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Kobayashi, Taishi*; Teshima, Takeshi*; Wang, P.*; Sasaki, Takayuki*; Kitamura, Akira
no journal, ,
We focused on the complexation of U(IV) and U(VI) with isosaccharinic acid (ISA) and measured U(IV) and U(VI) solubility in the presence of ISA. The solubility dependences on hydrogen ion concentration (pHc) and ISA concentration revealed the dominant U(IV) and U(VI) ISA complexes and determined their formation constants. Furthermore, the solubility of Zr(IV), as an analogous of An(IV), in the presence of organic acids with different number of hydroxyl groups were investigated to elucidate the strong complexation ability of ISA.
Sugiura, Yuki; Ishidera, Takamitsu; Suyama, Tadahiro*; Okazaki, Mitsuhiro*; Hamamoto, Takafumi*; Ishida, Keisuke*; Tachi, Yukio
no journal, ,
Iwatsuki, Teruki; Ishii, Eiichi
no journal, ,
The paper reviews the applicable knowledge of the migration properties in deep underground gained by R&D in Mizunami and Horonobe URL. Summing up the major migration path, it is necessary to consider the fracture continuity / connectivity of hundreds of meters in granite of Mizunami area, while several hundred meters in the shallow part of sedimentary rock and of tens m scale in the deep part of Horonobe. On the other hand, it was also demonstrated that analogue elements are practically immobile in rock masses and closed galleries.
Ozaki, Yusuke; Iwatsuki, Teruki; Onoe, Hironori
no journal, ,
In this study, we evaluate the effect of shotcrete on the geo-environment after closure of drift. The shotcrete is known to be dissolved into water and change the groundwater chemistry. The detail of chemical process of dissolution of shotcrete is analyzed with the in-situ groundwater collected during GREET experiment in MIU. In addition, reactive transportation simulation is performed to predict the movement of high pH groundwater affected by dissolution of shotcrete. Our simulation results show that the movement of high pH water is slow owing to the diffusive condition after closure of drift under our simulation condition.
Kimuro, Shingo; Terashima, Motoki; Tachi, Yukio; Kitatsuji, Yoshihiro; Miyakawa, Kazuya; Akiyama, Daisuke*; Sato, Nobuaki*; Kirishima, Akira*
no journal, ,
Humic acid is confirmed to be present even in deep underground where radioactive wastes are planned to be disposed. Although the characteristic properties and reaction mechanism of humic acid are strongly affected by its origin, the reaction enthalpy and entropy for groundwater humic acid complexation are only estimated values obtained from the equilibrium constants at different temperature despite these thermodynamic quantities is necessary for the discussion of reaction thermodynamics. In this study, the thermodynamic quantities of the complexation of deep groundwater humic acid at Horonobe, Hokkaido, Japan with copper (II) and uranyl (VI) ion were determined by the combination of the potentiometry and calorimetry to cultivate a better understanding of the reaction mechanism. By the comparison of thermodynamic quantities with typical humic acid and simple organic acid, the characteristic reaction mechanism of Horonobe humic acid was revealed. In addition, thermodynamic equilibrium calculations based on the determined thermodynamic quantities were performed for the discussion of the impact of humic acid complexation and the origin of humic acid in the migration of radionuclide.
Moroi, Yuriko*; Kirishima, Akira*; Akiyama, Daisuke*; Sato, Nobuaki*; Kitamura, Akira; Kimuro, Shingo
no journal, ,
Development of spent nuclear fuel direct disposal system is one of important options in Japan to maintain flexibility of the back-end strategy of nuclear fuel cycle. Other countries like Sweden and Finland advance in research and development of the direct disposal system. However, it is known that some groundwater in Japan contains higher concentration of carbonate ion than that in Sweden or Finland. Therefore, the effect of carbonate ion on the dissolution rate of UO has to be discussed to evaluate feasibility of the direct disposal system in Japan.
Sasamoto, Hiroshi; Arthur, R. C.*; Alt-Epping, P.*; Tachi, Yukio
no journal, ,
The present study performed an interpretation of natural tracers (non or weakly sorption elements) profiles of groundwater observed in the boreholes drilled from the surface around the Horonobe Underground Laboratory based on the transport processes of advection and diffusion. In the interpretation, due to several uncertainty ranges for transport parameters in initial and boundary conditions, sensitivity analyses considering the relevant model parameters defined uncertainty limits were also conducted to evaluate the plausible parameter sets and conditions to be compatible with observations.
