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Salty solutions

After the discovery of the remarkable acceleration of some Diels Alder reactions performed in water, a number of polar non-aqueous solvents and their salty solutions were investigated as reaction medium. This revolutionized the concept that the Diels-Alder reaction is quite insensitive to the effect of the medium and emphasized that a careful choice of the solvent is crucial for the success of the reaction. The polarity of the reaction medium is an important variable which also provides some insights into the mechanism of the reaction. If the reaction rate increases by using a polar medium, this means that the transition state probably has polar character, while the absence of a solvent effect is generally related to an uncharged transition state. [Pg.268]

Potential for salty solutions with a high ionic strength. [Pg.262]

In the above media the hydrolysis of bacterial cell walls has been studied between -1-20° and — 30°C. The rate constants lie on a straight line in the Arrhenius plot [logio k = /(1/T)]. Activation energies are 16.9 kcal mol in 40% methanol, and 20 kcal mol" in 50% MPD. The velocity in salty solutions is much more sensitive to salt action (inhibition) than to temperature. In the presence of 7 M NH4NO3, the rate factor it/ H20 9 X 10", and the calculated activation energy is =5.3 kcal mol". ... [Pg.260]

The major ions constitute about 99.8% of the mass of solutes dissolved in seawater. Sodium and chloride alone account for 86%. Thus, seawater is a very salty solution. Early oceanographers invented the term salinity to refer to the mass of dissolved salts in a given mass of seawater. The mathematical form of this theoretical definition is ... [Pg.45]

The interest in knowing the permeability of the membranes for a salty solution is to predict the fluxes which could be obtained for a real brackish water (total salinity near 6gL 1) without fouling. This parameter is not given by the membrane suppliers. [Pg.68]

In the Fig. 7, we have reported the flux as function of the transmembrane pressure (AP) for a NaCI solution at a concentration of 10-1molL-1 (6gL 1) which is typical of a synthetic brackish water. The linearity observed suggests that this salty solution follows the Kedem-Katchalscky model (i.e. Spiegler-Ke-dem model, with pressure and osmotic linear gradients). For linear gradients, equation (1) amounts to... [Pg.68]

Oxygen reacts with hydrogen in a ratio of one to two, as does sulfur, selenium, and tellurium. It is this chemical reactivity, the ability of elements to join chemically into compounds, that is responsible for transformation of the elements of the cosmos into the materials of Earth and ultimately the materials of life. Although we have to put off our detailed discussion of the complex molecules of life until we have a firmer foundation, we already have enough information to discuss two of the most important chemicals of life and decidedly life s necessary precursors salt and water. The first life formed in the salty oceans, as evidenced by the salty solutions of our cells, and is always present in the salty character of our bodies. [Pg.63]

Osmosis is the tendency for solvent to flow into salty solutions to dilute them. Osmosis is responsible for the revival of wilted celery when soaked in pure water water flows into the celery to dilute the salty cells. Osmosis is responsible for pickles pickling water flows out of the pickles in an attempt to dilute the salty brine. How does the taste get into the pickle Osmosis is also striving for equilibrium, and equilibrium situations in chemistry are dynamic. At equilibrium, the flavorful molecules will be redistributed between pickle and brine. Recall the demonstration with the paper towel and the food dye the paper towel was allowed to take on its equilibrium load of water from a puddle, and then food dye was added to the puddle. Because equilibrium is dynamic, some food dye eventually found its way into the towel. At equilibrium there will be more water outside the pickle cell than inside, but the flavoring in the brine will have found its way into the pickle. [Pg.239]

The inorganic chemist investigates the materials made from the other one hundred and some elements on the periodic table, an enormous undertaking. But while these compounds are rich and intricate in their behaviors, they do not form long, interconnected chains like the hydrocarbons do, so their diversity is in their elemental composition. Inorganic materials form the rock and salty solutions of Earth, the planets, and all the materials of the stars. Inorganic chemists devise syntheses for semiconductors, superconductors, alloys, and many other new materials. [Pg.268]

Seawater is certainly a salty solution. Mnety-nlne percent of all salt ions in the sea are sodium, chlorine, sulfate, magnesium, calcium, and potassium. The major gases in the sea are nitrogen, oxygen, carbon dioxide, argon, neon, and heUum. [Pg.88]

Both are salty solutions that protect you from harmful bacteria, keep tissues moist, and help spread nutrients. Bland-tasting saliva, however, is 99 percent water. The remaining one percent is a combination of many ions, including sodium and several proteins. [Pg.88]

The majority of the global lupin production is used by stockfeed manufacturers as a source of protein and fiber for ruminants, pig, and poultry or in aquaculture. Only 4% is currently consumed as human food. Seeds from bitter lupin cultivars are traditionally eaten as Lupini snacks in southern Europe. They are commonly sold in a salty solution in jars and can be eaten with or without the skin. However, since... [Pg.426]

