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In analogy with the thermal conductivity, derive an approximate formula for the diffusion coefficient of an ideal gas in terms of the mean free path and the average thermal speed. Evaluate your formula numerically for air at room temperature and atmospheric pressure, and compare to the experimental value quoted in the text. How does D depend on T, at fixed pressure?

Short Answer

Expert verified

The compare it to the experimental value . At constant pressure, how does D depend on T isD=12v¯

Dair=3.75×105m2s1

D(KT)32

Step by step solution

01

Step1:Given data

N2Consider a thin gas slab with cross-sectional area A. We cut the box in half so that the number of molecules on one side of the partition isN1 and the number of molecules on the other side is. We'll assume that the entire box is at a constant temperature N1and that Schroeder's approximations for mean free path and average speed are correct:

14πr2VN(1)

v¯3KTm(2)

where ris the molecular radius and m the mass of one molecule.

02

Step2:The time it takes a molecule to move distance 

Those molecules within a distanceof the midpoint of the slab can cross the midpoint if they are travelling towards the midpoint. Since only half the molecules will, on average, be moving towards the partition (statistically), the net numberΔNof molecules that cross the partition in a timeΔt, which is the time it takes a molecule to move distance , is:

ΔN=12N1N2(3)

If the molecule number gradient isdNdxthen we have:

N1N2=dNdx(4)

where is the distance that a molecule travels before colliding, substituting from intoN1N2=dNdxΔN=12N1N2so:

ΔN=12dNdx(5)

The flux is the net rate at which molecules cross the partition per unit area Jx, its given by:

Jx=ΔNAΔt(6)

substitute from equationΔN=12dNdxinto equation Jx=ΔNAΔtwith ΔN, so:

Jx=1AΔt12dNdx

multiply with ,so:

Jx=22AΔtdNdx(7)

However, the volume is equal to the free mean path multiplied by the cross sectional area, and the time it takes the molecule to move one free mean path is equal to the time it takes the molecule to move one free mean path, or:

A=VΔt=v¯

03

Step3:The measured value

substitute, so equationJx=22AΔtdNdx will become:

Jx=v¯2VdNdx

but NV=n, so:

This is the magnitude of the flux, as indicated by the absolute value. Because the flux is moving in the opposite direction of the gradient, we will have:

Jx=12v¯dndx(8)

The quantity 12v¯is a close approximation to the diffusion constant D for an ideal gas, with units of m2·s-1. The following is a more general form of this equation:

Jx=Ddndx

Using the values from Schroeder's book for air at room temperature, =1.5×10-7mand v¯=500m·s-1, so:

D=12v¯=12×1.5×107×500=3.75×105m2s1

Dair=3.75×105m2s1

The measured value is around 2×10-5m2·s-1so this isn't too far off for a rough estimate

04

Step4:Estimate dependence between the diffusion constant

From the values for andv¯in equations 14πr2VNand v¯3KTmWe can calculate the relationship between the diffusion constant and temperature at constant pressure as follows:

D=12[][v¯]=1214πr2VN3KTm

based on the ideal gas law,VN=kTP, so:

D=1214πr2kTP3KTm

D=18πr2(KT)32P3m

So, at constant pressure,

D(KT)32

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Most popular questions from this chapter

In Problem 1.16 you calculated the pressure of the earth’s atmosphere as a function of altitude, assuming constant temperature. Ordinarily, however, the temperature of the bottommost 10-15 km of the atmosphere (called the troposphere) decreases with increasing altitude, due to heating from the ground (which is warmed by sunlight). If the temperature gradient |dT/dz|exceeds a certain critical value, convection will occur: Warm, low-density air will rise, while cool, high-density air sinks. The decrease of pressure with altitude causes a rising air mass to expand adiabatically and thus to cool. The condition for convection to occur is that the rising air mass must remain warmer than the surrounding air despite this adiabatic cooling.

a. Show that when an ideal gas expands adiabatically, the temperature and pressure are related by the differential equation

dTdP=2f+2TP

b. Assume that dT/dzis just at the critical value for convection to begin so that the vertical forces on a convecting air mass are always approximately in balance. Use the result of Problem 1.16(b) to find a formula for dT/dzin this case. The result should be a constant, independent of temperature and pressure, which evaluates to approximately 10°C/km. This fundamental meteorological quantity is known as the dry adiabatic lapse rate.

Estimate how long it should take to bring a cup of water to boiling temperature in a typical 600 -watt microwave oven, assuming that all the energy ends up in the water. (Assume any reasonable initial temperature for the water.) Explain why no heat is involved in this process.

Calculate the rms speed of a nitrogen molecule at room temperature.

Given an example to illustrate why you cannot accurately judge the temperature of an object by how hot or cold it feels to the touch?

At about what pressure would the mean free path of an air molecule at room temperature equal 10cm, the size of a typical laboratory apparatus?

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