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Kayas

Nonose S, Sone Y, Onodera K and Kaya K 1990 Structure and reactivity of bimetallic Co V Clusters J. Phys. C Solid State Phys. 94 2744... [Pg.2401]

Fuke and Kaya [1989] studied the vibrational selectivity of concerted two-proton transfer in 7-azoindole in the excited electronic state... [Pg.97]

JCP4074 K. Fuke, K. Tsukamoto, F. Misaizu, and L. Kaya, J. Chem. Phys. 95,... [Pg.109]

Mishaeva RN, Kuznetsova NP, Samsonov GV, Gudkin LR, Papukova KP, Rozhets-kaya KM (1988) Vysokomol Soedin (A) 30 1707... [Pg.48]

Horiguchi, T., Kojima, M., and Kaya, M. et al. (2002). Tribntyltin and triphenyltin induce spermatogenesis in ovary of female abalone, Haliotis gigantea. Marine Environmental Research 54, 679-684. [Pg.352]

Figure 11. Distribution with depth of U/Th normahzed to the bedroek in two lateritic profiles of the Kaya toposeqnenee, about 300m apart (Burkina Faso) (Deqnineey et al. 2002 submitted). One profile is located downhill (Kaya 5) and the other one at the top of a residual hill (Kaya 1). The laterite consists of an uppermost fermginous hardtop, an intermediate pink clay nnit and a lowest pistachio unit. For Kaya 5 profile, U/Th distribntion shows a relative enrichment of U in the nppermost horizon and depletion in the lower part of the profile. This kind of distribution is quite conunon in weathering profiles bnt is not systematic as illnstrated by the Kaya 1 profile. In the latter, a relative depletion of U is observed in the npper part and a U-enriched level in the intermediate horizon. This lateral difference in U distribution is explained by vertical redistribntion of U from the ferruginons top to the nnderlying horizons, whose intensity is controlled by the evolntion of the iron oxides from the nppermost horizons (Dequincey et al. snbmitted). Figure 11. Distribution with depth of U/Th normahzed to the bedroek in two lateritic profiles of the Kaya toposeqnenee, about 300m apart (Burkina Faso) (Deqnineey et al. 2002 submitted). One profile is located downhill (Kaya 5) and the other one at the top of a residual hill (Kaya 1). The laterite consists of an uppermost fermginous hardtop, an intermediate pink clay nnit and a lowest pistachio unit. For Kaya 5 profile, U/Th distribntion shows a relative enrichment of U in the nppermost horizon and depletion in the lower part of the profile. This kind of distribution is quite conunon in weathering profiles bnt is not systematic as illnstrated by the Kaya 1 profile. In the latter, a relative depletion of U is observed in the npper part and a U-enriched level in the intermediate horizon. This lateral difference in U distribution is explained by vertical redistribntion of U from the ferruginons top to the nnderlying horizons, whose intensity is controlled by the evolntion of the iron oxides from the nppermost horizons (Dequincey et al. snbmitted).
SK Butcher, V Killampalli, H Chahal, E Kaya Alpar, JM Lord. Biochem Soc Trans 31 449-451, 2003. [Pg.959]

Froehlich, J. P., Bamberg, E. et al. Contribution of quaternary protein interactions to the mechanism of energy transduction in Na+/K+-ATPase. In K. Taniguchi and S. Kaya (eds.), Na/K-ATPase and Related ATPases. Amsterdam Elsevier, 2000. [Pg.92]

Demir AS, Sesenoglu O, Aksoy-Cam H, Kaya H, Aydogan K. Tetrahedron Asymmetry 2003 14 1335-1340. [Pg.746]

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See also in sourсe #XX -- [ Pg.77 ]



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