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P overtones

Floyd, D. H., Geva, A., Bruinsma, S. P., Overton, M. C., Blumer, K.J., and Baranski, T. J. (2003). C5a receptor oligomerization. II. Fluorescence resonance energy transfer studies of a human G protein-coupled receptor expressed in yeast. J. Biol. Chem. 278, 35354-35361. [Pg.435]

Atkins, P., Overton, T., Rourke, J. et al. (2006) Shriver and Atkins Inorganic Chemistry, 4th edn, Oxford University Press. This popular but lengthy general text for advanced students contains some clearly-presented sections on shape and stereochemistry of coordination complexes. [Pg.124]

Atkins P, Overton T, Rourke J. Weller M, Armstrong F, Hagerman M. Shriver Atkins Inorganic Chemistry. 5th ed. New York W. H. Freeman and Company 2010. [Pg.508]

Pohl, P. A new model of weak add permeation through membranes revisited does Overton still rule Biophys. J. 2006, 90, L86-88. [Pg.435]

It thus follows that the membrane concentration of typical P-gp substrates for halfmaximum activation of P-gp falls in the range of 1 to 10 mmole drug per mole lipid. This is a much narrower concentration range than that required for the same substances in the aqueous phase 10 8 to 10 3 M. A similar phenomenon has been observed in anesthesia. The membrane concentration of anesthetics required for anesthesia has been found to be 33 mM, independent of the anesthetic applied (Meyer-Overton rule). [Pg.467]

Fig. 1. Model Spectra re-binned to CRIRES Resolution To demonstrate the potential for precise isotopic abundance determination two representative sample absorption spectra, normalized to unity, are shown. They result from a radiative transfer calculation using a hydrostatic MARCS model atmosphere for 3400 K. MARCS stands for Model Atmosphere in a Radiative Convective Scheme the methodology is described in detail e.g. in [1] and references therein. The models are calculated with a spectral bin size corresponding to a Doppler velocity of 1 They are re-binned to the nominal CRIRES resolution (3 p), which even for the slowest rotators is sufficient to resolve absorption lines. The spectral range covers ss of the CRIRES detector-array and has been centered at the band-head of a 29 Si16 O overtone transition at 4029 nm. In both spectra the band-head is clearly visible between the forest of well-separated low- and high-j transitions of the common isotope. The lower spectrum is based on the telluric ratio of the isotopes 28Si/29Si/30Si (92.23 4.67 3.10) whereas the upper spectrum, offset by 0.4 in y-direction, has been calculated for a ratio of 96.00 2.00 2.00. Fig. 1. Model Spectra re-binned to CRIRES Resolution To demonstrate the potential for precise isotopic abundance determination two representative sample absorption spectra, normalized to unity, are shown. They result from a radiative transfer calculation using a hydrostatic MARCS model atmosphere for 3400 K. MARCS stands for Model Atmosphere in a Radiative Convective Scheme the methodology is described in detail e.g. in [1] and references therein. The models are calculated with a spectral bin size corresponding to a Doppler velocity of 1 They are re-binned to the nominal CRIRES resolution (3 p), which even for the slowest rotators is sufficient to resolve absorption lines. The spectral range covers ss of the CRIRES detector-array and has been centered at the band-head of a 29 Si16 O overtone transition at 4029 nm. In both spectra the band-head is clearly visible between the forest of well-separated low- and high-j transitions of the common isotope. The lower spectrum is based on the telluric ratio of the isotopes 28Si/29Si/30Si (92.23 4.67 3.10) whereas the upper spectrum, offset by 0.4 in y-direction, has been calculated for a ratio of 96.00 2.00 2.00.
DAVIDSON, S.B., OVERTON, C., BUNEMAN, P., Challenges in integrating biological data sources, J. Comp. Biol., 1995, 2, 557-572. [Pg.12]

L. England Kretzer and W. A. P. Luck, Band analysis of CH3OH and CH3OD H bond complexes in the first overtone region. J. Mol. Struct. 348, 373 376 (1995). [Pg.47]

P. W. Atkins, T. Overton, J. Rourke, M. Weller, F. Armstrong. Inorganic Chemistry (4th ed.). Oxford University Press Oxford, 2006. [Pg.78]


See other pages where P overtones is mentioned: [Pg.692]    [Pg.9]    [Pg.9]    [Pg.12]    [Pg.29]    [Pg.67]    [Pg.67]    [Pg.276]    [Pg.94]    [Pg.416]    [Pg.339]    [Pg.380]    [Pg.2531]    [Pg.12]    [Pg.692]    [Pg.9]    [Pg.9]    [Pg.12]    [Pg.29]    [Pg.67]    [Pg.67]    [Pg.276]    [Pg.94]    [Pg.416]    [Pg.339]    [Pg.380]    [Pg.2531]    [Pg.12]    [Pg.711]    [Pg.251]    [Pg.507]    [Pg.53]    [Pg.822]    [Pg.280]    [Pg.88]    [Pg.253]    [Pg.101]    [Pg.69]    [Pg.103]    [Pg.36]    [Pg.139]    [Pg.198]    [Pg.142]    [Pg.142]    [Pg.114]    [Pg.627]    [Pg.85]    [Pg.1130]    [Pg.156]   
See also in sourсe #XX -- [ Pg.522 , Pg.529 ]




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