{"id":479,"date":"2010-05-01T09:22:44","date_gmt":"2010-05-01T16:22:44","guid":{"rendered":"http:\/\/a4nr.org\/?p=479"},"modified":"2010-05-01T09:22:44","modified_gmt":"2010-05-01T16:22:44","slug":"the-bulletin-of-the-atomic-scientist-nuclear-safety-lessons-from-japans-summer-earthquake","status":"publish","type":"post","link":"https:\/\/a4nr.org\/?p=479","title":{"rendered":"THE BULLETIN OF THE ATOMIC SCIENTIST &#8211; Nuclear safety lessons from Japan&#8217;s summer earthquake"},"content":{"rendered":"<p>THE BULLETIN OF THE ATOMIC SCIENTIST<\/p>\n<p>Nuclear safety lessons from Japan&#8217;s summer earthquake<\/p>\n<p>BY ASHWIN KUMAR AND M. V. RAMANA | 4 DECEMBER 2007<\/p>\n<p>On July 16, 2007, an earthquake with a magnitude of somewhere between 6.6 and 6.8<br \/>\nstruck Japan. Its epicenter was about 16 kilometers north of the Kashiwazaki-Kariwa<br \/>\nNuclear Power Plant (KKNPP), the biggest such plant in the world. The known results of<br \/>\nthe earthquake include a fire and leaks of radioactivity. However, news of damage to the<br \/>\nreactors continues to emerge, the most recent being the discovery of a jammed control<br \/>\nrod in Unit-7. Though there was no major release of radioactivity, the many failures and<br \/>\nunanticipated events that occurred at the reactor after the earthquake have important<br \/>\nimplications for nuclear safety worldwide.<\/p>\n<p>To start, the Japanese nuclear establishment never anticipated the magnitude of the<br \/>\nearthquake. Under Japan&#8217;s old guidelines, which formed the basis of the KKNPP design,<br \/>\nthe seismic hazard for each nuclear site is defined in terms of two intensities, termed S1<br \/>\nand S2. (See <em>&#8220;Status Report on Seismic Re-Evaluation&#8221;.)<\/em> The S1 earthquake, referred to<br \/>\nas the &#8220;maximum design earthquake,&#8221; is less intense and determined by historical events<br \/>\nand current and past fault activity. The S2 earthquake, called the &#8220;extreme design<br \/>\nearthquake&#8221; and supposedly an impossibility, is derived from seismo-tectonic structures<br \/>\nand active faults. These requirements were believed to provide a &#8220;sufficient range of<br \/>\nearthquakes to assure reactor safety for any potential earthquake shaking.&#8221; (See <em>&#8220;A<br \/>\nDeveloping Risk-Informed Design Basis Earthquake Ground Motion Methodology&#8221;<\/em>.) But<br \/>\nclearly the S2 design earthquake wasn&#8217;t extreme enough: The peak ground acceleration of<br \/>\nthe July 16 earthquake was two-and-a-half times greater than what was assumed for the<br \/>\nS2 earthquake.<\/p>\n<p>After the recent earthquake, Takashi Nakata at the Hiroshima Institute of Technology and<br \/>\nYasuhiro Suzuki at Nagoya University analyzed the data in the Tokyo Electric Power<br \/>\nCo.&#8217;s (TEPCO) license application and concluded that it indicated a fault five times<br \/>\nlonger than the one TEPCO identified. Between 1979 and 1985, TEPCO found four small<br \/>\nfaults off the coast of Kashiwazaki-Kariwa, but it concluded that they were either inactive<br \/>\nor unimportant. However, Nakata and Suzuki believe that three of these small faults<br \/>\nconstitute one 36-kilometer long fault, which is probably active, too.<\/p>\n<p>Such differences in conclusions suggest that there were organizational pressures to ignore<br \/>\ninconvenient data or interpret it to ensure it supported vested interests&#8211;in this case,<br \/>\nbuilding the reactor at a specific site. A similar example (albeit from a different<br \/>\ntechnological arena) is the 1986 Challenger space shuttle explosion. In her 1996 book,<br \/>\nThe Challenger Launch Decision: Risky Technology, Culture, and Deviance at NASA,<br \/>\nsociologist Diane Vaughan observed that the ultimate origins of the accident &#8220;were in<br \/>\nroutine and taken-for-granted aspects of organizational life that created a way of seeing<br \/>\nthat was simultaneously a way of not seeing.&#8221;<\/p>\n<p>The July earthquake also points to how actual accidents could result in unexpected modes<br \/>\nof failure. Nuclear reactors are based on complex interactive technologies, operating at<br \/>\nhigh temperatures or pressures, with tightly coupled events occurring at a rapid pace, and<br \/>\ntherefore, prone to accidents. (See Charles Perrow&#8217;s 1984 book, <em>Normal Accidents:<br \/>\nLiving with High-Risk Technologies<\/em>.) By simultaneously affecting large parts of a nuclear<br \/>\npower plant, earthquakes increase the possibility of accidents. The Japanese earthquake<br \/>\ndamaged KKNPP&#8217;s switchyards and water piping for the fire-suppression systems. It also<br \/>\ncaused a fire when electrical equipment near a transformer slipped, causing separated<br \/>\ncables to short-circuit. There are reports that leaking oil was involved in this fire.