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Even before the industrial age, rainwater was slightly acidic due to dissolved CO2. Use the following data to calculate pHof unpolluted rainwater at role="math" localid="1663285066521" 25C:vol%inair of CO2=0.033vol%; solubility of CO2in pure water at 25Cand1atm=88mLCO2/100mLH2O;Ka1ofH2CO3=4.5×10-7.

Short Answer

Expert verified

The pHof unpolluted rainwater role="math" localid="1663285201168" 25Cat is pH=5.68.

Step by step solution

01

Concept Introduction.

Solubility refers to the greatest amount of solute that can dissolve in a known quantity of solvent at a given temperature.

The phrase "solubility product" refers to salts that are only sparingly soluble. It is the maximal product of the molar concentration of the ions produced by dissociation of the molecule (raised to their proper powers).

02

Dissociation of H2CO3.

The reactions involved in the acidification of rain water are as follows –

CO2(aq)+H2O(l)H2CO3(aq)H2CO3(aq)+H2O(l)H3O+(aq)+H2CO3-(aq)

The molar concentration of carbon dioxide depends on how much carbon dioxide is dissolved in pure water. At 25Cand 1atm,88mLof CO2can dissolve in 100mLof water.

The number of moles of CO2are calculated as follows –

n=PVRTn=1atm×88×10-3L0.0821L·atm/mol·K×298K×0.033%100%n=1.18693×10-6mol

The concentration of CO2in air –

CO2=1.18963×10-6mol100×10-3L=1.18963×10-5M

The dissociation of H2CO3is –

CO2=H2CO3Ka=H3O+HCO3-H2CO34.5×10-7=H3O+HCO3-CO2

03

Step 3: pH of unpolluted rain water.

The ICE table for the reaction can be drawn as –


CO2·H2CO3
H3O+
HCO3-
Initial1.18693×10-5
0
0
change-x

+x
role="math" localid="1663285998323" +x
Equilibrium
1.18693×10-5-x
role="math" localid="1663286016609" x
role="math" localid="1663286007397" x

Solve for the value of x.

role="math" localid="1663286143266" 4.5×10-7=(x)(x)1.18693×10-5m-x=x21.18693×10-5mx=2.0976596×10-6M

Now, calculate pHthe value –

pH=-logH3O+pH=-logH+H+=x=2.0970596×10-6MpH=-log2.0970596×10-6MpH=5.6783pH=5.68

Therefore, the value for pHis obtained as pH=5.68.

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Most popular questions from this chapter

Some kidney stones form by the precipitation of calcium oxalate monohydrate (CaC2O4×H2O,Ksp=2.3×10-9). Theof urine varies from 5.5 to 7.0, and the average [Ca2+]in urine is2.6×10-3M.

(a) If the [oxalic acid] in urine is3.0×10-13M, will kidney stones form atrole="math" localid="1663267818783" pH=5.5?

(b)atpH=7.0?

(c) Vegetarians have a urineabove7. Are they more or less likely to form kidney stones?

Use Figure 19.5 to find an indicator for these titrations:

(a) 0.10MCH3NH2(Appendix C) with0.10MHCl.

(b) 0.50MHI with0.10MKOH.

Choose specific acid-base conjugate pairs to make the following buffers: (a) pH3.5 ; (b)pH5.5
. (See Appendix C.)

An eco-botanist separates the components of a tropical bark extract by chromatography. She discovers a large proportion of quinidine, a dextrorotatory isomer of quinine used for control of arrhythmic heartbeat. Quinidine has two basic nitrogen’s (Kb1=4.0×10-6and Kb2=1.0×10-10). To measure the concentration, she carries out a titration. Because of the low solubility of quinidine, she first protonates both nitrogen’s with excessand titrates the acidified solution with standardized base. A 33.85-mg sample of quinidine (M=324.41g/mol)is acidified with6.55mLof0.150MHCl.

(a) How many milliliters of0.0133MNaOHare needed to titrate the excessHCl?

(b) How many additional milliliters of titrant are needed to reach the first equivalence point of quinidine dihydrochloride?

(c) What is theat the first equivalence point?

Choose specific acid-base conjugate pairs to make the following buffers: (a)pH4.5; (b)pH4.5. (See Appendix C.)

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