803
CHAPTER 20
THE NUCLEUS: A CHEMIST'S VIEW
Radioactive Decay and Nuclear Transformations
1. a. Thermodynamic stability: the potential energy of a particular nucleus compared to the
sum of the potential energies of its component protons and neutrons.
b. Kinetic stability: the probability that a nucleus will undergo decomposition to form a
different nucleus.
c. Radioactive decay: a spontaneous decomposition of a nucleus to form a different nucleus.
d. Beta-particle production: a decay process for radioactive nuclides where an electron is
produced; the mass number remains constant and the atomic number changes.
e. Alpha-particle production: a common mode of decay for heavy radioactive nuclides
where a helium nucleus is produced, causing the atomic number and the mass number
to change.
f. Positron production: a mode of nuclear decay in which a particle is formed having the
same mass as an electron but opposite in charge.
g. Electron capture: a process in which one of the inner-orbital electrons in an atom is
captured by the nucleus.
h. Gamma-ray emissions; the production of high-energy photons (gamma rays) that fre-
quently accompany nuclear decays and particle reactions.
2. Beta-particle production has the net effect of turning a neutron into a proton. Radioactive
nuclei having too many neutrons typically undergo beta-particle decay. Positron production
has the net effect of turning a proton into a neutron. Nuclei having too many protons typically
undergo positron decay.
3. All nuclear reactions must be charge balanced and mass balanced. To charge balance,
balance the sum of the atomic numbers on each side of the reaction, and to mass balance,
balance the sum of the mass numbers on each side of the reaction.
a. ThHeU 23490
42
23892 ; this is alpha-particle production.
b. ePaTh 01
23491
23490 ; this is -particle production.
804 CHAPTER 20 THE NUCLEUS: A CHEMIST'S VIEW
4. a. 7331
Ga 7332
Ge + 01e b. 192
78Pt 188
76Os + 4
2He
c. 20583
Bi 20582
Pb + 01 e d. 241
96Cm + 0
1e 241
95Am
e. eNiCo 01
6028
6027 f. MoeTc 97
4201
9743
g. eRuTc 01
9944
9943 h. HeUPu 4
223592
23994
5. a. ZneGa 6830
01
6831 b. NieCu 62
2801
6229
c. AtHeFr 20885
42
21287 d. TeeSb 129
5201
12951
6. a. eHeH 01
32
31 b. eBeLi 0
184
83
eHe2Li
________________He2Be
01
42
83
42
84
c. LieBe 73
01
74
d. eBeB 01
84
85
7. All nuclear reactions must be charge-balanced and mass-balanced. To charge-balance,
balance the sum of the atomic numbers on each side of the reaction, and to mass-balance,
balance the sum of the mass numbers on each side of the reaction.
a. VeCr 5123
01
5124 b. XeeI 131
5401
13153
c. SeP 3216
01
3215
8. Fe5326 has too many protons. It will undergo either positron production, electron capture,
and/or alpha-particle production. Fe5926 has too many neutrons and will undergo beta-particle
production. (See Table 20.2 of the text.) The reactions are:
eCoFe;HeCrFe;MneFe;eMnFe 01
5927
5926
42
4924
5326
5325
01
5326
01
5325
5326
9. Reference Table 20.2 of the text for potential radioactive decay processes. 17
F and 18
F contain
too many protons or too few neutrons. Electron capture and positron production are both
possible decay mechanisms that increase the neutron-to-proton ratio. Alpha-particle
production also increases the neutron-to-proton ratio, but it is not likely for these light nuclei. 21
F contains too many neutrons or too few protons. Beta-particle production lowers the
neutron-to-proton ratio, so we expect 21
F to be a β-emitter.
10. a. NpHeAm 23793
42
24195
b. .Biisproductfinalthe;Bie4He8Am 20983
20983
01
42
24195
CHAPTER 20 THE NUCLEUS: A CHEMIST'S VIEW 805
c. αRaαThβUαPaαNpAm 22588
22990
23392
23391
23793
24195
βAcαFrαAtαBiβPo 22589
22187
21785
21383
21384
βBiαPb 20983
20982
The intermediate radionuclides are:
Pband,Po,Bi,At,Fr,Ac,Ra,Th,U,Pa,Np 20982
21384
21383
21785
22187
22589
22588
22990
23392
23391
23793
11. ;e?He?PbBk 01
42
20782
24797 The change in mass number (247 - 207 = 40) is due ex-
exclusively to the alpha particles. A change in mass number of 40 requires 10 He42 particles
to be produced. The atomic number only changes by 97 82 = 15. The 10 alpha particles
change the atomic number by 20, so e5 01 (five beta particles) are produced in the decay
series of 247
Bk to 207
Pb.
