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Lectures 1

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1.1 User guide to these lectures. 1.2 Why study nuclear physics ... Used for 100 years but can be improved by better delivery and dosimetry ... – PowerPoint PPT presentation

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Title: Lectures 1


1
Lectures 1
  • Introduction and Overview
  • Nuclear sizes and isotope shifts

2
1.0 Overview
  • 1.1 User guide to these lectures
  • 1.2 Why study nuclear physics
  • 1.3 Why nuclear physics is diff(eren)??(icul)t
  • 1.4 Course synopsis
  • 1.5 Notation Units
  • 1.6 Nuclear Masses and Sizes
  • Mass measurements
  • Isotope Shifts

3
1.1 How to use these lectures
  • Definition of a classical lecture
  • A lecture is a process whereby notes are
    transferred from the pages of a lecturer to the
    pages of the student without passing through the
    head of either.
  • Disadvantages
  • obvious
  • Conclusion to make lectures useful YOU have to
    participate
  • annotate the notes
  • notes are not a replacement for text book(s!).
  • Without your comments writtend during and after
    the lectures they are of very little use to all
    but the lecturer
  • take your own notes As if you were never given
    these pages
  • exception might be good to write your notes onto
    the sides of these
  • ask questions
  • If you dont understand something the chances are
    gt50 of the audience doesnt either, so dont be
    shy !

4
1.1 Corrections
  • To err is human and I am giving half of this
    course for the first time ? lots of mistakes.
  • Please tell me about any mistakes you find in the
    notes (I will donate a bottle of wine to the
    person who finds the most mistakes!).

5
1.2 Why Study Nuclear Physics?
  • Understand origin of different nuclei
  • Big bang H, He and Li
  • Stars elements up to Fe
  • Supernova heavy elements
  • We are all made of stardust
  • Need to know nuclear cross sections to understand
    nucleosynthesis ? experimental nuclear
    astrophysics is a hot topic.

6
1.2 Energy Applications
  • Nuclear fission
  • No greenhouse gasses but
  • Safety and storage of radioactive material.
  • Nuclear fusion
  • Fewer safety issues (not a bomb)
  • Less radioactive material but still some.
  • Nuclear transmutation of radioactive waste with
    neutrons.
  • Turn long lived isotopes into stable or short
    lived ones
  • Every physicist should have an informed opinion
    on these important issues!

7
1.2 Medical Applications
  • Radiotherapy for cancer
  • Kill cancer cells.
  • Used for 100 years but can be improved by better
    delivery and dosimetry
  • Heavy ion beams can give more localised energy
    deposition.
  • Medical Imaging
  • MRI (Magnetic Resonance Imaging) uses nuclear
    magnetic resonances
  • X-rays (better detectors ? lower doses)
  • PET (Positron Emission Tomography)
  • Many otherssee Medical Environmental short
    option.

8
1.2 Other Applications
  • Radioactive Dating
  • C14/C12 gives ages for dead plants/animals/people.
  • Rb/Sr gives age of earth as 4.5 Gyr.
  • Element analysis
  • Forensic (eg date As in hair).
  • Biology (eg elements in blood cells)
  • Archaeology (eg provenance via isotope ratios).

9
1.3 Why is Nuclear Physics diff(eren)??(icul)t?
  • We have QCD as an exact theory of strong
    interactions ? just solve the equations
  • Thats fine at short distances ltlt size of proton
  • i.e. at large momentum transfers collisions
    with high CM energies gtgt mproton (HEP)
  • ? coupling constant is small (asymptotic freedom)
  • ? perturbation theory works
  • But it fails at large distances O(size of
    proton)
  • coupling constant becomes big
  • ? perturbation theory fails
  • ? we dont know how to solve the equations

Boo !
Not on syllabus !
10
1.3 Nuclear Physics (Super) Models
  • Progress with understanding nuclear physics from
    QCD0
  • ? use simple, approximate, phenomenological
    models
  • inspired by analogies to other system
  • Semi Empirical Mass Formula (SEMF)
  • SEMF Liquid Drop Model Fermi Gas Model
    phenomenology QM EM.
  • Shell Model look at quantum states of individual
    nucleons to understand ground and low lying
    excited states
  • spin, parity
  • magnetic moments (not on syllabus)
  • deviations from SEMF predictions for binding
    energy.

