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    Nuclear Physics

    J.Pearson

    April 28, 2008

    Abstract

    These are a set of notes I have made, based on lectures given by D.Cullen at the University ofManchester Jan-June 08. Please e-mail me with any comments/corrections: [email protected].

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    CONTENTS 1

    Contents

    0.1 Basic Terminology . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 1

    1 Nuclear Properties 1

    1.1 Nuclear Size . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 1

    1.2 Experimental Methods to Measure Nuclear Distribution . . . . . . . . . . . . . . . . 2

    1.2.1 Nuclear Charge . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 2

    1.2.2 Nuclear Matter . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 2

    1.2.3 Total Reaction Cross-Section . . . . . . . . . . . . . . . . . . . . . . . . . . . 2

    1.3 Differential Cross-Sections . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 4

    1.4 Distribution of Nuclear Chargec(r) . . . . . . . . . . . . . . . . . . . . . . . . . . . 5

    1.4.1 Electron Scattering. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 5

    1.4.2 Electron Scattering Theory . . . . . . . . . . . . . . . . . . . . . . . . . . . . 6

    1.4.3 Solutions . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 7

    1.4.4 Conclusions Frome Scattering on Stable Nuclei. . . . . . . . . . . . . . . . . 10

    1.5 c(r) From Perturbation of Atomic Energy Levels . . . . . . . . . . . . . . . . . . . . 11

    1.5.1 X-ray Isotope Shifts . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 13

    1.5.2 Isotope Shifts for Optical Transitions. . . . . . . . . . . . . . . . . . . . . . . 13

    1.5.3 Muonic Atoms . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 14

    1.6 Nuclear Matter Distributions . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 14

    1.6.1 Elastic Scattering ofp, , . . . . . . . . . . . . . . . . . . . . . . . . . . . . 14

    1.6.2 Pionic Atoms . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 15

    1.6.3 -barrier Penetration . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 16

    1.7 Summary . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 16

    2 Nuclear Models 17

    2.1 The Liquid Drop Description . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 17

    2.1.1 The Semi-empirical Mass Formula . . . . . . . . . . . . . . . . . . . . . . . . 17

    2.1.2 SEMF Predictions & Explanations . . . . . . . . . . . . . . . . . . . . . . . . 21

    2.1.3 Microscopic Effects . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 22

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    CONTENTS 2

    2.2 The Shell Model . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 23

    2.2.1 Solving Schrodinger Equation for Simple Central Potential . . . . . . . . . . 23

    2.2.2 Spin-Orbit Interaction . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 25

    2.2.3 Filling Orbits . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 262.2.4 Predictions of Ground State Spins & ParitiesI . . . . . . . . . . . . . . . . 26

    2.2.5 Excited States . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 26

    3 Collective Excitations 29

    3.1 Nuclear Vibrations . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 29

    3.1.1 Two Phonon States . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 29

    3.2 Nuclear Rotations . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 30

    3.2.1 Types of Deformed Shape . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 31

    3.2.2 Energies of Deformed Shapes . . . . . . . . . . . . . . . . . . . . . . . . . . . 31

    3.2.3 Predictions . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 31

    3.2.4 Excited Rotational Bands . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 33

    3.2.5 Population of Excited States . . . . . . . . . . . . . . . . . . . . . . . . . . . 33

    3.2.6 Information from-ray Spectroscopy . . . . . . . . . . . . . . . . . . . . . . . 35

    4 -decay 36

    4.1 Theory of-emission . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 37

    4.2 Fine Structure of-decay . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 39

    5 -decay 41

    5.1 Q-values . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 41

    5.2 Fermi Theory . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 42

    5.2.1 -decay Half-lifes . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 42

    5.3 Angular Momentum Rules for-decay . . . . . . . . . . . . . . . . . . . . . . . . . . 43

    5.3.1 Allowed Decays . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 44

    5.3.2 First Forbidden Decay . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 45

    5.4 Parity Violation in-decay Process. . . . . . . . . . . . . . . . . . . . . . . . . . . . 45

    6 -ray Emission 46

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    CONTENTS 3

    6.1 Angular Momentum Considerations . . . . . . . . . . . . . . . . . . . . . . . . . . . 46

    6.2 Parity Rules. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 47

    6.2.1 Angular Momentum Considerations . . . . . . . . . . . . . . . . . . . . . . . 48

    6.3 Parity Rule for E1 & Transition Rates . . . . . . . . . . . . . . . . . . . . . . . . . . 486.4 Single Particle Weiskopf Estimates . . . . . . . . . . . . . . . . . . . . . . . . . . . . 49

    6.5 Internal Conversion. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 50

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    1 NUCLEAR PROPERTIES 1

    0.1 Basic Terminology

    Let us just start with basic terminology.

    We write:AZXN

    To denote an atom/nucleus. We say that Zis the atomic number, which is the number of protons,which is also the same as the number of electrons. A is the mass number of the nucleus, which isthe integer ratio of nuclear mass and fundamental mass unit u. Whereu is defined such that 12Chas atomic mass 12.0000u. Note, we generally neglect the mass of the electrons. So, as examples,we write 11H0,

    23892 U146; however, we usually just write

    238U, as that we wrote U implies Z= 92.

    1u= 1.66 1027kg

    Nucleon Refers to either neutron or proton, when we dont want to specify which;

    Isotope Two nuclei which have the same Z, but different N. That is, the same proton number,but different number of neutrons.

    Isotone Converse: differentZ, same N. For example, 21H1 and 32He1.

    Isobar Nuclei with the same mass number A. For example, 3He and 3H. Note, we generallywork in MeV, as opposed to J, when we quote energies as opposed to masses.

    1u= 931.502 MeV/c2

    1 Nuclear Properties

    There is no simple theory which encompasses all nuclei: many models work in different situations.However, we can characterize nuclei by a relatively small number or parameters; such as radius,electric charge, mass, binding energy and energy of excited states.

    1.1 Nuclear Size

    Rutherfords

    scattering experiment at Manchester. He found that almost all of the mass ofan atom (the nuclear mass) is concentrated in a very small volume at its centre, and had highelectric charge, which was bound by the short range strong interaction. He curiously found someparticles bouncing back off the nucleus: it is like an artillery shell bouncing off tissue paper.Typical atomic radius is 1010m, and proton radius 1015m = 1fm.We shall see later that all nucleu have a similar density. Hence, nuclear volume:

    4

    3R3 A

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    1 NUCLEAR PROPERTIES 2

    WhereA is the atomic mass; experimentally, found to be:

    R= r0A1/3 r0 1.2f m

    So, for example, for 238U,r= 7.4fm.

    1.2 Experimental Methods to Measure Nuclear Distribution

    1.2.1 Nuclear Charge

    This will all be due to protons. We use the Coulomb interaction between the nucleus and a particleparticle/probe (such as e, ). The EM interaction is exactly understood. There will be nocontribution from the Strong force.

