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Handbook of Solvents - George Wypych - ChemTech - Ventech!

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13.1 Solvent effects on chemical reactivity 761<br />

polar solutes (the waters become less ice-like). The increase in H-bond length and angle has<br />

been found to decrease the water heat capacity contribution, while decreases in length and<br />

angle have been found to cause the opposite effect.<br />

Note further that a large heat capacity implies that the enthalpy and entropy are strong<br />

functions <strong>of</strong> temperature, and the free energy vs. temperature is a curved function, increasing<br />

at low temperatures and decreasing at higher temperatures. Hence there will be a temperature<br />

at which the solubility <strong>of</strong> nonpolar in water is a minimum. The low solubility <strong>of</strong><br />

nonpolar species in water at higher temperatures is caused by unfavorable enthalpic interactions,<br />

not unfavorable entropy changes. Some light on these features has been shed by using<br />

a “simple” statistical mechanical MB model <strong>of</strong> water in which the water molecules are represented<br />

as Lennard-Jones disks with hydrogen bonding arms. 113 (the MB model is called<br />

this because <strong>of</strong> the resemblance <strong>of</strong> each model water to the Mercedes-Benz logo.) As an important<br />

result, the insertion <strong>of</strong> a nonpolar solute into cold water causes ordering and<br />

strengthening <strong>of</strong> the H bonds in the first shell, but the reverse applies in hot water. This provides<br />

a physical interpretation for the crossover temperatures T H and T S, where the enthalpy<br />

and entropy <strong>of</strong> transfer equal zero. T H is the temperature at which H-bond reorganizations<br />

are balanced by solute-solvent interactions. On the other hand, T S is the temperature at<br />

which the relative H-bonding strengths and numbers <strong>of</strong> shell and bulk molecules reverse<br />

roles.<br />

Although the large positive free energy <strong>of</strong> mixing <strong>of</strong> hydrocarbons with water is dominated<br />

by entropy at 25°C, it is dominated by enthalpy at higher temperatures (112°C from<br />

Baldwin’s extrapolation for hydrocarbons, or 150°C from the measurements <strong>of</strong> Crovetto for<br />

argon) 113 where the disaffinity <strong>of</strong> oil for water is maximal. Ironically so, where<br />

hydrophobicity is strongest, entropy plays no role. For this reason, models and simulations<br />

<strong>of</strong> solutes that focus on cold water, around or below 25°C, miss much <strong>of</strong> the thermodynamics<br />

<strong>of</strong> the oil/water solvation process. Also, a clathrate-like solvation shell emerged from a<br />

recent computer simulation study <strong>of</strong> the temperature dependence <strong>of</strong> the structural and dynamical<br />

properties <strong>of</strong> dilute O 2 aqueous solutions. 114 In the first hydration shell around O 2,<br />

water-water interactions are stronger and water diffusional and rotational dynamics slower<br />

than in the bulk. This calls to one’s mind an older paper by Hildebrand 115 showing that at<br />

25°C, methane’s diffusion coefficient in water is 40% less than it is in carbon tetrachloride<br />

(D(H 2O) = 1.42x10 -5 cm 2 /s vs D(CCl 4) = 2.89x10 -5 cm 2 /s). Presumably the loose clathrate<br />

water cages serve to inhibit free diffusion <strong>of</strong> the nonpolar solute. From these data it seems<br />

that both the nonpolar solute and the aqueous solvent experience a decrease in entropy upon<br />

dissolving in water. It should also be mentioned in this context that pressure increases the<br />

solubility. The effect <strong>of</strong> pressure on the entropy was examined and it was found that increase<br />

in the pressure causes a reduction <strong>of</strong> orientational correlations, in agreement with the<br />

idea <strong>of</strong> pressure as a “structure breaker” in water. 116 Actually, frozen clathrate hydrates<br />

trapped beneath oceans and arctic permafrost may contain more than 50% <strong>of</strong> the world’s organic<br />

carbon reserves. 117,118 Likewise, the solubility <strong>of</strong> aromatics is increased at high pressure<br />

and temperature, with π bond interactions involved. 119<br />

Only at first glance, the two approaches, the clathrate cage model and the cavity-based<br />

model, looked very different, the former based on the hydrogen bonding <strong>of</strong> water, and the<br />

later on the hard core <strong>of</strong> water. But taken all results together it would appear that both are<br />

just different perspectives on the same physics with different diagnostics reporting consequences<br />

<strong>of</strong> the same shifted balance between H bonds and vdW interactions. Actually, in a

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