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Radiochemistry & Imaging Science
Roger Alberto, Jason P. Holland, Henrik BrabandDepartment of ChemistryUniversity of Zürich
CHE 438
Course overview
1. Short Historical Background2. The Atomic Nucleus
• General features• Nuclear stability, modes of decay• Nuclear forces• Nuclear states
3. Unstable Nuclides• Chart of isotopes• Law of decay• Types of decay• a-decay• b--decay / b+-decay / e-capture• g-radiation / iosomeric transitions• Internal conversion IC / Auger electrons• Other decays• Natural decay series 2
Course overview
4. Laws of Radioactive Decays• Parent-daughter relationships• Transient and secular equilibria• Radionuclide Generators
5. Interaction of Ionizing Radiation with Matter• Ionization with electrons• Bremsstrahlung• Photo effect• Compton scattering• Pair formation
6. Biological Action of Ionizing Radiation• Dose / Doserate• Shielding / Calculations• Dose calculations
3
Course overview
7. 99m-Technetium• Chemistry / Radiochemistry
8. Synthesis of Elements• Synthesis of transactinides / super heavy elements• Synthesis of the chemical elements: Nucleosynthesis
4
Historical Background
5
Atomic theory
Leukipp (about 450 b.C.): creates the expression „atomos“
Demokrit (ca 460 – 400 b. C.): Atomic theory
“Nur der Meinung nach gibt es süss, bitter, warm, kalt, Farbe, in Wahrheit gibt es Atome und leeren Raum”
“Atoms and Void“
Historical Background
6
“Ausserdem sind die kompakten Atomkörperchen, aus welchen die Stoff-zusammensetzungen entstehen und in welche sie sich auflösen, unerfasslichin Bezug auf die Verschiedenheit ihrer Formen......”
“Die Atome bewegen sich fortwährend,......die einen schweben dabei weitauseinan der, die anderen führen eine Schwingung am Ort aus, wenn sieetwa in einer Stoffverbindung verflochten und eingeschlossen sind.....”
Epikur (341 – 271 b.C): summarized Demokrit‘s theses (letter to Herodot)
J.C. Magien (1590 – 1679): Revival of Demokrit
Oft beobachtet, dass ein Weihrauchkorn durch Verbrennen das 8x108-fache seines Volumen (von Erbsengrösse auf Zimmergrösse) gleichmässig mit Duft erfüllt. Einerbsengrosses Volumen könnte mechanisch in ca. 103 noch sichtbare Teilchen geteiltwerden, jedes dieser Teilchen besteht sicher noch aus mindestens 106 Atomen.Beigleichmässiger Verteilung muss das Weihrauchkorn aus 8x108x103x106 ³ 8x1017
Atomen bestehen.
Historical Background
7
W.C. Röntgen (1896): X-rays
“MM. les Drs. Oudin et Barthélemy communiquent unephotographie des os de la main, obtenue à l’aide des “X-Strahlen” de M. le professeur Röntgen.”
c. r. 122, 1896, 150, séance du lundi 20 janvier 1896
A.H. Becquerel (1852 - 1908): Uranium rays
“...l’origine de ces expériences avait été l’idée de rechercher si les corps phosphor-escents, après avoir été excités par la lumière, émettaient des rayons pénétrants.”
In contrast to Röntgen‘s X-rays, the report of Becquerel did not find any interestand Becquerel stopped publishing anything for a long time!
Historical Background
8
Within 3 months, Becquerel found that K2SO4UO2SO4, a phosphorescingsubstance (t1/2 = 0.01 s) emits invisible, strongly penetrating radiation
“On doit donc conclure de ces expériences que la substance phophorescenteen question émet des radiations qui traversent le papier opaque à la lumièreet réduisent les sels d’argent.”
“On peut vérifier très simplement que les radiations émises par cette substance, quand elle est exposée au soleil ou à la lumière diffuse du jour, traversent, non seulement des feuilles de papier noir, mais encore divers métaux....”
A.H. Becquerel (1852 - 1908): Uranium rays
Historical Background
9
... and then that sunlight is not necessary at all !