    1.2.2 Nuclear Matter

    This will look at both protons & neutrons. We use probes which interact with the strong (nuclear)force (e.g. p, , ).If the probe has sufficiently high energy, we say that it has overcome the Coulomb force, and wecan hence neglect it.

    To go further, we need to discuss the idea ofcross-section; which is the same as reaction probability.

    1.2.3 Total Reaction Cross-Section

    Early methods from the 1960s are now used to very exotic nuclei; i.e. ones that are very short

    lived, have smallt 12 . An example of such an exotic nucleus, is that of 11Li. It has t12 8.7ms. The

    2 extra neutrons in going from the isotope 9Lito 11Lihas the effect of creating a halo - a so-calledhalo nucleus- which increases the size of the nucleus to something comparable with 208P b.

    Consider the classical collision between two spheres of radius R1, R2. We shall ignore any Coulombinteraction. Let their centres be a distance b apart. We call b the impact parameter. So, whathappens depends on b:

    Ifb > R1+ R2, then no interaction; Ifb < R1+ R2, then some interaction occurs.

    Possible interactions are elastic scattering, exchange of nucleons (a transfer interaction), or fusionof nuclei.All of these processes remove particles from the beam/path.Let us define a geometric limit as being the effective area that will remove a particle from the beam:

    T =(R1+ R2)2

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    1 NUCLEAR PROPERTIES 3

    Let us have a flux ofN0 particles per second in a beam. Let us have a slab of target, thickness x,exposed surface area A. Each target nucleus has the effective area T. The target has nnuclei perunit volume. Let the number of nuclei coming out of the target be N0 N, that is, the numberthat interact and do not get through is N. The interaction rate is thus N.So, the total effective area across target is T

    no.nuclei in target:

    =TnxA

    So, the probability of beam particle not getting through the thin target (i.e. that of interacting) isthe total effective area/total area

    total effective area

    total area =

    TnxA

    A= Tnx

    Hence, the reaction rate N is N0 probability of interaction:

    N=N0Tnx (1.1)

    Experiment measuresN0, N,n ,x; hence, we deduce the cross-section T. Thas the units of area.Let us do a quick order of magnitude calculation.Let us use 11Li, so we have R= r0A

    1/3 3fm. Hence, T is about:

    T = (R1+ R2)2

    (6 1015m)2 100 1030m2= 1028m2

    So, we use a unit of nuclear reactions for cross-section:

    1barn= 1028m 1b

    Now, the nuclear surface wont be well defined. There are a few ways to parameterize what we mean

    Figure 1: A density profile for a general nucleus. The dotted line is the ideal case, which wouldclassically be expected, but this is not the case,

    by the nuclear surface:

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    1 NUCLEAR PROPERTIES 4

    The point where (r) (0)2 ; By skin thickness: where the density drops from 90% to 10%; Use the mean square radius:

    r2 = r2(r) d(r) dThis is equal to 35R

    2 for a billiard ball.

    For 11Li, the profile is even more convoluted. The 2n in the halo completely mess things up!

    Figure 2: A charge density profile for 9Li and 11Li. Notice the difference. The extra 2n sit very farfrom the core: neutron-skin. This is an example of neutron rich material.

    1.3 Differential Cross-Sections

    These are denoted by dd , and are used to describe the distribution of scattered particles. So, ifdis the effective area of the target nucleus that scatters a particle into a cone, which has solid angled in a direction (, ); where is measured from the direction of incidence of the beam, and theangle of rotation around the beam.Normally, there is no -dependance, unless the beam is polarised. So, dd is a function of only,So, the total scattering cross section is just:

    =

    d

    = 2=0

    =0

    dd

    d

    =

    2=0

    =0

    d

    dsin dd

    Using spherical polars.

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    1 NUCLEAR PROPERTIES 5

    Figure 3: The radial charge distribution of various nuclei, found from electron scattering. The skinthickness is shown. Notice how the central density is approx constant.

    1.4 Distribution of Nuclear Charge c(r)

    The usual method to determine the size/shape of an object is to examine the radiation that scattersfrom it. We can only observe details that are of the same order of the de Broglie wavelength used.e.g. to see nuclear distribution using e, we need 10fm. Which, via:

    =

    h

    p =

    hc

    E

    Is an energy E 100MeV. Typically however we use E 1GeV.We analyse with a precise spectrometer the electrons that are elastically scattered from the nucleus.

    1.4.1 Electron Scattering

    This is a direct analogy to light scattering from a 2D black disc. We would get an interferencepattern out, with first minimum at= 1.22D , where D is the diameter of the disc.

    As is shown in Fig (5) (b), we see that the electron-scattering intensity dosent go to zero. This is

    because the nucleus is not an opaque disc, and that the nuclear surface is not well defined. However,we can still extract nuclear radii in the same way.

    From these types of experiment, we get 2.6fm and 2.3fm for 16O and 12C, respectively. Comparewith 3fm and 2.7fm as predicted by the r0A

    1/3 method.

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    1 NUCLEAR PROPERTIES 6

    Figure 4: The differential cross-section. A beam of particles is incident upon a nucleus, with effectivecross-sectiond . Beam particles are scattered into a cone of solid angle d, which is inclined at anangle to the incident direction. Note how various angles are defined.

    1.4.2 Electron Scattering Theory

    We shall neglect the spin of the electron, and only look at Coulomb effects.Consider:

    Mif=

    fV(r)i d

    So that e scattering probability is governed by the overlap integral, containing initial and finalstates of the electron, and scattering potential V(r).It can also be thought of in terms ofV(r) acting on the initial wavefunction i and converts it toa superposition of outgoing scattering waves. Mifthen selects amplitude of the component f.The scattered intensity has the relation:

    d()

    d M2if

    So, suppose that the incoming momentum of electrons is given by pi = hki, and outgoing bypf= hkf, so that the plane waves are:

    i = eikir f=e

    ikfr

    Using the concept of momentum transfer, and having q =ki kf. and that for elastic scattering|ki| = |kf| =k, say. It can be shown that:

    q= 2k sin

    2

    We derive it by considering the cosine rule. Consider:

    q2 = (ki kf)2= 2k2 2k2 cos

    Where we have used that ki = kf=k. Then, from the trig identity cos 2= 1 2sin2 , the abovebecomes:

    q2 = 4k2 sin2

    2

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    1 NUCLEAR PROPERTIES 7

    Figure 5: Intensity against scattering angle. (a) is for light off a disc diameter D, and (b) forelectron scattering off a nucleus. The minima for electron scattering dont go to zero as the nucleusis not an opaque disc, as was the case for light scattering.

    Square-rooting gives the desired result:

    q= 2k sin

    2

    So, combining all this, we have:

    Mif =

    V(r)eiqr

    d

    Which is just the 3D Fourier transform of the potential. So:

    d()

    d |Mif|2 =

    V(r)eiqr d

    2

    Where we generally use spherical polars, so that d=r2 sin drdd.

    1.4.3 Solutions

    We consider various solutions to the above Fourier transform, and forms of the potential.

