Radiocaesium-bearing microparticles (csMps), which are substantially silicate glass, were formed inside the damaged reactor and released to the environment by the fukushima Dai-ichi nuclear power plant accident in March 2011. The present study reports several valuable findings regarding their composition and structure using advanced microanalytical techniques. X-ray absorption near-edge structure of Fe L 3 -absorption indicated that the oxidation state of the iron dissolved in the glass matrix of the csMps was originally nearly divalent, suggesting that the atmosphere in which the csMps were formed during the accident was considerably reductive. Another major finding is that sodium, which has not been recognised as a constituent element of CsMPs thus far, is among the major elements in the glass matrix. The atomic percent of Na is higher than that of other alkali elements such as K and Cs. Furthermore, halite (NaCl) was found as an inclusion inside a CsMP. The existence of Na in CsMPs infers that seawater injected for cooling might reach the inside of the reactor before or during the formation of the CsMPs. these results are valuable to infer the environment inside the reactor during the accident and the debris materials to be removed during the decommissioning processes.A significant amount of radionuclides, including radiocaesium ( 134 Cs and 137 Cs), were released into the environment by the Fukushima Dai-ichi Nuclear Power Plant (FDNPP) accident in March 2011 1 . Radiation contamination around the nuclear plant is now mainly caused by 137 Cs because of its relatively high amount and long half-life (30.2 years). Most of the released radiocaesium was in a gaseous state at the time of the accident, fell onto the ground, and fixed to mineral grains, such as partially vermiculitised biotite, on the ground 2 . However, part of the radiocaesium was incorporated into micron-sized particles inside the reactor and these particles, termed radiocaesium-bearing microparticles (CsMPs), were emitted from the damaged reactor. In addition to the CsMPs which are also termed Type-A particles in some literature, Type-B particles larger than several dozen microns were found around the nuclear plant 3-5 . Although Type-B particles generally possess higher radioactivity than Type-A particles, specific radioactivity of Type-A is far higher than that of Type-B. Based on the activity ratios of the radiocaesium isotopes ( 134 Cs/ 137 Cs), Type-A and B particles are considered to have been formed in the Unit 2 or 3 and Unit 1 Reactors, respectively, because the activity ratios are varied by fuel burnup differences among the units 6 . All the CsMPs analysed in this study are classified to Type-A particles because they were spherules of a few microns and caesium could be detected using X-ray composition analysis owing to the high specific radioactivity 4 .CsMPs were first identified in aerosol filters collected in Tsukuba, Japan 7 . Microscopic analyses using synchrotron radiation (SR) X-ray and transmission electron microscopy (TEM) show...