 号機


Reactor № 4 of the Fukushima Daiichi Nuclear Power Station on the northeast coast of Japan roughly 150 miles north of Tokyo was shut down for service past November, and according to most sources, e.g. this Areva report with the title "The Fukushima Daiichi Incident"dated Mar. 27, 2011, the fuel was moved into the spent fuel pool (SPF) adjacent to the reactor vessel on the service floor of the reactor building.


The strong earthquake and more than 10-foot high tsunami on the afternoon of Mar. 11 disrupted water cooling to the SFP. In the aftermath, according to the first TEPCO press release on the issue with the title "Damage to the Unit 4 Nuclear Reactor Building at Fukushima Dai-ichi Nuclear Power Station" dated Mar. 15 a loud explosion destroyed the superstructure of the reactor building on that day. Hydrogen produced by radiolysis or the burn of fuel rod cladding were suspected causes. However, video footage taken with an underwater camera submersed in the SFP of reactor № 4 released by TEPCO on May 8, 2011, showed no major damage to the rod assemblies stored in the pool.

Fuel rod assemblies stored in spent fuel pool of reactor #4 (courtesy TEPCO).

Hypothetically, the hydrogen might have found its way from adjacent reactor № 3, which had exploded violently on Mar. 14 [TEPCO press release with the title "White smoke around the Fukushima Daiichi Nuclear Power Station Unit 3" dated Mar. 14, 2011]. However, the exact path the gas possibly could have taken has not been established yet. Radioactive fission products have been found at elevated concentrations in the pool water since the first sampling after the quake on Apr. 13 [TEPCO press release with the title "Results of analysis of spent fuel pool water of Fukushima Daiichi Nuclear Power Plant Unit 4 (2nd continued report)" dated May 9, 2011], and radiation dose levels at the inland side of the reactor building were measured at 100 milliSv/h (TEPCO press release with the title "Plant Status of Fukushima Daiichi Nuclear Power Station" as of 2:00 PM" dated Mar. 23). People spending 10 hours at that location would suffer from acute radiation syndrome.

Intriguingly, thermographs taken by Japanese Self-Defense Forces helicopter overflights consistently show a higher temperature over the reactor well than over the SFP. The example below was recorded on Mar. 24.

Thermograph of the surface of  the building of reactor № 4 taken from JSDF helicopter. The seaside is at the bottom. The reactor well co-localizes with the red spot, whereas the spent fuel pool is situated under the green area to the left (courtesy JSDF).
The degrees shown on the thermograph do not represent the actual temperatures in the pool accurately. According to this update with the title "Fukushima nuclear power plant update: get all the data" published online by The Guardian on May 20, the pool water temperature must have been roughly 70 °C at the time. Over time, SFP temperatures at reactor № 4 have been fluctuating excessively, while cooling water has been continuously added. Despite the constant replenishment, temperatures rose rapidly two weeks ago, reaching 80 °C on May 9, according to IAEA updates of 12 - 18 May entitled "Fukushima Nuclear Accident Update Log". Reactor water temperatures are not reported.

Taken together, the above observations suggest that nuclear fission has been proceeding at low levels in the building of reactor № 4. However, it is not yet established how and where precisely this fission occurs, and what constituted the source of the hydrogen accumulation leading to the March 15 explosion.

This TEPCO document with the title "Start of regular inspection Fukushima Daiichi Nuclear Power Station Unit 4" dated Nov. 30, 2010, details the work to be accomplished in reactor № 4 until Sep. 24, 2011. It mentions only fuel assembly replacement.

Addenda
  • Andrew Gilligan and Robert Mendick report an intriguing observation by a worker at the Fukushima I nuclear power station immediately after the earthquake. According to their post with the title "Japan tsunami: Fukushima Fifty, the first interview" published online by The Telegraph on Mar. 27, 2011, “(a) ghastly boom was heard in the suppression chamber of reactor 4” The suppression chamber is the torus under the reactor pressure vessel, constituting an instrumental part of the primary containment system. It remains difficult to understand why this boom occurred, since reactor № 4 was shutdown (06/05/11).
  • An instructive brief on the efforts of constructing a new closed-loop cooling water system and filtration for the spent fuel pool of reactor № 4 is shown in the video below (06/17/2011):

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Monday, January 18, 2010

Neuroanatomy of an Earthquake

Last Wednesday, Jan. 12, 2010, an earthquake of magnitude 7.0 shook the island nation of Haiti at 16:53 local time. The epicenter of the quake was located only about six miles from the nation's largest city and capital Port-au-Prince, where an estimated 2.5 million people live. The temblor collapsed buildings within seconds, burying hundreds of thousands under the rubble. The government was not able to mount any first response of note. No rescue teams showed up on the scene. No heavy equipment was rushed in to help free the trapped from under the rubble. People shoveled with bare hands. The police was not to be seen. A human catastrophe of apocalyptic proportions was going to unfold.

