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Pax

Sarid D, Pax P, Yi L, Howells S, Gallagher M, Chen T, Elings V and Booek D 1992 Improved atomio foroe miorosoope using a laser diode interferometer Rev. Sc/. Instrum. 63 3905... [Pg.1724]

Material Diameter X length, m Initial moisture, % dry basis Steam pressure. Pax 10 Agitator speed, r/min Batch dry weight, kg Final moisture, % dry basis Pa X 10 Time, h Evaporation, kg/(h-m")... [Pg.1214]

Wilson, D.S., et al. Crystal structure of a paired (PAX) class cooperative homeodomain dimer on DNA. Cell 82 709-719, 1995. [Pg.173]

Verh., abbrev. (Verhalten) behavior (Ver-haltnis) proportion, ratio, verhaften, v.t. arrest, apprehend, verhagera, v.i. become lean or thin, — ver-hagert, pax. lean, thin, poor, verhaken, v.t, r. hook together, hook on interlock. [Pg.481]

FIGURE 32.9 Cross-section of a typical mn-flat tire— Michelin PAX system. [Pg.928]

Luciano JS. PAX of mind for pathway researchers. Drug Discov Today 2005 10 937-42. [Pg.162]

AMX, this is possible, because there are three nonselective relaxation-rate values for three unknown py values (pam. Pax, Pmx)- For a system in which y > 3 proton spins, this analysis cannot be unambiguously applied, because there are j(j — )/2 values of py to be determined from j measured R (ns) values. However, under favorable circumstances (see Section IV), depending on the relative disposition of the proton spins in the molecular frame, some Py values may be disregarded. This affords a good estimate of the appropriate Py values, and, hence, information about molecular geometry and conformation. [Pg.132]

A correlation exists between the flux of particles collected by sediment traps and the ( Paxs/ °Thxs) of these particles (Kumar et al. 1995). In pelagic regions, particulate material settling through the deep sea is almost entirely of biogenic origin. A... [Pg.510]

Much of the geographic variability in sedimentary ( Paxs/ °Thxs) observed in modern sediments may be explained by variability in the composition of biogenic particles arising from variability in the structure of the planktonic ecosystem. This can be inferred from the composition-dependence of F(Th/Pa) (Fig. 8), and is shown explicitly by the relationship between sediment trap ( Paxs/ °Thxs) and the opal/calcite ratio of the trapped particles (Fig. 9). Sediment trap ( Paxs/ °Thxs) also exhibits a positive relationship with the mass flux of particles, but the correlation is poorer than that with particle composition (Fig. 9). Indeed, the relationship between particulate ( Paxs/ °Thxs)... [Pg.513]

Figure 9. A log-log plot of the annual average ( Paxs/ °Thxs) as a function of sediment trap particle composition, and as a function of total mass flux. Note the importance of particle composition on the ( Paxs/ °Thxs) of trapped material, with a high opal fraction leading to higher ratios. Note also the poor relationship between ( Paxs/ °Thxs) and mass flux. This data was compiled by Chase et al. (in press-b) and includes data from that study, as well as from Lao et al. (1993), Scholten et al. (2001), and Yu et al. (2001a). Figure 9. A log-log plot of the annual average ( Paxs/ °Thxs) as a function of sediment trap particle composition, and as a function of total mass flux. Note the importance of particle composition on the ( Paxs/ °Thxs) of trapped material, with a high opal fraction leading to higher ratios. Note also the poor relationship between ( Paxs/ °Thxs) and mass flux. This data was compiled by Chase et al. (in press-b) and includes data from that study, as well as from Lao et al. (1993), Scholten et al. (2001), and Yu et al. (2001a).

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See also in sourсe #XX -- [ Pg.109 ]

See also in sourсe #XX -- [ Pg.377 ]

See also in sourсe #XX -- [ Pg.328 ]




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