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Calculation of concentration

The value of v is important both in equation 7 and for accurate calculation of concentrations in other equations. For simplicity and accuracy, the Peng-Robinson equation of state has been used to calculate v for the model O). This equation expresses the P-V-T relationship as follows ... [Pg.203]

In principle, the calculation of concentrations of species of a complexation equilibrium is no different from any other calculation involving equilibrium constant expressions. In practice, we have to consider multiple equilibria whenever a complex is present. This is because each ligand associates with the complex in a separate process with its own equilibrium expression. For instance, the silver-ammonia equilibrium is composed of two steps ... [Pg.1324]

Chapter 8 presented the last of the computational approaches that I find widely useful in the numerical simulation of environmental properties. The routines of Chapter 8 can be applied to systems of several interacting species in a one-dimensional chain of identical reservoirs, whereas the routines of Chapter 7 are a somewhat more efficient approach to that chain of identical reservoirs that can be used when there is only one species to be considered. Chapter 7 also presented subroutines applicable to a generally useful but simple climate model, an energy balance climate model with seasonal change in temperature. Chapter 6 described the peculiar features of equations for changes in isotope ratios that arise because isotope ratios are ratios and not conserved quantities. Calculations of isotope ratios can be based directly on calculations of concentration, with essentially the same sources and sinks, provided that extra terms are included in the equations for rates of change of isotope ratios. These extra terms were derived in Chapter 6. [Pg.180]

In addition to the expression for the mass and energy fluxes, conservation equations for mass and energy are required to enable the calculation of concentration and temperature profiles. From these profiles the mass and heat transfer rates through the va-pour/gas-liquid interface can subsequently be obtained. The species conservation equations for the liquid and the vapour/gas phase are respectively given by... [Pg.3]

In most biological cases/(C) is nonlinear and analytical integration is difficult or impossible. Numerical integration again allows calculation of concentration at the end of each experiment. Differences between simulated and experimental data are then minimized using, e.g., the least squares criterion. Both experimental approaches are compared in Table 1, especially with respect to their suitability for kinetic screening. [Pg.8]

Desorption efficiencies were determined for each sampling device in our laboratory. Analysis of passive dosimeter samples and calculation of concentrations were done as recommended by each device s manufacturer 07, 8). Charcoal tube samples were analyzed as recommended by NIOSH Sampling and Analysis Method... [Pg.210]

Calculation of concentration of standard stock solution in miligram/mL... [Pg.294]

Table 12 Calculation of concentration using two PLS components for pyrene and case study 1, dataset A. Note that the concentration estimated is mean-centred... Table 12 Calculation of concentration using two PLS components for pyrene and case study 1, dataset A. Note that the concentration estimated is mean-centred...
HPLC analysis was performed with a Beckman system equipped with DA detector module using a RP 18 column. Detection was performed at 280 nm. Calculation of concentrations was based on external standard curves with the corresponding compounds. Each experiment was triplicated. [Pg.106]

Another factor which influences the speed in performing an analysis is calibration of the instrument. Calibration is especially time-consuming in cases where different elements are run on every analysis but even in cases where the same elements are determined time after time, the frequency of instrument calibration required to maintain a desired level of accuracy is an important consideration. Since manual data collection is not feasible in multielement determinations, the ideal system would undoubtedly be computerized. The computer would handle all data collection steps, the construction of calibration curves by mathematical curve-fitting methods, and the calculation of concentrations from these curves. [Pg.29]

Again, we know that equi-molar solutions will contain the same number of moles. That is how we know we can balance equations and trust our calculations of concentrations of solutions. [Pg.229]

Table 5.13 Calculation of concentration estimates for pyrene using two PLS components. Component 1 Component 2 Estimated... Table 5.13 Calculation of concentration estimates for pyrene using two PLS components. Component 1 Component 2 Estimated...
We referred in the last paragraph to the calculation of concentrations of excited species from emission intensity measurements, ft may, however, not always be possible to determine Am directly, and some other method of evaluating A factors may be needed. The A coefficient may be calculated from the B coefficient for the same transition by using the relation... [Pg.16]

Two of the standards directly related to worker health and important in design work are Toxic Hazardous Substances and Occupational Noise Exposure. The first of these two concerns the normal release of toxic and carcinogenic substances, carried via vapors, fumes, dust fibers, or other media. Compliance with the Act requires the designer to make calculations of concentrations and exposure time of plant personnel to toxic substances during normal operation of a process or plant. These releases could emanate from various types of seals and from control-valve packings or other similar sources. Normally, the designer can meet the limits set for exposure to toxic substances by specifying special valves, seals, vapor-recovery systems, and appropriate ventilation systems. [Pg.60]

H2CO3 in recharge water was made from six Rainier Mesa water samples for which reliable pH and HCO3 values were available. In simple silicate rock dissolution, all carbonate species result from reaction of H2CO3 with the rock. Thus, HCO3 + C03 + H2CO3 at any point in the flow path is assumed to be a constant. Calculations of concentrations of these species in the six samples previously mentioned allowed calculation of H2CQ3 initially available for reaction. These data are presented in Table I. The arithmetic mean was used in subsequent calculations. [Pg.777]

It has become customary to classify evaluation methods as "differential" or "integral." These terms stem from a time when practically all experiments were conducted in batch reactors, so that rates had to be found by differentiation of concentration-versus-time data, and the calculation of concentrations from postulated rate equations required integration. The terms do not fit the work-up of data from gradientless reactors such as CSTRs, in which rates and concentrations are related to one another by algebraic equations requiring no calculus, and are therefore avoided here. [Pg.45]


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See also in sourсe #XX -- [ Pg.94 , Pg.96 ]




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