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Hansen scale

Distribution of U-Th-Ra in weathering profiles. The first U-Th studies (Pliler and Adams 1962 Rosholt et al. 1966 Hansen and Stout 1968) generally showed a U loss relative to Th at the base of the profiles, and an enrichment in the uppermost horizons and/or in some accumulation layers. The development of weathering studies, however, point out that this situation is not to be generalized and that reverse trends can be observed even at the scale of a single toposequence (Fig. 11). [Pg.544]

A solution to this problem (Hansen and Ottino, 1996a) reveals that the cluster size distribution is bimodal, as expected, with c(x,t) for large x dependent upon the initial conditions (Fig. 35a). The distribution thus does not approach a self-similar form and the scaling results just given are not valid for this problem. This is a result of the non-homogeneous relative rate of breakup. [Pg.176]

Fig. 36. The spatial variation of agglomerate sizes in simulations of erosion in the journal bearing flow. Initially there are 10000 agglomerates consisting of 400-500 aggregates. The grey scale represents the number of aggregates in the agglomerates, (a) Poorly mixed flow after four periods, (b) Well-mixed flow after one period (Hansen, el al. 1998). Fig. 36. The spatial variation of agglomerate sizes in simulations of erosion in the journal bearing flow. Initially there are 10000 agglomerates consisting of 400-500 aggregates. The grey scale represents the number of aggregates in the agglomerates, (a) Poorly mixed flow after four periods, (b) Well-mixed flow after one period (Hansen, el al. 1998).
It should be noted that the predictions for the number average cluster size and polydispersity agree with analytical results for K(x, y) = 1, x + y, and xy. Furthermore, the short-time form of number average size in Eq. (81) matches the form of s(t) predicted by the scaling ansatz. Computational simulations (Hansen and Ottino, 1996b) also verify these predictions (Fig. 38). [Pg.185]

Fig. 39. (a) The growth of average cluster size for clusters with a constant capture radius in various 2D flows, (b) Variation of polydispersity with average cluster size, (c) Scaled distribution of the cluster sizes at different times. The regular flow is the journal bearing flow with only the inner cylinder rotating. One time unit is equivalent to the total displacement of the boundaries equal to the circumference of the outer cylinder (Hansen and Ottino, 1996b). [Pg.188]

Table 4. MZA Intraclass correlations for the Holland General Occupational Themes for the Hansen Brief Scales, the SCII Full-Length Scales and for factor measures based on two instruments... Table 4. MZA Intraclass correlations for the Holland General Occupational Themes for the Hansen Brief Scales, the SCII Full-Length Scales and for factor measures based on two instruments...
Scale Hansen brief scales SCII full- length scales Factor scales... [Pg.126]

Hansen, J. C. (1982). Hansen combined form scales for the SII. In Minneapolis University of Minnesota Center for Interest Measurement Research. [Pg.138]

S. Helveg, C. Lopez-Cartes, J. Sehested, P. Hansen, B. Clausen, J. Rostrup-Nielsen, F. Abild-Pedersen, and J. Norskov, Atomic-scale imaging of carbon nanofibre growtti. Nature 427,426-429 (2004). [Pg.179]

The oscillator strengths obtained for the different transitions studied in the present work with the RQDO methodology, and the use of the two forms of the transition operator, the standard one, and that corrected for core-valence polarization, are collected in Tables 1 to 8, where other data, from several theoretical and experimental sources, have been included for comparative purposes. The former comprise the large-scale configuration interaction performed with the use of the CIVS computer package [19] by Hibbert and Hansen [20] The configuration interaction (Cl) procedure of... [Pg.281]

The reliable experimental information on the absolute scale and thermal vibrations of beryllium metal made it possible to analyze the effect of the model on the least-squares scale factor, and test for a possible expansion of the 1 s core electron shell. The 0.03 A y-ray structure factors were found to be 0.7% lower than the LH data, when the scale factor from a high-order refinement (sin 6/X) > 0.65 A l) is applied. Larsen and Hansen (1984) conclude that because of the delocalization of the valence electrons, it is doubtful that diffraction data from a metallic substance can be determined reliably by high-order refinement, even with very high sin 0/X cut-off values. This conclusion, while valid for the lighter main-group metals, may not fully apply to metals of the transition elements, which have much heavier cores and show more directional bonding. [Pg.259]

A K-refinement of the 0.12 A y-ray data reproduces the absolute scale poorly when the neutron UtJ thermal parameter values are used (Hansen et al. 1987). The discrepancy can be removed by introduction of a core-tc-parameter, which refines t0 Kcore = 0.988 (2), corresponding to a 1.2% linear expansion. This is supported by a similar result obtained with the LH X-ray data, and related to the scale factor discrepancy noted above. Hansen, Schneider, Yellon, and Pearson (1987), conclude that without independent knowledge of either the scale or the thermal parameters, good agreement with experiment can be achieved, but the resulting scale factor may be in error by as much as 2.5%. [Pg.259]