In spite of the ensuing international rescue effort and the medical assistance that has begun to reach the country, hundreds of thousands are believed to have died. Many more are feared to succumb to their injuries in coming days. Many destroyed dwellings seem flimsily erected with cinder blocks and mortar. Reinforced concrete structures with multiple floors were not quake-proof.

The tumbling of concrete walls and ceilings caused countless blunt-force traumas and open fractures among the survivors. People with such injuries need immediate medical attention, including surgery. Only few help organizations were prepared for such assistance in the immediate aftermath of the quake. International medical teams including surgeons from Médecins Sans Frontières and Cuba were on location and are to be commended for their decisive action in the first hours after the quake. Meanwhile, aid is pouring in. The relief effort has become more coordinated. Field hospitals are being set up. Food and water are distributed. Security forces can be seen in action.

Hopefully, the basic needs of the survivors will be met in the coming days. It is clear that the horrific consequences of this catastrophe are not entirely natural. Rather, they seem in good part man-made. That is, the Haitian government has failed colossally in its role as a protector of its citizens. Numerous recent accounts of international volunteers who have been looking after the most profound needs of the country's impoverished population bear witness to the enduring insufficiency of medical care and the endemic shortages of the most basic medicines like antibiotics (e.g. Joani in Haiti). Hospitals had been strained at best before the disaster and have now been rendered completely inadequate. The temblor has laid bare once more the societal ills of this aggrieved nation.

I am ill-prepared to discuss the economical, social, and political reasons for Haiti's failure. The Duvaliers and their somewhat more benign successors certainly did not contribute much to lead the country out of its misery. The international community and the independent organizations providing aid to Haiti may wish to re-assess the ways they can possibly help build a more efficient infrastructure and social services in this country in the future.

Watching the horror take its course, I kept wondering whether we cannot find low-cost indicators to predict an earthquake, if only immediately before the temblor strikes. Even if long-term predictions similar to those advising us of the strength and the path of a hurricane do not seem feasible for earthquakes to date, a few more seconds of warning may make a huge difference.

A day after the quake, CBS News posted a video covering a road lined with a row of condominiums on the far side at the time the event.


The 35-second long footage was captured by a rigidly-mounted camera overlooking an intersection. Twenty seconds into the footage, a series of very strong vertical displacements of the ground brings the first building down, raising a huge plume of dust. Could we have noticed early signs in the video warning us that a strong quake was about to happen?

Though the quality of the video is not high fidelity, examining the pictures closely provides a few insights. We need to focus on the roof line of the condos first and then on the utility pole standing on the near corner of the intersection.

A subtle distortion of the roof line announces the first vertical jolt 12 seconds into the footage. Subsequent, arrhythmic displacements gain strength within the next 3 seconds. At 16 seconds, we see a distinct solitary vertical jolt followed by a pause of a second. Then the ground begins to violently shake up and down at precise periodicity. Note that the utility pole sways in elliptical counter-clockwise rotation. At 20 seconds, after six strong vertical jolts in four seconds, the front condo pancakes. Nothing in the first 12 seconds of movie foretells the impending disaster.

I found information on earthquakes pertinent for the interpretation of our observations in the movie on L. Braile's web page at Purdue University's Earth & Atmospheric Sciences. Three types of seismic ground waves that propagate parallel to the earth's surface appear to come to bear in the movie.

Compressional P waves are known to travel fastest and arrive first. They are longitudinal waves, shaking the soil particles back and forth in the direction of propagation like lined-up billiard balls. P waves cause comparably small vertical ground displacement. The next to arrive are shear or S waves. This type of wave propagates transversely with soil particles jolted up and down at larger amplitude than P waves. At last, Rayleigh or R waves arrive. These waves move soil particles in the direction of and vertical to propagation, causing the ground to rotate elliptically as the utility pole in the movie convincingly demonstrates. R waves brought the condo in the movie down. In addition, a fourth type of wave, Love or L waves, has been recognized. I could not detect any manifestation of L waves in the movie.

Braile exemplifies the different wave types in figure 7 on his web page. The figure shows seismograms recorded in Peru during a magnitude-6.5 quake off the Pacific coast in 1998. The trace representing the displacement in the z-direction (vertical) at the bottom of the figure is most applicable to our observations in the movie. The difference in time between the onset of the P and the S waves multiplied by 8 provides a rough estimate of the distance between recording site and the epicenter of the quake in kilometers. In the Peruvian example the seismic recorder was more than 1000 kilometers removed from the quake's epicenter. The S waves lagged the P waves about 7 minutes. By contrast, according to the United Nations Office for the Coordination of Humanitarian Affairs the distance between the epicenter of the quake in Haiti and downtown Port-au-Prince was only 10 kilometers. This leaves just 2 seconds between the arrival of the P waves and the S waves in the movie. If the P waves were strong enough to cause the earliest vertical displacements we noted, the inhabitants had seven seconds to vacate the condo complex before it crumbled. If the P waves were too weak to cause any visible displacement and the first detectable jolts were caused by S waves, we may add another two seconds according to the rule of thumb explained above. We would have had nine seconds to leave the building, after we first felt the ground shake. This may sound short. However, let us not forget that the world's fastest runner, the Jamaican Usain Bolt, covers 109 yards in that time.  

