Big Chemical Encyclopedia

Chemical substances, components, reactions, process design ...

Articles Figures Tables About

Showing proportion

It can be summarised that both chlorine dioxide and chlorite can be identified in many experiments at several time intervals. The C102 concentration depends on many influences but experiments with both rotating anode cells and parallel flow-through cells show proportional concentration values compared to the volume factor at constant current load on MIO anodes and using different analysis methods. [Pg.181]

Fig. 6-9 Ternary diagram showing proportions of dissolved Si(OH)4, carbonate alkalinity (HCOj + CO3"), and (Q + S04 ) in the Orinoco River and Amazon River basins. Charged species are in equivalents Si(OH)4 is in mole units. The curves in the larger figure are numbered in total cation concentration (mEq/L). Unlike previous figures, symbols represent the total cation concentration interval that includes the sample s concentration. The predominant symbol within each interval corresponds to samples whose concentrations plot within that interval. In the smaller figure, the patterned areas correspond to the predominant source of samples whose concentrations plot within the areas (A) streams that drain cratonic areas (B) streams that originate in mountain belts, but that drain large areas of cratons (C) streams that drain mountain belts with extensive black shales (D) streams that drain mountain belts with extensive carbonate rocks and evaporite deposits. Adapted from Stallard (1988) with the permission of Kluwer Academic Publishers. Fig. 6-9 Ternary diagram showing proportions of dissolved Si(OH)4, carbonate alkalinity (HCOj + CO3"), and (Q + S04 ) in the Orinoco River and Amazon River basins. Charged species are in equivalents Si(OH)4 is in mole units. The curves in the larger figure are numbered in total cation concentration (mEq/L). Unlike previous figures, symbols represent the total cation concentration interval that includes the sample s concentration. The predominant symbol within each interval corresponds to samples whose concentrations plot within that interval. In the smaller figure, the patterned areas correspond to the predominant source of samples whose concentrations plot within the areas (A) streams that drain cratonic areas (B) streams that originate in mountain belts, but that drain large areas of cratons (C) streams that drain mountain belts with extensive black shales (D) streams that drain mountain belts with extensive carbonate rocks and evaporite deposits. Adapted from Stallard (1988) with the permission of Kluwer Academic Publishers.
The lines showing proportion of free to total aluminum should meet in a smooth curve rather than at a 90° angle in the region where both fluoride and hydroxide species are important. A simple procedure for calculating the positions of such a curve has been described by the writer (5) for systems where only two complex species need to be considered at a time. [Pg.112]

Showing proportion of data items modified per call change... [Pg.315]

This model proposed by Kim and Has [73] shows proportional to (dy/dty at the lowest shear rates and proportional to dy/dt at higher shear rates. However it does not seem to be applicable at yet higher shear rates, where reaches a maximum and the sign changes... [Pg.378]

Due to the difference in mass between isotopes of the same element, the reactions and processes occur at different rates. Fractionations as a result of chemical reactions and physical processes (such as evaporation and condensation) produce products that are isoto-pically depleted (containing less of the heavy isotope) than their starting materials. These isotopic fractionations are more evident in lighter elements (e.g., hydrogen and deuterium) because their isotopes show proportionally larger differences in percentage mass than heavier elements (e.g., and C) [1,2,6]. [Pg.343]

Fig. 16.26. Landward distribution of overtopping discharge under impulsive conditions. Curves show proportion of total overtopping discharge which has landed within a particular distance shoreward of seaward crest. Fig. 16.26. Landward distribution of overtopping discharge under impulsive conditions. Curves show proportion of total overtopping discharge which has landed within a particular distance shoreward of seaward crest.
Small and medium-sijsed flat omed cylindrical tanks having capacities of 400 and. 300d bbl or under respectively are extensively used in the petroleun ttdtpM (100, 101). Figure 3.7 of the previous shows proportions for... [Pg.63]

Using linoleic acid siibstrate the absorbance at 234 nm showed proportional increase with the time /Figure 1/ allowing initied. reaction rate determination. [Pg.426]

FIGURE 9 Intensity distribution of light reflected from a perfectly diffuse (Lambertian) surface, showing proportion of reflected light within 5° of each indicated direction. [From Boynton, R. M. (1974). In Handbook of Perception (E. C. Carterette and M. P. Friedman, eds.), Vol. 1. Copyright 1974 Academic Press.]... [Pg.14]


See other pages where Showing proportion is mentioned: [Pg.443]    [Pg.215]    [Pg.190]    [Pg.1046]    [Pg.410]    [Pg.164]    [Pg.320]    [Pg.164]    [Pg.270]    [Pg.152]    [Pg.141]    [Pg.450]    [Pg.269]    [Pg.4721]    [Pg.834]    [Pg.18]   


SEARCH



Showing

© 2024 chempedia.info