“J’insisterai particulièrement sur le fait suivant, qui me paraît tout à fait important et en dehors des phénomènes que l’on pouvait s’attendre à observer: Les mêmes lamellescristallines...mais à l’abri de l’excitation des radiations incidentes et maintenues à l’obscurité produisent encore les mêmes impressions photographiques....Quelques-unes avaient été préparées le mercredi 26 et le jeudi 27 février et, commeces jours-là, le soleil ne s’est montré que d’une manière intermittante, j’avaisconservé les expériences.... dans le tiroir d’un meuble, en laissant en place les lamel-les du sel d’uranium. Le solei ne s’étant montré de nouveau les jours suivants, j’aidéveloppé les plaques photographiques le ler mars, en m’attendant à trouver des images très faibles. Les silhouettes apparurent, au contraire, avec une grandeintensité.“
A.H. Becquerel (1852 - 1908): Uranium rays
Historical Background
10
A.H. Becquerel (1852 - 1908): Uranium rays
In contrast to Röntgen‘s experiment‘s, reproduction of Becquerel‘s was rare.
“Hence the writer ventures to give to the new phenomenon thus independently observed by M. Becquerel and by himself the name of hyperphosphorescence. A hyperphosphorescent body is one which, after due stimulus, exhibits a persistent emission of invisible rays not included in the hitherto recognized spectrum.”
1. Die Angaben Becquerels bezüglich der physikalischen Eigenschaften der dunkeln, von Uransalzen ausgehenden Strahlen fanden wir, soweit wir sie prüften, durchweg bestätigt.
2. Die Energiequelle der diese Strahlen entstammen ist noch vollständig dunkel. Monatelanges Aufbewahren des Salzes unter Lichtabschluss vermindert die Strahlungsintensität nicht merklich.”
S. P. Thompson, On hyperphosphorescence, Phil. Mag. (5) 42, 1896, 128-135J. Elster, H. Geitel, Versuche über die Hyperphosphoreszenz10. Jahresber. Ver. Naturw. Braunschweig 10, 1897, 157
Historical Background
11
The first new elements 1898
“Nous croyons donc que la substance que nous avons retirée de la pechblende contient un métal se confirme, nous proposons de ’appeler polonium, du nom du pay d’origine du l’un de nous.”
“On réalise ainsi une source de lumière, à vrai dire très faible, mais qui fonctionnnesans source dénergie. Il y a là une contradiction, tout au moins apparente, avec le principe de Carnot.”
Accumulation of radium from pitchblend was very tedious, unknown problems emerged
- radioactivity of fresh samples increases steadily- nearby compounds start becoming radioactive
Polonium 4n+2 Po-210 138.38 d
Radium 4n+2 Ra-226 1600 y
Historical Background
12
F. Giesel (1852 – 1927): Excellent experimentalist
- fresh solid radium compounds increase in activity, solution activity decreases
- formation of coloured centers in crystals after irradiation
- physiological action of radiation
“Ich habe 0.27g Radium-Baryum-Bromid in doppelter Celluloidkapsel 2 Stunden auf die Innenfläche des Armes gelegt. Anfangs war nur eine schwache Rötung vorhanden; nach 2-3 Wochen stellte sich starke Entzündung mit Pigmentierung und schliesslich....Abstossung der Oberhaut ein, worauf bald Heilung erfolgte.”
“Als bequeme Kontrolle der fortschreitenden Reinigung benutzt man die Färbung der Bunsenflamme.”
Historical Background
13
Actinium 4n+3 Ac-227 21.77 y
Debierne finds a new activity (1899), chemically related to lanthanum
Giesel confirms finding 1902 (it produces emanation) and called it „Emanium“
Debierne wins, hence, the name „Actinium“ remains
Emanation and induced radioactivity
Emanation: Rn-222 4n+2 3.825 d U-238Rn-219 4n+3 3.96 s U-235Rn-220 4n 55.6 s Th-222
Historical Background
14
The nature of emanation remains mysterious:
Owens and Rutherford (1899): “It was very early observed that the radiation from thorium oxide was not constant, but varied in a most carpicious manner. This was the more peculiar as the sulphate and the nitrate were fairly constant. All the compounds of uranium give out a radiation which remains remarkably constant..... The sensitiveness of thorium oxide to slight currents of air is very remarkable and made it difficult to work with... A large number of experiments of various kinds have been tried, but so far, no clue has been obtained as to why this action should be so manifest in thorium oxide......”
Giesel (1903): “Legt man ein Filter mit einigen Centigrammen der Substanz auf den Schirm, so verbreitet sich die Emanation auf grössere Strecken desselben und erzeugt ein durch den leisesten Luftstrom hin- und herwogendes Phosphorescenzlicht.”
“Ein Gas scheint die Emanation jedenfalls nicht zu sein, wenigstens wurde unter Wasser keine Gasentwicklung von der Substanz bemerkt.
