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Text anomalies

For the following text, isotopic anomalies always stands for non-linear or non-mass dependent variations linear or mass dependent have the same meaning although mass dependent fractionation may not be strictly linear (Rayleigh). Usually, in the first approach the difference is not essential for description... [Pg.28]

Bostocke, Difference betwene the auncient phisicke... and the latter phisicke, s s. F4, F8. For arguments that Bostocke s text was an anomaly see Debus, English Paracelsians, ch. 2 Kocher, Paracelsian Medicine in England , 465. [Pg.193]

Fig. 2.46 EDPs from the incommensurate structures with [100] zone axis. (a) EDP shows spacing anomaly, (b) EDP shows orientation anomaly. (See text.)... Fig. 2.46 EDPs from the incommensurate structures with [100] zone axis. (a) EDP shows spacing anomaly, (b) EDP shows orientation anomaly. (See text.)...
The transition metals in periods 4 and 5 have the outer configurations of ns2(n — 1 )dl to ns2(n — 1 )dw, but there are some anomalies and the filling of the d shell is not uniform refer to your text. The transition metals in periods 6 and 7 fill the (n — 2)/ oribtals before the (n — 1 )d s are completed. There are many anomalies in the course of filling the/ shell. The lanthanides, period 6, and the actinides, period 7, are displayed separately below the body of the table and are handled by the guidelines outlined. [Pg.118]

Proposed model of genetic and environmental factors contributing to GSH deficit and neurobiological anomalies leading to schizophrenia phenotypes. Evidences are given in the text (O Section 2.5.5)... [Pg.301]

