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Derive the van't Hoff equation,

dlnKdT=ΔH°RT2

which gives the dependence of the equilibrium constant on temperature." Here ∆H°is the enthalpy change of the reaction, for pure substances in their standard states (1 bar pressure for gases). Notice that if ∆H°is positive (loosely speaking, if the reaction requires the absorption of heat), then higher temperature makes the reaction tend more to the right, as you might expect. Often you can neglect the temperature dependence of∆H°; solve the equation in this case to obtain

lnKT2-lnKT1=ΔH°R1T1-1T2

Short Answer

Expert verified

Hence the equation is derived.

Step by step solution

01

Given information

Vant Hoff's equation:

dlnKdT=ΔH°RT2
02

Explanation

The equilibrium constant in chemical reactions is given by:

K=e-ΔG°/RT(1)

Where

ΔG°is the Gibbs free energy:

Taking log on both sides

ln(K)=-ΔG°RT

Differentiate both sides with respect to T

ddT(ln(K))=-1RTdΔG°dT+ΔG°RT2(2)

Change in free Gibbs energy

dG=U-SdT+μdN

At constant N,dN=0

dGdT=-S

For standard Gibbs free energy, we have

dG°dT=-S°

Taking difference, we get

dΔG°dT=-ΔS°

Substitute into (2), to get

ddT(ln(K))=ΔS°RT+ΔG°RT2(3)

The Gibbs free energy is:

G=H-TS

At constant temperature, the standard change

ΔG°=ΔH°-TΔS°

Substitute into (3)

ddT(ln(K))=ΔS°RT+ΔH°-TΔS°RT2ddT(ln(K))=ΔS°RT+ΔH°RT2-ΔS°RTddT(ln(K))=ΔH°RT2

03

Explanation

Now that we have separated the variables, such as temperature in the RHS and natural logarithm in the LHS, we must integrate this equation.

dln(K)=ΔH°RT2dT

Integrate both sides from T1toT2

∫T1T2dln(K)=∫T1T2ΔH°RT2dT[ln(K)]T1T2=-ΔH°RT°T1T2lnKT2-lnKT1=ΔH°R1T1-1T2

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Most popular questions from this chapter

The methods of this section can also be applied to reactions in which one set of solids converts to another. A geologically important example is the transformation of albite into jadeite + quartz:

NaAlSi3O8⟷NaAlSi2O6+SiO2

Use the data at the back of this book to determine the temperatures and pressures under which a combination of jadeite and quartz is more stable than albite. Sketch the phase diagram of this system. For simplicity, neglect the temperature and pressure dependence of both ∆S and ∆V.

When carbon dioxide "dissolves" in water, essentially all of it reacts to form carbonic acid, H2CO3:

CO2(g)+H2O(l)⟷H2CO3(aq)

The carbonic acid can then dissociate into H* and bicarbonate ions,

H2CO3(aq)⟷H+(aq)+HCO3-(aq)

(The table at the back of this book gives thermodynamic data for both of these reactions.) Consider a body of otherwise pure water (or perhaps a raindrop) that is in equilibrium with the atmosphere near sea level, where the partial pressure of carbon dioxide is 3.4 x 10-4 bar (or 340 parts per million). Calculate the molality of carbonic acid and of bicarbonate ions in the water, and determine the pH of the solution. Note that even "natural" precipitation is somewhat acidic.

Figure 5.35 (left) shows the free energy curves at one particular temperature for a two-component system that has three possible solid phases (crystal structures), one of essentially pure A, one of essentially pure B, and one of intermediate composition. Draw tangent lines to determine which phases are present at which values of x. To determine qualitatively what happens at other temperatures, you can simply shift the liquid free energy curve up or down (since the entropy of the liquid is larger than that of any solid). Do so, and construct a qualitative phase diagram for this system. You should find two eutectic points. Examples of systems with this behaviour include water + ethylene glycol and tin - magnesium.

Osmotic pressure measurements can be used to determine the molecular weights of large molecules such as proteins. For a solution of large molecules to qualify as "dilute," its molar concentration must be very low and hence the osmotic pressure can be too small to measure accurately. For this reason, the usual procedure is to measure the osmotic pressure at a variety of concentrations, then extrapolate the results to the limit of zero concentration. Here are some data for the protein hemoglobin dissolved in water at 3oC:

Concentration (grams/liter)∆h (cm)
5.62.0
16.66.5
32.512.8
43.417.6
54.022.6

The quantity ∆his the equilibrium difference in fluid level between the solution and the pure solvent,. From these measurements, determine the approximate molecular weight of hemoglobin (in grams per mole).

An experimental arrangement for measuring osmotic pressure. Solvent flows across the membrane from left to right until the difference in fluid level,∆h, is just enough to supply the osmotic pressure.

A muscle can be thought of as a fuel cell, producing work from the metabolism of glucose:

C6H12O6+6O2⟶6CO2+6H2O

(a) Use the data at the back of this book to determine the values of ΔHand ΔGfor this reaction, for one mole of glucose. Assume that the reaction takes place at room temperature and atmospheric pressure.

(b) What is maximum amount of work that a muscle can perform , for each mole of glucose consumed, assuming ideal operation?

(c) Still assuming ideal operation, how much heat is absorbed or expelled by the chemicals during the metabolism of a mole of glucose?

(d) Use the concept of entropy to explain why the heat flows in the direction it does?

(e) How would your answers to parts (a) and (b) change, if the operation of the muscle is not ideal?

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