Though the core expansion leads to the appropriate fit, it may not be the proper explanation for the scale factor discrepancy. Hansen et al. (1987) note that the expansion of the core would lead to a decrease of 7.5 eV in the kinetic energy of the core electrons, at variance with the HF band structure calculations of Dovesi et al. (1982), which show the decrease to be only about 1.5 eV. An alternative interpretation by von Barth and Pedroza (1985) is based on the condition of orthogonality of the core and valence wave functions. The orthogonality requirement introduces a core-like cusp in the s-like valence states, but not in the p-states. Because of the promotion of electrons from s - p in Be metal, the high-order form factor for the crystal must be lower than that for the free atom. It is this effect that can be mimicked by the apparent core expansion. [Pg.259]

The parameters Pim , Pcore, and k can be refined within a least square procedure, together with positional and thermal parameters of a normal refinement to obtain a crystal structure. In the Hansen and Coppens model, the valence shell is allowed to contract or expand and to assume an aspherical form [last term in (11)], as it is conceivable when the atomic density is deformed by the chemical bonding. This is possible by refining the k and k radial scaling parameters and population coefficients Pim of the multipolar expansion. Spherical harmonics functions yim are used to describe the deformation part. Several software packages [68-71] are available for multipolar refinement of the electron density and some of them [68, 70, 72] also compute properties from the refined multipolar coefficients. [Pg.55]

Fig. 6. Calculated ATR spectra (angle of incidence 45°) for a monolayer adsorbate (thickness tZ3 = 3 A) on a 20-nm-thick metal film in contact with a solvent as a function of the complex refractive index of the metal film. Sohd line parallel polarized light dotted line perpendicular-polarized light. The appropriate complex refractive index n2 is given at the top of each spectrum. The vertical bars indicate the scale for the absorbance, which is different for each spectrum. Parameters ni = 4.01 (Ge), n4 = 1.4 (organic solvent), rfs = 3 A, He = 1.6, S = 280000cm , Vo = 2000cm , y = 60cm . The parameters correspond to adsorbed CO. The calculations were performed by using the formalism proposed by Hansen (76), and the results are given in terms of absorbance A = —logio(7 /7 o), where 77 is the reflectivity of the system Ge/Pt/ adsorbate/solvent and Rg is the reflectivity of the system Ge/Pt/solvent (7S). Fig. 6. Calculated ATR spectra (angle of incidence 45°) for a monolayer adsorbate (thickness tZ3 = 3 A) on a 20-nm-thick metal film in contact with a solvent as a function of the complex refractive index of the metal film. Sohd line parallel polarized light dotted line perpendicular-polarized light. The appropriate complex refractive index n2 is given at the top of each spectrum. The vertical bars indicate the scale for the absorbance, which is different for each spectrum. Parameters ni = 4.01 (Ge), n4 = 1.4 (organic solvent), rfs = 3 A, He = 1.6, S = 280000cm , Vo = 2000cm , y = 60cm . The parameters correspond to adsorbed CO. The calculations were performed by using the formalism proposed by Hansen (76), and the results are given in terms of absorbance A = —logio(7 /7 o), where 77 is the reflectivity of the system Ge/Pt/ adsorbate/solvent and Rg is the reflectivity of the system Ge/Pt/solvent (7S).
Payne Ak, Shuler ML, Brodelius P (1987) In Lydersen BK (ed) Large scale cell culture technology. Hansen Publishers, New York, p 193... [Pg.181]

Hansen PL, Helveg S, Datye A. Atomic-scale imaging of supported metal nanocluster catalysts in the working state. J Catal. 2006 50 77. [Pg.326]

Hansen PJ, Bjprnsen PK, Hansen BW (1997) Zooplankton grazing and growth scaling within the 2-2,000-pm body size range. Limnol Oceanogr 42 687-704 Hay ME, Fenical W (1988) Marine plant-herbivore interactions the ecology of chemical defense. Annu Rev Ecol Syst 19 111-145... [Pg.169]

Lihme, A., and Bendix Hansen, M. (1997). Protein A mimetic for large scale monoclonal antibody purification. Biotechnol. Lab. 15, 30-31. [Pg.631]

The PDT that is a central feature of this book dates from this period (Widom, 1963 Jackson and Klein, 1964), as does the related but separately developed scaled-particle theory (Reiss et al, 1959). Both the PDT and scaled-particle approaches have been somewhat bypassed as features of molecular theory, in contrast to their evident utility in simulation and engineering applications. Scaled-particle theories have been helpful in the development of sophisticated solution models (Ashbaugh and Pratt, 2004). Yet the scaled-particle results have been almost orthogonal to pedagogical presentations of the theory of liquids. This may be due to the specialization of the presentations of scaled-particle theory (Barrat and Hansen, 2003). [Pg.3]

The category of simple liquids is sometimes used to establish the complementary category of complex liquids (Barrat and Hansen, 2003). Another and a broad view of complex liquids is that they are colloid, polymer, and liquid crystalline solutions featuring a wide range of spatial length scales - sometimes called soft matter (de Gennes, 1992). Planting ourselves at an atomic spatial resolution, the models analyzed for those complex liquids are typically less detailed and less realistic on an atomic scale than models of atomic liquids. [Pg.4]


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See also in sourсe #XX -- [ Pg.68 ]




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