    Special Case: Point Nucleus Here we consider the Coulomb potential energy between theprobing electron and the nucleus; that is:

    V(r) =Z1Z2e

    2

    40r

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    1 NUCLEAR PROPERTIES 9

    Real - Extended - Charge Distribution We need to consider the potential that the electronfeels, at position r due to an element of charge dQ at r . That is:

    V(r) = Ze2

    40 c(r

    )

    |r

    r

    |

    d

    We have that the charge density is nomalised; that is: c(r

    )d = 1

    Hence, our matrix element:

    Mif =

    V(r)eiqr d

    = Ze2

    40

    c(r

    )

    |r r|d eiqr d

    Which, after a load of algebra (which we dont do), we get to:

    Mif=Ze2

    0

    1

    q2

    eiqrc(r

    )d

    So, we see that we get the product of what we had for our previous point nucleus, and the Fouriertransform of the charge density (the integral on the right). We call the Fourier transform the electric

    form factor of the nucleus F(q).

    We recall that d()d M2if. Hence, we have that the probability of scattering an electron at an

    angle is just given by:d()

    d real

    = d()

    d point

    F(q)2

    That is, the actual cross-section is the product of the Rutherford (point nucleus) cross section withthe square of the form-factor.

    Note:(1) We can measure d()d , which can fall below the calculated Rutherford cross-section (i.e. thatfor a point-nucleus); which tells us about the Fourier transform of the charge distribution.(2)F(q) depends on the electron beam momentum, and scattering angle , only through momentumtransfer, via q= 2k sin /2. So, we can combine data from various energies (and labs) by plottingd()d vs q.

    (3) We can get the charge distribution c(r) by finding the inverse Fourier transform of the form-

    factor. That is, we measure:F(q) = F{c(r)}

    Hence, we can calculate the inverse:

    c(r) = F1{F(q)}

    Note however, in principle, to invert properly, we need to know qup to infinity; which is obviouslyimpossible. Hence, we get experimental errors due to this, in c(r

    ) at smal r.

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    1 NUCLEAR PROPERTIES 10

    Figure 7: The plot on the left is the measured differential cross-section (for 450MeV electronsscattered by 58Ni), plotted as a function of q, where q = 2k sin /2; which is proportional to theFourier transform of the charge density, which is on the right, after finding the inverse Fouriertransform of the left.

    1.4.4 Conclusions Frome Scattering on Stable Nuclei

    c has a similar central density in all nuclei; That is, the number of nucleons per unit volume isapproximately constant. Thus:

    A

    V =

    A43R

    3 =const

    From which we get R = r0A1/3; and measurements give us r0= 1.2fm.

    We are also able to see that the nuclear surface is quite diffuse (FIG3.4); that is, the surfacethickness (going from 90% to 10% of(r= 0) is about 2.3fm in all stable nuclei.

    We are able to find the root-mean-square (rms) radius

    r2

    1/2 directly from scattered electrons.

    Plotting R against A1/3 gives us a slope 1.2fm.We see:

    r2 =

    r2c()d

    That is:

    r2 = 4

    0r4c(r)dr

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    1 NUCLEAR PROPERTIES 11

    1.5 c(r) From Perturbation of Atomic Energy Levels

    The nucleus is not a point source. Thus, this modifies the Coulomb potential in whiche moves,but only within the small volume of the nucleus. Ane spends some of its time inside the nucleus,where it feels a very different charge distribution.

    Figure 8: The deviation from ideal point charge, for inside the nucleus. Shown on the figure is thepotential: outside (i.e. r > R), we see that it is just equal to the point charge. Inside, we see thatit deviates off, with energy shift E. The potential inside is denoted V(r).

    This effect reduces the binding energy of an atomic electron, by E. Let us make a rough approx-imation:

    Assume the nucleus is a uniformly charged sphere with radius R. Thus:

    V(r) = Ze2

    40R

    3

    21

    2

    r2

    R2

    r R

    And outside:

    V0(r) = Ze2

    40r r > R

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    1 NUCLEAR PROPERTIES 12

    The energyEof an electron in a state e depends partly on the expectation value of the potential:

    V =

    eV(r)e d

    Now, we use first order perturbation theory, as the electron wavefunction varies slowly over thenuclear volume. Hence:

    E=

    e(r){V(r) V0(r)}e(t) d

    The effect will be largest for the wavfunction which penetrates most into the nucleus: the 1swavefunction:

    (r) = 2

    Z

    e2

    3/2eZr/a0

    Hence:

    E= Ze2

    404

    Z3

    a30

    e2Zr/a0

    1

    r 3

    2R+

    1

    2

    r2

    R3

    d

    Now, the exponential argument is very small: so, we take its term to be 1. Also, d = 4r2

    dr.Hence:

    E= Ze2

    40

    4Z3

    a304

    R0

    r 3r2

    2R+

    1

    2

    r4

    R3dr

    Which easily gives:

    E=2

    5

    Z4e2

    0

    R2

    a30

    However, just to make things more correct, R is actually just an expectation value. Hence:

    E=2

    5

    Z4e2

    0

    R2a30

    (1.2)

    Thus, we have that E is the difference in energy of a 1s state in an atom with a point nucleus,and that for a 1s state in an atom with a uniformly charged nucleus with radius R.

    However, we dont have an atoms with point nuclei, so we cannt directly measure E, and hencededuce R. So, the next best thing would be to calculate the point value E, from the 1s atomicwavefunction.However, again, we have a problem: atomic wavefunctions are not known to enough accuracy to beable to do this.

    Eis of the order 104E, which is very small!

    Thus, we cannot use this method to find c(r). However, there are 3 methods that can be used:

    Consider an electron transition from the L-shell to K-shell (that is, 2p to 1s). This will liberate aphoton: an X-ray, whose energy we can measure.If we set up a Muonic atom (muons orbiting instead of electrons), we can measure the energy dropsfor muonic X-rays.We can excite an atom using lasers: laser flouresence spectroscopy.

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    1 NUCLEAR PROPERTIES 13

    1.5.1 X-ray Isotope Shifts

    Here, we make a comparison of the rmsr2between different isotopes Aand A (remember, sameZ, different N). So, we can measure:

    E=h(A A)That is, the measured shift of X-ray energy (K X-rays are produced by electron transitions fromthe 2p down to 1s state) between two isotopes; such as 200Hg and 202Hg.Now, we previously showed, from first order perturbation theory, that:

    E=2

    5

    Z4e2

    0

    R2a30

    So, if we have EA being the difference in the 1s state in atom A, with point nucleus, and uniformlyextended charge distribution. Similarly for EA . Hence:

    E = h(A

    A)

    = EA EA=

    2

    5

    Z4e2

    0

    1

    a30R20(A

    2/3A A2/3A )

    Where we have used thatR2i = (R0A1/3i )2. So, we have subtracted out the point charge distribu-tion. The shift is, however, very small: 106.Typlically, E= 0.15eV; and the transition energy (energy of the X-ray) is of the order 100keV

    We also see thatR2 increases with N, that is, the proton distribution spreads out, as neutronsare added, because of the strong interaction between p, n in the nucleus.