12. a. nBkHeAm 10
24397
42
24095 b. n6CfCU 1
024498
126
23892
c. n4DbNCf 10
260105
157
24998 d. n2LrBCf 1
0257103
105
24998
13. a. n4SgOCf 10
263106
188
24998 b. RfHeSg;Rf 259
10442
263106
259104
14. The most abundant isotope is generally the most stable isotope. The periodic table predicts
that the most stable isotopes for parts a-d are 39
K, 56
Fe, 23
Na, and 204
Tl. (Reference Table 20.2
of the text for potential decay processes.)
a. Unstable; 45
K has too many neutrons and will undergo beta-particle production.
b. Stable
c. Unstable; 20
Na has too few neutrons and will most likely undergo electron capture or
positron production. Alpha-particle production makes too severe of a change to be a
likely decay process for the relatively light 20
Na nuclei. Alpha-particle production
usually occurs for heavy nuclei.
d. Unstable; 194
Tl has too few neutrons and will undergo electron capture, positron
production, and/or alpha-particle production.
Kinetics of Radioactive Decay
15. k = s3600
h1
h24
d1
d365
yr1
yr433
69315.0
t
2ln
2/1
= 5.08 × 111 s10
806 CHAPTER 20 THE NUCLEUS: A CHEMIST'S VIEW
Rate = kN = 5.08 × 111 s10 × 5.00 g mol
nuclei10022.6
g241
mol1 23
= 6.35 × 1011
decays/s
6.35 × 1011
alpha particles are emitted each second from a 5.00-g 241
Am sample.
16. Kr-81 is most stable because it has the longest half-life, whereas Kr-73 is hottest (least stable)
since it has the shortest half-life.
12.5% of each isotope will remain after 3 half-lives:
For Kr73: t = 3(27 s) = 81 seconds
For Kr74: t = 3(11.5 min) = 34.5 minutes
For Kr76: t = 3(14.8 h) = 44.4 hours
For Kr81: t = 3(2.1 × 105 yr) = 6.3 × 10
5 years
17. 175 mg Na332
PO4 4
32
3
32
PONamg0.165
Pmg0.32 = 33.9 mg
32P;
2/1t
2lnk
d3.14
)d0.35(6931.0
mg9.33
mln,
t
t)6931.0(kt
N
Nln
2/10
; carrying extra sig. figs.:
ln(m) = 1.696 + 3.523 = 1.827, m = e1.827
= 6.22 mg 32
P remains
18. ktN
Nln
0
; k = (ln 2)/t1/2 ; N = 0.001 × N0
,yr100,24
t)2(ln
N
N001.0ln
0
0
ln(0.001) = (2.88 × 105
)t, t = 200,000 years
19.
0
0
0 N
N17.0ln,
yr3.12
t)2(lnkt
N
Nln (5.64 × 102
)t, t = 31.4 years
It takes 31.4 years for the tritium to decay to 17% of the original amount. Hence the watch
stopped fluorescing enough to be read in 1975 (1944 + 31.4).
20. a. 0.0100 Ci × Ci
decays/s107.3 10 = 3.7 × 10
8 decays/s; k =
2/1t
2ln
100% 50% 25% 12.5t1/2
t1/2
t1/2
CHAPTER 20 THE NUCLEUS: A CHEMIST'S VIEW 807
Rate = kN, s
decays107.3 8 =
s3600
h1
h87.2
6931.0 × N, N = 5.5 × 10
12 atoms of
38S
5.5 × 1012
atoms 38
S × Smol
SONamol1
atoms1002.6
Smol138
4
38
2
23
38
= 9.1 × 1012 mol Na2
38SO4
9.1 × 1012 mol Na2
38SO4
4
38
2
4
38
2
SONamol
SONag0.148 = 1.3 × 109
g = 1.3 ng Na238
SO4
b. 99.99% decays, 0.01% left; lnh87.2
t)6931.0(kt
100
01.0
, t = 38.1 hours 40 hours
21. t = 67.0 yr; k = 2/1t
2ln;
0N
Nln = kt =
yr28.9
yr.0(0.6931)67 = 1.61,
0N
N =
1.61e = 0.200
20.0% of the 90
Sr remains as of July 16, 2012.
22. Assuming 2 significant figures in 1/100:
ln(N/N0) = kt; N = (0.010)N0; t1/2 = (ln 2)/k
ln(0.010) = d0.8
t)693.0(
t
t)2(ln
2/1
, t = 53 days
23. a. s3600
h1
h24
d1
d8.12
6931.0
t
2lnk
2/1
= 6.27 × 107 s
1
b. Rate = kN = 6.27 × 107 s
1
mol
nuclei10022.6
g0.64
mol1g100.28
233
Rate = 1.65 × 1014
decays/s
c. 25% of the 64
Cu will remain after 2 half-lives (100% decays to 50% after one half-life
which decays to 25% after a second half-life). Hence 2(12.8 days) = 25.6 days is the time
frame for the experiment.
24. Units for N and N0 are usually number of nuclei but can also be grams if the units are
identical for both N and N0. In this problem, m0 = the initial mass of 47
Ca2+
to be ordered.
31.0d5.4
)d0.2(693.0
m
Caμg0.5ln,
t
t)693.0(kt
N
Nln;
t
2lnk
0
2
2/102/1
808 CHAPTER 20 THE NUCLEUS: A CHEMIST'S VIEW
0m
0.5 = e
−0.31 = 0.73, m0 = 6.8 µg of
47Ca
2+ needed initially
6.8 µg 47
Ca2+
× 247
347
Cagμ0.47
CaCOgμ0.107 = 15 µg
47CaCO3 should be ordered at the minimum.
