Internal structure of cesium-bearing radioactive microparticles released from Fukushima nuclear power plant

被引:81
作者
Yamaguchi, Noriko [1 ]
Mitome, Masanori [2 ]
Kotone, Akiyama-Hasegawa [2 ]
Asano, Maki [1 ,3 ]
Adachi, Kouji [4 ]
Kogure, Toshihiro [5 ]
机构
[1] Natl Inst Agroenvironm Sci, Tsukuba, Ibaraki 3050864, Japan
[2] Natl Inst Mat Sci, Tsukuba, Ibaraki 3050044, Japan
[3] Univ Tsukuba, Grad Sch Life & Environm Sci, Tsukuba, Ibaraki 3058572, Japan
[4] Meteorol Res Inst, Tsukuba, Ibaraki 3050052, Japan
[5] Univ Tokyo, Grad Sch Sci, Bunkyo Ku, Tokyo 1130033, Japan
来源
SCIENTIFIC REPORTS | 2016年 / 6卷
关键词
RADIONUCLIDES; PARTICLES; SOIL; ACCIDENT;
D O I
10.1038/srep20548
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
Microparticles containing substantial amounts of radiocesium collected from the ground in Fukushima were investigated mainly by transmission electron microscopy (TEM) and X-ray microanalysis with scanning TEM (STEM). Particles of around 2 mu m in diameter are basically silicate glass containing Fe and Zn as transition metals, Cs, Rb and K as alkali ions, and Sn as substantial elements. These elements are homogeneously distributed in the glass except Cs which has a concentration gradient, increasing from center to surface. Nano-sized crystallites such as copper-zinc-and molybdenum sulfide, and silver telluride were found inside the microparticles, which probably resulted from the segregation of the silicate and sulfide (telluride) during molten-stage. An alkali-depleted layer of ca. 0.2 mu m thick exists at the outer side of the particle collected from cedar leaves 8 months after the nuclear accident, suggesting gradual leaching of radiocesium from the microparticles in the natural environment.
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页数:6
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