    So, X-ray isotope shifts work, but their shift is very small.

    1.5.2 Isotope Shifts for Optical Transitions

    Here we consider transitions which result in optical wavelengths, in the valence electrons. We seethat Eis smaller, as:

    |6s(r= 0)|2

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    1 NUCLEAR PROPERTIES 14

    1.5.3 Muonic Atoms

    The problems with the previous two methods are the the effects are small. This is not the case ifwe use a muonic atom:

    Get an atom, strip it of all its electrons, and fire a at it. The muon will spiral down, throughBohr-like orbits, emmiting photons as it goes.

    Now, m 207me; hence, as the Bohr radius (for an electron) is given by:

    a0= 1

    h

    mec

    Then we have that the equivalent, for a muon, is:

    r = a0207

    So, for example, 82Pb, the 1s orbit is inside the nuclear surface. That is:

    |1s(r= 0)|2 >> |e1s(r= 0)|2

    Here, the X-ray shifts are of the order 130 , which is huge compared with previous methods.

    Futhermore, wavefunctions are easier to calculate accurately enough, to be able to derive an abso-luter2for the nucleus.Muonic X-rays are 1MeV in Fe, and 5.5MeV in Pb; which are comparable to gamma-rays, whose

    detectors are very accurate.

    Infact, when spin-orbit coupling is taken into account, split states are visible.

    1.6 Nuclear Matter Distributions

    To do this, we need a probe that will interact, via the strong nuclear force, to be able to see bothp, n. Such as proton, alpha-particles and pions.

    1.6.1 Elastic Scattering ofp, ,

    Here, we have a scattering potential, which is Coulomb outside, and a deep attractive well inside.

    So, the Coulomb potential, for target nucleus Z1, probe Z2 is just:

    Vc =Z1Z2e

    2

    40r = 1.44

    Z1Z2r

    M eV

    Ifr in fm. So, ifr > R(i.e. probe energy is less than Coulomb repulsion), then we get the standardGauss law; and the scattering particle behaves as if it scattered off a point like nucleus - Rutherfordscattering.

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    1 NUCLEAR PROPERTIES 15

    Figure 9: Scattering potential for a probe incident upon a target nucleus. Notice, outside, it is aCoulomb potential; and inside a (complicated!) attractive nuclear potential.

    If the probes energy is greater than the Coulomb repulsion, then the strongly attractive force comesinto play. At this point, we expect deviation from the Rutherford formula, as other outcomes arepossible - such as adsorption - which are likely to reduce the probability of elactic scatter (R).

    Note, the analysis of data is far more complicated than for electron scattering, due to the complexnature of the strong nuclear force (the strong interaction).

    What we see depends on the wavelength of the probe:

    E=hc

    If we use a large wavelegth, small energy; then we see the matter radius;At small, large E, start to see more detail.

    The patterns we get on detection screens is akin to Fraunhoffer patterns in Optics: which providesinformation on the scattering surface, the internal density distribution.

    Some notation: 40Ca(, ) at 115MeV.Reading from left to right: target nucleus, incoming particle (probe), outcoming partcile, done atthe energy.

    1.6.2 Pionic Atoms

    This is another example of X-ray analysis.

    Basicaly, let pions get captured by a nucleus, and as they spiral in towards the nucleus, they emitphotons. This time however, pions (as they are mesons) will interact with both the Coulomb &

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    1 NUCLEAR PROPERTIES 16

    Figure 10: Possibilities for nuclear scattering. The dotted lines show direction of increasing probeenergy E, and impact parameter b (i.e. the distance between centre of nucleus & probe). Thedifferent trajectories correspond to: 1) Fusion; 2) Scattering, with direct & indirect interaction;3) Coulomb interaction, elastic & inelastic scattering; 4) Mainly Coulomb interaction, Rutherfordscattering.

    strong forces (c.f. just Coulomb for muons). The energy shifts are larger. The -mesons emit-mesic X-rays as they cascade through the electron-like oribits.

    When the wavefunction begins to overlap with the nuclear w.f., then the energy levels are shiftedfrom pure Coulomb values (calculated using pure Coulomb interaction), and the -mesons becomeabsorbed directly into the nucleus, from the inner orbits.

    Hence, we get a dissapearence rate of-mesons; hence another way to determine the nuclear radius.

    1.6.3 -barrier Penetration

    We merely state that this method exists, but we will discuss later.

    1.7 Summary

    So, considering stable nuclei (i.e. sit along the line of stability):

    Charge & matter radii are very similar; The n p attraction (via strong interaction) keeps nucleons in the same place;

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    2 NUCLEAR MODELS 17

    Heavy nucleu have about 50% more neutrons than protons, so, we may expect their neutronradius to be larger than proton radius. However, p repulsion pushes p out, dragging n withit; hence, neutrons and protons are mixed up; resulting in both the charge and matter radiibeing nearly equal.

    Nuclei with large n excess appear to formn-rich skin; even a halo, as in 11Li.

    The central density in all stable nucleu is similar;

    All have a similar diffuse surface.

    (r) = (0)

    1 + erRa

    Wherea = 0.6fm.

    We have the relation R = 1.2A1/3fm.

    2 Nuclear Models

    2.1 The Liquid Drop Description

    This is a classical, macroscopic description of the nucleus, however, the SEMF will use some elementsof quantum theory in its formulation.

    2.1.1 The Semi-empirical Mass Formula

    - SEMF

    The binding energyBE is defined as the energy needed to break an atom into its constituents.

    So, anatom, plusBEwill giveZp,Nn and Ze; which we will simplify to justZH+Nn (i.e. neglectBE of electrons, which is 13.6eV, compared with MeV for nucleons; and where Zp = ZH). The BEis dominated by the nuclear contribution. Usually, we write:

    M(Z, A) =ZMH+ NMn 1c2 BE(Z, A) (2.1)Since the BE increases with A, we generally plot BE/A as a function ofA. See plot.

    The SEMF attempts to parameterise this shape by a series of 6 (including mass) terms:

    BE(Z, A) =aVA

    aSA

    2/3

    aCZ(Z

    1)A1/3

    asym

    (A 2Z)2

    A

    + (2.2)

    We have, in order:

    The volume term: The nucleons only interact with near-neighbours. If each nucleon has thesame number of nearest- neighbours, then the BE has such a dependancs;

    The surface term: This takes into account that there are nucleons on the surface, which areless tightly bound. Surface area R2; and we have seen that R A1/3.

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    2 NUCLEAR MODELS 18

    The coulomb term: We have that the coulomb repulsion between protons, at a distance R( A1/3) is just given by the test charge, and whatever is left. That is, Zand (Z1) protons.

    The symmetry term: This acts to minimise the difference in the number of protons andneutrons; i.e. Z=Npreffered.

