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Salt, concentration

Fig. XIV-2. Dielectric relaxation spectrum of a water-in-oil emulsion containing water in triglyceride with a salt concentration of 5 wt % at a temperamre of 25°C. The squares are experimental points and the lines are fits to Eq. XIV-4. (From Ref. 9.)... Fig. XIV-2. Dielectric relaxation spectrum of a water-in-oil emulsion containing water in triglyceride with a salt concentration of 5 wt % at a temperamre of 25°C. The squares are experimental points and the lines are fits to Eq. XIV-4. (From Ref. 9.)...
Figure Bl.20.8. DLVO-type forces measured between two silica glass surfaces in aqueous solutions of NaCl at various concentrations. The inset shows the same data in the short-range regime up to D = 10 mn. The repulsive deviation at short range (<2 nm) is due to a monotonic solvation force, which seems not to depend on the salt concentration. Oscillatory surface forces are not observed. With pemiission from [73]. Figure Bl.20.8. DLVO-type forces measured between two silica glass surfaces in aqueous solutions of NaCl at various concentrations. The inset shows the same data in the short-range regime up to D = 10 mn. The repulsive deviation at short range (<2 nm) is due to a monotonic solvation force, which seems not to depend on the salt concentration. Oscillatory surface forces are not observed. With pemiission from [73].
Figure Bl.20.9. Schematic representation of DLVO-type forces measured between two mica surfaces in aqueous solutions of KNO3 or KCl at various concentrations. The inset reveals the existence of oscillatory and monotonic structural forces, of which the latter clearly depend on the salt concentration. Reproduced with pennission from [94]. Figure Bl.20.9. Schematic representation of DLVO-type forces measured between two mica surfaces in aqueous solutions of KNO3 or KCl at various concentrations. The inset reveals the existence of oscillatory and monotonic structural forces, of which the latter clearly depend on the salt concentration. Reproduced with pennission from [94].
In equation (C2.6.14) it can be seen that tire required salt concentration depends strongly on tire valency of tire ions... [Pg.2682]

For a more complete understanding of colloid stability, we need to address the kinetics of aggregation. The theory discussed here was developed to describe coagulation of charged colloids, but it does apply to other cases as well. First, we consider the case of so-called rapid coagulation, which means that two particles will aggregate as soon as they meet (at high salt concentration, for instance). This was considered by von Smoluchowski 1561 here we follow [39, 57]. [Pg.2683]

A combination of equation (C2.6.13), equation (C2.6.14), equation (C2.6.15), equation (C2.6.16), equation (C2.6.17), equation (C2.6.18) and equation (C2.6.19) tlien allows us to estimate how low the electrolyte concentration needs to be to provide kinetic stability for a desired lengtli of time. This tlieory successfully accounts for a number of observations on slowly aggregating systems, but two discrepancies are found (see, for instance, [33]). First, tire observed dependence of stability ratio on salt concentration tends to be much weaker tlian predicted. Second, tire variation of tire stability ratio witli particle size is not reproduced experimentally. Recently, however, it was reported that for model particles witli a low surface charge, where tire DL VO tlieory is expected to hold, tire aggregation kinetics do agree witli tire tlieoretical predictions (see [60], and references tlierein). [Pg.2684]

Porschke D and Obst A 1991 An electric field jump apparatus with ns time resolution for electro-optical measurements at physiological salt concentrations Rev. Sc/. Instnim. 62 818-20... [Pg.2969]

The hydration shell is formed with the increasing of the water content of the sample and the NA transforms from the unordered to A- and then to B form, in the case of DNA and DNA-like polynucleotides and salt concentrations similar to in vivo conditions. The reverse process, dehydration of NA, results in the reverse conformational transitions but they take place at the values of relative humidity (r.h.) less than the forward direction [12]. Thus, there is a conformational hysteresis over the hydration-dehydration loop. The adsorption isotherms of the NAs, i.e. the plots of the number of the adsorbed water molecules versus the r.h. of the sample at constant temperature, also demonstrate the hysteresis phenomena [13]. The hysteresis is i( producible and its value does not decrease for at least a week. [Pg.117]

Hydrophobic Interaction Chromatography. Hydrophobic interactions of solutes with a stationary phase result in thek adsorption on neutral or mildly hydrophobic stationary phases. The solutes are adsorbed at a high salt concentration, and then desorbed in order of increasing surface hydrophobicity, in a decreasing kosmotrope gradient. This characteristic follows the order of the lyotropic series for the anions ... [Pg.55]

The correct viscose age or ripeness for spinning varies according to the type of fiber being made. Ripeness can be assessed by estabHshing the salt concentration necessary to just coagulate the viscose dope. The preferred test uses sodium chloride (salt figure) although ammonium chloride is the basis of the alternative method (Hottenroth number). [Pg.347]

The viscosity of sodium algiaate solutioas is slightly depressed by the additioa of moaovaleat salts. As is frequeatly the case with polyelectrolytes, the polymer ia solutioa coatracts as the ionic strength of the solution is increased. The maximum viscosity effect is obtained at about 0.1 N salt concentration. [Pg.432]

The deposition of molten Na2S04 ia gas turbiaes is beheved to be related to the reaction between the residual sulfur ia fuel and sodium which may be contained either ia the fuel or the intake air. The sodium ia the air is normally present as an aerosol of sea salt. Salt concentrations of over 0.01 ppm ia the intake air may be necessary to initiate hot corrosion. [Pg.116]

