Die Strahlungsbelastung durch die Nuklearunfälle von Fukushima ist ein wesentlicher Teil der Nuklearkatastrophe von Fukushima. Ab dem 12. März 2011 kam es im japanischen Kernkraftwerk Fukushima Daiichi zu einer Serie katastrophaler Unfälle. Dabei wurde ein Teil der radioaktiven Stoffe, die in großen Mengen in Kernreaktoren entstehen, freigesetzt – flüchtige Stoffe bereits durch die gezielte Druckentlastung der Reaktoren, Partikel vor allem durch Explosionen und Brände und wasserlösliche Stoffe durch behelfsmäßige Kühlmaßnahmen. Es kam zu einer erheblichen Umweltbelastung auf dem Festland – vor allem in den Präfekturen Fukushima und Ibaraki – und im näheren Pazifischen Ozean. Die Emissionen in die Atmosphäre und ins Meer dauern an, allerdings in einem um Größenordnungen geringeren Ausmaß als während der ersten Wochen. Mit empfindlichen Messgeräten sind Spuren der radioaktiven Partikel aus Fukushima weltweit nachweisbar. (de)
Le 11 mars 2011, un séisme de magnitude 9 déclenche un tsunami qui dévaste la côte Pacifique du Tōhoku au Japon et provoque la catastrophe nucléaire de Fukushima : la centrale nucléaire est endommagée, provoquant un défaut de refroidissement, des fusions de cœur dans plusieurs réacteurs puis des ruptures de confinement et d'importants rejets radioactifs dans l'atmosphère mais également dans tout l'environnement. Cet événement entraîne des conséquences sanitaires et sociales importantes au Japon. Par ailleurs tant le panache radioactif que les rejets dans l'océan suscitent des inquiétudes dans le monde. Selon les estimations publiées par l'Agence japonaise de sûreté nucléaire, l'accident a dispersé l'équivalent de 10 % de l'accident de Tchernobyl : entre 1,3 et 1,5 × 1017 becquerels d'iode 131 (contre 1,8 × 1018 pour Tchernobyl), et entre 6,1 et 12 × 1015 becquerels de césium 137 (contre 8,5 × 1016 pour Tchernobyl). Environ 110 000 personnes sont évacuées dans un rayon de 20 km. (fr)
The radiation effects from the Fukushima Daiichi nuclear disaster are the observed and predicted effects as a result of the release of radioactive isotopes from the Fukushima Daiichii Nuclear Power Plant following the 2011 Tōhoku 9.0 magnitude earthquake and tsunami (Great East Japan Earthquake and the resultant tsunami). The release of radioactive isotopes from reactor containment vessels was a result of venting in order to reduce gaseous pressure, and the discharge of coolant water into the sea. This resulted in Japanese authorities implementing a 30-km exclusion zone around the power plant and the continued displacement of approximately 156,000 people as of early 2013. The number of evacuees has declined to 49,492 as of March 2018. Large quantities of radioactive particles from the incident, including iodine-131 and caesium-134/137, have since been detected around the world. Substantial levels have been seen in California and in the Pacific Ocean. The World Health Organization (WHO) released a report that estimates an increase in risk for specific cancers for certain subsets of the population inside the Fukushima Prefecture. A 2013 WHO report predicts that for populations living in the most affected areas there is a 70% higher risk of developing thyroid cancer for girls exposed as infants (the risk has risen from a lifetime risk of 0.75% to 1.25%), a 7% higher risk of leukemia in males exposed as infants, a 6% higher risk of breast cancer in females exposed as infants and a 4% higher risk, overall, of developing solid cancers for females. Preliminary dose-estimation reports by WHO and the United Nations Scientific Committee on the Effects of Atomic Radiation (UNSCEAR) indicate that, outside the geographical areas most affected by radiation, even in locations within Fukushima prefecture, the predicted risks remain low and no observable increases in cancer above natural variation in baseline rates are anticipated. In comparison, after the Chernobyl reactor accident, only 0.1% of the 110,000 cleanup workers surveyed have so far developed leukemia, although not all cases resulted from the accident. However, 167 Fukushima plant workers received radiation doses that slightly elevate their risk of developing cancer. Estimated effective doses from the accident outside of Japan are considered to be below, or far below the dose levels regarded as very small by the international radiological protection community. The United Nations Scientific Committee on the Effects of Atomic Radiation is expected to release a final report on the effects of radiation exposure from the accident by the end of 2013. A June 2012 Stanford University study estimated, using a linear no-threshold model, that the radioactivity release from the Fukushima Daiichi nuclear plant could cause 130 deaths from cancer globally (the lower bound for the estimate being 15 and the upper bound 1100) and 199 cancer cases in total (the lower bound being 24 and the upper bound 1800), most of which are estimated to occur in Japan. Radiation exposure to workers at the plant was projected to result in 2 to 12 deaths. However, a December 2012 UNSCEAR statement to the Fukushima Ministerial Conference on Nuclear Safety advised that "because of the great uncertainties in risk estimates at very low doses, UNSCEAR does not recommend multiplying very low doses by large numbers of individuals to estimate numbers of radiation-induced health effects within a population exposed to incremental doses at levels equivalent to or lower than natural background levels." (en)
Die Strahlungsbelastung durch die Nuklearunfälle von Fukushima ist ein wesentlicher Teil der Nuklearkatastrophe von Fukushima. Ab dem 12. März 2011 kam es im japanischen Kernkraftwerk Fukushima Daiichi zu einer Serie katastrophaler Unfälle. Dabei wurde ein Teil der radioaktiven Stoffe, die in großen Mengen in Kernreaktoren entstehen, freigesetzt – flüchtige Stoffe bereits durch die gezielte Druckentlastung der Reaktoren, Partikel vor allem durch Explosionen und Brände und wasserlösliche Stoffe durch behelfsmäßige Kühlmaßnahmen. Es kam zu einer erheblichen Umweltbelastung auf dem Festland – vor allem in den Präfekturen Fukushima und Ibaraki – und im näheren Pazifischen Ozean. (de)
The radiation effects from the Fukushima Daiichi nuclear disaster are the observed and predicted effects as a result of the release of radioactive isotopes from the Fukushima Daiichii Nuclear Power Plant following the 2011 Tōhoku 9.0 magnitude earthquake and tsunami (Great East Japan Earthquake and the resultant tsunami). The release of radioactive isotopes from reactor containment vessels was a result of venting in order to reduce gaseous pressure, and the discharge of coolant water into the sea. This resulted in Japanese authorities implementing a 30-km exclusion zone around the power plant and the continued displacement of approximately 156,000 people as of early 2013. The number of evacuees has declined to 49,492 as of March 2018. Large quantities of radioactive particles from the inci (en)
Le 11 mars 2011, un séisme de magnitude 9 déclenche un tsunami qui dévaste la côte Pacifique du Tōhoku au Japon et provoque la catastrophe nucléaire de Fukushima : la centrale nucléaire est endommagée, provoquant un défaut de refroidissement, des fusions de cœur dans plusieurs réacteurs puis des ruptures de confinement et d'importants rejets radioactifs dans l'atmosphère mais également dans tout l'environnement. Cet événement entraîne des conséquences sanitaires et sociales importantes au Japon. Par ailleurs tant le panache radioactif que les rejets dans l'océan suscitent des inquiétudes dans le monde. (fr)