    The pairing term: We will come to this later. However, = 34A3/4MeV; and we use + foreven (both Z, Neven) nuclei; 0 for odd (odd-even or even-odd) A nuclei; or for odd-oddnuclei. This is due to nucleons liking to couple into pairs with zero spin.

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    2 NUCLEAR MODELS 19

    Figure 11: The breakdown of Rutherford scattering. When incident particles get close enoughto the target (here, Pb), they interact through the nuclear force, hence the Rutherford formula no

    longer holds. The point at which breakdown occurs gives a measure of the size of the nucleus.

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    2 NUCLEAR MODELS 20

    Figure 12: Binding energy per nucleon. Notice that helium has a disproportionally high BE; thatiron is near the peak; that most have BE/A around 8MeV

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    2.1.2 SEMF Predictions & Explanations

    Odd Mass For a given odd mass A, there is only one stable isobar (same neutron, differentproton). We can show this by computing:

    MZ

    A

    = 0

    That is, at fixed A. Which gives:

    Zmin =A

    2

    1

    1 + 14A2/3 aC

    asym

    Thus, for a constant A, M(A, Z) is a quadratic function ofZ.Suppose the position of the minimum is Zmin, then, for Zmin+ 1, whatever nuclei exists there willwant to change a proton into a neutron; and will do so via + decay, which is just e-capture. For anucleus atZmin 1, a neutron will change into a proton, via decay; that is, electron emission.

    Even Mass For a given evenA, there can be several even-even stable isobars, due to the pairingterm in the SEMF.

    Figure 13: Even mass nuclei decay chains. Decays to the right go via +, and the left by .The two parabolas are sparated by 2.

    Energy From Fusion Consider:2H+2 H4 He

    The binding energy is:

    BE(2H) = 2 1.1MeV/A= 2.2MeVBE(4He) = 4 7MeV/A= 28MeV

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    2 NUCLEAR MODELS 22

    Where these numbers have been found from data. So:

    2H+2 H4 He + 23.6M eV

    Where the 23.6MeV comes frommfmi= 28 (2 2.2) = 23.6MeV. Thus, in the above reaction,23,6MeV is released.

    Energy From Fission If we look at the binding energy curve, we see that nuclei withA = 60 aremost tightly bound - they are at the top of the plot. So, when 238Ufissions (splits up), it produces2 more strongly-bound nuclei. Hence, a releas of energy. Consider:

    238U100 A1+138 A2Then, we see that, from BE data:

    BE(238U) = 238 7.5MeV/ABE(

    100

    A1) = 100 8.2MeV/A BE(138

    A2)

    So, this will release (100 8.2 + 138 8.2) (238 7.5) = 166MeV.

    -decay In heavy nuclei, the disruptive Coulomb energy increases at a faster rate ( Z2) thannuclear BE with A. Hence, emission of 4He nucleus of a favoured way to reduce charge.

    The BE for an alpha particle is about 7MeV/A; which is relatively high, for something with so fewnucleons.

    A Q-valueis the difference in masses before and after:

    Q=i

    minitali i

    mafteri (2.3)

    2.1.3 Microscopic Effects

    These are effects which are not explained by the liquid drop model. These show that we needquantum/shell structure of nucleus:

    Systematic Deviation in the smooth BE curve, from the SEMF: there is extra binding energyfor nuclei with Zor Nbeing 28, 50, 82, 126.

    Proton & Neutrons Separation Energies denotedSn, Sp, S2nS2p- equivalent to the ionisationenergy of atomic electrons. Where S2n is the energy needed to pull a neutron pair from the nucleus- hence, a measure of the BE of last pair ofn. We see that S2p greatest where N, Zare 8, 20, 28,50, 82, 126.

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    2 NUCLEAR MODELS 23

    Energy Required to Excite Nucleus to first excited state. We see that significantly moreenergy is required when N is 8, 20, 28, 50, 82, 126

    So, we see a pattern of the same magic numbers.

    2.2 The Shell Model

    Available evidence suggests that protons & neutrons fill orbits & shells similar to atomic electrons.We may initally think that a nucleon could not orbit independantly in dense nuclear interior.Internal scatterings are forbidden by the Pauli exclusion principle, as the nucleons are all belowtheir fermi surface.

    Indeed, it has been possible to map out the density distribution, ||2, for the last (i.e. 82nd) protonin 20582 P b, by comparison of charge radius c(r) for

    20582 T l and

    20682 P b by electron scattering.

    It turns out that||2 is very close to that of predicted 3s orbit which actually peaks in nuclearmaterial at r = 0.

    2.2.1 Solving Schrodinger Equation for Simple Central Potential

    Let us assume that each nucleon move independantly in a poential V(r); which we will take to bethe average interaction with all other nucleons.

    Figure 14: The Woods-Saxon potential model.

    The potetial is called a Woods-Saxon shape; and is similar to the (r) distribution. We canparameterise the shape thus:

    V(r) = V01 + e

    rRa

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    2 NUCLEAR MODELS 24

    Wherea is the surface diffusiveness parameter - which we have looked at previously.

    The single particle levels are calculated by solving the 3D Schrodinger equation:

    h2

    2m2 + V(r)(r) =E(r)

    We apply the usual solving methods: separation of variables. IfV(r) has no, dependance, thenwe have a central potential exactly like the H atom:

    nm(r,,) =Rn,(r)Ym(, )

    Where we have the usual spherical harmonics, and rules for the various quantum numbers:

    n = 1, 2, 3, . . .

    = 0, 1, . . .

    m = , . . . , 0, . . . ,

    For the nuclear potential, we have solutions which are similar to the 3D harmonic oscillator HO.We see that if we count up all the nucleons in a particular state, up to that state, we start to get

    Figure 15: Occupancies of the energy levels in the HO problem. Notice the magic numbers.

    the magic numbers fall out: 2, 8, 20. However, the next predicted is 40; however, experimentally,we get 28. So, this model is only of limited use in explaining whats going on.

    So, we have made an approximation to the Woods-Saxon potential, using the HO potential; butwe have seen that the prediction breaks down for high states. The higher states feel a deeperpotential; thus, nucleons are bound more. We chose V0 to reflect the density disribution; so,V0 35MeV.We should add in Coulomb energy term for protons, but this is a small effect, especially in lightnuclei; so, we ignore it.

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    2 NUCLEAR MODELS 25

    Figure 16: The difference between the Woods-Saxon potential, and the approximate harmonicoscillator potential.

    2.2.2 Spin-Orbit Interaction

    Early on, it was apparent that the a spin-orbit term was present. There is a direct analogy to atomicphysics, but the direction is reversed. We consider the interaction that a nucleon has with it self,when it is orbiting, with orbital angular momentum, and rotating, with spin angular momentum.We see that s parallel to is favored. So, we must add a term (VSO s) to the Hamiltonian.The result of which is that each nucleon orbit (except the s-state, where = 0) is split into 2components, labelled by the total spin j= + s.

