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Solution concentration measurement

C12-0024. Prepare a table of the various solution concentration measures. Describe how to convert from each of them to each of the others. [Pg.879]

Empirically determined retardation factors (either partition coefficients or breakthrough curve measurements, which are the change in solute concentration measured over time in laboratory or field experiments) have been widely used because of their inherent simplicity.162 Modeling of specific geochemical partition and transformation processes is not necessary if the retardation factor can be determined empirically. [Pg.835]

First, for the case in which only solute concentration measurements are available, pseudo-experimental data are simulated and used in the parameter estimation scheme. Even with noise-free data, the recovered parameters differ greatly from the true parameters and the uncertainties of the nucleation parameters are large. This indicates that there exists a large set of quite different b and ki, pairs that would lead to very similar solute concentration profiles. The insensitivity of the objective function to the nucleation parameters can be attributed to the fact that the mass of a nucleated particle is almost negligible and the change in the solute concentration is primarily due to seed growth. [Pg.106]

Measurements that can be expressed as a mole/mole ratio, the most basic measurements in chemistry, are typified by processes which react, interact, blend, or replace a described amount of substance A with a described amount of substance B. Included are solution concentration measurements when all solutes are known in a known solvent. Note especially that these measurements are independent of the magnitude of the unit mole. Note also that if these measurements are made by mass or volume determinations, the uncertainties in the corresponding atomic or molecular mass values must be taken into account. [Pg.3]

In the direct design approach, a desired supersaturation profile that falls between the solubility curve and the metastable limit of the system is followed based on feedback control of the concentration measurement. This is in contrast to the traditional first-principles approach, where a desired temperature profile or antisolvent addition rate profile is followed over time such as shown in Fig. 14. For a cooling crystallization, the direct design approach follows a setpoint profile that is solution concentration vs. temperature (or solvent-antisolvent ratio) as opposed to temperature (or addition rate) vs. time. Because the desired crystallizer temperature is determined from an in-situ solution concentration measurement, the batch time is not fixed. [Pg.867]

Fig. 15 shows an example of the direct design approach implemented for the isothermal antisolvent crystallization of acetaminophen (paracetamol) from acetone-water mixture. A constant relative supersaturation (Ac/c ) setpoint profile was followed. The flow rate setpoint of the antisolvent was calculated every minute based on the solution concentration measured using the IR spectra so that a setpoint supersaturation profile was followed. The change in solution concentration and antisolvent flow rate during the batch is shown in Fig. 16. After an initial start-up... Fig. 15 shows an example of the direct design approach implemented for the isothermal antisolvent crystallization of acetaminophen (paracetamol) from acetone-water mixture. A constant relative supersaturation (Ac/c ) setpoint profile was followed. The flow rate setpoint of the antisolvent was calculated every minute based on the solution concentration measured using the IR spectra so that a setpoint supersaturation profile was followed. The change in solution concentration and antisolvent flow rate during the batch is shown in Fig. 16. After an initial start-up...
Thompson, D.R. Kougoulos, E. Jones, A.G. Wood-Kaczmar, M.W. Solute concentration measurement of an 58. important organic compound using ATR-UV spectroscopy. [Pg.871]

Falciai R, Mignani AG, Vannini A (1998) Solution concentration measurements by means of optical fibre long-period gratings. Proc SPIE 3483 95-98... [Pg.174]

We see that the decrease in vapor pressure, AP, is directly proportional to the solute concentration (measured in mole fraction). [Pg.481]

Activities predicted by the D-H equation decrease monotonically with solute concentration. Measured activity coefficients typically decrease at first, but then increase at higher concentrations. This indicates that the simple Coulombic primitive model used by the D-H theory must be inadequate in more concentrated solutions. There have been many theoretical attempts to model the additional interactions that occur at high concentrations—see summaries by Friedman (1962), Pytkowicz (1979), and Helgeson et al. (1981). [Pg.444]

A test of the stability of the extractable contents of a single soil was carried out for EDTA, acetic acid, ammonium acetate and calcium chloride extracts. With the exception of chromium, the EDTA extractable contents were shown to be stable over 3 year intervals within about 10% for the elements Cd, Cu, Fe, Mn, Ni, Pb and Zn [193]. For acetic acid extracts, one-year changes for Cr, Fe, Mn and Zn were poorer than for EDTA, but for Cd, Cu, Ni and Pb the extracts were reasonably stable. For ammonium acetate and calcium chloride extracts, however, the results, apart from Cd and Ni in ammonium acetate, were useless. These failures in ammonium acetate and calcium chloride were probably related to the fact that the solution concentrations measured were too low for reliable determination by the FAAS and ICP-AES methods used. [Pg.184]

HiS levels in pore waters. In these locations, Fe phosphate minerals may control Fe solubility. The combination of laboratory equilibration studies and pore water solute concentration measurements led Martens et al., for example, to conclude that deep pore waters were in equilibrium with vivianite -F63P04 8H2O - in a coastal sediment. Hyacinthe et al. found that iron was sequestered as an Fe(iii) phosphate in low-salinity, estuarine sediments. This ferric phosphate may have been formed in surface sediments (see below) or in the water column. [Pg.451]

In view of the frequent need to make interconversions of composition units it is recommended that, whenever solution concentration measurements are made, the density of the solution at the relevant temperature is also measured and recorded (see section 3.9). [Pg.90]

Solute concentrations measured in mole fractions tend to be very small, which is inconvenient. So we use molalities which, being independent of density and hence of T and P are by far the most convenient measure of concentration. But this means... [Pg.218]

The ultimate test of the comparison between the measurements and the computer predictions is the washing efficiency, i.e. the solute concentration (measured as ppm Na20) in the system underflow. [Pg.467]


See other pages where Solution concentration measurement is mentioned: [Pg.162]    [Pg.2400]    [Pg.863]    [Pg.869]    [Pg.869]    [Pg.114]    [Pg.244]    [Pg.436]    [Pg.837]    [Pg.30]   


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