25. Plants take in CO2 during the photosynthesis process, which incorporates carbon, including 14
C, into its molecules. As long as the plant is alive, the 14
C/12
C ratio in the plant will equal
the ratio in the atmosphere. When the plant dies, 14
C is not replenished because 14
C decays by
beta-particle production. By measuring the 14
C activity today in the artifact and comparing
this to the assumed 14
C activity when the plant died to make the artifact, an age can be
determined for the artifact. The assumptions are that the 14
C level in the atmosphere is
constant or that the 14
C level at the time the plant died can be calculated. A constant 14
C level
is a pure assumption, and accounting for variation is complicated. Another problem is that
some of the material must be destroyed to determine the 14
C level.
26. 238
U has a half-life of 4.5 × 109 years. In order to be useful, we need a significant number of
decay events by 238
U to have occurred. With the extremely long half-life of 238
U, the period of
time required for a significant number of decay events is on the order of 108 years. This is the
time frame of when the earth was formed. 238
U is not useful for aging 10,000-year-old objects
or less because a measurable quantity of decay events has not occurred in 10,000 years or
less. 14
C is good at dating these objects because 14
C has a half-life on the order of 103 years.
14C is not useful for dating ancient objects because of the relatively short half-life; no
discernable amount of 14
C will remain after 108 years.
27. Assuming 1.000 g 238
U present in a sample, then 0.688 g 206
Pb is present. Because 1 mol 206
Pb is produced per mol 238
U decayed:
238
U decayed = 0.688 g Pb Umol
Ug238
Pbmol
Umol1
Pbg206
Pbmol1 = 0.795 g
238U
Original mass 238
U present = 1.000 g + 0.795 g = 1.795 g 238
U
yr105.4
t)693.0(
g795.1
g000.1ln,
t
t)2(lnkt
N
Nln
92/10
, t = 3.8 × 10
9 years
28. a. The decay of 40
K is not the sole source of 40
Ca.
b. Decay of 40
K is the sole source of 40
Ar and no 40
Ar is lost over the years.
c. Kg00.1
Arg95.040
40
= current mass ratio
0.95 g of 40
K decayed to 40
Ar; 0.95 g of 40
K is only 10.7% of the total 40
K that decayed,
or:
(0.107)m = 0.95 g, m = 8.9 g = total mass of 40
K that decayed
CHAPTER 20 THE NUCLEUS: A CHEMIST'S VIEW 809
Mass of 40
K when the rock was formed was 1.00 g + 8.9 g = 9.9 g.
Kg9.9
Kg00.1ln
40
40
yr1027.1
t)6931.0(
t
t)2(lnkt
92/1
, t = 4.2 × 10
9 years
d. If some 40
Ar escaped, then the measured ratio of 40
Ar/40
K would be less than it should
be. We would calculate the age of the rocks to be less than it actually is.
29. t1/2 = 5730 y; k = (ln 2)/t1/2; ln (N/N0) = kt; lnyr5730
t)2(ln
3.15
1.15 , t = 109 years
No; from 14
C dating, the painting was produced during the early 1900s.
30. yr5730
)yr000,15(6931.0
3.15
Nln,
t
t)6931.0(kt
N
Nln
t
2lnk
2/102/1
= 1.8
3.15
N = e
1.8 = 0.17, N = 15.3 × 0.17 = 2.6 counts per minute per g of C
If we had 10. mg C, we would see:
10. mg min
counts026.0
gmin
counts6.2
mg1000
g1
It would take roughly 40 minutes to see a single disintegration. This is too long to wait, and
the background radiation would probably be much greater than the 14
C activity. Thus 14
C
dating is not practical for very small samples.
Energy Changes in Nuclear Reactions
31. ΔE = Δmc2, Δm
28
2223
2 m/s)10(3.00
/smkg103.9
c
EΔ 4.3 × 10
6 kg
The sun loses 4.3 × 106 kg of mass each second. Note: 1 J = 1 kg m
2/s
2.
32. day
h24
h
s3600
kJ
J1000
s
kJ108.1 14
= 1.6 × 1022
J/day
ΔE = Δmc2, Δm
28
22
2 m/s)10(3.00
J101.6
c
EΔ 1.8 × 10
5 kg of solar material provides
1 day of solar energy to the earth.
1.6 × 1022
J g1000
kg1
kJ32
g1
J1000
kJ1 = 5.0 × 10
14 kg of coal is needed to provide the
same amount of energy.
810 CHAPTER 20 THE NUCLEUS: A CHEMIST'S VIEW
33. From the text, the mass of a proton = 1.00728 amu, the mass of a neutron = 1.00866 amu, and
the mass of an electron = 5.486 × 104 amu.
