[Express] “Acquaintance died of subarachnoid hemorrhage, a nurse suddenly died in Fukushima”

Introducing important tweets as [Express] for simultaneous updates.

 

<Translate>

My mom called to tell me, an acquaintance died of subarachnoid hemorrhage, another acquaintance found bladder cancer last year and had it spread all over the body now. Also, a nurse suddenly had a health problem and passed away 2 weeks after. They all happened in Fukushima.

<End>

 

 

 
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ご寄付ありがとうございます。これは新しく出来たFukushima Diaryの会社への寄付になります。
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Fukushima Diary can accept donation directly at PoBox too. You don't need to write the receiver's name (Only the address below is needed) but you can write it as Mochizuki Iori or Fukushima Diary SRL as well.

Fukushima Diaryは私書箱でも直接寄付などの郵便を受けられるようになりました。下記の住所が記載されていれば受取人の名前を書く必要はありませんが、Mochizuki Iori または Fukushima Diary SRLというように書いても問題ありません。

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[Express] “Recently I often see people falling down on the street in Tokyo”

Introducing important tweets as [Express] for simultaneous updates.

 

<Translate>

Today I saw a woman around 60 years old down on the crosswalk when I was walking in Ochanomizu with my friend. Someone walking neary helped her get to sidewalk. My friend told me she saw 3 people falling down on the street that day. I saw an old man fall down in Okachimachi the other day too. ・・・

<End>

 

 

 
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Cs-134/137 detected from zooplankton and seawater at over 10 locations of the Pacific, “Even from 2100km”

On 5/21/2013, Fukushima Diary reported “Meteorological Research Institute, “Cs-134/137 going deeper under ocean due to the subduction of winter” [URL]”

Another researching group reported about “Horizontal distribution of Fukushima-derived radiocesium in zooplankton in the northwestern Pacific Ocean” in Japan Geoscience Union Meeting 2013 as well.

The researching group consists of Japan Agency for Marine-Earth Science and Technology, and NOAA.

According to their study, Cs-134/137 were detected from zooplankton and seawater at over 10 locations of the Pacific Ocean.

The sampling locations were 500~2100km from Fukushima nuclear plant. The sampling date was 10 months after the accident.

Because Cs-134 was detected, it was surely from Fukushima nuclear accident.

They reported this below,

The magnitude of the 9.0 Tohoku earthquake and the ensuing tsunami on March 11, 2011, inflicted heavy damage on the Fukushima Dai-ichi nuclear power plant (FDNPP). Fission products were emitted, falling over a broad range in the northern hemisphere, and water contaminated with radionuclides leaked into the ocean. In this study, we described the horizontal distribution of the Fukushima-derived radiocesium in zooplankton and in surface seawater in the western North Pacific Ocean (500-2100km from the FDNPP) 10 months after the accident. 134Cs and 137Cs were detected in all zooplankton and seawater samples.
Because of its short half-lives, 134Cs detected in our samples could only be derived from the FDNPP accident. The radiocesium concentrations in zooplankton were high at around 25N while those in surface seawater were high at around the transition area between the Kuroshio and the Oyashio Currents (36-40N). We analyzed the structure of the zooplankton communities but could
not find out evidence which biological factors (taxa composition and relative biomass of carnivores) influenced 137Cs concentration in bulk zooplankton. Zooplankton communities contaminated with the Fukushima-derived radiocesium included many kinds of diel vertical migratory species. These migrants were exposed to higher concentrations of radiocesium while feeding at night in the ocean surface; however, exposure to contamination was lower as these species swam in the deeper mesopelagic layer during the day. In the subtropical region, 20-60% of krill and 3-36% of copepods on abundance basis were diel vertical migrants. On the other hand, 80-100% of krill and 77-88% of copepods were the migrants in the transition and the subarctic regions. Accumulated radiocesium in the migrant bodies are transported and may be taken into the mesopelagic food web.

