Everything in this section so far has ignored the boundary between two phases, as if each molecule were unequivocally part of one phase or the other. In fact, the boundary is a kind of transition zone where molecules are in an environment that differs from both phases. Since the boundary zone is only a few molecules thick, its contribution to the total free energy of a system is very often negligible. One important exception, however, is the first tiny droplets or bubbles or grains that form as a material begins to undergo a phase transformation. The formation of these initial specks of a new phase is called nucleation. In this problem we will consider the nucleation of water droplets in a cloud. The surface forming the boundary between any two given phases generally has a fixed thickness, regardless of its area. The additional Gibbs free energy of this surface is therefore directly proportional to its area; the constant of proportionality is called the surface tension, α

σGboundaryA

ff you have a blob of liquid in equilibrium with its vapor and you wish to stretch it into a shape that has the same volume but more surface area, then u is the minimum work that you must perform, per unit of additional area, at fixed temperature and pressure. For water at 20°C,σ=0.073J/m2

(a) Consider a spherical droplet of water containing N1 molecules, surrounded by N-N1molecules of water vapor. Neglecting surface tension for the moment, write down a formula for the total Gibbs free energy of this system in terms of N,N1, and the chemical potentials of the liquid and vapor. Rewrite N1in terms of V1, the volume per molecule in the liquid, and T, the radius of the droplet.

(b) Now add to your expression for Ga term to represent the surface tension, written in terms of Tand u.

(c) Sketch a qualitative graph of G vs. T for both signs of µg - µ1, and discuss the implications. For which sign of μg-μ1does there exist a nonzero equilibrium radius? Is this equilibrium stable?

(d) Let TCrepresent the critical equilibrium radius that you discussed qualitatively in part (c). Find an expression for TCin terms of μg-μ. Then rewrite the difference of chemical potentials in terms of the relative humidity (see Problem 5.42), assuming that the vapor behaves as an ideal gas. (The relative humidity is defined in terms of equilibrium of a vapor with a flat surface, or with an infinitely large droplet.) Sketch a graph of the critical radius as a function of the relative humidity, including numbers. Discuss the implications. In particular, explain why it is unlikely that the clouds in our atmosphere would form by spontaneous aggregation of water molecules into droplets. (In fact, cloud droplets form around nuclei of dust particles and other foreign material, when the relative humidity is close to 100%.)

Short Answer

Expert verified

Result is:

(a). The formula for total Gibbs free energy of this system isG=4πr33vlμl-μg+Nμg.

(b). The improved formula is G=4πr33vlμl-μg+Nμg+4πσr2.

(c). The qualitative graph betweenGvs.Tis

(c)Gr=4πrc2vlμl-μg+8πσrc=0

(d)h=e2σvl/kTrc

Step by step solution

01

part(a) Step 1: Given information

we have been given thatGextra=σA

02

part(a) Step 2:Simplify

The gibbs energy is given by:

G=Nlμl+N-Nlμg

the volume of droplet

Vr=4πr33

vl=4πr33NlNl=4πr33vl

03

part(b) Step 1: Given information

we have been given that replaceAwith2πr2

04

part(b) Step 2:Simplify

After solving we get,

G=4πr33vlμl-μg+Nμg+4πσr2
05

part(c) Step 1: Given information

we have been given thatGμl-μgr3+r2

06

part(c) Step 2:Simplify

it is clear that

μl>μg,Gr3+r2+C

μl<μg,G-r3+r2+C

07

part(d) Step 1: Given information

we have been given thatGr=4πrc2vlμl-μg+8πσrc=0

08

part(d) Step 2:Simplify

The change in gibbs energy is:

dG=-SdT+VdP+μdN

at constant temperatur and number

dG=VdP

hence,dμg-μl=vg-vldP

solve for h to get:

h=e2σvl/kTrc

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Most popular questions from this chapter

Use the data at the back of this book to calculate the slope of the calcite-aragonite phase boundary (at 298 K). You located one point on this phase boundary in Problem 5.28; use this information to sketch the phase diagram of calcium carbonate.

Compare expression 5.68 for the Gibbs free energy of a dilute solution to expression 5.61 for the Gibbs free energy of an ideal mixture. Under what circumstances should these two expressions agree? Show that they do agree under these circumstances, and identify the function f(T, P) in this case.

Derive the thermodynamic identity for G (equation 5.23), and from it the three partial derivative relations 5.24.

Repeat the preceding problem with T/TC=0.8

In this problem you will investigate the behavior of a van der Waals fluid near the critical point. It is easiest to work in terms of reduced variables throughout.

(a) Expand the van der Waals equation in a Taylor series in , keeping terms through order . Argue that, for T sufficiently close to Tc, the term quadratic in (V-VC)becomes negligible compared to the others and may be dropped.

(b) The resulting expression for P(V) is antisymmetric about the point V = Ve. Use this fact to find an approximate formula for the vapor pressure as a function of temperature. (You may find it helpful to plot the isotherm.) Evaluate the slope of the phase boundary,dP/dT

( c) Still working in the same limit, find an expression for the difference in volume between the gas and liquid phases at the vapor pressure. You should find Vg-VlTc-Tβ.8, where (3 is known as a critical exponent. Experiments show that (3 has a universal value of about 1/3, but the van der Waals model predicts a larger value.

(d) Use the previous result to calculate the predicted latent heat of the transformation as a function of temperature, and sketch this function.

The shape of the T = Tc isotherm defines another critical exponent, called P-PcV-VcδCalculate 5 in the van der Waals model. (Experimental values of 5 are typically around 4 or 5.)

A third critical exponent describes the temperature dependence of the isothermal compressibility, K=-t This quantity diverges at the critical point, in proportion to a power of (T-Tc) that in principle could differ depending on whether one approaches the critical point from above or below. Therefore the critical exponents 'Y and -y' are defined by the relations

κT-Tc-γTc-T-γ'

Calculate K on both sides of the critical point in the van der Waals model, and show that 'Y = -y' in this model.

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