E. Rutherford, R. B. Owens, Thorium and uranium radiation, Trans. Roy. Soc. Canada (3) 2, 1899, 9-12F. Giesel Über Radium und radioaktive Stoffe Ber. 35, 1902, 3608 1
The Atomic Nucleus
15
neutrons and protons ® Baryonselectrons and neutrinos ® Leptons
p+ and p- Mesons are responsible for the attractive forces betweenp and n or n and p respectively.
p- / p+ Meson: 0.15 a.u. @ 273 em t½ = 2 ·10-8 spO Meson: 0.145 a.u. t½ = 10-16 s
p-Mesonen have been detected in cosmic radiation.
exchange forces explain, why neutrons have a magnetic moment.
The Atomic Nucleus
17
The structure of the nucleus is almost a sphere.
range of radii: 3 ·10-15 - 16 · 10-15 m (3 fm – 16 fm)
Original determination by Rutherford with a-particle scattering experiments
The Atomic Nucleus
18
Newer definition through the extremely short range nuclear forces
The potential energy of a p+ approaching the nucleus increases strongly.
At a certain distance (radii of nuclei) nuclear forces start and Epot decreases.
empirical relation: R = ro (9.1 fm für A = 222)
with A = number of nucleous and ro = 1.4 fm (radius of nucleons)
3 A
Atomic Radius
The Atomic Nucleus
19
The density of the nucleus is about 1.5 · 1017 kg/m3
Compare mass of earth: 5.972 · 1024 kg
for A > 16 charge density constant over a certain range
Atomic density
The Atomic Nucleus
20
The mass and charge distribution are constant
Layer of decreasing density (dn ~ 2.5 fm) follows Fermi statistics
For nuclear reactions, a charged nucleon needs to reach that distance to overcome the Coulomb potential.
Charge distribution
The Atomic Nucleus
21
The wall potential can be calculated from Ec if the radius is known.
The wall is 14.7 MeV for a proton
(226Ra, 9Be) C-12 226Ra = 4.8 MeV
Epot(Be) = = 4.25 MeV
first neutron sources !!
Potential wall
Epot = = 29.5 MeV (r = 9.1 fm)
Natural a-particles don‘t have such high energies but nuclear reactions with lighter elements are possible
The Atomic Nucleus
22
follows within a nucleus also the Coulomb potential
nuclear forces go to saturation but Coulomb forces increases
Nucleon-nucleon interactions
Considering 2 p+ with d ~ 3fm
and EC = Þ EPP ~ 0.5 MeV
Þ instability of heavy nuclei
The Atomic Nucleus
23
strong Gluon 1electromagnetic Photon 10-2
weak Boson 10-5
gravitation Graviton 10-40
interaction mediating particle force constant
further fundamental particles
Comparison of the 4 principal forces in nature
Name Symbol Rest mass[u]
Electric charge [units]
Correspondingantiparticle(a)
Up u 0.33 + 2/3
Down d 0.33 - 1/3
Charm c 1.6 + 2/3
Strange s 0.54 - 1/3
Top t 24.2 + 2/3
Bottom b 5.3 - 1/3(a) Electric charge and quantum numbers are opposite to those of the corresponding particles.
The Atomic Nucleus
24
The nucleon-nucleon interaction shown previously resembles the Morse potential for chemical bonds
nucleon interacts with essentially one partner
Binding energies
the mean binding energy is about constant
The Atomic Nucleus
25
E = mc2, 1 u @ 931.5 MeV
with dM = Þ the higher EB, the more stable the nucleus
Empirical calculation of binding energy
Binding energies
MZ,N= Z·M(1H) + N·M(n) - dM
The Atomic Nucleus
26
fission of 238U to 2 equal nuclei of same mass should deliver about 200 · 1 MeV = 200 MeV which is the amount experimentally found
Exact masses are knownfrom high resolution MS
®
7.01822 < 4.0026 + 3.017012 doesn‘t work
® does work
8.0053 > 2 x 4.0026
Binding energies
Stability of a nucleus in respect of a decay can be predicted (as in chemistry)
The Atomic Nucleus
27
Semi-empirical calculation of binding energy
Bohr compared the nucleus with a incompressibel drop of liquidÞ the larger the drop, the less stable it is
Bethe-Weizsäcker: EB = EV + EC + EF + ES + EG
EB = total binding energy of all nucleous
EV = Volume energy = aV·A aV = 15.8 MeV
EC = mutual repulsion = -aC· aC = 0.71 MeV
