A drop in the ocean: photographic witnessing and the Fukushima wastewater release

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Abstract. Ever since the Japanese Government's 2021 announcement approving Tokyo Electric Power Company (TEPCO)'s plan to discharge this wastewater into the Pacific Ocean, there has been widespread public dissension. In efforts to control public opinion and mistrust, words such as “treated”, “purified”, and “diluted” circulated among official government and scientific discourse concerning TEPCO's plan. These words are mundane, deceptive and distracting. For example, remaining traces of tritium were proposed as so diluted that the water is akin to drinkable standards. Furthermore, the vast scale of the Pacific Ocean reinforced just how diluted the Fukushima wastewater would ultimately become, totalling to 0.000183 %, meaning quite literally a drop in the ocean. This article responds to this context by exploring how this language of dilution and trace function to mask the slow eco-cultural violence embedded in Japan's wastewater release. Specifically, I focus on how my photographic series Listening to Seaweed attempts to visualize what is largely imageless – diluted trace evidence of tritium. Through close readings of these artworks, I explore how photographic film's inherent sensitivity to ionizing radiation can register, and thereby witness, the presence of environmental radiation. I am interested in how this witnessing functions to critique the ideological contexts that continue to perpetuate nuclear power as a safe by-product of the technology developed to produce nuclear weapons. Methodologically framed via artist and theorist Susan Schuppli's (2020) conception of material witnessing, I argue for forms of politicized witnessing that move beyond visibility itself; instead, quantifiable evidence of nuclear ideology is physically embedded in the image. This article questions how these materially oriented methods can establish forms of socio-ethical listening and material witnessing that promote transgenerational nuclear justice concerning this current geo-political moment.

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  • 10.54691/bcpbm.v23i.1394
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On April 13, 2021, the Japanese government officially issued a statement saying that it will discharge the nuclear waste water stored in the Tokyo Electric Power Company's Fukushima Daiichi Nuclear Power Plant into the sea around the spring of 2023 for a period of 30 years. Despite almost overwhelming opposition domestic and abroad, the Japanese government has not withdrawn or delayed the plan. Based on the six stakeholders and the PEST analysis method, this paper deeply discusses the reasons for the Japanese government's unilateral decision to discharge nuclear waste water into the sea. Research shows that Japan's discharge of nuclear waste water is not just an environmental protection issue, it is a consequence of Japan's political, economic, technological, cultural and even historical factors. The purpose of this paper is to provide a reference for effective measures in the future, in the hope of better protecting the legitimate rights and interests of stakeholders by introducing international environmental law to prevent and postpone the discharge of nuclear wastewater from Japan.

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Deprivation of Furusato: The damage faced by evacuees after the Fukushima nuclear power plant accident
  • Mar 1, 2023
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  • Reiko Seki

This paper considers the damage caused by the Great East Japan Earthquake and the meaning of the Fukushima Nuclear Power Plant accident, and reflects on the evacuees' experiences over past 12 years. During this time, several lawsuits demanding the clarification of responsibility for the accident and compensation for damages have been filed against TEPCO (Tokyo Electric Power Company) and the Japanese Government. The “loss and transformation of hometowns (furusato in Japanese)” has become one of the key issues in these lawsuits. While the casees were being litigated, the mandated “evacuation designated zones” were gradually lifted. Even in the “Difficult‐to‐Return Areas” where annual integrated doses of radioactive substances are over 50 mSv and evacuation orders are still in effect, efforts are being made to lift the evacuation orders. Because they were forced to leave their places of residence, evacuees have claimed, “we lost oue furusato [hometown].” However, because they are able to return after evacuation orders are lifted, both TEPCO and the Japanese Government have insisted that “their furusato has not been lost” and “they cannot claim compensation for furusato damages.” In this paper, I call the irreversible and absolute damage caused by the nuclear power plant accident “the deprivation of furusato.” I look at furusato from three aspects: the relationship between people and nature, the connection between people, and notions of persistence and sustainability. Then, I discuss what kind of reconstruction is being promoted to respond to the deprivation of furusato and for whom.

