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Edward D. Blandford is Assistant Professor of Nuclear Engineering at the University of New Mexico. He was formerly a Stanton Nuclear Security Fellow at Stanford's Center for International Security and Cooperation. Scott D. Sagan is the Caroline S.G. Munro Professor of Political Science, the Mimi and Peter Haas University Fellow in Undergraduate Education, and Senior Fellow at CISAC and the Freeman Spogli Institute at Stanford University.
Acknowledgments,
Contributors,
PART I: THE FUKUSHIMA ACCIDENT,
Introduction: Learning from a Man-made Disaster Scott D. Sagan,
1. Japan's Fukushima Nuclear Disaster: An Overview Kenji E. Kushida,
PART II: LEARNING LESSONS FROM FUKUSHIMA,
2. The Accident That Could Never Happen: Deluded by a Design Basis Gregory D. Wyss,
3. Security Implications of the Fukushima Accident Kaoru Naito,
4. Political Leadership in Nuclear Emergency: Institutional and Structural Constraints Nobumasa Akiyama,
5. Radiation Protection by Numbers: Another "Man-made" Disaster Toshihiro Higuchi,
6. Encouraging Transnational Organizational Learning Kazuto Suzuki,
PART III: LESSONS LEARNED ABOUT LESSONS LEARNED,
7. Were Japan's Nuclear Plants Uniquely Vulnerable? Phillip Lipscy, Kenji E. Kushida, and Trevor Incerti,
8. Beyond Fukushima: Enhancing Nuclear Safety and Security in the Twenty-first Century Edward D. Blandford and Michael M. May,
Index,
Japan's Fukushima Nuclear Disaster: An Overview
Kenji E. Kushida
The Tohoku earthquake that struck off the northeastern coast of Japan on March 11, 2011, had a magnitude of 9.0, the world's fourth largest in modern recorded history. The island of Honshu moved 2.4 meters to the east. A massive tsunami followed shortly thereafter, reaching an estimated height of over 30 meters in some places. A 500-kilometer section of Japan's northeastern coast was devastated, with a death toll of more than 15,000 people. Damage from the earthquake and tsunami led to one of the world's most serious nuclear disasters, at the Fukushima Daiichi (number one) Nuclear Power Station on Japan's eastern coast, owned and operated by the Tokyo Electric Power Company (TEPCO).
The Fukushima Daiichi plant had six nuclear reactors, three of which were in operation at the time of the earthquake and tsunami, with the rest undergoing routine maintenance. As the earthquake hit, the active reactors were successfully scrammed (that is, placed under emergency shutdown). All off-site power from the external power grid was lost as a result of severed power lines and earthquake damage to transformer stations, but the on-site emergency backup power sources, consisting of diesel generators and batteries, immediately came online to operate the cooling pumps and other functions.
The tsunami hit the plant approximately forty minutes later, reaching a height of over 12 meters. It well exceeded the maximum safety design of 5.7 meters and obliterated the 10-meter-high seawall. The tsunami destroyed almost all on-site backup power sources, as well as most of the pumps necessary to cool the reactors. Over the next three days, despite desperate attempts on the ground to restore cooling, the three reactors that had been active before the earthquake experienced fuel core meltdowns, and hydrogen explosions blew away the roofs, walls, and upper floors of three reactor buildings.
Although the catastrophe at Fukushima Daiichi emitted at least 168 times the amount of radioactive cesium 137 as the Hiroshima atomic bomb, there were no direct deaths from radiation exposure. A mandatory evacuation zone with a radius of 10 kilometers was imposed in the early hours of March 12, expanded to 20 kilometers later that day, displacing more than
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