EF = surface energy = -aF· aF = 17.8 MeV
ES = symmetry energy = -aS· aS = 23.7 MeV
+ 33.6 MeV eeEG = considers ee / oo nucleii = aG/A-3/4 aG = 0 MeV oe / eo
- 33.6 MeV oo
31
2
A
Z
32
A
Binding energies
The Atomic Nucleus
28
The B-W Formula allows calculation of all BE for A > 15 within 1%
example: calculated experimental
235U + 1n ® 236U: binding energy of neutron 6.81 MeV 236U „ ® 237U: „ 5.51 MeV237U „ ® 238U: „ 6.56 MeV 238U „ ® 239U: „ 5.31 MeV
97.947 97.943
51.959 51.956
Binding energies
Þ very useful for unknown nuclides
The Atomic Nucleus
29
The high potential of the B-W Formula can be seen from EB within nuclides with equal A (Isobares)
which yields a parabolic curve (for oe/eo)
the larger A, the flatter the potential pot
if A is kept constant: MZA – M = g (z – z0)2
with g
Binding energies
the more stable nuclides
The Atomic Nucleus
30
This explains:
For even mass numbers we receive two parabolas,
separated by
Z N A type numberse e e ee 162e o o eo 55o e o oe 50o o e oo 5
Statistic of stable nuclides:
Binding energies
why ee nuclides are particularly stableand oo nuclides not
The Atomic Nucleus
31
Binding energiesThe most stable nuclides are close to the maximum EB
Nuclides with odd mass number have only one stable nuclidesThe others along the slope are b- or b+ unstable
1. Rule of Mattauch
The Atomic Nucleus
32
More complex situation with even A (ee and oo nuclides)
2. Rule of Mattauch
Binding energies
depending on the shape of the parabolas, more than one stable nuclide is possible
Nuclides with even mass number frequently have two or three stable Isotopes which atomic numbers must be separated by 2.
The Atomic Nucleus
33
Inspection of isotope chart confirms the rules and explains...
... why 43Tc has no stable nuclides
... why 61Pm has no stable nuclides
and why oo nuclides may decay
with either b- or b+.
K1940
K1940
Ca2040
Ar1840
(stable)
(stable)
0.01%natural abundancet1/2 = 1.28·109y
Binding energies
The Atomic Nucleus
34
Þ most stable nuclides are found for Z = 26 or 28
Inspecting the valley of stability, it looks like a smooth landscape
Binding energies
The stability of a nuclide depends on the sum of Z and N and their relative ratio
The Atomic Nucleus
36
Dark blue line:
A=N+Z
ZN=Z
Electron capture
b- emission
The valley of b-stability
Valley of b-stability
The Atomic Nucleus
45
closer look shows that the energy landscape is rather bumpy with local minima along
Z / N = 2, 8, 20, 28, 50, 82, 126 and
theoretically predicted Z = 114 N = 184
The valley of b-stability
These numbers are called „magic numbers“
The Atomic Nucleus
46
unstable double magic nuclides have a relatively long t½ compared to their neighbors
Magic numbers
elements with magic Z have many stable Isotopes (Sn = 10 Isotopes)
elements with magic N have many stable Isotones
so called „double magic“ nuclides are particularly stable and abundant (Pb – 208, Ca – 40)
The Atomic Nucleus
47
Magic numbers
The observation of particularly stable numbers can be explained with a shell model (similar to electrons).
Filled shells are more stable than partly filled ones.
Unstable Nuclides
48
DE = DM×c2 = [MA-(MB-MX)]c2
If an atomic nucleus is along the wall of the Epot parabola, it canenergetically relax to a lower state according to
An activation barrier has to be surmounted or crossed by quantum mechanical tunneling
A sort of activation energy comparable to chemical first order kinetics
Unstable Nuclides
49
Chart of nuclides
The chart of the nuclides lists all known nuclei together with most important decay data (energy, decay type, daughter nuclide, etc.)
Unstable Nuclides
50
Example 102Rh (oo)-nuclide
left column
metastable nuclidee ³ 95%
conversion electrons £ 5%
right column
ground state nuclide95% £ b+ < 50%5% £ b- < 50%
Rh 102
2,9 a 207 de e
g 475 b+ 1,3631; b- 1,2697... g 475lg (42); e- 628...