 

http://www2.jpgu.org/meeting/2013/session/PDF/M-AG35/MAG35-06_E.pdf

http://www2.jpgu.org/meeting/2013/session/PDF/M-AG35/MAG35-06.pdf

http://www2.jpgu.org/meeting/2013/session/M-AG35.html

 

 

 
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Cs-134:137 ratio of reactor3 sub-drain is 91.3% on 5/20/2013

According to Tepco, Cs-134:137 ratio of reactor3 sub-drain is unusually high.

The half-life of Cs-134 is 2 years, the one of Cs-137 is 30.1 years.

From the samples of 5/20/2013, the Cs-134:137 ratio of reactor1 sub-drain was 41.94 %, the one of reactor2 sub-drain was 46.34 %, where the ratio of reactor3 sub-drain was 91.30 %.  (The graph below)

It suggests the possibility that Cs-134 is being produced to raise the ratio.

On 5/22/2013, Tepco didn’t release the radioactivity density data of sub-drain so it’s impossible to investigate the trend.

Cs-134:137 ratio of reactor3 sub-drain is 91.3% on 5/20/2013

 

http://www.tepco.co.jp/en/nu/fukushima-np/f1/smp/2013/images/subsurface_130521-e.pdf

 

 

 
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[Underground penetration] All β detected from 2 more observation holes of reservoir No.2, “Max as 380,000 Bq/m3″

On 5/21/2013, Fukushima Diary reported, “[Major leakage] All β nuclide detected in 1.5 m from reservoir No.2 [URL]”

According to Tepco, all β was detected from 2 more observation holes. In total, Tritium was detected from 3 holes at North East corner of reservoir No.2.

Samples were taken on 5/22/2013. The highest reading was 380,000 Bq/m3. The leaking contaminated water is possibly penetrating underground further.

[Major leakage] All β detected from 2 more observation holes of reservoir No.2, "Max as 380,000 Bq/m3"

 

http://www.tepco.co.jp/nu/fukushima-np/handouts/2013/images/handouts_130522_08-j.pdf

 

 

 
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[Major leakage] Tritium detected from 13 of 14 observation holes, “To be discharged to the sea”

Having the contaminated water keep increasing, Tepco is running out of the storage. Tepco made 7 reservoirs, but so far, Tepco has admitted 3 of them are leaking.

In order to investigate how far the leaking contaminated water is penetrating underground, Tepco is analyzing ground water of observation holes and bypass wells.

According to Tepco, radioactive water Tritium was detected from 13 of 14 holes. The sampling dates are 5/13 and 5/14/2013.

From the samples taken from 4/29 to 5/1/2013, Tritium was detected from only 3 of 14 holes.

It strongly suggests the possibility that the leaking Tritium is penetrating underground increasingly.

In the latest analysis, the highest reading was 3,500,000 Bq/m3.

They detected Tritium from all the bypass pumping wells, but Tepco will discharge it to the sea when they obtain the approvals of Fukushima Prefectual Federation of Fishries Co-operative Associations.

 

[Major leakage] Tritium detected from 13 of 14 observation holes, "To be discharged to the sea"

 

http://www.tepco.co.jp/en/nu/fukushima-np/f1/smp/2013/images/chosui_13052202-e.pdf

http://www.tepco.co.jp/nu/fukushima-np/f1/smp/2013/images/chosui_13052202-j.pdf

http://www.tepco.co.jp/nu/fukushima-np/f1/smp/2013/images/chosui_13050802-j.pdf

 

 

 
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The author of ONE PIECE hospitalized for quinsy

Even if it does not seem to have anything to do with radiation, Fukushima Diary sometimes posts articles for the potential study in future. It may become meaningful to investigate our history.

On 3/14/2013, Fukushima Diary reported, “The strip of ONE PIECE not to appear due to the author’s sudden illness [URL]”

This article may sound irrelevant but numbers of health problems of Japanese famous people have been reported everyday.

Fukushima Diary picked up one of them because ONE PIECE is widely known internationally.
Not to mention, it has nothing to do with radiation.

ONE PIECE is a comic strip on the weekly comic magazine Jump.
On the issue to be published on 3/18/2013, ONE PIECE will not appear due to the sudden illness of the author, Oda. He is still 38 years old.

The comic started in August of 1997, already has over 700 stories.
It hasn’t been stopped before due to the sudden illness of the author.