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  • Chinese Science Bulletin
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<p indent="0mm">Ten years after the Fukushima nuclear accident (FNA), Japan announced the planned discharge of over one million tons of Fukushima radioactive wastewater (FRW) into the Pacific Ocean in two years. This decision regarding FRW disposal has aroused worldwide concerns and public fears, which may be exacerbated by reputational damage and the lack of a clear public understanding of the possible adverse impacts of the FRW. As one of the countries surrounding the Pacific Ocean, China is a stakeholder in this decision regarding the FRW disposal. In this study, we compared the FRW source and its associated radionuclide components with the liquid effluent from routine operation of the nuclear power plant and its associated radionuclides. The activity concentrations of 13 radionuclides in the pre- and post-treated FRW by the Advanced Liquid Processing Systems (ALPS) were quantitatively compared with limits for radionuclide concentrations required by Japan law, guidance levels for radionuclides in drinking water provided by the World Health Organization (WHO), and baseline concentrations of radionuclides in surface seawater from the Pacific Ocean before the FNA. Sediment-seawater distribution coefficients and bioconcentration factors are also shown to provide insights into the mobility and biological availability of radionuclides derived from the FRW in the marine environment. Although 62 radionuclides can be recovered from the FRW by ALPS according to a report from the Tokyo Electric Power Company (TEPCO), a large amount of <sup>3</sup>H remains in the ALPS-treated FRW. 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Following the accident at the Fukushima Daiichi Nuclear Power Plant (FDNPP) in March 2011, large quantities of radioactive materials were released into the atmosphere and ocean. Since the FDNPP nuclear accident, Tokyo Electric Power Company (TEPCO) operators have been implementing measures to reduce groundwater inflow into the FDNPP damaged reactor buildings while pumping water to cool the&amp;#160;nuclear reactors and fuel debris. The resulting huge water volume began the discharge into the ocean from August 2023, after being treated by an Advanced Liquid Processing System (ALPS) to remove radionuclides for acceptable discharge levels except tritium. Tritium releases from the FDNPP accident and the ALPS treated water raise questions about the impact on tritium in precipitation in Japan, the removal time of anthropogenic tritium in groundwater and the oceanic transport of tritium from released ALPS treated water.&amp;#160;In this two-part study, we present (1) the modeling of tritium in precipitation during the FDNPP accident using an atmosphere general circulation model (AGCM), and (2) a sensitivity simulation of tritium concentration in the ocean due to planned ALPS treated water release in the next decades by TEPCO using an ocean general circulation model (OGCM).&amp;#160;For the atmospheric part, we used the isotope-enabled AGCM MIROC5-iso, in which tritium has been implemented [1], and adapted an estimated atmospheric release of iodine-131 [2] for the anthropogenic tritium source. We found good agreement with the tritium in precipitation observations in Japan for 2011 and subsequent years, despite MIROC5-iso&amp;#8217;s rather coarse horizontal resolution (approximately 2.8&amp;#176;). Together with measured tritium data in Japan, our modeled results can be used to interpret mean transit times of Fukushima surface and groundwater systems and in other Asian systems (see abstract of Gusyev et al. in the same session).For the oceanic part, we used the OGCM COCO4.9, which is the ocean component of the Model for Interdisciplinary Research on Climate, version 6 (MIROC6 [3]), and the tritium discharge scenario from TEPCO. Tritium concentration at the ocean surface reaches approximately 3 Bq/m3 near the release site and varies between 0.01 and 0.25 Bq/m3 in the North Pacific Ocean, well below the natural tritium level (approximately 50 Bq/m3 [4]). For this kind of projection simulation, the use of a fully coupled atmosphere-ocean model would make it possible to model tritium concentration in both the atmosphere and the ocean, as well as the dynamics of exchanges within and between these water cycle reservoirs.&amp;#160;[1] Cauquoin et al.: Modeling natural tritium in precipitation and its dependence on decadal variations of solar activity using the atmospheric general circulation model MIROC5-iso, J. Geophys. Res. Atmos., in review (minor revisions).[2] Katata et al., Atmos. Chem. Phys., 15, 1029&amp;#8211;1070, https://doi.org/10.5194/acp-15-1029-2015, 2015.[3] Tatebe et al., Geosci. Model Dev., 12, 2727&amp;#8211;2765, https://doi.org/10.5194/gmd-12-2727-2019, 2019.[4] Jenkins et al., Earth Syst. Sci. Data, 11, 441&amp;#8211;454, https://doi.org/10.5194/essd-11-441-2019, 2019.