    So, we have a state being split; with total energy splitting E, and each level being split by j(j= s, i.e. up) and j (j= + s i.e. down) from the centroid. Note thats = 12 . So, we requirethe energy shifts j = VSO s. So:

    j = +s j2 = 2 + s2 + 2 s s = 12(j2 2 s2)

    VSO s = VSO h2

    2[j(j+ 1) ( + 1) s(s + 1)]

    Hence, for the j shift (i.e. that for j = 12), we have:

    j = VSO

    2 [( 12)( + 12) ( + 1) s(s + 1)]

    Similarly:

    j =VSO

    2 [( + 12)( +

    32) ( + 1) s(s + 1)]

    Thus:

    E=j j =VSO h

    2

    2 ( + 12)[( +

    32) ( 12)]

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    2 NUCLEAR MODELS 26

    After we have used that s = 12 . Hence, this is just:

    E=VSO h

    2

    2 (2 + 1) (2.4)

    The introduction of the S-O interaction is able to account for the experimental shell closures at 2,

    8, 20, 28, 50, 82, 126.NOTE: all magic numbers (i.e. shell gaps) above N, Z= 20 are produced by S-O splitting.

    2.2.3 Filling Orbits

    The shell model uses the standard quantum-numbers system, except that n is the number of timesa particularhas occurred in the level sequence.

    As examples, we have:1s1/2: = 0, j = + s=

    12 .

    1p3/2: = 1, j = 1 + 1/2 = 3/2.

    We also have parity = (1). We also use the standard= 0, 1, 2, 3, . . . or s , p, d , f , . . . system.Shells are filled according to the Pauli principle.

    2.2.4 Predictions of Ground State Spins & Parities I

    We assume the pairing interaction couples pairs of protons and pairs of neutrons into I = 0+ pairs(this is not always a good approximation). All even nuclei have I = 0+ ground state.

    For odd mass nuclei, spin and parity is determined by orbital of the last unpaired nucleon. So, forexamples, see the figure

    For odd-odd nuclei, the low lying states are made by vector coupling of the spins of the unpairednucleons,j

    pp and jnn . Then, the possible spins are found from:

    I= |jp jn|, . . . , |jp+jn|All will exist as states, but difficult to predict which is lowest in energy. That is, it is hard todetermine which is the ground state. The overall-partity is multiplicative pn. That is: (+)(+) + and (+)() .So, as an example, in 169 F7, we have that the unpaired proton is a 1d5/2, and the neutron is 1p1/2.

    Hence,jpp =

    52

    +and jnn =

    12

    . Hence, we expect either 2 or 3 states.Suppose we promoted the proton to a higher energy state. That is, to a 2 s1/2 state. Then, we mayexpect 0 or 1.

    There is a one-to-one correspondance with all low-lying excited states.

    2.2.5 Excited States

    Such states can be made in all nuclei by either promoting nucleons up to higher levels, and/orbreaking an 0+ pair, and recoupling their spins.

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    Figure 17: Nuclear shell filling. The nuclei shown as doubly magic, as both the protons andneutrons occupy filled shells; and are hence very stable nuclei.

    PPT

    This happens at low excitation energy in f7/2 shell. This is all to do with the size of the shell-gap.

    This illustrates the difference between the complete shell model & extreme independant particlelimit. 3 particles in 43Ca can affect each other, and allow many more possibilities.

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    2 NUCLEAR MODELS 28

    Figure 18: Nuclear shell filling, for various nuclei, for even-odd nuclei (odd mass). The nucleonwhich contributes to the spin & partity is the unpaired nucleon, which has been circled in all cases.The parity is found from = (1), where = 0, 1, 2, 3 according to the usual s, p, d, f labelling.

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    3 Collective Excitations

    Here we consider the nucleus as a collective, as opposed to being composed of nucleons.

    3.1 Nuclear Vibrations

    Consider a liquid drop vibrating at high frequency, about a spherical equilibrium shape. We candescribe instantaneous shape by radius vectorR(, ) of the surface, at time t.

    Figure 19: Vibrations of a liquid drop. The radius R(t) at some , .

    So, we have:

    R(t) =Rav[1 + 2cos tYm(, )] (3.1)

    Where we have that Rav =r0A1/3, as usual. 2 is the deformation parameter - see later.

    SEE PPT - MODES OF VIBRATIONS

    We see the modes of vibration for = 1, 2, 3. A quantum vibration is called a phonon. AddingYmterm into nuclear wavefunction introduces h units of angular momentum, with parity (1). Thevibrations carry angular momentum h, and are bosons. Consider the following possibilities:

    Adding an = 1, dipole phonon This gives the term I = 1; and is equivalent to a netdisplacement of the centre of mass of an isolated system. Hence, this is not observed.

    Adding an = 2, quadrupole phonon Here, I = 2+. That is, it creates an excited 2+ state.Usually the lowest excited state of even spherical nucleus.

    Adding an = 3, octupole phonon So, we create a 3

    state. This state is commonly seen athigher excitation energies than 2+ quadrupole vibrations.

    3.1.1 Two Phonon States

    Consider two phonons, so an energy of 2h. There are 25 combinations ofm = m1 + m2. However,by symmetry & indistinguishability arguments, this is reduced to 15. Leaving us with = 4, 2, 0

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    3 COLLECTIVE EXCITATIONS 30

    states. That is, we excite a triplet of states 0+, 2+, 4+ ; each with twice the energy of the first 2+

    state. By similar considerations, 3 quadrupole phonon states can be constructed. That is, energy

    Figure 20: Ordering of the first few quadrupole-phonon-states. The subscript refers to how many

    times that particular state has occured. The energy is the 2+1 state is E(2+1)500 1200keV.

    of 3h. Giving the states 6+, 4+, 3+, 2+, 0+.

    The best examples of vibrational states are in nuclei within the region 50N 82 closed shels,with A= 120. Such as 120T e.

    So, the predictions from the vibrational model:

    0+, 2+2, 4+ at the same energy 2h, and at 2 E(2+1). And is roughly ok!

    0+

    , 2+

    3, 3+

    , 4+

    2, 6+

    states, energy 3h; should be at 3 E(2+

    1 ). But, this is not always true,because 3h states start to overlap with shell model states.

    The number of possible states increases rapidly with energy (or phonon number).

    3.2 Nuclear Rotations

    Nuclei which lie close to the magic numbers are roughly spherical, and therefore cannot rotate inQM.

    However, in certain regions of the nuclear chart: 150A190 or A >220; that is, regions nearmiddle of shell gaps; nuclei have substantial distortions from spherical shape. e.g. 15266 Dy86.

    Many nucleons participate in the motion: hence, a collective effect collective rotation.

    SEE PPT FOR EVIDENCE

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    3.2.1 Types of Deformed Shape

    The most common deformed shape of rugby-ball shaped: axially symmetric, prolate shape (note:prolate is when the equator is squashed in; and oblate when the poles are squashed in. Thinkthat the earth is oblate).

