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「安全です」と繰り返し市民に電話回答してた”いわき市の職員”
『健康被害』で、北九州へ避難
202 :名無しに影響はない(三重県):2014/04/20(日) 11:30:36.54 ID:4h5vQDQs.net>>198
福島県いわき市の事。ツイッターで福島県I市→北九州に移住と書いてる。
この人の旦那がいわき市の職員。旦那は「安全です」と繰り返し市民に
電話回答してた。でも健康被害出て離婚して娘を連れ北九州へ避難した。
http://ameblo.jp/kitakyu-mamoru/entry-11683413759.html
203 :名無しに影響はない(三重県):2014/04/20(日) 11:39:04.95 ID:4h5vQDQs.net
>>198
ブログでははっきり「いわき市」と書いてる。
そんな中、放射能が低いはずの、安全なはずのいわき市に住む私の友人の甥が先日、
白血病と診断されました。 元気だった従兄弟が突然死した次の日、友人も突然、
死にました。311前は知り合いがこんなに死ぬことはなかったのですが・・
http://ameblo.jp/kitakyu-mamoru/entry-11683413759.html
(宇都宮在住)身体に紫斑ができはじめて、1週間で死亡『白血病』
678 :名無しに影響はない(三重県):2014/05/08(木) 04:55:44.27 ID:O++qBqss
おっけい @26bath(宇都宮在住) 6 May
実は父方の伯母は白血病で亡くなりました。身体に紫斑が
できはじめて、1週間で亡くなりました。
686 :名無しに影響はない(catv?):2014/05/08(木) 06:26:42.38 ID:pViWBLGa.net
『はだしのゲン』でも死ぬ前の紫斑は出ていたね。
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栃木県。宇都宮ちかくの会社に勤める知人より
”ここ最近、社内で未成年の訃報が多い”と。
http://blog.goo.ne.jp/jpnx05/e/05a03ee4f99741eb7a059bc5edccad3b
2012-08-25
高濃度汚染地区(緑色):100,000-1,000,000Bq/m2
福島県中部の大部分、宮城県の約8割、山形県の南東部、茨城県のほぼ全域、栃木県の約5割、千葉県の北部・東部と南端部、埼玉県の約4割、群馬県の約2割、東京都の奥多摩を除く大部分、神奈川県の約5割(横浜市の一部含む)、静岡県伊豆半島(熱海市から伊東市にかけて)などのエリア。
The simulation was performed with a specific version of the numerical atmospheric chemistry and transport model Polyphemus/Polair3D. The parametrisations used for the transport and physical removal of the radionuclides are described in [6,7,8,9].
The source term has been estimated by the assimilation of activity concentrations in the air as well as activity deposited on the ground [1,2].
The magnitude of the deposition field is uncertain and the simulated values of deposited radionuclides could be significantly different from the actual deposition. In particular, the source term remains uncertain, athough its uncertainty has been narrowed down thanks to data assimilation.
Other results obtained by collaborators about the Fukushima radionuclides dispersion accident are references below [3,4,5].
The simulation was performed with a specific version of the numerical atmospheric chemistry and transport model Polyphemus/Polair3D. The parametrisation used for the transport and physical removal of the radionuclides are described in [6,7,8,9].
The source term has been estimated by the assimilation of activity concentrations in the air [8].
The magnitude of the deposition field is uncertain and the simulated value of deposited radionuclides could be different from the actual from the actual deposition. However the source term is much better known than for Fukushima-Daichii. A comparison with deposition measurements will be conducted to evaluate the simulation.
The simulation was performed with a specific version of the numerical atmospheric chemistry and transport model Polyphemus/Polair3D. The parametrisations used for the transport and physical removal of the radionuclides are described in [6,7,8,9].
The source term has been estimated by the assimilation of activity concentrations in the air as well as activity deposited on the ground [1,2].
The magnitude of activity concentration field is uncertain and could be significantly different from the actual one. In particular, the source term remains uncertain. Therefore, these results should be seen as preliminary and they are likely to be revised as new information become available to better constrain the source term and when radionuclides data can be used to evaluate the model simulation results.
Estimation of Errors in the Inverse Modeling of Accidental Release of Atmospheric Pollutant: Application to the Reconstruction of the Cesium-137 and Iodine-131 Source Terms from the Fukushima Daiichi Power Plant
V. Winiarek, M. Bocquet, O. Saunier and A. Mathieu. J. Geophys. Res. Atmospheres, 117, D05122, 2012.
Estimation of the caesium-137 source term from the Fukushima Daiichi nuclear power plant using a consistent joint assimilation of air concentration and deposition observations
V. Winiarek, M. Bocquet, N. Duhanyan, Y. Roustan, O. Saunier and A. Mathieu. Submitted, Atmo. Env., 82, 268-279, 2014.
An inverse modeling method to assess the source term of the Fukushima nuclear power plant accident using gamma dose rate observations
O. Saunier, A. Mathieu, D. Didier, M. Tombette, D. Quélo, V. Winiarek, and M. Bocquet. Atmos. Chem. Phys., 13, 11403--11421, 2013.
Assessment of the amount of Cesium-137 released into the Pacific Ocean after the Fukushima accident and analysis of its dispersion in Japanese coastal waters.
C. Estournel, E. Bosc, M. Bocquet, C. Ulses, P. Marsaleix, V. Winiarek, I. Osvath, C. Nguyen, T. Duhaut, F. Lyard, H. Michaud, and F. Auclair, Journal of Geophysical Research Oceans, 117, C11014, 2012.
État de la modélisation pour simuler l'accident nucléaire de la centrale Fukushima Daiichi.
Mathieu, A., I. Korsakissok, D. Quélo, O. Saunier, J. Groëll, D. Didier, D. Corbin, J. Denis, M. Tombette, V. Winiarek, M. Bocquet, E. Quentric, J.-P. Benoit. Pollut. Atmos., 217, in press, 2013.
Towards the operational estimation of a radiological plume using data assimilation after a radiological accidental atmospheric release
V. Winiarek, J. Vira, M. Bocquet, M. Sofiev and O. Saunier. Atmos. Env., 45, 2944-2955, 2011.
Targeting of observations for accidental atmospheric release monitoring
R. Abida and M. Bocquet. Atmos. Env., 43, 6312-6327, 2009.
Inverse modelling-based reconstruction of the Chernobyl source term available for long-range transport
X. Davoine and M. Bocquet, Atmo. Chem. Phys., 7, 1549-1564, 2007.
Validation of the Polyphemus platform on the ETEX, Chernobyl and Algeciras cases