<br \/>\nSome events were unexpected: For example, underground electric cables were pulled<br \/>\ndown by ground subsidence, creating a large opening in the outer wall of the reactor&#8217;s<br \/>\nbasement&#8211;a so-called &#8220;radiation-controlled area&#8221; that must be completely shut off from<br \/>\nthe outside. According to a TEPCO official, &#8220;It was beyond our imagination that a space<br \/>\ncould be made in the hole on the outer wall for the electric cables.&#8221;<\/p>\n<p>Finally, the earthquake showed how emergency plans that look great on paper can fail<br \/>\nwhen disaster strikes, with KKNPP managers admitting that &#8220;disaster-prevention<br \/>\nmeasures did not function successfully.&#8221; For example, the fire-extinguishing system at<br \/>\none reactor couldn&#8217;t be used because of pipe damage, resulting in the water hose only<br \/>\nbeing able to spray water at a distance of a meter rather than the normal dozens of meters.<br \/>\nSince the plant didn&#8217;t have chemical fire extinguishers, workers had no choice but to<br \/>\nwatch the fire burn. The earthquake also knocked out a hotline to the local fire station.<br \/>\nMeanwhile, Plant Director Akio Takahashi was told of the fire immediately after the<br \/>\nearthquake, but didn&#8217;t dispatch the facility&#8217;s firefighters because he thought management<br \/>\nwould have already done so&#8211;an example of the human error even high-level officials are<br \/>\ncapable of during stressful moments. When they were notified, the fire brigade struggled<br \/>\nto reach the plant because of the area&#8217;s other damage. So although the transformer fire<br \/>\nwas detected at 10:15 a.m., firefighters didn&#8217;t start fighting it until more than an hour<br \/>\nlater. Takahashi also admitted to problems in the facility&#8217;s primary firefighting system<br \/>\nand cooperation between related organizations.<\/p>\n<p>Throughout, TEPCO&#8217;s primary aim seemed to be to quell fear rather than accurately<br \/>\nreport facts. For example, TEPCO employees knew about the leak by 12:50 p.m., but the<br \/>\ncompany didn&#8217;t publicly report it until 8:28 p.m. Similarly, the initial estimates of<br \/>\nradioactivity TEPCO released were significantly smaller than the final figure. If this was<br \/>\nthe case during a relatively major accident that was displayed on television screens<br \/>\naround the world, it&#8217;s easy to imagine the paucity of information nuclear authorities<br \/>\nwould make available during a smaller accident.<\/p>\n<p>The prevention of accidents at nuclear facilities depends on both technological and<br \/>\norganizational factors. The efficacy of these factors is contingent upon them performing<br \/>\naccording to design. Though there wasn&#8217;t a large-scale release of radioactivity, events at<br \/>\nKKNPP after the July earthquake demonstrate both technological and organizational<br \/>\nfailures. Discussions about nuclear safety should begin by acknowledging the possibility<br \/>\nof such failures.<\/p>\n<p>Copyright \u00a9 2009 Bulletin of the Atomic Scientists. All Rights Reserved.<br \/>\nSource URL (retrieved on 04\/15\/2009 &#8211; 16:21):<br \/>\n<a href=\"http:\/\/www.thebulletin.org\/node\/168\">http:\/\/www.thebulletin.org\/node\/168<\/a><\/p>\n","protected":false},"excerpt":{"rendered":"<p>THE BULLETIN OF THE ATOMIC SCIENTIST Nuclear safety lessons from Japan&#8217;s summer earthquake BY ASHWIN KUMAR AND M. V. RAMANA | 4 DECEMBER 2007 On July 16, 2007, an earthquake with a magnitude of somewhere between 6.6 and 6.8 struck Japan. Its epicenter was about 16 kilometers north of the Kashiwazaki-Kariwa Nuclear Power Plant (KKNPP), [&hellip;]<\/p>\n","protected":false},"author":1,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[25],"tags":[],"class_list":["post-479","post","type-post","status-publish","format-standard","hentry","category-kariwa-kashiwazaki-kk-japan-reactor-quake"],"_links":{"self":[{"href":"https:\/\/a4nr.org\/index.php?rest_route=\/wp\/v2\/posts\/479","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/a4nr.org\/index.php?rest_route=\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/a4nr.org\/index.php?rest_route=\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/a4nr.org\/index.php?rest_route=\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/a4nr.org\/index.php?rest_route=%2Fwp%2Fv2%2Fcomments&post=479"}],"version-history":[{"count":2,"href":"https:\/\/a4nr.org\/index.php?rest_route=\/wp\/v2\/posts\/479\/revisions"}],"predecessor-version":[{"id":481,"href":"https:\/\/a4nr.org\/index.php?rest_route=\/wp\/v2\/posts\/479\/revisions\/481"}],"wp:attachment":[{"href":"https:\/\/a4nr.org\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=479"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/a4nr.org\/index.php?rest_route=%2Fwp%2Fv2%2Fcategories&post=479"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/a4nr.org\/index.php?rest_route=%2Fwp%2Fv2%2Ftags&post=479"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}