Chart of nuclides
Unstable Nuclides
51
Example a-emitter: Pa-230 (oo) nuclide
* The exact numbers are known
less than 5% * (0.003%)5% < e, b+ < 95% * (90%)5% < b- £ 50% * (10%)
Pa 230
17,4 d
Î; b- 0.5...a 5,345; 5,32g 952; 919, 455;899; 444...; sf 150
Chart of nuclides
Unstable Nuclides
52
Vertical green bar: Excited states decay exclusively by spontaneous fission
Cf 252
2,645 a
a 6,118; 6,076...sf
g (43...); e-
s 20; sf 32
Am 241
432,2 a
sf a 5,486; 5,443...
sf; g 60; 26...
e-; gs 50 + 570; sf 3,1
Chart of nuclides
Green: Spontaneous fission in the ground state with emission of neutrons
Unstable Nuclides
53
Radionuclides decay with a first order rate law
A(t) = AO· e-lt
l = decay constant or the probability to decay per unit time
a radionuclide has a certain probability l to decay per unit time
N(t) – N(t + Dt) = N(t) × l × Dt
Law of decay
AO = activity at time t = 0
Unstable Nuclides
54
and if Dt ® 0, we receive
simple first order kineticsN(t) = NO × e-lt
telling us how many „active“ atoms are still around at a certain time point
slightly rearranged gives with e =
and from 1st order kinetics
corresponds to the number of half life times
Law of decay
4.4·10-8 (1:23 millions) better play lotto !!!
Unstable Nuclides
55
l is the important constant
Examples: 99mTc (6h) l = 3.21×10-5 sec-1
3H (12.3y) l = 1.78×10-9 „
14C (5730y) l = 9.66×10-12 „
238U (4.47×109y) l = 4.92×10-18 „
137Cs (30y) l = 7.33×10-10 „
if we look at one single C atom, the probability for its decay in 1 min is
Law of decay
Unstable Nuclides
56
Switching from nuclides to activity: activity = number of decays per time
A(t) =
one of the most useful relationships
A = l×N
1 decay / sec = 1 Bq
Dt ® 0
Law of decay
3.7×1010 Bq = 1 Ci = 37 GBq
Unstable Nuclides
57
l = decay const [sec-1]1st order rate law: NdtdN l=-
integrated: N(t) = NO × e-l×t
compare to activity:
t1/2 = ll69.02ln
=
or N = NO t* = number of half-lives
1280AÞ after 7 t1/2 < 0.1% after 10 t1/2
Law of decay
A(t) = AO × e-l×t and A = l×N
Unstable Nuclides
59
mass of radioactive nuclidesAVNMNm ×
=
if radioactive nuclides are diluted with inactive isotopes
]/[ gBqmAAS =the specific activity AS is then
for some specific applications, no carrier added radionuclides are required
Specific activity
1 MBq 32P = 10-10 g1 MBq 99mTc = 5× 10-12 g
carrier added radionuclides (geträgert)
no carrier added means only radionuclides are present and the specific activity reaches a maximum
Unstable Nuclides
61
Types of decayUnstable nuclides may transform by:
emission of nucleons (a, b-, b+)
leads to an excited state of daughter nuclides0.16
0.04962+
4+
g(0.1105)g(0.1105)
g(0.0496)
Th(24.1d)234
g(0.1105)
a(4.04) 0.23%
a(4.15) 23%
a(4.20) 77%
O U(4.47 1 )× 0 g
0+
0+238 9
0
If „forbidden“, long lived metastable states occur
rarely p or n
capture an electron from the shell
Relaxation with emission of g-rays (< 10-13 sec)
Unstable Nuclides
62
a-Decay
consider: the a-particle has an unusual high binding energy of ~ 28.3 MeV
The total energy of an a-decay is represented by:
DE = (MX - MY - )×c2
EB of is only 2.2 MeV ® „endothermic“ process
chemically spoken, a very stable compound with high DGf°(such as CO2)
Unstable Nuclides
63
Observed for Z > 83 and some nuclides far away of b-stability line
Spontaneous fission starts for high Z (> 92) and begins prevailing for Z > 96 since fission barrier is high, a-decay is still dominant for Z > 106
Bild vorhanden
a-Decay
b-- and b+-decay is observed throughout the nuclide chart
Conditions for e electron capture see later
Unstable Nuclides
64
written in a slightly different way
gives an expression for the decay energy
law of momentum conservation
Z×mpusing
with Q = Ea + EY; EY = Energy of recoiling nucleus
a-Decay
ma × ca = mY × cY
Unstable Nuclides
65
since DE = Ea and ma << mY
the a-particle obtains ~ 98% of the full energy Q
consider that i.e. 2% of 4 MeV is still 80 keV
compounds are completely destroyed after decay due to recoil (compare to b- decay later)
a-Decay
this is much larger than any chemical bond energies
Unstable Nuclides
66
Geiger and Nuttall (1911): empirical relationship between Q and decay constant l
and log l = a logQ + bl =
increasing decay energy leads to increased decay constant and strongly decreasing t1/2
Q varies by a factor of ~ 2,
a-Decay
(a, b constant)
t1/2 by 24 log units
Unstable Nuclides
67
To understand this relationship we must have a look into theory of a-decays
The a-particle is surrounded by a high Potential barrier Epot
much larger than Ea = 4.2 MeV
Epot is!