If the hides were not deshed before curing, the soaked hides are usually deshed and trimmed at this time. If the hides are not to be trimmed or deshed, they are drained and washed to decrease the salt concentration, drained, and the dmm refilled with cold water. [Pg.83]

The salt flux, across a reverse osmosis membrane can be described by equation 5 where is a constant and and < 2 the salt concentration differences across the membrane. [Pg.81]

Although the principal appHcation of reverse osmosis membranes is still desalination of brackish water or seawater to provide drinking water, a significant market is production of ultrapure water. Such water is used in steam boilers or in the electronics industry, where huge amounts of extremely pure water with a total salt concentration significantly below 1 ppm are required to wash siUcon wafers. [Pg.81]

Tannins occur in many plants and are separated by extraction. At present, only quebracho extract is used as a mud thinner in significant quantity in the United States. Quebracho is an acidic material and performs best at high pH. It is an excellent thinner for lime-treated and cement-contaminated muds. However, it is not effective at high salt concentrations. Sulfomethylated tannin products are functional over a wide range of pH and salinity and have either been treated with chromium for good thermal stabiUty (58) or are chrome free. Concentrations of tannin additives are ca 1.5—18 kg/m (0.5—6 lb/bbl). [Pg.180]

A variety of methods have been devised to stabilize shales. The most successful method uses an oil or synthetic mud that avoids direct contact between the shale and the emulsified water. However, preventing direct contact does not prevent water uptake by the shale, because the organic phase forms a semipermeable membrane on the surface of the wellbore between the emulsified water in the mud and the water in the shale. Depending on the activity of the water, it can be drawn into the shale (activity lower in the shale) or into the mud (activity higher in the shale) (95—97). This osmotic effect is favorable when water is drawn out of the shale thus the aqueous phase of the oil or synthetic mud is maintained at a low water activity by a dding a salt, either sodium chloride or more commonly, calcium chloride. The salt concentration is carried somewhat above the concentration required to balance the water activity in the shale to ensure water movement into the mud. [Pg.182]

Addition of a salt can transform the shale by cation exchange to a less sensitive form of clay, or reduce the osmotic swelling effect by reducing the water activity in the mud below that which occurs in the shale. These effects depend on the salt concentration and the nature of the cation. Salts containing sodium, potassium, calcium, magnesium, and ammonium ions ate used to varying degrees. [Pg.182]

Refractive Index. The effect of mol wt (1400-4000) on the refractive index (RI) increment of PPG in ben2ene has been measured (167). The RI increments of polyglycols containing aUphatic ether moieties are negative drj/dc (mL/g) = —0.055. A plot of RI vs 1/Af is linear and approaches the value for PO itself (109). The RI, density, and viscosity of PPG—salt complexes, which maybe useful as polymer electrolytes in batteries and fuel cells have been measured (168). The variation of RI with temperature and salt concentration was measured for complexes formed with PPG and some sodium and lithium salts. Generally, the RI decreases with temperature, with the rate of change increasing as the concentration increases. [Pg.354]


See other pages where Salt, concentration is mentioned: [Pg.512]    [Pg.1740]    [Pg.2681]    [Pg.2681]    [Pg.582]    [Pg.47]    [Pg.48]    [Pg.48]    [Pg.56]    [Pg.150]    [Pg.140]    [Pg.144]    [Pg.503]    [Pg.44]    [Pg.33]    [Pg.54]    [Pg.384]    [Pg.386]    [Pg.510]    [Pg.301]    [Pg.302]    [Pg.302]    [Pg.302]    [Pg.207]    [Pg.181]    [Pg.340]    [Pg.354]    [Pg.548]    [Pg.155]    [Pg.479]    [Pg.489]    [Pg.490]   
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Activity coefficients concentrated, mixed salt solutions

Activity coefficients high salt concentration

Adsorption trends with increasing salt concentration

Aqueous salt concentration

Association process salt concentration

At varying salt concentrations

Bile salts Critical Micellar Concentration

Capacitance salt concentration dependence

Concentrated salt solution, proton

Concentrated salt solution, proton dissociation

Concentrated salt solutions

Concentrated salt solutions chemistry

Concentrated, Mixed-Salt Solutions

Concentration molal salt

Concentration of salt solutions

Critical salt concentration

Debye screening lengths salt concentration

Electrophoresis at High Salt Concentration

Eluent salt concentrations

Feeds, salt concentration

Herring salt concentration

High salt concentrations

Immobilization salt concentration

Inert Salts concentration effect

Ionization salt concentration

Magnesium salt concentrations, effect

Micelle Formation and Critical Micellar Concentration (CMC) of Bile Salts

Molar salt concentration

Molten salts equilibrium concentrations

Multilayer salt concentration change

Phase transition temperatures salt concentration

Reverse osmosis concentrated salt solution

Salt Concentration Change

Salt aerosol concentration

Salt concentration Raman band intensity

Salt concentration and temperature

Salt concentration bending behavior

Salt concentration dependence

Salt concentration effect

Salt concentration, influence

Salt concentration, interfacial potential

Salt concentration, polyelectrolyte adsorption

Salt concentrations dehydrogenase

Salt concentrations force distance curves

Salt concentrations spacings, interlayer

Salt concentrations swelling

Salt concentrations temperatures

Salt concentrations, polyelectrolyte dynamics

Salt, concentration dopant

Salt: concentration, maximum allowable

Salts reducing concentration

Salts, concentration IPECs

Sea salt concentrations

Sea-salt aerosol concentration

Spacings salt concentration

Stability impact salt concentration

Temperature-salt concentration phase diagram

The effect of salt concentration

Total salt concentration, determination

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