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Aqueous solution data

R.K. Freier Aqueous solutions data for inorganic and organic components, Walter de Gruyter, Berlin - New York, 1976. [Pg.376]

Fig. 20 Log EM for interaction of end-groups on polymer chains with average polymerisation degree 3c (i) pyridine-catalysed hydrolysis of the p-nitrophenyl ester group of [27] ( ) and [28] ( ) in aqueous solution (data from Sisido et at., 1976, 1978), (f i) intramolecular charge-transfer complexes of [29] in chloroform ( ) and in ethanol (O). (Data from Sisido et at., 1977 Takagi et at., 1977)... Fig. 20 Log EM for interaction of end-groups on polymer chains with average polymerisation degree 3c (i) pyridine-catalysed hydrolysis of the p-nitrophenyl ester group of [27] ( ) and [28] ( ) in aqueous solution (data from Sisido et at., 1976, 1978), (f i) intramolecular charge-transfer complexes of [29] in chloroform ( ) and in ethanol (O). (Data from Sisido et at., 1977 Takagi et at., 1977)...
Figure 9.3 Current-potential curves for chloride evolution on platinum from aqueous solutions data taken from Ref. 4. Figure 9.3 Current-potential curves for chloride evolution on platinum from aqueous solutions data taken from Ref. 4.
Freier, R. K. "Aqueous Solutions. Data for Inorganic and Organic Compounds" Vol. 1, Walter de Gruyter,... [Pg.486]

Figure 18.7. Relative partial molar enthalpy of serine in aqueous solutions. Data from Ref. 3. Figure 18.7. Relative partial molar enthalpy of serine in aqueous solutions. Data from Ref. 3.
Figure 1-12 Control mechanisms of mineral dissolution in aqueous solutions. Data are from Berner (1978). A straight line is drawn to separate transport control and interface reaction control although there is no theoretical basis for whether the boundary should be linear. Almost without exception, those with transport control lie above a straight line, and those with interface reaction control lie below the line. The only significant departure from the rule is the dissolution of PbS04 (cross in the figure) that lies inside the region for the interface reaction control, but is actually controlled by both interface reaction and mass transport. Figure 1-12 Control mechanisms of mineral dissolution in aqueous solutions. Data are from Berner (1978). A straight line is drawn to separate transport control and interface reaction control although there is no theoretical basis for whether the boundary should be linear. Almost without exception, those with transport control lie above a straight line, and those with interface reaction control lie below the line. The only significant departure from the rule is the dissolution of PbS04 (cross in the figure) that lies inside the region for the interface reaction control, but is actually controlled by both interface reaction and mass transport.
Pseudo First Order Rate Constant, kobs, for the Disappearance of Quadricyclane at Various pH Values in Aqueous Solution (Data from Hill et al., 1997). [Pg.554]

Kxtemivc work has been done on measuring liquid viscosities of the pure Penh. indthcu aqueous solutions Fig-uie 24-9 is a plm of ilw pure ncid viscosities up to I50T. Figures 24-U> 24-11. and 24 12 present aqueous solution data from the Iniwiuttonul CrUiait rj/tfri. ... [Pg.24]

Now that the orders in the gas phase have been obtained we return to the aqueous solution data. [Pg.256]

Figure 5-8. Absorp tion spectra of phycoery thrin from a red alga and phycocyanin from a cyanobacterium in aqueous solutions. [Data are from 6 hEocha (1965) used by permission.]... Figure 5-8. Absorp tion spectra of phycoery thrin from a red alga and phycocyanin from a cyanobacterium in aqueous solutions. [Data are from 6 hEocha (1965) used by permission.]...
See also in sourсe #XX -- [ Pg.2 , Pg.3 , Pg.5 , Pg.75 , Pg.715 ]



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