Fukatsu, Yuta; Ito, Tsuyoshi*; Tachi, Yukio; Ishida, Keisuke*; Martin, A.*
no journal, ,
Chen, Y.; Sawaguchi, Takuma
no journal, ,
Sorption of boron in compacted Na-montmorillonite was studied for a better understanding of the boron migration behavior. Boron adsorption at various pH and ionic strength conditions was investigated by batch studies. Sorption distribution ratio value (K [m/kg]) was found to be at the order of magnitude of -3. At fixed pH, sorption can be described using Freundlich isotherm expressions. Boron sorption generally increased with pH. Above about pH 8, however sorption decreased. It was assumed that adsorption was via ligand exchange with aluminol groups at clay surfaces. Both charges of adsorbent and adsorbate were taken into account to explain the pH effects.
Martin, A.*; Fukatsu, Yuta; Tachi, Yukio; Ishida, Keisuke*; Muuri, E.*; Siitari-Kauppi, M.*; Havlov, V.*; Vokal, A.*
no journal, ,
Takeda, Masaki; Ishii, Eiichi; Ono, Hirokazu; Tachi, Yukio; Ito, Tsuyoshi*; Nemoto, Kazuaki*
no journal, ,
Tachi, Yukio; Takeda, Masaki; Ono, Hirokazu; Ito, Tsuyoshi*; Sato, Tomofumi*; Nemoto, Kazuaki*
no journal, ,
Ochs, M.*; Dolder, F.*; Tachi, Yukio
no journal, ,
Niizato, Tadafumi; Sasaki, Yoshito; Ito, Satomi; Mitachi, Katsuaki*; Watanabe, Takayoshi
no journal, ,
Kurikami, Hiroshi; Malins, A.; Niizato, Tadafumi; Iijima, Kazuki; Tsukada, Hirofumi*
no journal, ,
This study examined the evolution of reversibly sorbed Cs in forest soil using a vertical transport model considering kinetic sorption. The simulated distributions and physicochemical forms of Cs were consistent with measurements, indicating the modelling approach was reasonable. The results suggest that Cs concentrations in wild animals are somewhat linked with the concentration of reversibly sorbed Cs in forest soil.
Meier, R.; Kitagaki, Toru; Kozai, Naofumi; Fellhauer, D.*; Kobayashi, Taishi*; Onuki, Toshihiko
no journal, ,
Liu, J.; Dotsuta, Yuma; Kitagaki, Toru; Kozai, Naofumi; Yamaji, Keiko*; Onuki, Toshihiko
no journal, ,
Fuel debris was formed in severe accident in nuclear power plant. After the confirmation of microorganisms in water in damaged plant, it is necessary to consider the element migration of fuel debris. Here, some widespread bacteria were applied. By cultivation with simulant fuel debris, the migration mechanism was estimated.
Havlov, V.*; Zuna, M.*; Brzda, L.*; Rosendorf, T.*; Sammaljrvi, J.*; Nenonen, V.*; Siitari-Kauppi, M.*; Sasao, Eiji; Gvodk, L.*
no journal, ,
Anion exclusion is a process that has been widely observed mainly with concern to clay materials. However, this process has also been observed in some types of crystalline rock. Because anion exclusion exerts the impact on migration in the most constricted parts of nanometre-scale pores, this study focused on H, Cl and I diffusion together with the characterisation of the rock pore structure of magmatic and metamorphic rocks. Both the anionic species exhibited lower diffusion coefficients than that of H, thus indicating anionic exclusion mainly in the metamorphic rocks studied. The De values for the anions in the metamorphic rocks differed from those in the magmatic rocks by around one order of magnitude. The difference between the De values for magmatic and metamorphic rocks is clearly supported by pore structure visualisation by autoradiography. Preliminary results showed decreasing accessible porosity for anionic species rather than decreasing pore diffusion coefficients.
Kozai, Naofumi; Suzuki, Shinichi; Sakamoto, Fuminori; Onuki, Toshihiko
no journal, ,
A fraction of radiocesium (Cs) released by the Fukushima Daiichi Nuclear Power Plant accident was accumulated in sewage sludge ash (SSA). It was previously reported that more than 80% of Cs is fixed in iron oxides of SSA and approximately 10% of Cs is tightly fixed in unidentified amorphous silicon oxides of SSA. This study reports that silicon in paper flowing in sewage and that in organic flocculant added to sewage at sewage treatment plants are origin of the silicon in SSA. Next, to contribute to developing measures for SSA disposal, we prepared geopolymer and cement solidified bodies containing SSA and evaluated their characteristics. We report a high barrier performance of geopolymer solidified bodies.
Yamaguchi, Akiko; Kuribara, Yuichi; Okumura, Masahiko; Takahashi, Yoshio*
no journal, ,
no abstracts in English