Mass of Fe5626 nucleus = mass of atom mass of electrons = 55.9349 26(0.0005486)
= 55.9206 amu
;Fen30H26 5626
11
11 Δm = 55.9206 amu [26(1.00728) + 30(1.00866)] amu
= 0.5285 amu
ΔE = Δmc2 = 0.5285 amu
amu
kg106605.1 27 (2.9979 × 10
8 m/s)
2 = 7.887 × 1011 J
nucleons56
J10887.7
Nucleon
energyBinding 11
1.408 × 1012 J/nucleon
34. For H21 : mass defect = Δm = mass of H2
1 nucleus mass of proton mass of neutron. The
mass of the 2H nucleus will equal the atomic mass of
2H minus the mass of the electron in an
2H atom. From the text, the pertinent masses are: me = 5.49 × 104
amu, mp = 1.00728 amu,
and mn = 1.00866 amu.
Δm = 2.01410 amu 0.000549 amu (1.00728 amu + 1.00866 amu) = 2.39 × 103 amu
ΔE = Δmc2 = 2.39 × 103
amu × amu
kg106605.1 27× (2.998 × 10
8 m/s)
2
= 3.57 × 1013 J
nucleons2
J1057.3
Nucleon
energyBinding 13
1.79 × 1013 J/nucleon
For H31 : Δm = 3.01605 0.000549 [1.00728 + 2(1.00866)] = 9.10 × 103
amu
ΔE = 9.10 × 103 amu ×
amu
kg106605.1 27 × (2.998 × 10
8 m/s)
2 = 1.36 × 1012
J
nucleons3
J1036.1
Nucleon
energyBinding 12
4.53 × 1013 J/nucleon
35. Let me = mass of electron; for 12
C (6e, 6p, 6n): mass defect = Δm = [mass of 12
C nucleus]
[mass of 6 protons + mass of 6 neutrons]. Note: Atomic masses given include the mass of the
electrons.
Δm = 12.00000 amu 6me [6(1.00782 me) + 6(1.00866)]; mass of electrons cancel.
Δm = 12.00000 [6(1.00782) + 6(1.00866)] = 0.09888 amu
CHAPTER 20 THE NUCLEUS: A CHEMIST'S VIEW 811
ΔE = Δmc2 = 0.09888 amu
amu
kg106605.1 27 (2.9979 × 10
8 m/s)
2
= 1.476 × 1011 J
nucleons12
J10476.1
Nucleon
energyBinding 11
1.230 × 1012 J/nucleon
For 235
U (92e, 92p, 143n):
Δm = 235.0439 92me [92(1.00782 me) + 143(1.00866)] = 1.9139 amu
ΔE = Δmc2 = 1.9139 ×
amu
kg1066054.1 27 (2.99792 × 10
8 m/s)
2 = 2.8563 × 1010
J
nucleons235
J108563.2
Nucleon
energyBinding 10
1.2154 × 1012 J/nucleon
Because 56
Fe is the most stable known nucleus, the binding energy per nucleon for 56
Fe
(1.408 × 1012 J/nucleon) will be larger than that of
12C or
235U (see Figure 20.9 of the text).
36. Let mLi = mass of 6Li nucleus; an
6Li nucleus has 3p and 3n.
0.03434 amu = mLi (3mp + 3mn) = mLi [3(1.00728 amu) + 3(1.00866 amu)]
mLi = 6.01348 amu
Mass of 6Li atom = 6.01348 amu + 3me = 6.01348 + 3(5.49 × 410 amu) = 6.01513 amu
(includes mass of 3 e)
37. Binding energy = nucleon
J10326.1 12 × 27 nucleons = 3.580 × 1110 J for each
27Mg nucleus
ΔE = Δmc2, Δm =
2c
EΔ =
28
11
)m/s109979.2(
J10580.3
= 3.983 2810 kg
Δm = 3.983 2810 kg × kg106605.1
amu127
= 0.2399 amu = mass defect
Let mMg = mass of 27
Mg nucleus; an 27
Mg nucleus has 12 p and 15 n.
0.2399 amu = mMg (12mp + 15mn) = mMg [12(1.00728 amu) + 15(1.00866 amu)]
mMg = 26.9764 amu
Mass of 27
Mg atom = 26.9764 amu + 12me, 26.9764 + 12(5.49 × 410 amu) = 26.9830 amu
(includes mass of 12 e)
812 CHAPTER 20 THE NUCLEUS: A CHEMIST'S VIEW
38. ;eHHH 01
21
11
11 Δm = (2.01410 amu - me + me) 2(1.00782 amu me)
Δm = 2.01410 2(1.00782) + 2(0.000549) = 4.4 × 104 amu for two protons reacting
When 2 mol protons undergo fusion, Δm = 4.4 × 104 g.
ΔE = Δmc2 = 4.4 × 107
kg × (3.00 × 108 m/s)
2 = 4.0 × 10
10 J
g01.1
mol1
protonsmol2
J100.4 10
= 2.0 × 1010
J/g of hydrogen nuclei
39. ;nHeHH 10
42
31
21 mass of electrons cancel when determining Δm for this nuclear
reaction.