Conventional RO membranes are not suitable because FO differs from RO in having salty solutions on both sides of the membrane. The porous support exposed to the draw solution is subject to fording and internal polarisation from the draw solution. This means that the concentration of salt ions inside the membrane is very diC ferent from the bulk solution, resulting in a loss of osmotic pressure driving force such that conventional RO membranes only achieve <50% of their capability in FO. [Pg.62]

When you dissolve something in water, for example, salt, the solution has slightly different properties than pure water. For example, a salty solution boils at a higher temperature and freezes at a lower temperature than pure water. Physical chemists have established that these changes, from pure solvent to solution, depend on the number of particles of the solute and not so much on the type of solute. The common name for these effects is colligative properties of mixtures and solutions. Outside of a physical chemical laboratory those of us who live in colder climates are well familiar with the phenomenon of freezing point depression or cryoscopy. This is also a physical chemical experiment actively practiced by the fish swimming in arctic seas. [Pg.100]

Figure 9.5 The mechanism of double-diffusive convection in the fingering regime. A/o and Apr are in the opposite direction, and the net density gradient appears to be stable. However, if a small parcel of the warm, salty solution enters the lower section, then because the heat diffuses faster than the salt, the parcel is left with a greater density than the surroimding... Figure 9.5 The mechanism of double-diffusive convection in the fingering regime. A/o and Apr are in the opposite direction, and the net density gradient appears to be stable. However, if a small parcel of the warm, salty solution enters the lower section, then because the heat diffuses faster than the salt, the parcel is left with a greater density than the surroimding...
Figure 9.6 The mechanism of double-diffusive convection in the diffusive regime. The parcel of hot, salty solution that enters the cold, fresh region above loses heat, becoming more dense than the surrounding region. It sinks back to the hot region and regains heat, leading to an oscillatory motion. Figure 9.6 The mechanism of double-diffusive convection in the diffusive regime. The parcel of hot, salty solution that enters the cold, fresh region above loses heat, becoming more dense than the surrounding region. It sinks back to the hot region and regains heat, leading to an oscillatory motion.
Approximately 70% of the Earth s surface is covered with water in the form of salty solutions called oceans or seas. Massive rivers of moving water flow between these oceans. One of these rivers, called the Gulf Stream, is made up of warm surface water from the South Atlantic Ocean. It flows through the North Atlantic past Europe on its way north toward Iceland. As it passes Europe, the water cools significantly, releasing heat that increases the average temperature of European countries by 5-8°C. [Pg.275]

This type of melting converter was later used as a basis for developing a method of vitrification of medium- and HLRAW. The main features of the proposed method combine all three stages of saturated salty solution reprocessing evaporation (concentration), calcination, and vitrification, in one continuous process in a single melting apparatus. [Pg.59]

Figure 10. Principle scheme of SCM TOROS-3k (Pioro and Pioro, 2006) (1) SCM, (II) cyclone, and (111) bubbler, 1 - combustion products, 2 - salty-solution inlet, 3 - lining (melt-lining), 4 - tap-hole, 5 -cooling-water inlet, 6 - gas-oxygen-air burner, 7 - water-cooled flue-gases duct, and 8 - inertial precipitator. Figure 10. Principle scheme of SCM TOROS-3k (Pioro and Pioro, 2006) (1) SCM, (II) cyclone, and (111) bubbler, 1 - combustion products, 2 - salty-solution inlet, 3 - lining (melt-lining), 4 - tap-hole, 5 -cooling-water inlet, 6 - gas-oxygen-air burner, 7 - water-cooled flue-gases duct, and 8 - inertial precipitator.
Desahnation can also be attempted with cycles of washing-and-vacuuming, where it is expected that water spraying will penetrate in the porous material and dissolve the salts, being the salty solution extracted afterwards by the vacuuming (Dragovich and Egan 2011). [Pg.22]

We now give the results of this calculation for the two cases of (a) salt-free solutions and (b) salty solutions. [Pg.61]

The various aspects of the polymer appear only through its diffusion coefficient. In dilute solutions, the diffusion coefficient of the polyelectrolyte in sufficiently salty solutions obeys the Stokes-Einstein law (Section 7.3),... [Pg.249]


See other pages where Salty solutions is mentioned: [Pg.160]    [Pg.747]    [Pg.260]    [Pg.115]    [Pg.68]    [Pg.236]    [Pg.88]    [Pg.220]    [Pg.897]    [Pg.23]    [Pg.59]    [Pg.59]    [Pg.101]    [Pg.114]    [Pg.131]    [Pg.248]   
See also in sourсe #XX -- [ Pg.240 ]




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