The Fukushima Daiichi nuclear power plant has begun discharging treated radioactive water into the sea for a third time. The emissions are 7,800 tons per discharge, and the same amount is planned for this discharge. The emissions program runs through Nov. 20 and lasts for a decade. The reason for the discharge is because the storage tanks are almost full and need to be decommissioned. The move has been strongly opposed by fishermen's groups and neighboring countries including South Korea and China.
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The Fukushima Daiichi nuclear power plant has begun discharging treated radioactive water into the sea for a third time. The emissions are 7,800 tons per discharge, and the same amount is planned for this discharge. The emissions program runs through Nov. 20 and lasts for a decade. The reason for the discharge is because the storage tanks are almost full and need to be decommissioned. The move has been strongly opposed by fishermen's groups and neighboring countries including South Korea and China.
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Elements released from the hydrothermal vents can be diluted in seawater or scavenged onto sinking particles23. We used dissolved manganese (dMn) as an index to assess the importance of Hg removal processes following venting. Owing to its slow oxidation rate, dMn has been used as a conservative tracer of the dilution of vent fluids along hydrothermal plumes. During the cruise transit, particulate manganese (pMn) was lower than dMn with concentrations consistent with oceanic background levels24 (Extended Data Fig. 3). Average pMn considering all stations and depths within the plume was 2.5% of the total manganese (tMn) (Extended Data Fig. 4). Following previous studies19,25,26, we thus use dMn as a conservative tracer along the plume, being affected only by dilution. Combining manganese (Mn) data of the plume with our previously reported Mn concentration of the vent fluid end member at TAG (0.43 mmol l−1) (ref. 27), we calculate the dilution factor from the vent fluid end member to the non-buoyant plume (equation (1) and Extended Data Fig. 5). For comparison, dilution factors were calculated separately using tMn and dMn concentrations in the plume. No substantial difference was found between the two approaches, thus in further discussions, we refer to the dilution factor calculated with dMn (Extended Data Fig. 5). The average calculated dilution factor considering all depths with the plume and stations is 2.79 × 105 ± 1.4 × 103. The dilution factor is 2.36 × 104 at the TAG vent site and increases with distance to reach 1.21 × 106 at station 9 located 10 km away (Extended Data Fig. 5). Dilution factors are rather similar within the non-buoyant plume at each station.
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