Figure 5 Plot of variations in (which arise from the decay of the extinct nuclide versus time expressed as ppm differences from present-day compositions. An initial Stn/ Sm = 0.007 is assumed (Prinzhofer et al., 1992). If an LREE-depleted mantle (high Sm/Nd) formed within the first 200-300Ma of Earth history, then with the current 5-10 ppm analytical precision, a positive Nd deviation would be expected to be observed in any sample derived from this source. Lunar samples (Nyquist et al, 1995) and martian meteorites (Harper et al., 1995) show clear evidence of Nd variations reflecting very early differentiation on these bodies. Nd anomalies have now been suggested for some 3.7-3.S Ga terrestrial samples from southwest Greenland (Harper and Jacobsen, 1992 Boyet et al, 2002 Caro et al., 2003). Most of the 3.8 Ga gneisses that have been measured do not show these effects and recent re-measurement of the original Harper and Jacobsen sample by Papanastassiou et al. (2003) has not confirmed the original result (see text). The different/curves are for different degrees of depletion (20% and 40%) of... Figure 5 Plot of variations in (which arise from the decay of the extinct nuclide versus time expressed as ppm differences from present-day compositions. An initial Stn/ Sm = 0.007 is assumed (Prinzhofer et al., 1992). If an LREE-depleted mantle (high Sm/Nd) formed within the first 200-300Ma of Earth history, then with the current 5-10 ppm analytical precision, a positive Nd deviation would be expected to be observed in any sample derived from this source. Lunar samples (Nyquist et al, 1995) and martian meteorites (Harper et al., 1995) show clear evidence of Nd variations reflecting very early differentiation on these bodies. Nd anomalies have now been suggested for some 3.7-3.S Ga terrestrial samples from southwest Greenland (Harper and Jacobsen, 1992 Boyet et al, 2002 Caro et al., 2003). Most of the 3.8 Ga gneisses that have been measured do not show these effects and recent re-measurement of the original Harper and Jacobsen sample by Papanastassiou et al. (2003) has not confirmed the original result (see text). The different/curves are for different degrees of depletion (20% and 40%) of...
Figure 4. Sulfur isotope anomalous fractionations (see text) plotted v. age in Ga. Sharp change in magnitude of anomalies at 2.5 Ga is found worldwide in rocks from Australia, Canada, India, and South Africa (29, 30, 31, 32, 33, 34, 35)... Figure 4. Sulfur isotope anomalous fractionations (see text) plotted v. age in Ga. Sharp change in magnitude of anomalies at 2.5 Ga is found worldwide in rocks from Australia, Canada, India, and South Africa (29, 30, 31, 32, 33, 34, 35)...
Fig. 16. Temperature dependence of 4f-derived specific heat, C, and entropy in units of the gas constant, SJR, for (a) CeRu j Gcj and (b) CeCu GCj (Felten et al. 1987). Solid curves in upper parts show Schottky anomalies corresponding to the CF splitting of Ce given in the text. Fig. 16. Temperature dependence of 4f-derived specific heat, C, and entropy in units of the gas constant, SJR, for (a) CeRu j Gcj and (b) CeCu GCj (Felten et al. 1987). Solid curves in upper parts show Schottky anomalies corresponding to the CF splitting of Ce given in the text.
Fig. 6.22. The high field magnetization of neodymium at 4.2 K (after McEwen et al. 1973). The inset shows Johansson s (1971) data with the anomalies discussed in the text. Fig. 6.22. The high field magnetization of neodymium at 4.2 K (after McEwen et al. 1973). The inset shows Johansson s (1971) data with the anomalies discussed in the text.
Fig. 30. DO, like BAO samples, show typical anomalies of their lattice parameters at 6.75, 6.80, 6.90, 6.95 and 6.97. These anomalies seem to be sensitively dependent on the existence of latent structural and electronic transitions. For a discussion see the text. XRD, 7 =300K (a) a-paiameter vs. x. (b) 6-parameter vs. x. Note that only the 6-parameter changes slope at x 6.75 (cf. sect. 5.4.2). (c) Orthorhombicity vs. x. (d) c-parameter vs. x. Note the overlap of the DO data with those of the BAO (dotted line). In the 6.97 >x > 6.75 range, both are appreciably smaller than the CAR data for the c-paiameter (black circles), (e) Unit cell volume vs, x. After data of Conder et al. (1994a, 1999) and Conder and Kaldis (1995). Fig. 30. DO, like BAO samples, show typical anomalies of their lattice parameters at 6.75, 6.80, 6.90, 6.95 and 6.97. These anomalies seem to be sensitively dependent on the existence of latent structural and electronic transitions. For a discussion see the text. XRD, 7 =300K (a) a-paiameter vs. x. (b) 6-parameter vs. x. Note that only the 6-parameter changes slope at x 6.75 (cf. sect. 5.4.2). (c) Orthorhombicity vs. x. (d) c-parameter vs. x. Note the overlap of the DO data with those of the BAO (dotted line). In the 6.97 >x > 6.75 range, both are appreciably smaller than the CAR data for the c-paiameter (black circles), (e) Unit cell volume vs, x. After data of Conder et al. (1994a, 1999) and Conder and Kaldis (1995).
Fig. 42. The Debye-Waller factors vs. T (see Fig. 43. Correlation parameters vs T for the text) for the single scattering (SS) paths. Only the Cul-04 and Cul-04 pairs show clear anomalies... Fig. 42. The Debye-Waller factors vs. T (see Fig. 43. Correlation parameters vs T for the text) for the single scattering (SS) paths. Only the Cul-04 and Cul-04 pairs show clear anomalies...
Fig. 22 Activation energy of segmental motion within glass transition vs temperature plots, illustrating schematically the possible dynamic anomalies in different complex polymer systems (see text) [128,129]. The transition widths are indicated above... Fig. 22 Activation energy of segmental motion within glass transition vs temperature plots, illustrating schematically the possible dynamic anomalies in different complex polymer systems (see text) [128,129]. The transition widths are indicated above...
Band intensities some spectral bands involving electronic transitions have intensities other than those which might be expected in terms of a purely ionic model. This evidence tends to be more speculative than the others listed above and so it has not been discussed earlier in the text. There are four intensity anomalies which may be taken to indicate covalency. [Pg.296]

Fig. 11.23 Left Position kfsDP of the FSDP (in A ) of different partial structure factors of NS2. Right Width Akpsop of the FSDP (in A ). The gray zones correspond to pressure regions of dynamic and rigidity anomalies (see text for details)... Fig. 11.23 Left Position kfsDP of the FSDP (in A ) of different partial structure factors of NS2. Right Width Akpsop of the FSDP (in A ). The gray zones correspond to pressure regions of dynamic and rigidity anomalies (see text for details)...
While there was on occasions some reticence initially on the part of the auditee, there was never a problem at the end of the audit to agree the text of the audit report, in particular the formulation of the audit findings, that is to say, anomalies needing correction, because the points noted were concrete ones, tied back to contractual documents. [Pg.120]

The definition oifugacity can be attributed to the thermodynamics giant G. N. Lewis. Unlike the other concepts we have seen so far in this text, it developed inductively rather than deductively. In fact, fugacity is undoubtedly but one of many ways to get around the mathematical anomalies of the chemical potential however, it is the way that is used in practice, and we will learn about it next. [Pg.392]


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See also in sourсe #XX -- [ Pg.105 ]

See also in sourсe #XX -- [ Pg.105 ]




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