Δm = [4.00260 + 1.00866 - (2.01410 + 3.01605)] amu = 1.889 × 102 amu
For the production of 1 mol of :He42 Δm = 1.889 × 102
g = 1.889 × 105 kg
ΔE = Δmc2 = 1.889 × 105
kg × (2.9979 × 108 m/s)
2 = 1.698 × 10
12 J/mol
For one nucleus of :He42
nuclei100221.6
mol1
mol
J10698.123
12
= 2.820 × 1012
J/nucleus
40. Δm = 2(5.486 × 104 amu) = 1.097 × 103
amu
ΔE = Δmc2 = 1.097 × 10
-3 amu ×
amu
kg106605.1 27 × (2.9979 × 10
8 m/s)
2
= 1.637 × 1013 J
Ephoton = 1/2 (1.637 × 1013 J) = 8.185 × 1014
J = hc/λ
λ
J10185.8
m/s109979.2sJ106261.6
E
hc14
834
2.427 × 1012 m = 2.427 × 103
nm
Detection, Uses, and Health Effects of Radiation
41. The Geiger-Müller tube has a certain response time. After the gas in the tube ionizes to
produce a "count," some time must elapse for the gas to return to an electrically neutral state.
The response of the tube levels out because at high activities, radioactive particles are
entering the tube faster than the tube can respond to them.
CHAPTER 20 THE NUCLEUS: A CHEMIST'S VIEW 813
42. Not all the emitted radiation enters the Geiger-Müller tube. The fraction of radiation entering
the tube must be constant for a meaningful measurement.
43. In order to sustain a nuclear chain reaction, the neutrons produced by the fission process must
be contained within the fissionable material so that they can go on to cause other fissions.
The fissionable material must be closely packed together to ensure that neutrons are not lost
to the outside. The critical mass is the mass of material in which exactly one neutron from
each fission event causes another fission event so that the process sustains itself. A
supercritical situation occurs when more than one neutron from each fission event causes
another fission event. In this case the process rapidly escalates, and the heat buildup causes a
violent explosion.
44. No, coal fired power plants also pose risks. A partial list of risks are:
Coal Nuclear
Air pollution Radiation exposure to workers
Coal mine accidents Disposal of wastes
Health risks to miners Meltdown
(black lung disease) Terrorists
45. Fission: Splitting of a heavy nucleus into two (or more) lighter nuclei.
Fusion: Combining two light nuclei to form a heavier nucleus.
The maximum binding energy per nucleon occurs at Fe. Nuclei smaller than Fe become
more stable by fusing to form heavier nuclei closer in mass to Fe. Nuclei larger than Fe form
more stable nuclei by splitting to form lighter nuclei closer in mass to Fe.
46. The temperatures of fusion reactions are so high that all physical containers would be
destroyed. At these high temperatures, most of the electrons are stripped from the atoms. A
plasma of gaseous ions is formed that can be controlled by magnetic fields.
47. Moderator: Slows the neutrons to increase the efficiency of the fission reaction.
Control rods: Absorbs neutrons to slow or halt the fission reaction.
48. For fusion reactions, a collision of sufficient energy must occur between two positively
charged particles to initiate the reaction. This requires high temperatures. In fission, an
electrically neutral neutron collides with the positively charged nucleus. This has a much
lower activation energy.
49. All evolved oxygen in O2 comes from water and not from carbon dioxide.
50. Radiotracer: a radioactive nuclide introduced into an organism for diagnostic purposes whose
pathway can be traced by monitoring its radioactivity. 14
C and 32
P work well as radiotracers
because the molecules in the body contain carbon and/or phosphorus; they will be
incorporated into the worker molecules of the body easily, which allows monitoring of the
pathways of these worker molecules.
814 CHAPTER 20 THE NUCLEUS: A CHEMIST'S VIEW
51. (i) and (ii) mean that Pu is not a significant threat outside the body. Our skin is sufficient to
keep out the α particles. If Pu gets inside the body, it is easily oxidized to Pu4+
(iv), which is
chemically similar to Fe3+
(iii). Thus Pu4+
will concentrate in tissues where Fe3+
is found,
including the bone marrow, where red blood cells are produced. Once inside the body, α
particles can cause considerable damage.
52. Even though gamma rays penetrate human tissue very deeply, they are very small and cause
only occasional ionization of biomolecules. Alpha particles, because they are much more
massive, are very effective at causing ionization of biomolecules; these produce a dense trail
of damage once they get inside an organism.
53. A nonradioactive substance can be put in equilibrium with a radioactive substance. The two
materials can then be checked to see whether all the radioactivity remains in the original
material or if it has been scrambled by the equilibrium.
54. Water is produced in this reaction by removing an OH group from one substance and an H
from the other substance. There are two ways to do this:
Because the water produced is not radioactive, methyl acetate forms by the first reaction
where all of the oxygen-18 ends up in methyl acetate.
55. Some factors for the biological effects of radiation exposure are:
a. The energy of the radiation. The higher the energy, the more damage it can cause.
b. The penetrating ability of radiation. The ability of specific radiation to penetrate human
tissue where it can do damage must be considered.
c. The ionizing ability of the radiation. When biomolecules are ionized, their function is
usually disturbed.
d. The chemical properties of the radiation source. Specifically, can the radioactive
substance be readily incorporated into the body, or is the radiation source inert
chemically so that it passes through the body relatively quickly.
