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The standard enthalpy change upon dissolving one mole of oxygen at 25°C is -11.7 kJ. Use this number and the van't Hoff equation (Problem 5.85) to calculate the equilibrium (Henry's law) constant for oxygen in water at 0°C and at 100° C. Discuss the results briefly.

Short Answer

Expert verified

The equilibrium constant at 0 degree is nearly identical to the equilibrium constant at ambient temperature, but decreases as the temperature rises.

Step by step solution

01

Given information

The standard enthalpy change upon dissolving one mole of oxygen at 25°C is -11.7 kJ.

02

Explanation

The equilibrium constant from the problem 5.85 is given by:

lnKT2=lnKT1+ΔH°R1T1-1T2KT2=explnKT1+ΔH°R1T1-1T2

Where,

KT1is the equilibrium constant and is given as KT1=1750

We need to calculate the equilibrium constant at temperature of T2 =0°C = 273 K, substitute with the values:

K(273K)=expln1750-11.7×103J8.314J/mol·K1298K-1273KK(273K)=2.0547×10-3

03

Calculations

Now we need to calculate the equilibrium constant at temperature of T2 = 100 C = 373 K, substituting the values

K(373K)=expln1750-11.7×103J8.314J/mol·K1298K-1373KK(373K)=5.159×10-4

The equilibrium constant at 0 degree is nearly identical to the equilibrium constant at ambient temperature, but decreases as the temperature rises.

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Most popular questions from this chapter

Functions encountered in physics are generally well enough behaved that their mixed partial derivatives do not depend on which derivative is taken first. Therefore, for instance,
VUS=SUV

where each /Vis taken with S fixed, each/S is taken with V fixed, and N is always held fixed. From the thermodynamic identity (for U ) you can evaluate the partial derivatives in parentheses to obtain

TVS=-PSV

a nontrivial identity called a Maxwell relation. Go through the derivation of this relation step by step. Then derive an analogous Maxwell relation from each of the other three thermodynamic identities discussed in the text (for H, F, and G ). Hold N fixed in all the partial derivatives; other Maxwell relations can be derived by considering partial derivatives with respect to N, but after you've done four of them the novelty begins to wear off. For applications of these Maxwell relations, see the next four problems.


Suppose you have a box of atomic hydrogen, initially at room temperature and atmospheric pressure. You then raise the temperature, keeping the volume fixed.

(a) Find an expression for the fraction of the hydrogen that is ionised as a function of temperature. (You'll have to solve a quadratic equation.) Check that your expression has the expected behaviour at very low and very high temperatures.

(b) At what temperature is exactly half of the hydrogen ionised?

(c) Would raising the initial pressure cause the temperature you found in part (b) to increase or decrease? Explain.

(d) Plot the expression you found in part (a) as a function of the dimension- less variable t = kT/I. Choose the range of t values to clearly show the interesting part of the graph.

Repeat the previous problem for the diagram in Figure 5.35 (right), which has an important qualitative difference. In this phase diagram, you should find that β and liquid are in equilibrium only at temperatures below the point where the liquid is in equilibrium with infinitesimal amounts of αandβ . This point is called a peritectic point. Examples of systems with this behaviour include water + NaCl and leucite + quartz.

Repeat the previous problem for the opposite case where the liquid has a substantial negative mixing energy, so that its free energy curve dips |below the gas's free energy curve at a temperature higher than TB. Construct the phase diagram and show that this system also has an azeotrope.

Seawater has a salinity of 3.5%, meaning that if you boil away a kilogram of seawater, when you're finished you'll have 35gof solids (mostly localid="1647507373105" NaCl) left in the pot. When dissolved, sodium chloride dissociates into separate Na+and Cl-ions.

(a) Calculate the osmotic pressure difference between seawater and fresh water. Assume for simplicity that all the dissolved salts in seawater are NaCl.

(b) If you apply a pressure difference greater than the osmotic pressure to a solution separated from pure solvent by a semipermeable membrane, you get reverse osmosis: a flow of solvent out of the solution. This process can be used to desalinate seawater. Calculate the minimum work required to desalinate one liter of seawater. Discuss some reasons why the actual work required would be greater than the minimum.

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