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  • 76.50.Jx  (1)
  • Mercury-thiolate charge-transfer bands  (1)
  • Najas  (1)
  • 1
    Electronic Resource
    Electronic Resource
    Springer
    The European physical journal 350 (1995), S. 311-318 
    ISSN: 1434-601X
    Keywords: 21.10.Ky ; 76.50.Jx ; 76.80.+ y
    Source: Springer Online Journal Archives 1860-2000
    Topics: Physics
    Notes: Abstract We report measurements of nuclear magnetic resonance on oriented nuclei (NMR-ON) on94Tc (Iπ=7+,T 1/2=4.9 h),95Tc (I π=9/2+,T 1/2=20 h) and96Tc (I π=7+,T 1/2=4.3 d) in Fe and on95Tc and96Tc in Ni. In order to elucidate the discrepancies on the hyperfine field of TcFe in the literature, the resonances were measured with high precision as a function of the external magnetic field Bext up to 2.0 T. In addition, TDPAC measurements were performed on99TcFe at T=300 K and 13 K. TheT=0 K hyperfine fields of Tc in Fe and Ni were determined to be −314(3) kG and −51.8(5) kG, respectively. The g-factors of93Tc,94Tc,95Tc,96Tc and99Tc(E=181 keV;I π=5/2+) are redetermined as g(93Tc)=1.405(14), g(94Tc)=0.731(7),g(95Tc)=1.321(13), g(96Tc)=0.727(7), g(99Tc)=1.390(17).
    Type of Medium: Electronic Resource
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  • 2
    ISSN: 1432-1327
    Keywords: Mercury-substituted rubredoxin ; Mercury-thiolate charge-transfer bands ; Cysteine ligation ; Electronic spectroscopy ; Perturbed angular correlation of γ-rays spectroscopy
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Chemistry and Pharmacology
    Notes: Desulfovibrio gigas has been studied by electronic absorption, circular dichroism (CD), magnetic circular dichroism (MCD), and time differential perturbed angular correlation of γ-rays (TDPAC) spectroscopies. The TDPAC spectrum of 199mHg-Rd at pH 8 exhibits a prevailing nuclear quadrupole interaction (NQI) with a precession frequency of ω 1=0.09 Grad/s and an asymmetry parameter η=0, features characteristic of a slightly distorted tetrahedral tetrathiolate metal coordination, i.e, a HgCysS4 center. In addition, three minor populated NQIs have also been detected. They may represent a trigonal HgS3 (ω 1=1.13 Grad/s, η=0.21), a digonal HgS2 (ω 1= 1.34 Grad/s, η=0.20), and a digonal Hg(II) coordination (ω 1=1.58 Grad/s, η=0.18) with unidentified ligands. Since similar studies at pH 2.5 revealed a time-dependent increase of the HgCysS4 population, the low populated sites may represent intermediate Hg(II) complexes formed prior to the generation of the thermodynamically stable structure. The metal-induced absorption envelope of Hg-Rd reveals three distinct transitions with Gaussian-resolved maxima located at 230, 257, and 284 nm, which are paralleled by dichroic features in the corresponding difference CD spectrum of Hg(II)-Rd versus apo-Rd. Based on the optical electronegativity theory of Jørgensen, the lowest energy transition has been attributed to a CysS-Hg(II) charge-transfer excitation. The T d type of metal coordination in Hg-Rd is supported by the presence of an unresolved A-term with a negative lobe at 295 nm in the difference MCD spectrum. These results point to the usefulness of optical and TDPAC spectroscopies for studying Hg(II) sites in other proteins.
    Type of Medium: Electronic Resource
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  • 3
    ISSN: 1573-5117
    Keywords: Fertilizer ; Nutrients ; Soluble Phosphate ; Pond ; Sediment ; Erosion ; Najas ; Charales ; Potamogeton ; Phosphate Transport ; Phosphate Fixation ; Sediment phosphate uptake
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Abstract Two surfaces soils with contrasting physical and chemical characteristics were placed in model ponds to provide a sediment phosphate (P) source. Water samples were obtained weekly or biweekly and analyzed for total, total soluble, and soluble reactive P. Fertilizer P additions which exceeded sediment P absorption capacity occasionally tended to produce significantly higher P concentrations. Smaller P additions had no influence on pond P concentrations and no relationship between pond P concentrations and sediment EPC values was found. Soluble reactive P concentrations in most of the ponds were similar and seldom 〉 5 µg/1. Two mechanisms significantly affected P transport from the sediments. The first were macrophytic plants which provided a large P sink in the water column. The second was fixation of readily soluble P within the sediments. Plant growth within the ponds used 〈 5% of the readily soluble P initially present. Diffusion of P from the sediments did not support large SRP concentrations within the ponds.
    Type of Medium: Electronic Resource
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