Friday  october 1

chem 127

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background:

        exam on Wednesday (evening)

        sunday, 7 PM Overman (meet by the lab; west door access)

        web site added information, including a 2003 exam II and review

notes

 

added remark: the page of problems I distributed last Friday (copy on the Web with solutions.) These were NOT intended to be typical of exam problems. Many of the questions were deliberately complicated so we could focus on the task of dissecting a question, finding what tools we can bring to bear (equilibrium tools), and how we could attack the problem. On this coming exam, I’d like the problems to be much more direct.

 

Equilibrium

 

Chapter 16 includes Ksp and solubility

        not a new topic, been using examples since Ch 13

 

salt ----water---100% ---> ions

 

PbCl2 --> Pb2+ + 2Cl-

AgCl ---> Ag+ + Cl-

CuS ---> Cu2+ + S=

 

Ksp is the equilibrium constant for solubility process

 

        Ksp = [Pb2+ ] [Cl-]2

        Ksp = [Ag+] [Cl-]

        Ksp= [Cu2+ ] [ S=]

(Technically this is valid for all ionic compounds, but results are

only good for salts with relatively low solubility.)

The reverse is basically a discussion of precipitation

 

No new questions, equations, methods

        same core equilibrium problems

        But some examples appear frequently.

 

Throw a salt in water, how much will dissolve ?

        Ag2SO4  ----> 2Ag+ + SO42-

Classic Equilibrium, but easier than most

        initial concentrations -- zero

        change -- s and 2s  (both same sign)

                        s = # moles that dissolved (per liter)

                        reactant (solid salt)-- doesn't enter

calculation

        equilibrium values are 2s for Ag+ and s for SO42--

        

        2s = [Ag+]

        s= [SO42-]

 

        Ksp = (2s)2 (s)     or   Ksp = 4 s3

        s = { Ksp/4} = conc of salt in solution.

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Common Ion Version-- how much ____ will dissolve in       _____ Molar  Na ______?

Common Ion Version-- how much Ca(OH)2 will dissolve in 0.50 Molar 

NaOH? (Ksp= 4.7 x 10-6)

        Ca(OH)2 ---> Ca2+ + 2 OH-

        s= # moles that dissolve

        Initial [Ca2+]=0    so final [Ca2+] = s

        Initial [OH- ] = 0.50   so final [OH-] = 0.50+2s

 

        Ksp = [Ca2+ ][OH-]2

        4.7 x 10-6= s * (0.50 +2s)2     ... solve for s

        0 = -4.7 x 10-6 +0.25 s + 2 s2 + 4s3    ...cubic eq (ugh)

 

        could we cheat ?   approximate

                small Ksp so solubility in water is small

                common ion, so s will c quite small here

                let's approximate 0.50 + x      as   0.50

        now

        4.7 x 10-6= s * (0.50 +2s)2 = 0.25 s

        s = 4.7 x 10-6/ 0.25 = 1.87 x 10-5

a great approximation: 

         0.50    and     0.50+2*1.87 x 10-5  are nearly the  same?

 

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The other major solubility problem is really the reverse

        will a precipitate form if we mix cation and anion ?

We start with a little fiction...

        we mix some solutions, but turn off equilibrium process

        we find the initial concentrations

        then we turn equilibrium back on

                do concentrations in Q  exceed Ksp  (if so, ppt)

        then, if requested, we solve for final equil concentrations

 

we add 1 ml of 5.0 M NaOH to 1.0 liters of 0.0020 M Mg2+

        will we get Mg(OH)2 to precipitate?

minor cheating... let's assume volume remains 1.0 liters

        initial [Mg2+] = 0.0020

        initial [OH- ]=(0.001 L * 5.0 mol/L) / 1.001 L= 0.0050 M

        

        Q = [Mg2+ [OH-]2 = (2x10-3) (5 x 10-3)2 = 50 x 10-9

        Ksp (tables) = 5.6 x 10-12

                yes, we get precipitate to form

                in fact, Q>>Ksp & we need massive reduction in Q.

if limiting reagent idea is used Mg2+ could be totally removed and OH-

would still be 0.0010M, so we should expect most of the Mg2+ to be

consumed.

 

        if x is the extent of precipitation (conc change)

        [Mg2+] initially 0.0020 and finally  0.0020-x

        [OH-] initially 0.0050 and finally  0.0050 - 2x

        Ksp =[Mg2+] [OH-]2 

        5.6 x 10-12 = (0.0020-x ) (0.0050 - 2x)2  

another ugly cubic equation , but mathematically, one step from a solution

            this actually is easy to approximate

            since almost all Mg2+ is consumed,

the remaining [OH-] = 0.0050 – 2*0.002 = 0.0010

of 5.6 x 10-12 = [Mg+2] * (0.0010)2

[Mg2+] at equil = 5.6 x 10-6   (tiny enough to validate our approximations)

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The last common solubility problem is associated with another simultaneous equilibrium...

        example... what is the solubility of Silver Acetate if

        we manage to keep the pH at 3.00 ? (a pH buffer)

 

(similar examples-- will CdS ppt if we supply H2S at pH 5.0?)

 

calculation is more complex (very poor exam question)

I hope you can follow, and see that this is valid. I don’t expect that you will figure out how to do this on your own or that your would now be able to solve a similar problem if it showed up.

        1)    Ksp = [Ag+] [Ac-]

        2)      Ka = [H+] [Ac-] / [HAc]

                        if H+ conc is large, [Ac-] is kept low

 

        3) stoichiometry links these ... [Ag+] = [Ac-] + [HAc]

 

        If x = final Ag+ concentration, eq 1 becomes

                [Ac-] = Ksp /x

        and eq 3 becomes

                x = (Ksp/x)  + [H+] (Ksp/x) /Ka

                x2 = Ksp + [H+]/ Ka       right side = known numbers

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Closely related

        why AgCl (in photographic film) dissolves in "fixer"

        sodium thiosulfate, even though Ksp is tiny.

                reaction with thiosulfate keeps [Ag+]free very tiny

        can even dissolve in conc NaCl, forming  AgCl2- ion

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Review ... types of exam questions and type of problems

 

 

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