!
!rZe22
41
×pe
3 A
3 A
= 28.1 MeV for
and R =
Epot = 0.96 × z · Z
a-Decay
Unstable Nuclides
68
Typical a-energies are 4 – 10 MeV
Gamow and Gurney wave mechanics:
EC = 28.0 MeV but Ea » 4.8 MeV
the a-particle has to overcomeFor the reaction
a-Decay
the Coulomb wall, which is about
According to classical physics, not possible
There is a certain probability to find the a-particle outside the pot
Unstable Nuclides
69
Tunneling is the answer
with Epot (r) = potential energy at distance r
from Schrödinger equation:
P decreases with increasing height and extension of the pot
drErEmh
ER
Rpotò -- a
p )(24
P = e
reduced formula: P = e-2gg = e-2G G = Gamow factor
b
rglp2
=a
gEEC=
CC EE
EE aa -- 1, across
lb = de Broglie Wellenlänge for EC and EC = Coulombbarriere
with l = f × P, the decay constant can calculated with f = n/2R = number of collisions with the Potential pot f is usually ~1020 s-1
a-Decay
m = reduced mass- a-particle-recoil nucleus
Unstable Nuclides
70
coming back to Geiger-Nuttall rule
log l = a × log R + b or log t1/2 = - logEa
we can also approximate from the Gamow rule by log l = a - baE
Z22-
a-Decay
Unstable Nuclides
71
a-Spectra
General decay schemes
Excited states are drawn above the ground states of the corresponding element
Daughter products with decreased atomic number A are drawn on the left, with increased A to the right
Unstable Nuclides
72
no third particles are involved for ee nuclides, we frequently find one single line
Consider, that for the true decay energy the recoil energy of the nuclide must be added
a-Spectra
a-spectra show distinct lines since the change of nuclear angular momentumchanges by integers
Unstable Nuclides
73
More complex spectra:
a-Spectra
Decay leads to excited states
Excited states decay very rapidly (<10-10 sec) to ground state
Unstable Nuclides
74
One major decay line and some more weak ones of much higher energy
The mother nuclide possesses some excited states from which decay to ground state of daughter occurs
a-Spectra
Unstable Nuclides
75
Three different b-decays are known:
b-: electron (+ antineutrino)
b+: positron (+ neutrino)
e: electron capture (+ neutrino)
if A is odd, then I = ,...25,
23,
21
Since A doesn‘t change (b-decay) and the electron e- carries away s = 1/2,something else (n) takes the other s = 1/2
b-Decay
Neutrino and antineutrino have different helicity
Neutrino and antineutrino had to be postulated due to the energy conservation laws
In addition: nuclear spin depends on A
if A is even, then I = integer: 0, 1, 2, ...
Unstable Nuclides
76
DE = [M1 – Z1× me – M2 + (Z1 + 1) × me – me]c2
Since neutrino has no mass:
> + meMAZ MAZ 1-
21MA
Z-1MAZ + Z× me > + me +(Z-1) × me
M1 > M2 + 2me
This means, that b+ is only possible if DE = 2×me× c2 ³ 1.022 MeV
b-Decay
Energy conditions for b--decay
= (M1 – M2) c2
taking the masses of nuclides
M1 > M2 + me
Energy conditions for b+-decay
Unstable Nuclides
77
from higher shells ® more energetic, characteristic X-rays
If DE is < 1.022 MeV: we find electron capture e
Energy conditions
b-Decay
for which the same conditions as for a b--decay apply
and >MAZ MAZ 1-DE = (M1 – M2)·c2
some nuclides do both, e and b+
the captured e- from the K-shell are replaced by e-
Unstable Nuclides
78
which is very small compared to DE
Emax = Ee + En
b-Spectra
Emax = Ee + En + EN EN = recoil nucleusmore precise
since Mn >>Me, En is neglectable (for Mn) > 5 u, DE – Emax ~ 0.01%)
for e decay, Ee is the binding energy in the shell
the n gets all the energy
Unstable Nuclides
79
maximum betweendtdN
31
21
Emax and Emax
b-Spectra
The coulomb field of nucleus accelerate b+ Þ low energy b+ particles are rare
b- are attracted by the nucleus Þ many low energy b- particles
Unstable Nuclides
80
The simplest case for b- decay is DE = 0.78 MeVt1/2 = 889 s-1
which is allowed since mn > mH
b- decays often result in excited daughter Þ prompt g-emission might follow
b-Spectra
Unstable Nuclides
81
The nucleus receives essentially no recoil
g-Radiation
g-radiation accompanies the b- (or b+) decay
the g-spectrum of a radionuclide represents its finger print
the nucleus might exist in excited states
The overall occurrence of g-transitions can be calculated
Unstable Nuclides
82
Upon emission of a g-quant, the angular momentum number changes by an integer l since g-quants also have an integer l
Dipolradiation l = 1Quadrapolradiation l = 2Oktopolradiation l = 3
g-Radiation
g-Energies are between 10 keV and 18 MeV.