 

On 5/21/2013, the weekly comic magazine Jump announced on the issues to be published on 5/27 and 6/3, ONE PIECE will not appear because the author, Oda is going to be hospitalized for peritonsillar abscess.

 

Peritonsillar abscess [Wikipedia]

Peritonsillar abscess (PTA), also known as a quinsy or quinsey, is a recognized complication of tonsillitis and consists of a collection of pus beside the tonsil in what is referred to as Peritonsilar space (Peri – meaning surrounding).

Symptoms and signs

Unlike tonsillitis, which is more common in the pediatric age group, PTA has a more even age spread — from children to adults. Symptoms start appearing two to eight days before the formation of an abscess. Progressively worsening, unilateral sore throat and pain during swallowing usually are the earliest symptoms. As the abscess develops, persistent pain in the peritonsillar area, fever, malaise, headache and a distortion of vowels informally known as “hot potato voice” may appear. Neck pain associated with tender, swollen lymph nodes, referred ear pain and halitosis are also common. While these signs may be present in tonsillitis itself, a PTA should be specifically considered if there is limited ability to open the mouth (trismus). In short:
Severe unilateral pain in the throat;
Pyrexia above 103 degree F (39ºC);
Unilateral Earache;
Odynophagia and difficulty swallowing saliva;
Change in voice — muffled voice, “hot potato” voice;
Intense salivation and dribbling,Thickened speech, Foetor oris, Halitosis;
Pain in the neck;
Malaise, Headache, Rigor.

Causes

PTA usually arises as a complication of an untreated or partially treated episode of acute tonsillitis. The infection, in these cases, spreads to the peritonsillar area (peritonsillitis). This region comprises loose connective tissue and is hence susceptible to formation of abscess. PTA can also occur de novo. Both aerobic and anaerobic bacteria can be causative. Commonly involved species include streptococci, staphylococci and hemophilus.

 

Related article..Death cases of famous people by Yahoo news spiked up by 70% from 2010 to 2012 [URL 2]

 

http://www.shonenjump.com/j/information/wj26%E5%8F%B7%EF%BC%88527%E7%99%BA%E5%A3%B2%EF%BC%89wj27%E5%8F%B7%EF%BC%8863%E7%99%BA%E5%A3%B2%EF%BC%89%E3%81%AEone-piece%E4%BC%91%E8%BC%89%E3%81%AB%E3%81%A4%E3%81%84%E3%81%A6

 

 

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Français :

L’auteur de ONE PIECE hospitalisé pour amygdalite

 

Même si cela semble ne rien avoir avec la radioactivité, le Fukushima Diary publie parfois des articles pour de possibles études futures. Il pourra devenir intéressant d’explorer notre histoire.

Le 14 mars 2013, le Fukushima Diary publiait Interruption de la parution de la BD ONE PIECE à cause de la maladie de son auteur

Cet article va sembler hors de propos à certains mais de nombreux problèmes de santé des célébrités japonaises ont été rapportés tous les jours.
Le Fukushima Diary en relève un parce que la BD ONE PIECE est largement connue internationalement.
Cela va sans dire, ça n’a rien à voir avec la radioactivité.
ONE PIECE est une bande dessinée de l’hebdomadaire Jump.
Dans le numéro à paraître le 18 mars 2013, ONE PIECE ne sera pas présente parce que son auteur, M. Oda, est malade. Il n’a que 38 ans.
La BD a commencé en août 1997, elle fait déjà plus de 700 planches.
Elle n’avait pas été arrêtée avant à cause de la soudaine maladie de son auteur.

Le 21 mai 2013, l’hebdomadaire Jump annonce sur les parution prévues pour les 27 mai et 3 juin que ONE PIECE n’y apparaîtra pas parce que son auteur, M. Oda, va être hospitalisé pour abcès des amygdales.

Peritonsillar abscess [Wikipedia-en] (pas d’équivalent en français, voyez Angines)

Le Peritonsillar abscess (PTA), également connu sous quinsy ou quinsey, est une complication connue de l’amygdalite et consiste en un amas de pus à côté des amygdales dans ce qui appelé l’espace péri-amygdalien (péri- signifiant autour).

