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Handbook of Solvents - George Wypych - ChemTech - Ventech!

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770 Roland Schmid<br />

sequently, there are so many different sets <strong>of</strong> ionic radii and hydration free energies available<br />

that it is very difficult to decide which to prefer.<br />

In a most recent paper, 82 a new table <strong>of</strong> absolute single-ion thermodynamic quantities<br />

<strong>of</strong> hydration at 298 K has been presented, based on conventional enthalpies and entropies<br />

upon implication <strong>of</strong> the thermodynamics <strong>of</strong> water dissociation. From the values <strong>of</strong> Δ hydG*<br />

the Born radii were calculated from<br />

r B (Å) = -695 z 2 /Δ hydG*(kJ) [13.1.30]<br />

as given in Table 13.1.7. This is at first a formal definition whose significance may be tested<br />

in the framework <strong>of</strong> the position <strong>of</strong> the first maximum <strong>of</strong> the radial distribution function<br />

(RDF) measured by solution X-ray and neutron diffraction. 177 However, the procedure is<br />

not unambiguous as is already reflected by the names given to this quantity, viz. (for the<br />

Table 13.1.7. Some radii (Å). Data are from<br />

ref. 82<br />

Atom rB a<br />

raq b<br />

rmetal<br />

Li 1.46 1.50 1.52<br />

Na 1.87 1.87 1.86<br />

K 2.33 2.32 2.27<br />

Rb 2.52 2.48<br />

Cs 2.75 2.58 2.65<br />

Be 1.18 1.06 1.12<br />

Mg 1.53 1.52 1.60<br />

Ca 1.86 1.86 1.97<br />

Sr 2.03 2.02 2.15<br />

Ba 2.24 2.27 2.17<br />

F 1.39 1.29<br />

Cl 1.86 1.85<br />

Br 2.00 2.00<br />

I 2.23 2.30<br />

a From eqn. [13.1.30], b eqns. [13.1.31] and [13.1.32].<br />

case <strong>of</strong> a cation) ion-water 178 or ion-oxygen<br />

distance. The ambiguity <strong>of</strong> the underlying<br />

interpretation resides in the circumstance<br />

that the same value <strong>of</strong> 1.40 Å is assigned in<br />

the literature to the radius <strong>of</strong> the oxide anion,<br />

the water molecule and the vdW radius<br />

<strong>of</strong> the oxygen atom.<br />

It seems that many workers would<br />

tend to equate the distance (d) corresponding<br />

to the first RDF peak with the average<br />

distance between the center <strong>of</strong> the ion and<br />

the centers <strong>of</strong> the nearest water molecules,<br />

d=r ion +r water. Actually, Marcus 179,180 presented<br />

a nice relationship between d, averaged<br />

over diffraction and simulation data,<br />

and the Pauling crystal radius in the form<br />

d=1.38 + 1.102 r p. Notwithstanding this success,<br />

it is preferable to implicate not the water<br />

radius but instead the oxygen radius.<br />

This follows from the close correspondence<br />

between d and the metal-oxygen bond<br />

lengths in crystalline metal hydrates. 82<br />

The gross coincidence <strong>of</strong> the solid and<br />

solution state distances is strong evidence<br />

that the value <strong>of</strong> d measures the distance between<br />

the nuclei <strong>of</strong> the cation ad the oxygen<br />

rather than the center <strong>of</strong> the electron cloud<br />

<strong>of</strong> the whole ligand molecule. Actually, first<br />

RDF peaks for ion solvation in water and in nonaqueous oxygen donor solvents are very<br />

similar despite the different ligand sizes. Examples include methanol, formamide and<br />

dimethyl sulfoxide. 180<br />

Nevertheless, the division <strong>of</strong> d into ion and ligand components is still not unequivocal.<br />

Since the traditional ionic radius is <strong>of</strong>ten considered as a literal measure <strong>of</strong> size, it is usual to

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