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Localization basin

A description in terms of local spins, however, raises the question of how to define these localized surrogate spins, where we have to move from one-electron spin operators Sj to multi-electron spin operators Sa that are located at one center and summarize all electronic contributions attributed to this center. This can be solved by the introduction of projection operators Pa (33,113,114,122-124). The projection operators do not alter any property of the molecule but divide it into local basins A. They add up to the identity operator,... [Pg.203]

Finley, P., Krason, J., Geological Evolution and Analysis of Confirmed or Suspected Gas Hydrate Localities Basin Analysis, Formation and Stability of Gas Hydrates in the Middle America Trench, U.S. Department of Energy, DOE/MC/21181-1950, 9 (1986a). [Pg.632]

From a quantitative point of view a localization basin (core or valence) is characterized by its population, i.e. the integrated one-electron density p(r) over the basin (equation 15)... [Pg.69]

According to the local basins, 60-80 % of the total area is nsed for agriculture (maize, wheat, sunflower, soya beans, etc.) and breeding (dncks, cattle, etc.). In this PRB, nitrate and pesticides are widespread in snrface waters. [Pg.438]

Fig. 27. Our conclusive model for filling of Smorbukk. Migration from the western regions, where the Spekk Formation is currently over-mature, must have occurred through the now pressure sealing Smorbukk main fault zone. The low abundance of petroleum inclusions in Smorbukk Sor testify to its late filling from the local basin between Smorbukk and Smorbukk Sor. Fig. 27. Our conclusive model for filling of Smorbukk. Migration from the western regions, where the Spekk Formation is currently over-mature, must have occurred through the now pressure sealing Smorbukk main fault zone. The low abundance of petroleum inclusions in Smorbukk Sor testify to its late filling from the local basin between Smorbukk and Smorbukk Sor.
The same abundance of fluorescent petroleum inclusions in the Halten Vest dry wells as was found in Smorbukk implies, according to our model, that the time during which the presently dry Halten Vest structures actually held oil is roughly similar to the time petroleum has been present in Smorbukk. In contrast the Smorbukk Sor and the 6406/3-1 structures filled during the past 10 Ma from local basins. [Pg.355]

Fig. 10 ELF for porphyrin. In both parts, pmtioiis of ELF = 0.66 iso-surface are shown to highlight different features. The ELF shows the same delocalization features as benzene in Fig. 9. The nitrogen lone pairs show a slightly larger localization basin than NH bonds. NH induces a small interruption in the delocalized ring between N and neighbor C(H) this small interruption disappears in deprotonated porphyrin and in metal-porphyrin... Fig. 10 ELF for porphyrin. In both parts, pmtioiis of ELF = 0.66 iso-surface are shown to highlight different features. The ELF shows the same delocalization features as benzene in Fig. 9. The nitrogen lone pairs show a slightly larger localization basin than NH bonds. NH induces a small interruption in the delocalized ring between N and neighbor C(H) this small interruption disappears in deprotonated porphyrin and in metal-porphyrin...
In future, framing detailed investigations of disparity and taxonomic richness, such as that of Klug et al. (2005), in a phylogenetic context within the Germanic and Sephardic provinces may represent an ideal way to further investigate this question at the level of local basins. [Pg.198]


See other pages where Localization basin is mentioned: [Pg.315]    [Pg.144]    [Pg.14]    [Pg.242]    [Pg.304]    [Pg.70]    [Pg.249]    [Pg.118]    [Pg.140]    [Pg.318]    [Pg.189]    [Pg.189]    [Pg.182]    [Pg.343]    [Pg.377]    [Pg.265]    [Pg.462]    [Pg.1619]   
See also in sourсe #XX -- [ Pg.187 ]




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