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Educación Química, vol. 08, núm. 3 - Coordinación de Actualización ...

Educación Química, vol. 08, núm. 3 - Coordinación de Actualización ...

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PROFESORES AL DÍA<br />

a) Form a uniform emulsion using the method of fractional<br />

centrifugation.<br />

b) Determine the radius of the particles with a microscope.<br />

c) Use a very small sample of emulsion, and analyze it<br />

in a microscope, Figure 5. Varying the distance of the objective<br />

lens one can count (by taking instantaneous pictures) the<br />

number <strong>de</strong>nsity as a function of height by just consi<strong>de</strong>ring<br />

particles in focus. In other words, neglect the particle out of<br />

focus.<br />

The best value that Perrin (19<strong>08</strong>) obtained for Avogadro’s<br />

number was:<br />

N 0 = (6.5 ± 0.6) × 10 23<br />

Figure 5. Diagram representing Perrin’s experimental setting. M is a microscope<br />

and s is a sample of emulsion.<br />

F osm = 2s<br />

3 W ∆ n<br />

On the other hand, the weight of the droplets need to be<br />

corrected for the ‘‘push’’ that buoyancy exerts on them.<br />

Calling ρ drop and ρ water the <strong>de</strong>nsities of the droplets and the<br />

solvent, and using formulas from elementary physics, we find<br />

the correct gravitational force to be<br />

F grav = ns ∆hv drop (ρ drop − ρ water ) g<br />

where v drop is the <strong>vol</strong>ume of the droplet and g is the constant<br />

gravitational acceleration.<br />

At equilibrium<br />

F osm = F grav<br />

so one gets<br />

2<br />

3 W ∆n<br />

n = ∆h 4 3 πr3 (ρ drop − ρ water ) g<br />

integrating last equation from (h 0 , n 0 ) to (h, n) one finds<br />

2.303 W log n 0<br />

n = 2 π r3 h (ρ drop − ρ water ) g (11)<br />

for spherical droplets of radius r.<br />

When one substitutes in Eq. (11) the kinetic energy of<br />

a monoatomic gas, 2 RT<br />

, a calculation of Avogadro’s constant<br />

3 N 0<br />

N 0 is possible. Notice that the experimentally difficult quantities<br />

to <strong>de</strong>termine in Eq. (11) are the number <strong>de</strong>nsities n 0 and n.<br />

What Perrin did to <strong>de</strong>termine number <strong>de</strong>nsities<br />

Perrin (19<strong>08</strong>, 1914) and his stu<strong>de</strong>nts measured the <strong>de</strong>nsity<br />

using a procedure that we summarize as follows<br />

Conclusions<br />

We have analyzed a phenomenon which has a fundamental<br />

connection with the microscopic world of atoms and molecules.<br />

The key point of the paper comes in our discussion about<br />

the <strong>de</strong>termination of Avogadro’s number by Perrin. Something<br />

really relevant to notice is the almost ‘‘symbiotic’’<br />

relation that theoretical thinking has with the experimental<br />

world. For example, Perrin used the kinetic theory of heat to<br />

measure N 0 .<br />

We end up this section making a calculation of N 0 using<br />

constants from three different sources. We evaluate<br />

(12)<br />

for the diffusion of atoms of Argon in water when t is equal<br />

to one second. The diffusion coefficient at 298 K is (Li<strong>de</strong>,<br />

1991)<br />

−5<br />

cm2<br />

D = 2.00 × 10<br />

s<br />

The viscosity of water at 298 K is (Noggle, 1989)<br />

η waterr = 8.937 mp<br />

We take the atomic radius of Ar from Oxtoby’s book (Oxtoby<br />

et al., 1990)<br />

r = 0.97 Å<br />

For an interval of one second, we get using Eq. (9)<br />

and<br />

λ y = 4.472 × 10 −3 cm<br />

N 0 = 15 × 10 23<br />

N<br />

t RT<br />

= ⋅<br />

λ 3πη<br />

r<br />

0 2<br />

y<br />

We obtain the correct or<strong>de</strong>r of magnitu<strong>de</strong> for Avogadro’s<br />

number, but a really bad precision. That is not so tragic<br />

128 <strong>Educación</strong> <strong>Química</strong> 8[3]

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