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Co, Ni, and 
Co and the influence of the 
orbitalAjayi, S.*; Tripathi, V.*; Rubino, E.*; Bhattacharya, S.*; Baby, L. T.*; Lubna, R. S.*; Benetti, C.*; Wibisono, C.*; Wheeler, M. B.*; Tabor, S. L.*; et al.
Physical Review C, 109(1), p.014305_1 - 014305_21, 2024/01
Times Cited Count：1 Percentile：26.14(Physics, Nuclear)no abstracts in English
NiBhattacharya, S.*; Tripathi, V.*; Rubino, E.*; Ajayi, S.*; Baby, L. T.*; Benetti, C.*; Lubna, R. S.*; Tabor, S. L.*; D
ring, J.*; Utsuno, Yutaka; et al.
Physical Review C, 107(5), p.054311_1 - 054311_17, 2023/05
Times Cited Count：5 Percentile：61.23(Physics, Nuclear)no abstracts in English
Ghobadi, A. F.*; Letteri, R.*; Parelkar, S. S.*; Zhao, Y.; Chan-Seng, D.*; Emrick, T.*; Jayaraman, A.*
Biomacromolecules, 17(2), p.546 - 557, 2016/02
Times Cited Count：20 Percentile：60.57(Biochemistry & Molecular Biology)
AV1934, a classic alkaliphile isolated from human feces in 1934Attie, O.*; Jayaprakash, A.*; Shah, H.*; Paulsen, I. T.*; Morino, Masato*; Takahashi, Yuka*; Narumi, Issey*; Sachidanandam, R.*; Sato, Katsuya; Ito, Masahiro*; et al.
Genome Announcements (Internet), 2(6), p.e01175-14_1 - e01175-14_2, 2014/11
identification of the metastable phase during solidification from the undercooled YFeO
melt by fast X-ray diffractometry at 250 HzNagashio, Kosuke*; Kuribayashi, Kazuhiko*; Vijaya Kumar, M. S.*; Niwata, Kenji*; Hibiya, Taketoshi*; Mizuno, Akitoshi*; Watanabe, Masahito*; Katayama, Yoshinori
Applied Physics Letters, 89(24), p.241923_1 - 241923_3, 2006/12
Times Cited Count：23 Percentile：61.01(Physics, Applied)A time-resolved X-ray diffraction (XRD) experiment at 250 Hz using a synchrotron radiation source was carried out during the containerless solidification of ReFeO (Re=Y and Lu) in order to identify the metastable phase 
. The metastable phase solidified primarily from the undercooled YFeO melt finally transformed to the stable orthorhombic YFeO phase during the short period of recalescence (
0.035 s). Although the metastable phase could not be detected in the as-solidified sample by the powder XRD, the successfully obtained diffraction pattern of the metastable phase in the YFeO system was consistent with that of the metastable hexagonal LuFeO phase.
Okuno, Kiyoshi; R.Vieira*; D.Bessette*; B.Stepanov*; R.Jayakumar*; N.Martovetsky*; Tsuji, Hiroshi; Ando, Toshinari; Isono, Takaaki; E.Salpietro*; et al.
Proc. of 15th Int. Conf. on Magnet Technology (MT-15), p.365 - 368, 1997/00
no abstracts in English
Shimamoto, Susumi; Tsuji, Hiroshi; Ando, Toshinari; J.Jayakumar*; J.Minervini*; R.Thome*; Okuno, Kiyoshi; N.Mitchell*
Proc. of 16th Int. Cryogenic Engineering Conf. /Int. Cryogenic Materials Conf., 0, p.763 - 766, 1996/00
no abstracts in English
center in QuartzTanaka, Kiriha*; Muto, Jun*; Takahashi, Miki*; Jayawickrama, E.*; Sasaki, Osamu*; Oka, Toshitaka; Nagahama, Hiroyuki*
no journal, ,
A fault dating using electron spin resonance (ESR) is a developing direct method to estimate the age of the last fault movement. This method hypothesizes that natural radiation-induced ESR intensity, which is proportional to the concentration of charges trapped in defects accumulated in the interseismic period, is completely reset due to fracture, stress, and frictional heating by a seismic fault slip. The incomplete zeroing can result in age overestimation, hence, the understanding of its detailed conditions and mechanism is required. We have performed high-velocity friction experiments under various normal stresses to investigate the possibility for the signal zeroing by seismic fault slips at various depths. We infer that the degrees of grain fracture and frictional heating associated with the seismic fault slip originating from fault heterogeneity yield the complicated zeroing mechanism of the E center.
Tanaka, Kiriha*; Muto, Jun*; Takahashi, Miki*; Jayawickrama, E. G.*; Sasaki, Osamu*; Oka, Toshitaka; Nagahama, Hiroyuki*
no journal, ,
A fault dating using electron spin resonance (ESR) is a developing direct method to estimate the age of the last fault movement. This method hypothesizes that natural radiation-induced ESR intensity, which is proportional to the concentration of charges trapped in defects accumulated in the interseismic period, is completely reset due to fracture, stress, and frictional heating by a seismic fault slip. We have performed high-velocity friction experiments under various normal stresses to investigate the possibility for the signal zeroing by seismic fault slips at various depths. We infer that the degrees of grain fracture and frictional heating associated with the seismic fault slip originating from fault heterogeneity yield the complicated zeroing mechanism of the ESR signal.