    We describe the surface by:

    R(, ) =Rav[1 + 2Y2,0(, )] (3.2)

    Notice that we use an axially symmetric spherical harmonic; which is (up to factors) a Legendrepolynomial.We say that 2 is the quadrupole deformation parameter; so, if 2 = +0.3, then prolate; and if2< 0, then oblate.

    3.2.2 Energies of Deformed Shapes

    A deformed nucleus has a rotational degree of freedom. The classical expression for rotationalkinetic energy is just:

    T =1

    2J2

    WhereJ is the moment of inertia. If we have angular momentum Ih, then it is related toJ by:

    Ih= J

    Hence, we have:

    T =(J)2

    2

    J

    =(Ih)2

    2

    JHence, we have the expression for our QM rotor:

    T=h2I(I+ 1)

    2JFor even nuclei, the 0+ state is always the ground state. Then, the next states are I = 2+, 4+, 6+, 8+, . .on symmetry grounds.

    3.2.3 Predictions

    If we take the moment of inertia for a rigid body:

    Jrigid = 25

    M R2av(1 + 0.312)

    Then, we end up with:h2

    2Jrigid = 6keV

    After taking A = 170, 2= +0.3. So, from this, we expect:

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    Figure 21: The energy level scheme for the rotational band formed, on top of the ground state.Shown are experimental values obtained for 164Er.

    E(2+) = 36keV. However, experimentally, we find that this is more like 90-100keV; as per the

    figure. However, if we take the ratio E(4+)E(2+) =

    206 = 3.33, then this is an extremely good prediction;

    as it divides out the moment of inertia.

    Thus, by usingIrigid, we have overestimated the actual moment of inertia.Infact, the completely filled (inner) shells cannot contribute to this angular momentum, as they

    are paired up. So, we should really just regard the rotational motion as due to the valence nucleonsonly. So, we imagine that we have an 0+ core, with the rest of the nucleus rotating around it. Thisleads to other extremes of motion, where we consider the nucleus as a fluid inside an ellipsoidalvessel. In this case, we calculate:

    h2

    2Jfluid = 90keV

    But, this is too high, in comparison with experiment.

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    Hence, we conclude:Jfluid< Jnuclear < Jrigid

    That is, the actual value of the moment of inertia is somewhere between that predicted by thenucleus being fluid, and that being a rigid body.

    3.2.4 Excited Rotational Bands

    So far, we have only discussed collective rotational bands built upon the ground state of even nuclei,such as 164Er. We do actually have more than one rotational band however; each of which is builton different states. There is one ground state rotational band, and two bands built on differentvibrational states.

    -Vibration Here,2 oscillates about an equilibrium value. So, the picture to have in mind hereis that of a rugby ball, on its tip (i.e. prolate), rotating about its centre (not its axis of symmetry),

    and vibrating along its axis of symmetry.

    -Vibration Here, 2 remains constant, but the axial symmetry is now lost.

    Figure 22: (a)-vibrations: notice that the axial symmetry is kept. (b)-vibrations: notice thataxial symmetry will be lost. The bottom figures show how the shape will vibrate. NB: it is very

    hard to draw these things in 3D, so I wont even bother!

    3.2.5 Population of Excited States

    We use the technique ofheavy ion fusion evaporation

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    3 COLLECTIVE EXCITATIONS 34

    Figure 23: The process of heavy ion fusion evaporation. Shown is for the process48Ca +130 T e 178Hf 174 Hf+ 4n. As the beam particles will not hit the target dead-on, the compound nucleuswill rotate, in states of anything in excess of 60 h. This whole process takes place about 1012secsafter collision.

    Heavy ion fusion evaporation reactions populate high spin states (i.e. high states); as long as theenergy of the beam is above the Coulomb barrier; which is given by:

    E > Z1Z240r

    So, we see many excited states and sequences of states, as the products undergo gamma-decay.We use an accelerator to provide the beam, and have large arrays of high resolution germianiumsemi-conductor detectors.ASIDE: the accelerator (such as the Oak Ridge National Lab, Tennessee) shoots beams of particlesalong tunnels, funneling them towards a van-der-Graff generator. The generator has a pd of MV -when it sparks, and hits the cavity in which it is housed, sparks hit with a force equivalent to thatof a car going at 40mph, hitting a brick wall! And makes a massive cracking sound!

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    3.2.6 Information from -ray Spectroscopy

    Spins of the States Since = rp, the beam imparts a large angular momentum to thecompound nucleus. The angular momentum (with reference to the previous figure), will be intoor outof the page, depending on which side the beam hits. That is, the compound nucleus will be

    aligned (perpendicular to the beam direction), in a particular direction, relative to the lab beamline. So, we can measure the angular distribution of-rays in the final nucleus, by moving a detectoraround the nucleus (or, as how it is actually done, have arrays of hundreds of detectors around thenucleus).

    Figure 24: The diagram above shows the classical radiation pattern for both a dipole and quadrupole

    -ray transition; the beam direction = 0

    is shown. (a) Dipole transition. This is for = 1. Noticethat most intensity will be picked up at = 90, and virtually none along the beam direction. (b)Quadrupole transition. Here, = 2. Notice that the main difference here, is that there is a moreeven distribution of intensity along the beam direction.

    We measure -ray intensity, as a function of detector angle, and use to determine what type ofradiation (i.e. angular momentum) is carried by the -ray.

    An important technique is Directional Correlation from Orientated states DCO. For example, ifeven-even nucleus (e.g. 180Os) has ground state I = 0+; we measure the lowest -ray transitionto first excited state (about 90keV). If we find (roughly) equal intensities at 90, 0, then it mustbe a quadrupole transition. Hence, the spin of the first excited state must be 2.

    Rotational Bands Rotational bands in even-even nuclei de-excite by cascades of-ray transi-tions, between adjacent states.

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    Figure 25: Here, we see the energies of the transitions between different spin states; and the spectrumwe will see. The spacing of the states (i.e. -ray energy increases linearly) will be the same, unlessthe moment of inertia changesJ, which is seen in experiment.

    So, with reference to the figure, the energy of a state with angular momentum Iis given by:

    E(I) = h2

    2JI(I+ 1)

    Thus, -ray energies:

    E(I) =E(I) E(I 2) = h2

    2J[I(I+ 1) (I 2)(I 1)]

    Giving:

    E(I) = h2

    2J(4I 2)And, as the caption on the figure says, the energy of-rays should increase linearly with angularmomentum; but this is only the case if the moment of inertia is constant.

    4 -decay

    This is a process where a heavy nucleus reduces its charge, and therefore reduces the disruptiveCoulomb force. -particle emission is particularly favours, as it is very tightly bound. It has a largeQ-value.

    Q= mbefore mafterFor example:

    23492 U23090 T h +42H e

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    4 -DECAY 37

    Where, looking up the masses:

    23492 U = 234.040947u

    23090 T h = 230.033128u42He = 4.002603u

    Giving a Q-value for the reaction ofQ= 5.216 103u = 4.86MeV. By way of terminology, the Uis the parent nucleus, and T h the daughter nucleus.

