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

Unlock Step-by-Step Solutions & Ace Your Exams!

  • Full Textbook Solutions

    Get detailed explanations and key concepts

  • Unlimited Al creation

    Al flashcards, explanations, exams and more...

  • Ads-free access

    To over 500 millions flashcards

  • Money-back guarantee

    We refund you if you fail your exam.

Over 30 million students worldwide already upgrade their learning with Vaia!

One App. One Place for Learning.

All the tools & learning materials you need for study success - in one app.

Get started for free

Most popular questions from this chapter

The partial-derivative relations derived in Problems 1.46,3.33, and 5.12, plus a bit more partial-derivative trickery, can be used to derive a completely general relation between CPandCV.

(a) With the heat capacity expressions from Problem 3.33 in mind, first considerSto be a function of TandV.Expand dSin terms of the partial derivatives (S/T)Vand (S/V)T. Note that one of these derivatives is related toCV

(b) To bring in CP, considerlocalid="1648430264419" Vto be a function ofTand P and expand dV in terms of partial derivatives in a similar way. Plug this expression for dV into the result of part (a), then set dP=0and note that you have derived a nontrivial expression for (S/T)P. This derivative is related to CP, so you now have a formula for the difference CP-CV

(c) Write the remaining partial derivatives in terms of measurable quantities using a Maxwell relation and the result of Problem 1.46. Your final result should be

CP=CV+TVβ2κT

(d) Check that this formula gives the correct value of CP-CVfor an ideal gas.

(e) Use this formula to argue that CPcannot be less than CV.

(f) Use the data in Problem 1.46 to evaluateCP-CVfor water and for mercury at room temperature. By what percentage do the two heat capacities differ?

(g) Figure 1.14 shows measured values of CPfor three elemental solids, compared to predicted values of CV. It turns out that a graph of βvs.T for a solid has same general appearance as a graph of heat capacity. Use this fact to explain why CPand CVagree at low temperatures but diverge in the way they do at higher temperatures.

Consider again the aluminosilicate system treated in Problem 5.29. Calculate the slopes of all three phase boundaries for this system: kyanite andalusite, kyanite-sillimanite, and andalusite-sillimanite. Sketch the phase diagram, and calculate the temperature and pressure of the triple point.

Suppose you start with a liquid mixture of 60% nitrogen and 40% oxygen. Describe what happens as the temperature of this mixture increases. Be sure to give the temperatures and compositions at which boiling begins and ends.

Sulfuric acid, H2SO4,readily dissociates intoH+andHSO4-H+andHSO4-ions

H2SO4H++HSO4-

The hydrogen sulfate ion, in turn, can dissociate again:

HSO4-H++SO42-

The equilibrium constants for these reactions, in aqueous solutions at 298 K, are approximately 10 and 10*, respectively. (For dissociation of acids it is usually more convenient to look up K than G°. By the way, the negative base-10 logarithm of K for such a reaction is called pK, in analogy to pH. So for the first reaction pK = -2, while for the second reaction pK = 1.9.)

(a) Argue that the first reaction tends so strongly to the right that we might as well consider it to have gone to completion, in any solution that could possibly be considered dilute. At what pH values would a significant fraction of the sulfuric acid not be dissociated?

(b) In industrialized regions where lots of coal is burned, the concentration of sulfate in rainwater is typically 5 x 10 mol/kg. The sulfate can take any of the chemical forms mentioned above. Show that, at this concentration, the second reaction will also have gone essentially to completion, so all the sulfate is in the form of SOg. What is the pH of this rainwater?

(c) Explain why you can neglect dissociation of water into H* and OH in answering the previous question. (d) At what pH would dissolved sulfate be equally distributed between HSO and SO2-?

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.

See all solutions

Recommended explanations on Physics Textbooks

View all explanations

What do you think about this solution?

We value your feedback to improve our textbook solutions.

Study anywhere. Anytime. Across all devices.

Sign-up for free