The probability for a transition depends on the energy of the excited state on the numbers of nucleus and the multipole order of the radiation
Unstable Nuclides
83
between t½ of the excited state and the energy
g-Radiation
for an allowed g-transition there is a relationship (=selection rule)
Unstable Nuclides
85
If the change between Ia and Ie is large, the probability for the transition is low and t½ long
Such long lived isomeric states are very important for medicinal application
Tc 99
6,0 h 2,1×105 a
lg 141... b- 0,3...e- g (90)b- b- 1,2
s 20g (322...)
Isomeric transition (IT)
Unstable Nuclides
86
The t½ of isomeric states can be precisely calculated from a formula developed by Weisskopf et al.
Type of Change of the orbital spin Change ofradiation quantum number, DL the parity
Half-life (s) at energies of
1 MeV 0.2 MeV 0.05MeV
E1 1 Yes 2 × 10-16 3 × 10-14 2 × 10-12
M1 1 No 2 × 10-14 2 × 10-12 2 × 10-10
E2 2 No 1 × 10-11 3 × 10-8 3 × 10-5
M2 2 Yes 9 × 10-10 3 × 10-6 3 × 10-3
E3 3 Yes 7 × 10-7 6 × 10-2 9 × 102
M3 3 No 7 × 10-5 5 8 × 104
E4 4 No 8 × 10-2 2 × 105 4 × 1010
M4 4 Yes 7 1 × 107 4 × 1012
Isomeric transition (IT)
Unstable Nuclides
87
excited nuclides can transfer the full energy „Eg“ to one of the electrons in the shell which is then emitted
IC electrons are monoenergetic Ee = Eg – EK,L,
99mTc [99Tc]+
Such an electron is called a conversion electron
Internal conversion (IC)
Instead of emitting a g-quant:
IC and g-emission compete
Unstable Nuclides
88
Since the electron density increases near the nucleus,IC with K electrons are more likely then with L, M, etc.
The magnitude depends on the shell (K, L, ...)
g
aNNe=
Internal conversion (IC)
The ratio between Ng and NIC is called: Conversion coefficient
Unstable Nuclides
89
Internal conversion is not an internal photo effect
X-ray emission
by emitting further e- from higher shells with low energy „Auger electrons“ or an „Auger cascade“
http://commons.wikimedia.org/wiki/File:Atom_model_for_Auger_process_DE.svg
Internal conversion (IC)
After IC, the „hole“ in the inner shells is filled with e- from outer shells
or
Unstable Nuclides
90
4th decay series has been reactivated by the artificial production of plutonium in nuclear reactors
Cosmic Radiation
Without decay series
20 Radioactive primordial nuclides
Long half-life times
Most important representative 40K
Terrestrial Radiation
From decay series
232Th ® 208Pb235U ® 207Pb238U ® 206Pb241Pu ® 209Bi
Natural RadioactivityProtons (93 %)
a-Particles (6.3 %)
Heavier nuclides (0.7 %)
Unstable Nuclides
91
Secondary radiation 14C: Formation pCnN 11
146
10
147 +®+
Decay eNC 0
1147
146 -+®
3H: Formation CHnN 126
31
10
147 +®+
Decay eHeH 0
132
31 -+®
Energy of the protons can be up to 1014 MeV
Initialization of nuclear reactions 3H, 7Be, 14C, 22Na
t1/2 = 5730 y
t1/2 = 12.32 y
Cosmic RadiationProtons (93 %)
a-Particles (6.3 %)
Heavier nuclides (0.7 %)
Unstable Nuclides
92
Radioactive nuclides without decay series
Electron capture
Nuclide T1/2 Decay Isotopic abundance
187Re 5 x 1010 y ß- 62.60 115In 4.4 x 1014 y ß- 95.7 123Te 1.24 x 1013 y K 0.908 87Rb 4.8 x 1010 y ß- 27.8 113Cd 9.3 x 1015 y ß- 12.2
Other examples
20 Radioactive nuclides
From primordial resources
Very long half-lives
Most important: is 40K (T1/2 = 1.28 x 109 y)
Terrestrial Radiation
Unstable Nuclides
93
