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Oral presentation

An Overview and key results from the long term in situ diffusion project (ltd) at the Grimsel Test Site, Switzerland

Martin, A.*; Fukatsu, Yuta; Tachi, Yukio; Ishida, Keisuke*; Muuri, E.*; Siitari-Kauppi, M.*; Havlov$'a$, V.*; Vokal, A.*

no journal, , 

Oral presentation

Evaluating the mass transport characteristics for fault zone in mudstone at the Horonobe Underground Research Laboratory

Takeda, Masaki; Ishii, Eiichi; Ono, Hirokazu; Tachi, Yukio; Ito, Tsuyoshi*; Nemoto, Kazuaki*

no journal, , 

Oral presentation

In situ diffusion experiment in mudstone at the Horonobe URL; Comparative study between in situ and laboratory tests

Tachi, Yukio; Takeda, Masaki; Ono, Hirokazu; Ito, Tsuyoshi*; Sato, Tomofumi*; Nemoto, Kazuaki*

no journal, , 

Oral presentation

Estimation of sorption reduction by organic ligands in actinide-cement systems

Ochs, M.*; Dolder, F.*; Tachi, Yukio

no journal, , 

Oral presentation

Above- and belowground distribution of radiocesium released from TEPCO' FDNPP accident in the mountainous forest of Fukushima

Niizato, Tadafumi; Sasaki, Yoshito; Ito, Satomi; Mitachi, Katsuaki*; Watanabe, Takayoshi

no journal, , 

Oral presentation

Numerical study on sorption kinetics of radiocesium in forest soil

Kurikami, Hiroshi; Malins, A.; Niizato, Tadafumi; Iijima, Kazuki; Tsukada, Hirofumi*

no journal, , 

This study examined the evolution of reversibly sorbed $$^{137}$$Cs in forest soil using a vertical transport model considering kinetic sorption. The simulated distributions and physicochemical forms of $$^{137}$$Cs were consistent with measurements, indicating the modelling approach was reasonable. The results suggest that $$^{137}$$Cs concentrations in wild animals are somewhat linked with the concentration of reversibly sorbed $$^{137}$$Cs in forest soil.

Oral presentation

Radiocesium in sewage sludge ash

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.

Oral presentation

Fixation of radium by adsorption on clay minerals based on analyses of core samples around Ningyo-toge uranium mine

Yamaguchi, Akiko; Kuribara, Yuichi; Okumura, Masahiko; Takahashi, Yoshio*

no journal, , 

no abstracts in English

Oral presentation

Computational molecular study of predominant organic molecules in forest ecosystems concerning cesium accumulation and transport

Suno, Hiroya; Machida, Masahiko; Dohi, Terumi; Omura, Yoshihito*; Sasaki, Yoshito

no journal, , 

Complexation of biomolecules with radiocesium is known to play an important role in the accumulation and migration of radioactivity on the organic matter in forests. In this work, we identify typical molecules forming a metal complex in the forest organic matter and carry out atomistic analyses by performing quantum mechanical calculations in order to understand the alkali metal cation complexation selectivity of these organic molecules. Among these molecules, of particular interest are norbadione A (C$$_{35}$$H$$_{18}$$O$$_{15}$$), a primary pigment molecule present in mushrooms, oxalic acid (C$$_{2}$$H$$_{2}$$O$$_{4}$$), atranorin (C$$_{19}$$H$$_{18}$$O$$_{8}$$), lecanoric acid (C$$_{16}$$H$$_{14}$$O$$_{7}$$), and usnic acid (C$$_{18}$$H$$_{16}$$O$$_{7}$$), main secondary metabolites in lichens.

Oral presentation

Estimation of fuel debris properties by experimental approach for Fukushima Daiichi NPS

Takano, Masahide; Hirano, Hiroyasu; Yano, Kimihiko; Mitsugi, Takeshi; Washiya, Tadahiro

no journal, , 

Fuel debris was generated in the reactor core in the Fukushima Daiichi Nuclear Power Station (hereafter, 1F) where the severe accident occurred in March, 2011. The information of debris properties is essential in the entire course of the decommissioning work: debris removal process, storage, treatment and disposal. The Japan Atomic Energy Agency (JAEA) is a member of International Research Institute for Nuclear Decommissioning (IRID) who has been conducting studies to estimate the fuel debris properties and to contribute to the decommissioning. In this conference, outline of these research and development in CLADS will be reported.

Oral presentation

Ba AND Sr adsorption on microbially formed Mn oxide; Implication to removal of Ra from U mining wastewater

Tanaka, Kazuya; Kozai, Naofumi; Yamaji, Keiko*; Masuya, Hayato*; Grambow, B.

no journal, , 

Radium-226, a descendant nuclide of $$^{238}$$U, is of serious concern in Ningyo-toge Environmental Engineering Center because its radioactive concentration in mining wastewater exceeds the effluent standard. In this study, we examined Ba and Sr adsorption on biogenic Mn oxide as a preliminary surrogate for Ra adsorption. Both Ba and Sr show the dependence of adsorption on NaCl concentration. Overall, Ba gave an order of magnitude higher Kd values than Sr. Adsorption behavior of Ra would be similar to that of Ba in terms of ionic radius. Barium showed Kd value greater than 10$$^{5}$$ in 10 mM NaCl solution, similar to the ionic strength of the fresh water system in the Ningyo-toge center. Therefore, it is expected that the biogenic Mn can work effectively for removal of Ra from mining wastewater.