Signes et symptômes
Contrairement à l’amygdalite, qui est plus fréquente chez les enfants, le PTA a une répartition plus équilibrée entre les âges – des enfants aux adultes. Les symptômes commencent à apparaître deux à huit jours avant la formation d’un abcès. S’aggravant progressivement, les les premiers symptômes sont généralement des maux de gorge et des douleurs lors de la déglutition d’un seul côté. Pendant que l’abcès se développe, peut apparaître une douleur persistante dans la zone péri-amygdalienne, de la fièvre, des nausées, des maux de tête et une distorsion des voyelles communément appelée “voix de patates chaudes”. Des douleurs au cou associées à des sensibilités, un gonflement des ganglions lymphatiques, des douleurs à l’oreille en regard et l’halitose sont également fréquents. Bien que ces signes peuvent être présents dans l’amygdalite elle-même, un PTA devrait être spécifiquement envisagé dès qu’il y a une capacité limitée à ouvrir la bouche (trismus). En bref:
Douleur latérale sévère dans la gorge;
Pyrexie au-dessus de 103 °F (39 º C);
Otite latérale;
Odynophagie et difficulté à avaler la salive;
Changement de voix – voix étouffée, voix de «patate chaude»;
Salivation intense et bave, parole épaissie, foetor oris, mauvaise haleine;
Douleur dans le cou;
Malaises, maux de tête, raideurs.

Causes

Le PTA est généralement une complication d’un épisode d’amygdalite aiguë non traitée ou partiellement traitée. Dans ce cas, l’infection, se propage à la zone péri-amygdalienne (phlegmons). Cette région comprend un tissu conjonctif lâche et est donc susceptible de former un abcès. Le PTA peut également survenir de novo. Des bactéries aérobies et anaérobies peuvent en être la cause. Les espèces communément impliqués sont les streptocoques, les staphylocoques et l’haemophilus.

 

Article lié : Sous Yahoo News, le nombre de décès de gens célèbres est monté de 70 % entre 2010 et 2012

 

http://www.shonenjump.com/j/information/wj26%E5%8F%B7%EF%BC%88527%E7%99%BA%E5%A3%B2%EF%BC%89wj27%E5%8F%B7%EF%BC%8863%E7%99%BA%E5%A3%B2%EF%BC%89%E3%81%AEone-piece%E4%BC%91%E8%BC%89%E3%81%AB%E3%81%A4%E3%81%84%E3%81%A6

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Meteorological Research Institute, “Cs-134/137 going deeper under ocean due to the subduction of winter”

On 5/21/2013, the researching group reported about “Surface pathway and subduction of Fukushima radioactivity in the North Pacific Ocean in March 2011 – June 2012″ in Japan Geoscience Union Meeting 2013.

The researching group consists of Meteorological Research Institute, Atmosphere and Ocean Research Institute, The University of Tokyo, et al.

They concluded that Cs-134/137 released from Fukushima nuclear plant sank deeper layer of ocean by subduction in winter of 2011 and 2012.

It suggests the possibility that radiation measurement of ocean surface water doesn’t represent the actual sea contamination. The actual sea contamination which may affect fish contamination is likely to be worse than the measurement data.

They reported,

134Cs and 137Cs were released to the North Pacific Ocean by two major likely pathways, direct discharge from the Fukushima NPP1 accident site and atmospheric deposition. High density observations of 134Cs and 137Cs in the surface water were carried out at 322 stations by 17 cruises of cargo ships and several research vessel cruises since March 2011 till March 2012. Main
body of radioactive surface plume of which activity was exceed 10 Bq m−3 had been travelling along 40 oN, and reached International Date Line on March 2012. A feature was that the radioactive plume was confined along 40 oN when the plume reached International Date Line. Although activities of 134Cs and 137Cs in the surface water decreased rapidly, a maximum of
activities of 134Cs and 137Cs in seawater at about 300 meters depth was observed at 40 oN 165 oE in June 2012. We can say that the observed maximum of 134Cs and 137Cs was formed by subduction in winter 2011/2012 because a density of Central Mode Water of 26.3 kg m−3
corresponded to about 300 meters depth in this region. Water column inventory of 134Cs from surface to 1000 meters depth was 2710 +- 210 Bq m−2 in October 2011 at 40 oN 165 oE and 80 % of water column inventory of 134Cs existed shallower than 200 meters, however only 20 % of water column inventory of 134Cs was shallower than 200 meters while 80% was deeper than 200 meters in June 2012 due to subduction in winter 2011/2012.