90
Sr will be incorporated into the body by replacing calcium in the bones. Once incorporated, 90
Sr can cause leukemia and bone cancer. Krypton is chemically inert, so it will not be
incorporated into the body.
18+ HO HCH3C OCH3
O
18+ H OCH3CH3C OH
O
H OHCH3CO CH3
O
H O CH3 ++CH3CO H
O
ii.
i.
18 18
CHAPTER 20 THE NUCLEUS: A CHEMIST'S VIEW 815
Additional Exercises
56. The third-life will be the time required for the number of nuclides to reach one-third of the
original value (N0/3).
0N
Nln = kt =
2/1t
t)6931.0(,
3
1ln = ,
yr4.31
t)6931.0( t = 49.8 years
The third-life of this nuclide is 49.8 years.
57. 20,000 ton TNT Umol
Ug235
J102
Umol1
TNTton
J104235
235
13
2359
= 940 g 235
U 900 g 235
U
This assumes that all of the 235
U undergoes fission.
58. a. Nothing; binding energy is related to thermodynamic stability, and is not related to
kinetics. Binding energy indicates nothing about how fast or slow a specific nucleon
decays.
b. 56
Fe has the largest binding energy per nucleon, so it is the most stable nuclide. 56
Fe has
the greatest mass loss per nucleon when the protons and neutrons are brought together to
form the 56
Fe nucleus. The least stable nuclide shown, having the smallest binding
energy per nucleon, is 2H.
c. Fusion refers to combining two light nuclei having relatively small binding energies per
nucleon to form a heavier nucleus which has a larger binding energy per nucleon. The
difference in binding energies per nucleon is related to the energy released in a fusion
reaction. Nuclides to the left of 56
Fe can undergo fusion.
Nuclides to the right of 56
Fe can undergo fission. In fission, a heavier nucleus having a
relatively small binding energy per nucleon is split into two smaller nuclei having larger
binding energy per nucleons. The difference in binding energies per nucleon is related to
the energy released in a fission reaction.
59. Assuming that the radionuclide is long lived enough that no significant decay occurs during
the time of the experiment, the total counts of radioactivity injected are:
0.10 mL × mL
cpm100.5 3 = 5.0 × 10
2 cpm
Assuming that the total activity is uniformly distributed only in the rat’s blood, the blood
volume is:
V × mL
cpm48 = 5.0 × 10
2 cpm, V = 10.4 mL = 10. mL
816 CHAPTER 20 THE NUCLEUS: A CHEMIST'S VIEW
60. Mass of nucleus = atomic mass – mass of electron = 2.01410 amu – 0.000549 amu
= 2.01355 amu
urms =
2/1
M
RT3
=
1/2711
)g1000/kg1(g01355.2
)K104)(molKJ3145.8(3
= 7 × 105 m/s
KEavg =
amu
kg1066.1amu01355.2
2
1mu
2
1 272 (7 × 10
5 m/s)
2 = 8 × 1610 J/nucleus
We could have used KEave = (3/2) RT to determine the same average kinetic energy.
61. N = 180 lb Cg14
Cmol1
Cg100
Cg106.1
bodyg100
Cg18
lb
g6.45314
141410
Cnuclei100.1Cmol
Cnuclei10022.6 1415
14
1423
Rate = kN; k = 112
1/2
s108.3s3600
h1
h24
d1
d365
yr1
yr5730
693.0
t
2ln
Rate = kN; k = decays/s3800C)nuclei101.0(s103.8 1415112
A typical 180 lb person produces 3800 beta particles each second.
62. a. 12
C; it takes part in the first step of the reaction but is regenerated in the last step. 12
C is
not consumed, so it is not a reactant.
b. 13
N, 13
C, 14
N, 15
O, and 15
N are the intermediates.
c. ;e2HeH4 01
42
11 ; Δm = 4.00260 amu 2me + 2me [4(1.00782 amu me)]
Δm = 4.00260 4(1.00782) + 4(0.000549) = 0.02648 amu for four protons reacting
For 4 mol of protons, Δm = 0.02648 g, and ΔE for the reaction is:
ΔE = Δmc2 = 2.648 × 10
-5 kg × (2.9979 × 10
8 m/s)
2 = 2.380 × 10
12 J
For 1 mol of protons reacting: Hmol4
J10380.21
12 = 5.950 × 10
11 J/mol
1H
63. The only product in the fast-equilibrium step is assumed to be N16
O18
O2, where N is the
central atom. However, this is a reversible reaction where N16
O18
O2 will decompose to NO
and O2. Because any two oxygen atoms can leave N16
O18
O2 to form O2, we would expect (at
equilibrium) one-third of the NO present in this fast equilibrium step to be N16
O and two-
thirds to be N18
O. In the second step (the slow step), the intermediate N16
O18
O2 reacts with
CHAPTER 20 THE NUCLEUS: A CHEMIST'S VIEW 817
the scrambled NO to form the NO2 product, where N is the central atom in NO2. Any one of
the three oxygen atoms can be transferred from N16
O18
O2 to NO when the NO2 product is
formed. The distribution of 18
O in the product can best be determined by forming a
probability table.