232Th ® 208Pb (Thorium family 4n)235U ® 207Pb (Actinium family 4n+3)238U ® 206Pb (Uranium family 4n+2)241Pu ® 209Bi (Neptunium family 4n+1)
Pu/Bi series was decayed in nature due to the relatively short half-life of 237Np (t1/2 = 2.144 ∙106 a)
Cascades of radioactive decays which origin from a certain radioactive nuclide and ends with a certain stable nuclide (lead or bismuth)
Decay series include a-, ß- and g-decays
They can have branches but always end with the same final product
Four natural decay series were established
Natural decay series
Unstable Nuclides
94
232Th ® 208Pb235U ® 207Pb238U ® 206Pb241Pu ® 209Bi
Thorium family Actinium family Neptunium familyUranium family
Crucial element:Radon, inert gascan leave the compartment
Natural decay series
Unstable Nuclides
95
Daughterisotopes in the air
Daughterisotopes in the walls
Daughterisotopes in the soil
Radon is a main source of natural radioactivity
228Rn, 224Rn, 220Rn from 232Th
226Rn, 222Rn from 238U
219Rn from 235U (227Ac series)
Radon is a mobile radioelement
Formation from decay series:
Radon
Unstable Nuclides
97
Durchschnittliche Strahlenbelastung pro Jahr: 3,2 mSv9% kosmische
Strahlung
7% körperinnere Strahlung
13% terristische Strahlung
29% Rn-222 im Mauerwerk
42% Röntgenstrahlung
Mean radiation exposure per year: 3.2 mSv
42%
X-Ray
13% terrestrial
radiation
29% Rn in
building material
9% Rn cosmic
radiation7% internal
radiation
Mean radiation exposure to persons in industrial countries
Natural Radioactivity
Laws of Radioactive Decays
98
or substituted with t1/2
chemical reaction with no reversible steps
BdtdN
dtdB
×--= 21 l gives )( 210
112
12
tt eeNN ×-×- -×-
= ll
lll
úúû
ù
êêë
é÷øö
çèæ-
-=
- )1()2(
1)2/12/1
2/12/12
2/12/1
211
)1(/)2(1)1(/)2( tt
NttttN
Equilibrium N1 = N2 is achieved after a certain time, depending on t½(1) and t½(2)
Equilibria in decay series
Laws of Radioactive Decays
99
For all cases t1/2(A) / t1/2(B) are important
)1( 201
2
1 teNN ll l
l --×= a normal exponential
a) t1/2(A) >> t1/2(B) this is called secular equilibrium
The N(A) / N(B) equation reduces to
http://www.epa.gov/radiation/understand/equilibrium.html
Equilibria in decay series
Laws of Radioactive Decays
100
After t >> t1/2(2) equilibrium is achieved (~ 10 half lives of B)
and at equilibrium)1()2(
2/1
2/1
2
1
1
2
tt
NN
==ll
The activities of mother and all daughters are the same after some time if secular conditions applies
allows determination of very long half lives from daughter products. Explain!
calculation of mass ratios of radionuclides and other applications
Equilibria in decay series
Laws of Radioactive Decays
101
If t1/2(A) » t1/2 (B) but ratio ³5 the equilibrium is called transient
and at equilibrium)()(
)(
2/12/1
2/1
1
2
BtAtBt
NN
-=
daughter activity2
1
22
21
2
1 1ll
ll
-=××
=NN
AA
now all terms have to be considered
http://www.epa.gov/radiation/understand/equilibrium.html
Equilibria in decay series
Laws of Radioactive Decays
102
t1/2(A) < t1/2 (B)
no equilibrium is achieved!
Equilibria in decay series
Laws of Radioactive Decays
103
A ® B ® C ® D ® ...
typically the natural decay series
...+×+×= ×-×- tB
tAn
BA ececN llthe decay law yields
with etc.0
11312
121
))()((...
An
nA Nc ×
---××
= -
lllllllll
úû
ùêë
é--
+--
+--
=---
))(())(())(( 313223211312
01213
321
llllllllllllll
lll ttt eeeNN
which can be rewritten
Successive transformations