 

http://www2.jpgu.org/meeting/2013/session/PDF/M-AG35/MAG35-03.pdf

http://www2.jpgu.org/meeting/2013/session/sessionday.html

 

 

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L’Institut de Recherches Météorologiques : Le Cs 134/137 descend plus loin sous l’océan à cause de la subduction hivernale

 

Le 21 mai 2013, le groupe de recherche publie sur “Surface pathway and subduction of Fukushima radioactivity in the North Pacific Ocean in March 2011 – June 2012” dans Japan Geoscience Union Meeting 2013.

Le groupe de recherche est composé par le Meteorological Research Institute, l’Atmosphere and Ocean Research Institute, l’Université de Tokyo, et al.
Ils concluent que le césium 134/137 émis par la centrale nucléaire de Fukushima s’est enfoncé par subduction dans des couches plus profondes de l’océan au cours des hivers 2011 et 2012.

Ceci laisse penser que les mesures de la radioactivité en surface de l’océan ne sont pas représentatives de sa réelle contamination. La contamination réelle de la mer, qui influe sur celle des poissons, a toutes les chances d’être pire que celle mesurée.

Ils publient :

Les césiums 134 et 137 ont été émis dans l’océan Pacifique Nord en suivant deux principales voies de dispersion, le déversement direct depuis le site de l’accident de la NPP1 (= centrale d’électricité nucléaire N°1) de Fukushima et les retombées atmosphériques. Des observations des hautes concentrations en Cs 134 et Cs 137 en surface de l’eau ont été faites entre mars 2011 et mars 2012 en 322 points au cours de 17 croisières de cargos et plusieurs croisières de vaisseaux de recherche. Le gros du panache radioactif de surface pour lequel l’activité dépassait 10 Bq m−³ a dérivé le long du 40eN et a atteint la ligne de changement de date en mars 2012.

Une caractéristique en a été que ce panache radioactif est resté confiné le long du 40eN au moment où il a atteint la ligne de changement de date. Bien que l’activité en Cs 134 et Cs 137 de surface décroissait rapidement, un maximum d’activité des Cs134 et Cs137 a été observé en juin 2012 en 40°N 165°E à environ 300 mètres de profondeur. Nous pouvons dire que ce maximum observé pour les Cs134 et Cs137 s’est constitué par subduction au cours de l’hiver 2011/2012 parce que dans cette région la densité de l’eau de 26,3 kg m−³ en Mode Central correspondait à 300 mètres de profondeur environ.

Le sondage vertical en 40°N 165°E du Cs 134 entre la surface et 1000 mètres de profondeur donnait 2710 +- 210 Bq m−² en octobre 2011 et 80 % du Cs 134 de la colonne d’eau inventoriée se situait à une profondeur inférieure à 200 mètres alors qu’en juin 2012 seulement 20 % du Cs 134 était encore à moins de 200 mètres alors que 80% étaient passés en-dessous, à cause de la subduction hivernale de 2011/2012.

http://www2.jpgu.org/meeting/2013/session/PDF/M-AG35/MAG35-03.pdf
http://www2.jpgu.org/meeting/2013/session/sessionday.html

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Sr-90 detected 6 times much as safety limit from seawater of water intake

According to Tepco, 170,000 Bq/m3 of Sr-90 was measured from seawater.

Density Limit Specified by the Reactor Regulation is 30,000 Bq/m3. The measurement reading is 5.7 times much as the density limit.

The sampling location is north of reactor 1-4 water intake.

Also, 120,000 Bq/m3 of Tritium was measured.