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Making Sense of the Disaster
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Now a word Japanese, is date when earth's tectonic forces physically reconfigured Japan. Nearly three years since March 11, 2011, nightmare began, Japanese government has confirmed deaths of 16,000 people; addition, several thousand more remain missing and presumed killed by devastation unleashed from 9.0-magnitude earthquake and monstrous tsunami ensued. Three of six reactors at Fukushima Daiichi nuclear power plant experienced meltdowns, and according to official statistics, 282,000 people are still refugees within Japan, unable to return home. Many have moved from country's northeastern Tohoku region because of infrastructure damage, while many more have dispersed because radiation levels their houses and villages exceed acceptable norms. Fear and mistrust concerning what Japanese government and Tokyo Electric Power Company (TEPCO) deem safe levels of radiation propel them as well.With characteristic clarity, intellect, and scholarly rigor, Richard Samuels has engaged this unfolding maelstrom head-on to produce 3.11: Disaster and Change Japan. Moving categorically through three areas-security, energy, and local public administration-Samuels argues thus far fallout from this unimaginable trifecta of disasters has been not only imaginable but also predictable. Samuels explains of post-3.11 Japan political actors spun stories to help make sense of disaster, always ways consistent with what they already 'knew' to be true (p. 184). His elaboration brings him to conclude was simply continuation of normal politics by additional means (p. 185). Throughout book, Samuels thoughtfully explicates his thesis of continuity over rupture: Japan which who thought utilities were villains before 3.11 insisted 3.11 proved their point. Those who believed DJP [Democratic Party of Japan] was a collection of incompetent parvenus...now had additional evidence...[and] supporters of Japan-U.S. and of Japanese military renewed their claim they were right all along (p. 184-85). Writing most specifically about security, he emphasizes that, in short, there was no major Tohoku dividend-either for war-fighting capacity of Japanese troops or for U.S.-Japan alliance (p. 109).All this notwithstanding-and what will likely be his pathbreaking contribution to assessments of 3.11-Samuels's own detailed examination of rescue and relief operations conducted by Japanese Self-Defense Forces (SDF) suggests if we wait just a little bit longer, dividend for SDF may be rather lucrative indeed. In short, Samuels describes how during 3.11 a discursive shift took place alongside troops' actions, one has continued to secure widespread buy-in for SDF throughout Japanese society ways that-if not entirely new-have greatly expanded level of support beyond anything seen before 2011 post-1945 era.The SDF's moment 3.11 spotlight shapes book's fourth chapter, Dueling Security Narratives, which Samuels establishes three categories of responses to what took place: wake-up call (comments from those largely on right who urged nation to get in gear and prepare for its real enemies), proof of concept (views held by centrists who saw the deterrent power of alliance SDF's performance working together with U.S. troops), and disarm (the largely leftist perspective that Japan's soldiers get more shovels than guns) (p. 83-86). Next, Samuels views these categories through secondary prisms interrogate what we might glean for future place and function of SDF Japanese society. Taken as a whole, analysis ties well with his previous work on Japanese military, as well as with other analyses of soft changes were already afoot within SDF long before March 11, 2011, order to make its existence more palatable to Japanese society general. …

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Fukushima: The myth of safety, the reality of geoscience
  • Sep 1, 2011
  • Bulletin of the Atomic Scientists
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Estimation of radioactive leakages into the Pacific Ocean due to Fukushima nuclear accident
  • May 4, 2013
  • Environmental Earth Sciences
  • R N Nair + 5 more

High concentrations of several radionuclides were reported in the sea near the Fukushima Daiichi Nuclear Power Station (FDNPS) in Japan due to the nuclear accident that occurred on 11 March 2011. The main source of these concentrations was leakage of highly radioactive liquid effluent from a pit in the turbine building near the intake canal of Unit-2 of FDNPS through a crack in the concrete wall. In the immediate vicinity of the plant, seawater concentrations reached 68 MBq m−3 for 134Cs and 137Cs, and exceeded 100 MBq m−3 for 131I in early April 2011. These concentrations began to fall as of 11 April 2011 and, at the end of April, had reached a value close to 0.1 MBq m−3 for 137Cs. Following the nuclear accident, the Tokyo Electric Power Company (TEPCO) had initiated intense monitoring of the environment including the Pacific Ocean. Seawater samples were collected and the concentrations of few radionuclides were measured on a wide spatial and temporal scale. In this study, the measured concentrations of different radionuclides near the south discharge canal of the FDNPS were used to estimate their leakages into the Pacific Ocean. The method is based on estimating the release rates that reproduce the concentration of radionuclides in seawater at a chosen location using a two-dimensional advection–dispersion model in an iterative manner. The radioactive leakages were estimated as 5.68 PBq for 131I, 2.24 PBq for 134Cs and 2.25 PBq for 137Cs. Leakages were also estimated for 99mTc, 136Cs, 140Ba and 140La and they range between 0.02 PBq (99mTc) and 0.53 PBq (140Ba). It was estimated that about 11.28 PBq of radioactivity in total was leaked into the Pacific Ocean from the damaged FDNPS. Out of this, 131I constitutes 50.3 %; 134Cs 20 %; 137Cs 20 %; 140Ba 4.6 %; 136Cs 2.6 %; 140La 2.3 % and 99mTc 0.2 % of the total radioactive leakage. Such quantitative estimates of radioactive leakages are essential prerequisites for short-term and local-scale as well as long-term and large-scale radiological impact assessment of the nuclear accident.

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