Would we have recognized that the first mild vibrations were the harbingers of a temblor of catastrophic force arriving shortly? Animals may possess a better sense of such danger than humans. In another contribution, CBS News broadcast a segment interviewing geologists who foresaw a major quake near Haiti a couple of years ago. They just could not predict when disaster would strike. In that broadcast, a video from a different quake shows a dog in an office that unequivocally recognizes the imminent catastrophe before any human. The dog takes flight about 5 seconds before the room begins to shake violently.


Animals are known to behave conspicuously in advance of an earthquake, and researchers have tried to associate specific types of behavior with the event (Mott, 2003). To date, the findings of these studies have not yielded any consistent predictors. However, I would not be surprised, if burrowing animals, that are particularly attuned to the processing of low frequency vibrations, would sense earthquakes early, displaying distinct behaviors that could be useful as warning signs. I have written about such animals in my post entitled "The Quest for the Infrasound Fovea" dated Oct. 12, 2009. In fact, the mammal that survived in the pumice zone after the catastrophic eruption of Mt. St. Helens in 1980 was a tiny whiskered burrowing rodent (Force & Resilience).

Addenda
  • According to Madeline Brand's segment with the title "Technology Works to Provide Early Quake Warning" broadcast on National Public Radio's All Things Considered today, sophisticated technology exists that permits us to identify a dangerous earthquake early enough to provide minutes of advance warning. However, when we listen to the podcast, we must keep in mind that the warning time dwindles as we near the quake's center. Even if such equipment had been installed in Haiti, we still would have had only seconds to act in Port-au-Prince (01/29/10).
  • On Saturday, Feb. 27, 2010, 3:34 local time an earthquake of magnitude 8.8 on the Richter scale originated under the Pacific Ocean at a depth of 22 miles 60 miles offshore Chile near Maule. An account of the event is currently being developed on Wikipedia (2010 Chile earthquake).

    The temblor was measured fifth strongest on record, inflicting wide-spread, severe damage along the coast of Chile. Ensuing tsunami waves, which topped ten feet in some locations caused additional devastation. To date, the loss of life stands at about 800. Mostly old, historic structures suffered catastrophic failure. Earthquake-resistant construction methods in modern buildings saved many lives in metropolitan areas. By contrast, in Haiti such building practices constituted a rarity (03/03/10).
  • According to Terry Wade and Fabian Cambero's post entitled "Chile quake-area still shaking, death toll unclear" on Reuters today, the loss of life owing to last Saturday's earthquake off the Chilean coast and the ensuing tsunami is much smaller than believed earlier. The Chilean government now claims that roughly 300 people died as a result of the catastrophe (03/05/10).
  • In today's post on Reuters with the title "Chileans' quake knowledge saved thousands of lives", Daniel Trotta provides a few more details released by the U.S. Geological Survey about the Chilean quake three weeks ago. A 41-foot jump of the tectonic Nazca plate toward the South America plate triggered the 8.8-magnitude quake, 500 times more powerful than the magnitude-7.0 quake that struck Port-au-Prince six weeks earlier. The Nazca plate usually moves roughly 3 inches per year. In addition to strict building codes enforced in Chile, the low loss of lives compared with Haiti may be attributable to the atypically late arrival of the most destructive jolts after the first noticeable tremors. R and L waves arrived between 20 and 30 seconds after the P waves. In Port-au-Prince, this difference in time was only about 5 to 8 seconds. The Chilean coast was hit by three tsunami waves, surging 26 to 33 feet in some locations. Most lives may have been lost because of the flooding (03/19/10).
  • Hough and others (2010) demonstrate in a recently published seismological research study that topographic features around Port-au-Prince, like a steep ridge, must have amplified ground motion by constructive interference during the Haiti earthquake, in addition to the composition of superficial sedimentary layers in low-lying areas. Perhaps the ridge is the best location to detect an impending quake (10/18/10).
  • Not much progress in a year as this Reuters slide show published today with the title "Haiti's somber anniversary" illustrates (01/11/11).
  • Nova aired this informative program entitled "Deadliest Earthquakes" on recent advances in understanding the nature of earthquakes on Jan. 11, 2011 (01/30/11).
Amplification of seismic waves transitioning through geological layers of different density (courtesy Nuclear and Industrial Safety Agency,  Japan).
References
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