Sr-90 detected 6 times much as safety limit from seawater of water intake

 

↓ The location of water intake

2 Sr-90 detected 6 times much as safety limit from seawater of water intake

 

http://www.tepco.co.jp/en/nu/fukushima-np/f1/smp/2013/images/intake_canal_130521-e.pdf

http://www.tepco.co.jp/nu/fukushima-np/f1/smp/2013/images/intake_canal_130521-j.pdf

 

 

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Français :

A la prise d’eau de mer, le strontium 90 détecté est 6 fois supérieur à la limite de sécurité

 

Selon Tepco, 170 000 Bq/m³ de Sr 90 ont été relevés dans l’eau de mer.

La limite de concentration spécifiée par la règlementation des réacteurs est de 30 000 Bq/m³. Le relevé est 5,7 fois au-dessus de cette limite.
L’échantillon provient de la prise d’eau au nord des réacteurs 1-4.
Ils ont aussi relevé 120 000 Bq/m³ de tritium.

A la prise d'eau de mer, le strontium 90 détecté est 6 fois supérieur à la limite de sécurité

↓ L’endroit de la prise d’eau

2 A la prise d'eau de mer, le strontium 90 détecté est 6 fois supérieur à la limite de sécurité

http://www.tepco.co.jp/en/nu/fukushima-np/f1/smp/2013/images/intake_canal_130521-e.pdf
http://www.tepco.co.jp/nu/fukushima-np/f1/smp/2013/images/intake_canal_130521-j.pdf

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[Major leakage] All β nuclide detected in 1.5 m from reservoir No.2

According to Tepco, all β nuclides were detected from the outside of reservoir No.2

Tepco is running out of contaminated water storage facility. They made 7 underground reservoirs, but some of them ended up leaking to underground. So far, Tepco has admitted 3 of them are officially leaking.

On 5/2/2013, Tepco announced they were going to make 6 borings with an angle and a vertical boring. It is to investigate the leakage and contamination situation underground.

(cf, [Reservoir Leakage] Tepco to make 7 more borings beside each the leaking reservoir [URL])

On 5/21/2013, they measured 290,000 Bq/m3 of all β nuclide in one of the borings, which is located at North East corner of the reservoir.

The boring is 1.5m far from the wall of the reservoir. It’s proved that the leaking contaminated water is already penetrating underground.

[Major leakage] All β nuclide detected in 1.5 m from reservoir No.2

 

http://www.tepco.co.jp/nu/fukushima-np/handouts/2013/images/handouts_130521_07-j.pdf

 

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Français :

[Fuites majeures] Les β nucléides détectés à 1,5 m du réservoir N°2

 

Selon Tepco, les β nucléides ont été détectés à l’extérieur du réservoir N°2

Tepco est en manque d’espace de stockage pour les eaux extrêmement radioactives. Ils ont construit 7 réservoirs enfouis mais certains d’entre eux on fini par fuir dans le sous-sol. Pour l’instant, Tepco a officiellement reconnu que 3 d’entre eux fuient.

le 2 mai 2013, Tepco avait déclaré qu’ils allaient faire 6 forages inclinés et un vertical pour surveiller la fuite et l’état de la contamination du sous-sol. (cf. [Fuites des réservoirs] Tepco va faire 7 forages de plus à côté de chaque réservoir percé)
Le 21 mai 2013, ils relèvent 290 000 Bq/m³ de β nucléides dans l’un des forages situé au coin NE du réservoir.
Le forage est à 1,5 m de la paroi du réservoir. Ça prouve que la fuite d’eau extrêmement radioactive est déjà en train de s’infiltrer en sous-sol.

[Fuites majeures] Tous les β nucléides détectés à 1,5 m du réservoir N°2

http://www.tepco.co.jp/nu/fukushima-np/handouts/2013/images/handouts_130521_07-j.pdf

Merci pour votre aide.
A présent, vos dons vont être utilisés pour la recherche suivante d’un possible village japonais en Roumanie. (560 €)
Pour l’instant, il manque 471 €.

(Euro)
Train : 100
Hôtel à Sighisoara : 30×7 nuits
Hôtel à Arad : 30×7 nuits
Bus : 40
Total : 560

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