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Isotopic signature and nano-texture of cesium-rich micro-particles: Release of uranium and fission products from the Fukushima Daiichi Nuclear Power Plant

机译:富铯微粒的同位素特征和纳米结构:福岛第一核电站的铀和裂变产物的释放

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摘要

Highly radioactive cesium-rich microparticles (CsMPs) released from the Fukushima Daiichi Nuclear Power Plant (FDNPP) provide nano-scale chemical fingerprints of the 2011 tragedy. U, Cs, Ba, Rb, K, and Ca isotopic ratios were determined on three CsMPs (3.79–780 Bq) collected within ~10 km from the FDNPP to determine the CsMPs’ origin and mechanism of formation. Apart from crystalline Fe-pollucite, CsFeSi2O6 · nH2O, CsMPs are comprised mainly of Zn–Fe-oxide nanoparticles in a SiO2 glass matrix (up to ~30 wt% of Cs and ~1 wt% of U mainly associated with Zn–Fe-oxide). The 235U/238U values in two CsMPs: 0.030 (±0.005) and 0.029 (±0.003), are consistent with that of enriched nuclear fuel. The values are higher than the average burnup estimated by the ORIGEN code and lower than non-irradiated fuel, suggesting non-uniform volatilization of U from melted fuels with different levels of burnup, followed by sorption onto Zn–Fe-oxides. The nano-scale texture and isotopic analyses provide a partial record of the chemical reactions that occurred in the fuel during meltdown. Also, the CsMPs were an important medium of transport for the released radionuclides in a respirable form.
机译:从福岛第一核电站(FDNPP)释放的高放射性富铯微粒(CsMP)提供了2011年悲剧的纳米级化学指纹。在离FDNPP约10公里以内的三个CsMP(3.79–780 Bq)上测定U,Cs,Ba,Rb,K和Ca同位素比,以确定CsMP的起源和形成机理。除了结晶铁硅藻土,CsFeSi2O6··nH2O外,CsMPs还包括SiO2玻璃基质中的Zn-Fe氧化物纳米颗粒(高达约30wt%的Cs和〜1%wt%的U主要与Zn–Fe-氧化物)。两个CsMP中的 235 U / 238 U值分别为0.030(±0.005)和0.029(±0.003),与浓缩核燃料的值一致。该值高于ORIGEN编码估计的平均燃耗,但低于未辐照的燃料,这表明U会从具有不同燃耗水平的熔融燃料中不均匀挥发,然后吸附到Zn-Fe-氧化物上。纳米尺度的质构和同位素分析提供了熔化期间燃料中发生的化学反应的部分记录。而且,CsMPs是可释放形式的释放放射性核素的重要运输媒介。

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