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Cation-water radial

Figure 11. Calculated cation-water radial distribution function ui. center of mass separation R for the dilute aqueous solution of lithium at T = 25°C... Figure 11. Calculated cation-water radial distribution function ui. center of mass separation R for the dilute aqueous solution of lithium at T = 25°C...
We have recently carried out Monte Carlo computer simulation of dilute aqueous solutions of the monatomic cations Li, Na and K and the monatomic anions F and Cl using the KPC-HF functions for the ion-water interaction and the MCY-CI potential for the water-water interaction. The temperature of the systems was taken to be 25° and the density chosen to be commensurate with the partial molar volumes as reported by Millero. - The calculated average quantities are based on from 600- 900K configurations after equilibration of the systems. The calculated ion-water radial distribution functions are given for the dilute aqueous solutions of Li", K" ", Na" ", F and Cl" in Figures 11-15, respectively. [Pg.214]

Figure 15.20. Fixed bed ion exchange vessels and arrangements, (a) Typical design of a water softener, showing bed support, distributor, and effluent collector, (b) Vessel with radial-type distributors and collectors (Illinois Water Treatment Co.), (c) A double-dish underdrain system (Permutit Co.), (d) Some arrangements of vessels for cation and anion exchange. Figure 15.20. Fixed bed ion exchange vessels and arrangements, (a) Typical design of a water softener, showing bed support, distributor, and effluent collector, (b) Vessel with radial-type distributors and collectors (Illinois Water Treatment Co.), (c) A double-dish underdrain system (Permutit Co.), (d) Some arrangements of vessels for cation and anion exchange.
As described in further details in Section 5, we analyze the scans using the software DCDT+ (Philo, 2006), which converts the raw concentration profiles into time derivatives (dc/dt) and fits these values to approximate unbounded solutions of the Lamm equation (Philo, 2000 Stafford, 1994). As the rotor speed (ft)) and the concentration of the macromolecules (c) are known, and the time (t) and the radial concentration distribution [c(x, f)] are obtained from the scans of absorbance profiles, the fitting yields values of s and D. As both parameters are dependent on the solvent viscosity and temperature, they are transformed to standard values with reference to a standard temperature (20 °C) and a standard solvent (water) and reported as 52o,w and /92o,w This standardization allows analysis of the changes in the intrinsic properties of solute molecules with changes in solution condition and is a prerequisite in cation-mediated folding studies of RNA molecules. [Pg.215]

Information on the second coordination shell of water molecules around cations is much poorer than that regarding the first shell [4]. Properties of solvent molecules in this coordination shell are often very similar to those of the bulk, making their investigation extremely difficult. The analysis of radial distribution functions, g(r),... [Pg.155]

Styrene is one of the oldest and most studied monomers. It spontaneously generates free radials upon heating above 100 °C and polymerizes yielding amorphous polystyrene (PS). Styrene can also be polymerized by other mechanisms (anionic, cationic, or Zeigler-Natta) with the aid of chemical initiators. Commercially, over twenty billion pounds of PS are produced annually worldwide. All of this polystyrene is produced via free radical (FR) chemistry, and mostly via continuous solution polymerization processes. The commercial preference for the continuous solution process is due mainly to economic factors. Non-solution polymerization processes (suspension and emulsion) have lower reactor efficiency (product/reactor volume) due to reactor volume occupied by the water which adds to the manufacturing cost. [Pg.69]

Salomon have shown that if Verwey s model of cation solvation is considered (see Fig. 2.11.1), then the orientation of a water molecule at the cation is 52° to the radial direction. If anions lie along this direction, then the difference in ion-dipole energy is fie(l — cos S2°)jR which is the term included in eqn. 2.11.25. By fitting the conventional enthalpies to a least square power series... [Pg.268]

In contrast to the behavior of noble gases, the radial distribution functions of water around the infinitely dilute anion (C/ ) and cations (Na and Lt) exhibit a rather strong re-structuring, Le,y relative to unperturbed water there is a substantial increase in the local water density around the ions due to strong ion-dipole interactions (Figure 13). The presence of an ion induces an increase in the solvent... [Pg.370]

Figure 13. Radial distribution functions for the water-cation and water-anion at infinite dilution at 7 = 1.0 and = 1.5. Figure 13. Radial distribution functions for the water-cation and water-anion at infinite dilution at 7 = 1.0 and = 1.5.
The experimental measurements that provide the hydration number and hydrated radius information are made on lanthanide solutions of moderate concentration with dilFerent counter ions. The data in Rizkalla and Choppin (1991) indicate that hydration numbers and Ln-O distances change slightly with both the nature of the counter ion and the concentration of the salt. It appears likely that composition of the primary coordination sphere of the lanthanide ion does not vary appreciably with the concentration (or identity of the counterion) of the lanthanide salts. However, the reduced water activity that occurs in concentrated salt solutions would suggest that overall hydration numbers will be higher in dilute solutions. Thus the values reported for overall hydration and hydrated radii determined in concentrated aqueous salt solutions probably underestimate the hydration of lanthanide cations in the dilute solutions that are typical of analytical applications. It has been suggested that as many as 40 water molecules may feel the presence of a trivalent lanthanide ion in solution (Choppin 1997). Using Lundqvist s (1981) estimate of 30 for the volume of a water molecule, the radial distance of the lanthanide iQrdration sphere... [Pg.335]

The solvation of cation and electrical double layer structure near clay surface was studied by neutron diffraction methods (156-158). The intaplay between molecular simulations and neutron diffraction techniques also has been also applied to this clay mineral-water-cation interface system. Park and Sposito (112) simulated the total radial distribution function (TRDF) of interlayer water from Na-, Li-, and K-montmorillonite hydrates as a physical quantity from molecular simulations. They obtained TRDF values from Monte Carlo simulations and directly compared with previously obtained H/ D isotopic difference neutron diffraction results (9,10). [Pg.87]


See other pages where Cation-water radial is mentioned: [Pg.433]    [Pg.214]    [Pg.211]    [Pg.312]    [Pg.316]    [Pg.218]    [Pg.100]    [Pg.502]    [Pg.133]    [Pg.454]    [Pg.512]    [Pg.246]    [Pg.164]    [Pg.230]    [Pg.252]    [Pg.438]    [Pg.441]    [Pg.795]    [Pg.197]    [Pg.15]    [Pg.6]    [Pg.673]    [Pg.96]    [Pg.563]    [Pg.1708]    [Pg.22]    [Pg.515]    [Pg.399]    [Pg.85]    [Pg.195]    [Pg.475]    [Pg.35]   
See also in sourсe #XX -- [ Pg.207 , Pg.208 ]




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