Oral presentation

Thermodynamic study of complexation of deep groundwater humic acid by calorimetry

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.

Oral presentation

The Effect of carbonate ion on the dissolution rate of UO$$_{2}$$ pellet

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$$_{2}$$ has to be discussed to evaluate feasibility of the direct disposal system in Japan.

Oral presentation

Sensitivity analyses of natural tracer profiles in sedimentary rocks of the Horonobe URL, 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.

Oral presentation

Modelling analysis on in situ Long Term Diffusion (LTD-II) test at the Grimsel test site

Fukatsu, Yuta; Ito, Tsuyoshi*; Tachi, Yukio; Ishida, Keisuke*; Martin, A.*

no journal, , 

Oral presentation

Boron sorption in Na-montmorillonite

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$$_{d}$$ [m$$^{3}$$/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.

Oral presentation

Addressing radiocesium contamination in Fukushima waste soil through the lens of systematic numerical simulations

Okumura, Masahiko; Kerisit, S.*; Bourg, I.*; Lammers, L.*; Ikeda, Takashi*; Sassi, M.*; Rosso, K.*; Machida, Masahiko

no journal, , 

no abstracts in English

Oral presentation

Upward migration of radiocesium in soil via abiotic process

Sakamoto, Fuminori; Kozai, Naofumi; Guido-Garcia, F.; Kimura, Tatsuki; Grambow, B.

no journal, , 

Soil microorganisms are known to remove a fraction of tightly fixed radiocesium and make it bioavailable. In this study, we attempted to nondestructively recover available radiocesium from soil using microorganisms instead of plants. Microbial activity was tested to form bioavailable radiocesium by the comparing the addition of nutrients and microbicide. Powdered minerals, a water absorbent material, and paper towels were packed in a fine mesh cloth bag (mineral bag) with a size of 50 cm $$times$$ 50 cm. The radiocesium concentration analysis revealed that the surface soil contained approximately 0.3-1.2 Bq/g. The mineral mat was replaced with a new one every two weeks. Two control experiments were established: one with 1 L of nutrient solution to activate microorganisms, and another with sodium hypochlorite aqueous solution to suppress microbial activity. These solutions were added every week. After eight weeks, radiocesium concentrations of the top soil and in the soil core were measured. The accumulative radiocesium concentration in the four mats after eight weeks was within 4.2$$times$$10$$^{2}$$ and 9.0$$times$$10$$^{2}$$ Bq, indicating that the mats indeed absorbed radiocesium from soil. The driving force of upward migration of radiocesium is thought to be soil water flow due to continuous water absorption from soil by the mat and evaporation from itself. These results suggest that cesium upward migration flow along with water is a behavior expected to happen in the environment.

Oral presentation

Clay mineral dissolution by activities of siderophore producing bacteria

Kimura, Tatsuki; Guido-Garcia, F.; Kozai, Naofumi; Zhang, S.*; Yamaji, Keiko*; Yu, Q.*; Grambow, B.

no journal, , 

To understand bacterial ability to dissolve clay minerals, we isolated siderophore-producing bacteria from white clover roots grown in south Osaka, Japan. The ability to produce siderophores was evaluated by CAS plate method. llite, biotite, vermiculite and nontronite were used for testing as clay minerals. Three different bacteria strains were cultivated. Bacteria cells were centrifuged and washed before inoculation tests. Fifty mg dry weight of bacteria were inoculated into 100 mL modified Balland media and 100 mg of each clay mineral added. The suspension was sampled and new media was added. The concentrations of iron, aluminium and silicon were determined by ICP-OES. The presence of organic molecules was determined by SEC-ICP-OES. The peaks of siderophores were determined using the 405 nm absorbance. As a result, siderophore producing bacteria are able to dissolve clay. This suggests that the effect of siderophore on cesium dissolution is an indirectly process.

Oral presentation

$$^{137}$$Cs uptake by lentinula edodes (shiitake) mushrooms

Guido-Garcia, F.; Sakamoto, Fuminori; Kozai, Naofumi; Grambow, B.; Devid, K.*

no journal, , 

The uptake of Cs by fungi has been thought to be similar to the uptake of K due to their chemical similarities. In this research we aimed to evaluate the impact of different concentrations of K in Cs uptake during mushrooms growth, as well as determine the spatial distribution of both within fruit bodies. Lentinula edodes (shiitake) was used as a model organism due to their capacity to produce fruit body. Preliminary results have shown that the concentrations of $$^{137}$$Cs in the obtained mushroom samples from mushroom bed did not show any clear relationship to the different concentrations of added K. Higher concentrations of $$^{137}$$Cs were observed in pileus than in stem, consistently. The results of Cs and K mapping did not show a significant spatial variation. This result suggest that Cs and K are distributed evenly, and that there is no specific or selective binding site for cesium.

32 (Records 1-20 displayed on this page)