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Hu, Q.*; Wang, Q. M.*; Zhang, T.*; Zhao, C.*; Iltaf, K. H.*; Liu, S. Q.*; Fukatsu, Yuta
Energy Reports (Internet), 9, p.3661 - 3682, 2023/12
Times Cited Count：4 Percentile：78.27(Energy & Fuels)Soler, J. M.*; Kek
linen, P.*; Pulkkanen, V.-M.*; Moreno, L.*; Iraola, A.*; Trinchero, P.*; Hokr, M.*; 
ha, J.*; Havlov
, V.*; Trpko
ov, D.*; et al.
Nuclear Technology, 209(11), p.1765 - 1784, 2023/11
Times Cited Count：2 Percentile：84.55(Nuclear Science & Technology)Yuan, X.*; Hu, Q.*; Lin, X.*; Zhao, C.*; Wang, Q.*; Tachi, Yukio; Fukatsu, Yuta; Hamamoto, Shoichiro*; Siitari-Kauppi, M.*; Li, X.*
Journal of Hydrology, 618, p.129172_1 - 129172_15, 2023/03
Times Cited Count：0 Percentile：0.00(Engineering, Civil)
Cs NMR chemical shift of clay minerals via machine learning and DFT-GIPAW calculationsOkubo, Takahiro*; Takei, Akihiro*; Tachi, Yukio; Fukatsu, Yuta; Deguchi, Kenzo*; Oki, Shinobu*; Shimizu, Tadashi*
Journal of Physical Chemistry A, 127(4), p.973 - 986, 2023/02
Times Cited Count：1 Percentile：44.88(Chemistry, Physical)The identification of adsorption sites of Cs on clay minerals has been studied in the fields of environmental chemistry. The nuclear magnetic resonance (NMR) experiments allow direct observations of the local structures of adsorbed Cs. The NMR parameters of Cs, derived from solid-state NMR experiments, are sensitive to the local neighboring structures of adsorbed Cs. However, determining the Cs positions from NMR data alone is difficult. This paper describes an approach for identifying the expected atomic positions of Cs adsorbed on clay minerals by combining machine learning (ML) with experimentally observed chemical shifts. A linear ridge regression model for ML is constructed from the smooth overlap of atomic positions descriptor and gauge-including projector augmented wave (GIPAW) ab initio data. The Cs chemical shifts can be instantaneously calculated from the Cs positions on any clay layers using ML. The inverse analysis from the ML model can derive the atomic positions from experimentally observed chemical shifts.
Soler, J. M.*; Keklinen, P.*; Pulkkanen, V.-M.*; Moreno, L.*; Iraola, A.*; Trinchero, P.*; Hokr, M.*; ha, J.*; Havlov, V.*; Trpkoov, D.*; et al.
SKB TR-21-09, 204 Pages, 2021/11
Cs
, and 
I
in compacted Ca-montmorillonite; Experimental and modeling approachesFukatsu, Yuta; Yotsuji, Kenji*; Okubo, Takahiro*; Tachi, Yukio
Applied Clay Science, 211, p.106176_1 - 106176_10, 2021/09
Times Cited Count：10 Percentile：77.49(Chemistry, Physical)Okubo, Takahiro*; Yamazaki, Akio*; Fukatsu, Yuta; Tachi, Yukio
Microporous and Mesoporous Materials, 313, p.110841_1 - 110841_11, 2021/01
Times Cited Count：6 Percentile：40.45(Chemistry, Applied)Pore distributions in water-saturated Ca-montmorillonite were investigated using 
H NMR measurements under various dry densities (0.8 - 1.6 g/cm
) and porewater salinity conditions (deionized water, 0.1 and 1 M CaCl
), at the temperature range of 233 - 303 K. The volume fractions of the interlayer pore including two and three hydrated layers and the non-interlayer pore in compacted Ca-montmorillonite were quantified by NMR relaxometry including 
and 
distribution analysis, and were compared with NMR cryoporometry and X-ray diffractometry. These analysis provided consistent pictures on the pore distributions in compacted Ca-montmorillonite, in contrast to Na-montmorillonite. The main factor affecting the pore distribution in compacted Ca- and Na-montmorillonite is the density, whereas the effect of porewater salinity is relatively smaller. The effect of interlayer cations is also relatively smaller at higher density, although the differences in the pore structures are significant at low density.
Fukatsu, Yuta; Tachi, Yukio
no journal, ,
Hu, Q.*; Wang, Q.*; Oware, P.*; Tachi, Yukio; Fukatsu, Yuta; Ilavsky, J.*; Almer, J.*
no journal, ,
Fukatsu, Yuta; Tachi, Yukio
no journal, ,
Fukatsu, Yuta; Ishidera, Takamitsu; Tachi, Yukio
no journal, ,
no abstracts in English
Tachi, Yukio; Ito, Tsuyoshi*; Fukatsu, Yuta; Akagi, Yosuke*; Sato, Hisao*; Martin, A. J.*
no journal, ,
Hu, Q.*; Wang, Q.*; Zhao, C.*; Zhang, T.*; Tachi, Yukio; Fukatsu, Yuta
no journal, ,
Hu, Q.*; Wang, Q. M.*; Zhao, C.*; Zhang, T.*; Iltaf, H.*; Tachi, Yukio; Fukatsu, Yuta
no journal, ,
Tachi, Yukio; Yotsuji, Kenji*; Fukatsu, Yuta; Sugiura, Yuki; Okubo, Takahiro*
no journal, ,
Understanding the radionuclide migration in clay minerals contained in the buffer material bentonite and rocks is important for the safety assessment of geological disposal of radioactive waste. The pore structures and the electrostatic interactions at the surface, formed by the clay mineral with a layered structure, are key components for developing the radionuclide migration model in clay minerals. In this study, in order to evaluate the influence of alteration from Na- to Ca-montmorillonite on radionuclide migration, the diffusion and sorption model was developed by considering the effects of both pore structures and electrostatic interactions in the compacted montmorillonite.
Hu, Q. H.*; Zhang, T.*; Shen, Y. Q.*; Tachi, Yukio; Fukatsu, Yuta; Borglin, S.*; Chang, C.*; Hampton, J.*
no journal, ,
Murayama, Shota*; Fukatsu, Yuta; Ishidera, Takamitsu; Tachi, Yukio
no journal, ,
no abstracts in English
Fukatsu, Yuta; Hu, Q.*; Tachi, Yukio
no journal, ,
Wang, Q. M.*; Hu, Q.*; Zhao, C.*; Zhang, T.*; Fukatsu, Yuta; Tachi, Yukio
no journal, ,
Fukatsu, Yuta; Akagi, Yosuke*; Sato, Hisao*; Murayama, Shota*; Ishidera, Takamitsu; Tachi, Yukio
no journal, ,
no abstracts in English