N16
O (1/3) N18
O (2/3) 16
O (1/3) from N16
O18
O2 N16
O2 (1/9) N18
O16
O (2/9) 18
O (2/3) from N16
O18
O2 N16
O18
O (2/9) N18
O2 (4/9)
From the probability table, 1/9 of the NO2 is N16
O2, 4/9 of the NO2 is N18
O2, and 4/9 of the
NO2 is N16
O18
O (2/9 + 2/9 = 4/9). Note: N16
O18
O is the same as N18
O16
O. In addition,
N16
O18
O2 is not the only NO3 intermediate formed; N16
O218
O and N18
O3 can also form in the
fast-equilibrium first step. However, the distribution of 18
O in the NO2 product is the same as
calculated above, even when these other NO3 intermediates are considered.
64. Characteristic frequencies of energies emitted in a nuclear reaction suggest that discrete
energy levels exist in the nucleus. Extra stability of certain numbers of nucleons and the
predominance of nuclei with even numbers of nucleons suggests that the nuclear structure
might be described by using quantum numbers.
Challenge Problems
65. mol I = counts100.5
minImol1
min
counts3311
= 6.6 × 10
11 mol I
[I] =
L150.0
Imol106.6 11 = 4.4 × 1010
mol/L
Hg2I2(s) Hg22+
(aq) + 2 I(aq) Ksp = [Hg2
2+][I
]
2
Initial s = solubility (mol/L) 0 0
Equil. s 2s
From the problem, 2s = 4.4 × 1010 mol/L, s = 2.2 × 1010
mol/L.
Ksp = (s)(2s)2 = (2.2 × 1010
)(4.4 × 1010)
2 = 4.3 × 1029
66. a. From Table 11.1: 2 H2O + 2 e
- → H2 + 2 OH
- E° = -0.83 V
oZr
oOH
ocell EEE
2 = -0.83 V + 2.36 V = 1.53 V
Yes, the reduction of H2O to H2 by Zr is spontaneous at standard conditions because
ocellE > 0.
818 CHAPTER 20 THE NUCLEUS: A CHEMIST'S VIEW
b. (2 H2O + 2 e H2 + 2 OH
) × 2
Zr + 4 OH ZrO2H2O + H2O + 4 e
3 H2O(l) + Zr(s) 2 H2(g) + ZrO2H2O(s)
c. ΔG° = nFE° = (4 mol e)(96,485 C/mol e
)(1.53 J/C) = 5.90 × 10
5 J = 590. kJ
E = E° n
0591.0log Q; at equilibrium, E = 0 and Q = K.
E° = n
0591.0log K, log K =
0591.0
)53.1(4 = 104, K 10
104
d. 1.00 × 103 kg Zr
Zrmol
Hmol2
Zrg22.91
Zrmol1
kg
g1000 2 = 2.19 × 104 mol H2
2.19 × 104 mol H2
2
2
Hmol
Hg016.2 = 4.42 × 10
4 g H2
atm0.1
)K1273)(molKatmL08206.0)(mol1019.2(
P
nRTV
114
2.3 × 106 L H2
e. Probably yes; less radioactivity overall was released by venting the H2 than what would
have been released if the H2 exploded inside the reactor (as happened at Chernobyl).
Neither alternative is pleasant, but venting the radioactive hydrogen is the less unpleasant
of the two alternatives.
67. k =
02/1 N
Nln;
t
2ln
1/2t
(0.693)tkt
For 238
U: 50.0eN
N,693.0
yr105.4
)yr105.4)(693.0(
N
Nln 693.0
09
9
0
For 235
U: 012.0eN
N,39.4
yr101.7
)yr105.4)(693.0(
N
Nln 39.4
08
9
0
If we have a current sample of 10,000 uranium nuclei, 9928 nuclei of 238
U and 72 nuclei of 235
U are present. Now let’s calculate the initial number of nuclei that must have been present
4.5 × 109 years ago to produce these 10,000 uranium nuclei.
For 238
U: nucleiU100.250.0
nuclei9928
50.0
NN,50.0
N
N 23840
0
CHAPTER 20 THE NUCLEUS: A CHEMIST'S VIEW 819
For 235
U: nucleiU100.6012.0
nuclei72
012.0
NN 2353
0
So 4.5 billion years ago, the 10,000-nuclei sample of uranium was composed of 2.0 × 104
238U nuclei and 6.0 × 10
3
235U nuclei. The percent composition 4.5 billion years ago would
have been:
100nucleitotal)100.2100.6(
nucleiU100.243
2384
= 77%
238U and 23%
235U
68. a. 23892 U → 222
86 Rn + ? 42 He + ? e0
1 ; to account for the mass number change, four alpha
particles are needed. To balance the number of protons, two beta particles are needed.
