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.

Short Answer

Expert verified

Therefore,

mH2CO3=1.141×10-5mol/LiterpH=5.67

Step by step solution

01

Given information

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)

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 3.4x 10 bar (or 340 parts per million).

02

Explanation

Consider the following two reactions, each of which symbolises the carbon dioxide dissolving in water:

CO2+H2OH2CO3H2CO3H++HCO3-

The concentration of carbon acid in terms of partial pressure and the change in the Gibbs free energy can be calculated using Henry's law:

mH2CO3PCO2/P°=exp-ΔG°RTmH2CO3=PCO2P°exp-ΔG°RT(1)

We need to find the change in the Gibbs free energy

G°(kJ)H2CO3-623.08H2O-237.13CO2-394.36

Change in Gibbs free energy is:

ΔG°=GH2CO3°-GH2O°-GCO2°=-623.08kJ+237.13kJ+394.36kJ=8.41kJ

03

Calculations

Substitute the values in the equation

mH2CO3=3.4×10-4bar1barexp-8.41×103J(8.314J/mol·K)(298K)mH2CO3=1.141×10-5mol/Liter

Using the law of mass action for the second reaction, we can write the concentration as:

mH+mHCO3-mH2CO3=e-ΔG°/RT(2)

To find ΔG°

G°(kJ)H2CO3-623.08H+0HCO3--586.77

Change in Gibbs energy is:

ΔG°=GH+°+GHCO3-°-GH2CO3°=-586.77kJ+623.08kJ=36.31kJ

04

Calculations

The molarity of the HT ions equals the molarity of the bicarbonate ions, so equation (2) will become:

mHCO3-2mH2CO3=e-ΔG°/RTmHCO3-2=mH2CO3e-ΔG°/RTmHCO3-=mH2CO3e-ΔG°/RT

Substituting the values,

mHCO3-=1.141×10-5mol/Litere-36310J/(8.314J/mol·K)(298K)=2.22×10-6mol/Liter

The molarity of the H+ ions is:

mH+=mHCO3-=2.22×10-6mol/Liter

The pH of solution is:

pH=-log10mH+=-log102.22×10-6mol/Liter=5.67

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Most popular questions from this chapter

Suppose you have a liquid (say, water) in equilibrium with its gas phase, inside some closed container. You then pump in an inert gas (say, air), thus raising the pressure exerted on the liquid. What happens?

(a) For the liquid to remain in diffusive equilibrium with its gas phase, the chemical potentials of each must change by the same amount: dμl=dμg Use this fact and equation 5.40 to derive a differential equation for the equilibrium vapour pressure, Pv as a function of the total pressure P. (Treat the gases as ideal, and assume that none of the inert gas dissolves in the liquid.)

(b) Solve the differential equation to obtain

Pv(P)-PvPv=eP-PvV/NkT

where the ratio V/N in the exponent is that of the liquid. (The term Pv(Pv) is just the vapour pressure in the absence of the inert gas.) Thus, the presence of the inert gas leads to a slight increase in the vapour pressure: It causes more of the liquid to evaporate.

(c) Calculate the percent increase in vapour pressure when air at atmospheric pressure is added to a system of water and water vapour in equilibrium at 25°C. Argue more generally that the increase in vapour pressure due to the presence of an inert gas will be negligible except under extreme conditions.

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.


Problem 5.35. The Clausius-Clapeyron relation 5.47 is a differential equation that can, in principle, be solved to find the shape of the entire phase-boundary curve. To solve it, however, you have to know how both L and V depend on temperature and pressure. Often, over a reasonably small section of the curve, you can take L to be constant. Moreover, if one of the phases is a gas, you can usually neglect the volume of the condensed phase and just take V to be the volume of the gas, expressed in terms of temperature and pressure using the ideal gas law. Making all these assumptions, solve the differential equation explicitly to obtain the following formula for the phase boundary curve:

P= (constant) x e-L/RT

This result is called the vapour pressure equation. Caution: Be sure to use this formula only when all the assumptions just listed are valid.

Show that equation 5.40 is in agreement with the explicit formula for the chemical potential of a monatomic ideal gas derived in Section 3.5. Show how to calculate μ°for a monatomic ideal gas.

Use the result of the previous problem to estimate the equilibrium constant of the reactionN2+3H22NH3at 500° C, using only the room- temperature data at the back of this book. Compare your result to the actual value of K at 500° C quoted in the text.

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