11
1.4 Overview of Lectures (I)
  • Introduction
  • Fri. Week 1, Lindemann (L)
  • Why do we study Nuclear Physics
  • What will this course cover
  • Shape and density of the nuclei
  • 2. The Semi Empirical Mass Formula (SEMF)
  • Thu. Week 2, Martin Wood (MW)
  • The liquid drop model
  • The Fermi Gas Model
  • Experimental verification
  • 3./4./5. Using the SEMF and transition to Shell
    Model
  • Fri. (L) Week 2 Thu. (MW), Fri (L) Week 3
  • The valley of nuclear stability
  • Nuclear decays (a, b, fission, others)
  • Natural radioactivity
  • The end of SEMF Evidence of magic numbers
  • The Shell Model

Note lectures in the Martin Wood lecture theatre
starting 1205 lectures in the
Lindemann lecture theatre starting 1405
12
1.4 Overview of Lectures (II)
  • 6./7. Crossections
  • Thu. (MW), Frid (L) Week 4,
  • Experiments, natural units, conventions and
    definitions
  • Fermis Golden Rule
  • Rutherford Scattering
  • Breit-Wigner resonances and partial decay widths
  • Note No nuclear physics lectures in week 5 !
  • 8./9. Theory of Decays
  • Thu. Fri. Week 6, (MW)
  • Tunnelling model of a-decay
  • Selection rules and decay rates in g-decay
  • Fermi theory of b-decay

13
1.4 Overview of Lectures (III)
  • 10./11. Particle Interactions with Matter
  • Thu. Fri. Week 7, (MW)
  • dE/dx by ionisation and the Bethe-Bloch formula
    (9)
  • Photoeffect, Compton Scattering, Bremsstrahlung,
    Pair Production
  • Cherenkov radiation
  • 12./13. Applications of Nuclear Physics
  • Thy. Fri. Week 8, (MW)
  • Particle Detectors
  • Fission Reactors
  • Bombs
  • Fusion reactors
  • Radioactive dating (notes only)

14
The Minister of Science
  • This is a true story honest.
  • Once upon a time the UK science minister visited
    the Rutherford Lab (UK national lab. near Didcot)
    and after a days visit of the lab was discussing
    his visit with the lab director and he said
    ltcensoredgt
  • Your answer should at least have been as good as
    air!

15
1.5 Notation
  • Nuclei are labelled e.g.
  • El chemical symbol of the element
  • Z number of protons
  • N number of neutrons
  • A mass number N Z
  • Excited states labelled by or m if they are
    metastable (long lived).

16
1.5 Units
  • SI units are fine for macroscopic objects like
    footballs but are very inconvenient for nuclei
    and particles ? use appropriate units.
  • Energy 1 MeV kinetic energy gained by an
    electron in being accelerated by 1MV.
  • 1 eV 106 x e/C x 1 J 1.602 x 10-19 J
  • Mass MeV/c2 (or GeV/c2)
  • 1 MeV/c2 106 x e/C / c2 x 1kg 1.783 x 10-30
    kg
  • Or use Atomic Mass Unit (AMU or u) defined by
  • mass of 12C 12 u
  • 1 u 1.661 x 10-27 kg 0.93 GeV/c2
  • Momentum MeV/c (or GeV/c)
  • 1 MeV/c 106 x e/C / c x kg
  • Length fermi 1 fm 10-15 m
  • Cross sections barn as big as a barn door (to
    a particle physicists)
  • 1 barn 10-28 m2 100 fm2

Note C Coulomb c speed of light
17
1.6 Nuclear Masses and Sizes
  • Masses and binding energies
  • Absolute values measured with mass spectrometers.
  • Relative values from reactions and decays.
  • Nuclear Sizes
  • Measured with scattering experiments (leave
    discussion until after we have looked at
    Rutherford scattering).
  • Isotope shifts in atomic spectra

18
1.6 Nuclear Mass Measurements
  • Lets collect all the experimental facts first !
  • Measure relative masses by energy released in
    decays or reactions.
  • X ? Y Z DE
  • Mass difference between X and YZ is DE/c2.
  • Absolute masses measured by mass spectrometers
    (next transparency).
  • Relation between Mass and Binding energy
  • B Z MH N Mn Matom(A,Z)/c2 or
  • B Z Mp N Mn Mnucleus(A,Z)/c2
  • (neglecting atomic binding energy of electrons)

19
1.6 Mass Spectrometer
  • Ion Source (e.g. strong laser takes out
    electrons)
  • Velocity selector
  • for electric and magnetic forces to be equal and
    opposite need
  • Momentum selector, circular orbit satisfies
  • Measurement of x gives rcurv
  • rcurv and v gives M

xx(rcurv)
position sensitive detector
velocity selector
ion source
B
E
B
momentum selector
20
1.6 Binding Energy per nucleon vs. A
  • Typical way of representing mass measurements
  • B increases with A up to 56Fe and then slowly
    decreases.
  • B is very small and not smooth at small A.
  • Why?
  • See SEMF and Shell Modell.