222
86 Rn → 42 He + 218
84 Po; polonium-218 is produced when 222
Rn decays.
b. Alpha particles cause significant ionization damage when inside a living organism.
Because the half-life of 222
Rn is relatively short, a significant number of alpha particles
will be produced when 222
Rn is present (even for a short period of time) in the lungs.
c. 22286 Rn → 4
2 He + 21884 Po; 218
84 Po → 42 He + 214
82 Pb; polonium-218 is produced when
radon-222 decays. 218
Po is a more potent alpha-particle producer because it has a much
shorter half-life than 222
Rn. In addition, 218
Po is a solid, so it can get trapped in the lung
tissue once it is produced. Once trapped, the alpha particles produced from polonium-
218 (with its very short half-life) can cause significant ionization damage.
d. Rate = kN; rate = Ci
sdecays/107.3
pCi
Ci101
L
pCi0.4 1012
= 0.15 decays s1
L1
k = s3600
h1
h24
d1
d82.3
6391.0
t
2ln
2/1
= 2.10 × 16 s10
N = 16
11
s1010.2
Lsdecays15.0
K
rate
= 7.1 × 10
4 atoms
222Rn/L
atoms106.02
Rnmol1
L
Rn atoms107.123
2222224
= 1.2 × 1910 mol
222Rn/L
69. 21 H +
21 H → 4
2 He; Q for 21 H = 1.6 ×
1910 C; mass of deuterium = 2 amu.
E = r
)QQ(C/mJ100.9 2129
= m102
)C106.1(C/mJ100.915
21929
= 1 × 1310 J per alpha particle
KE = 1/2 mv2; 1 × 1310 J = 1/2 (2 amu × 1.66 × 2710 kg/amu)v
2, v = 8 × 10
6 m/s
820 CHAPTER 20 THE NUCLEUS: A CHEMIST'S VIEW
From the kinetic molecular theory discussed in Chapter 5:
urms =
2/1
M
RT3
where M = molar mass in kilograms = 2 × 310 kg/mol for deuterium
8 × 106 m/s =
2/1
3
11
kg102
)T)(molKJ3145.8(3
, T = 5 × 109 K
70. Total activity injected = 86.5 × 103
Ci
Activity withdrawn OHmL
Ci108.1
OHmL2.0
Ci106.3
2
6
2
6
Assuming no significant decay occurs, then the total volume of water in the body multiplied
by 1.8 × 106
Ci/mL must equal the total activity injected.
V × OHmL
Ci108.1
2
6 = 8.65 × 10
2 Ci, V = 4.8 × 10
4 mL H2O
Assuming a density of 1.0 g/mL for water, the mass percent of water in this 150-lb person is:
100lb150
g6.453
lb1
mL
OHg0.1OHmL108.4 2
24
= 71%
71. a. For a gas, uavg = 8RT/πR where M is the molar mass in kg. From the equation, the
lighter the gas molecule, the faster is the average velocity. Therefore, 235
UF6 will have
the greater average velocity at a certain temperature because it is the lighter molecule.
b. From Graham’s law (see Section 5.7 of the text):
g/mol03.349
g/mol05.352
)UF(M
)UF(M
UFforratediffusion
UFforratediffusion
6235
6238
6238
6235
= 1.0043
Each diffusion step increases the 235
UF6 concentration by a factor of 1.0043. To
determine the number of steps to get to the desired 3.00% 235
U, we use the following
formula:
6
238
6235
N
6238
6235
UF0.97
UF00.3)0043.1(
UF3.99
UF700.0
original ratio final ratio
where N represents the number of steps required.
CHAPTER 20 THE NUCLEUS: A CHEMIST'S VIEW 821
Solving (and carrying extra sig. figs.):
(1.0043)N =
9.67
9.297 = 4.387, N log(1.0043) = log(4.387)
N = 310863.1
6422.0
= 345 steps
Thus 345 steps are required to obtain the desired enrichment.
c. 98500
15265358.1
UF
UF,
152610000.1
1526)0043.1(
UF
UF
6238
6235
5
100
6238
6235
original ratio final ratio
6
238
6235
UF
UF = 1.01 × 10
2 = initial 235
U to 238
U atom ratio
72. 5826 Fe + 2 1
0 n → 6027 Co + ?; in order to balance the equation, the missing particle has no
mass and a charge of 1; this is an electron.
An atom of 6027 Co has 27 e, 27 p, and 33 n. The mass defect of the
60Co nucleus is:
m = (59.9338 – 27me) – [27(1.00782 – me) + 33(1.00866)] = 0.5631 amu
E = mc2 = 0.5631 amu ×
amu
kg106605.1 27 × (2.9979 × 10
8 m/s)
2 = 8.403 × 1110 J
Nucleon
energyBinding =
nucleons60
J10403.8 11 = 1.401 × 1210 J/nucleon
The emitted particle was an electron, which has a mass of 9.109 × 3110 kg. The deBroglie
wavelength is:
mv
hλ =
)s/m10998.290.0(kg10109.9
sJ10626.6831
34
= 2.7 × 1210 m