21
1.6 Nuclear Sizes and Isotope Shifts
  • Measure size of nucleus by the effect of its
    charge distribution on the energy levels of
    atomic electrons
  • Simple point like Coulomb field will be modified
    by finite size of nucleus.
  • This should be felt most by electrons close to
    the nucleus i.e. k-shell L0
  • And should be negligible for electrons with
    minimal overlap with the nucleus, i.e. Lgt0 (Yr
    L)
  • ? study this assuming Hydrogenic ground state
    wave functions for the electrons
  • thats justified even for large Z atoms since
    k-shell electron does not see much of outer
    electrons

22
1.6 Nuclear Sizes Isotope Shifts
  • Assume a uniform distribution of charge Ze in a
    spherical nucleus of radius R.
  • Calculate potential inside nucleus Vinside
  • Einside via Gausss law
  • Vinside by integrating Einside and applying
    boundary conditions at rR to match Vinside to
    usual 1r2 potential
  • Difference between actual potential and Coulomb

23
1.6 Nuclear Sizes Isotope Shifts
  • Use 1st order perturbation theory to calculate
    energy shift ?E
  • Insert approximate Hydrogenic ground state wave
    function

24
1.6 Nuclear Sizes Isotope Shifts
  • Note ?E is proportional to Z4 and R2? most
    noticeable effect deep inside large Z nuclei
  • a0 0.5 10-10 m

25
1.6 Isotope Shifts
  • Look at transitions from l1 (no isotope shift)
    to l0 (large isotope shift)
  • Preferably look for transitions at low n.
  • Types of isotope shifts in increasing shift
    order
  • Isotope shift for optical spectra ?E O(meV)
  • Isotope shift for X-ray spectra (bigger effect
    then optical because electrons closer to
    nucleus) ?E O(0.1 eV)
  • Isotope shift for X-ray spectra for muonic atoms.
    Effect greatly enhanced because mm 207 me and
    a01/m. ?E O(keV)
  • All data consistent with RR0 A1/3 using
    R01.25fm.

26
1.6 Isotope Shift in Optical Spectra
  • Need to use higher n wave functions to calculate
    this
  • Use Zeff Z-n
  • expect (Zeff/Z)4 dependence in ?E
  • Why is ?E A2/3 ?
  • ?E R2 (see before)
  • and RR0A1/3

Energy shift of an optical transition in Hg at
?253.7nm for different A relative to A198. Data
obtained by Doppler free laser spectroscopy. The
effect is about 1 in 107. (Note the even/odd
structure.) Bonn et al Z Phys A 276, 203 (1976)
27
1.6 Isotope Shift in X-Ray Spectra
  • Bigger shifts as expected
  • Again two lines A2/3

0.5
DE (eV)
Data on the isotope shift of K X ray lines in Hg.
The effect is about 1 in 106. Again the data show
the R2 A2/3 dependence and the even/odd effect.
Lee et al, Phys Rev C 17, 1859 (1978)
0
A2/3
28
1.6 Isotope Shift in muonic atoms
  • See dependence on Rnucl
  • Because a0 1/m the effect is 0.4, i.e. much
    larger than for an electron
  • Changing Rnucl by increasing A gives changes in
    isotope shifts of 2 keV

Data on Isotope Shift of K Xrays from muonic
atoms in which a muon with m207me takes the
place of the atomic electron. The large peak is
2p3/2 to 1s1/2. The small peak is 2p1/2 to 1s1/2.
The size comes from the 2j1 statistical weight.
Shera et al Phys Rev C 14, 731 (1976)
29
1.6 Isotope Shift Conclusions
  • All types of isotopes shifts show A2/3 as
    expected for an R2nucl dependence
  • This holds for all types of nuclei
  • When fitting the slopes we find the same R0 in
    RnuclR0A1/3
  • This tells us that the nuclear density is a
    universal constant
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