    4.1 Theory of-emission

    Assume that an -particle is preformed, moving in the spherical potential of what will become thedaughter nucleus. There are two parts to the potential: the attractive nuclear (Woods Saxon) andCoulomb repulsion.

    Figure 26: The Woods-Saxon and Coulomb potential. The Coulomb potential is given by the charge

    of the daughter nucleus, and -particle: V = (Z2)2e2

    40r . These two potentials combine, to form the

    nuclear potential, below.

    The velocity of the particle is (non-relativistic):

    v=

    2Em

    =

    2(Q + V0)

    m 105ms1

    Classically, the alpha particle has KE = Q + V0 inside the nucleus, and can never escape.The region between a and b form a potential barrier: the Coulomb barrier. It has height B and

    width (b a); and it is these parameter which determine the probability of tunnelling.For example, in 238U, the particle hits the barrier on average 1038 times before it escapes!

    To calculate this number, consider that the particle travelling at 106ms1 (as we just calculated),traverses a distance of 1015m. Thus, the time that it takes to do this is just the distance over thespeed, giving 1021s. Then, given that the half-life is t1/2 = 10

    9yrs 1016secs. Hence, the half-lifedivided by the time taken for the particle to traverse the nucleus, gives the number of goes the particle has before it escapes the nucleus.

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    4 -DECAY 39

    Figure 28: The spectrum from-decay. Notice that most have high energy, but a few have lower.This is because most alphas leave low exicted states of the daughter nucleus, but some do exictethe daughter nucleus, hence having lower energy themselves.

    4.2 Fine Structure of-decay

    Let us use 242Cm as an example. We note:

    In general, higher Q-values have higher decay rates.

    Figure 29: The decay branches for 242Cm 238 P u+ . Notice the branching ratios (i.e. therelative percentages) of a particular decay to that excited state of the daughter.

    Let us use the following data:

    M(242Cm) = 242.05883u

    M(238P u) = 238.04955u

    M() = 4.0026033u

    To computeQ: add up masses before, add up masses after, subtract after from before; convert intokg, convert into an energy. We then find Q= 6.216MeV.

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    4 -DECAY 40

    As a second thing to note, we see that decays to states of higher spin appear to be hindered.Experimentally, decays to 8+ have branching ratio 0.00002%, and to 1, 0.00024%; but have roughlythe same Q-value.

    Thirdly, decays to some states do not occur at all; such as to 2, 3+, 4. Such decays are forbidden

    due to parity conservation.To explain the last two points, we must consider the angular momentum carried away by the

    particle.Now, by considering the particle to be a doubly magic nucleus, with spin/parity 0+, we see thatthe only angular momentum it can carry away is orbital.

    So, considering the emission of an particle, from some pointr from the centre of the nucleus. The particle will then have energy E and momentum p. Hence, angular momentumL= r p.And L = h with = 0, 1, 2, . . .. Hence, we see that the maximum possible angular momentumarises from emission at the maximum possible radius (i.e r = r0A

    1/3). Classically:

    p= 2mE= 2mQWhere by definition, the energy of the particle is the Q-value.Thus, for our 242Cm decay, with Q = 6.216MeV = 9.95 1013J, and m = 4 1.673 1027 =6.692 1027kg, we have that p= 1.15 1019kgms1. Hence, using the maximum possible, onecan (apparently) show thatmax = 8h.Hence, 2 reasons why high is unfavoured:

    First, particle must originate from a more restricted region of the nucleus: the larger radius-bithas a higher Coulomb barrier. Secondly, there is an additional contribution to the barrier height-width: the angular momentum barrier, which is a QM effect.

    Now, spin difference between parent (Ii) and daughter (If) can change by h, where:

    Ii= If+

    Where parity change is (1).So, if parent nucleus is Ii = 0

    +, then If can be, for = 0 0+; for = 1 1, = 2 2+ etc.

    Where is that carried by the . Hence, all others are forbidden: 1+, 2, 3+, 4.

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    5 -DECAY 41

    5 -decay

    This allows nucleus to reach most stable p to n ratio.

    On the mass parabola from the SEMF, for odd-mass (i.e. one parabola only), get decay to the

    right, and + and to the left. is electron capture, where the nucleus absorbs an electron fromits orbital.

    The processes are:

    : n p + e + e+ : p n + e+ + e

    : p + e n + eNote, all particles involved are fermions, having spin 1/2. Energy, momentum and angular momen-tum must be conserved in the decay.

    5.1 Q-values

    This is the KE released by a reaction.

    Q, = [mN(parent) mN(daughter)] c2Q+ = [mN(parent) mN(daughter)] c2 2mec2

    See the examples sheet for derivation.

    In-decays, theQ-value is shared between the decay products, in a way that considers momentumconservation. That is, ifPm,P,Pare the daughter nucleus, electron an neutrino recoil momenta,

    then:Pm=P+ P= 0

    The Q-value is given by:

    Q= p2

    2m+ KE() + Pc

    Where the m in the first term makes its contribution very small; and the last two terms arerelativistic, assumingis massless.

    We see from the Figure that the spectrum is continuous, up to a maximum Q. The shape ofthe spectrum is determined by the density of final states: electron and neutrino Fermi theory; aswell as the Coulomb effect on the electron/positron as it leaves the nucleus.

    From the plot, we see that we can gain information on m; which has important consequences forelectroweak decays. Experimentally, it gives the limit:

    mc2

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    5 -DECAY 42

    Figure 30: (Left) The spectrum from-decay. Notice that it is continuous (unlike-decay). The

    shape is determined by the density of final states, from Fermi theory. (Right) Notice on the rightplot, the intercept gives information about the mass of the .

    5.2 Fermi Theory

    The Fermi theory of-decay states that the decay rate is given by the Fermi Golden rule:

    =2

    h

    fVi d

    3r

    2

    (EF) (5.1)

    Where(EF) is the density of states, for electrons and neutrinos KE.

    It is the overlap integral involving the -decay operator V, connecting initial and final states.Hence, it is particularly large when decaying nuceon keeps the same wavefunction; hence, shorthalf-life. These are called superallowed transitions.

    From Krane, we write that the number of electrons with a specific kinetic energy Te is:

    N(Te)

    T2e + 2Temec2(Q Te)2(Te+ mec2)

    WhereQ Te+ T; shared between two particles.

    5.2.1 -decay Half-lifes

    From the Figure, we see that the different half-lifes are determined by Q; and infact, the decay rateis Q5:

    Q5 (5.2)

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    5 -DECAY 43

    Figure 31: Two decay modes to Nitrogen. Notice the very different half-lifes, for slightly differentQ-values of the parents.

    ft-Values If the energy dependance on half-life is taken out, a comparitive half-life, or ft-valuecan be deduced for a -transition, which depends on the inverse of the matrix element. That is:

    fVi d3r

    2

    1

    Since such values range from 103 103secs, a log10ft is usually quoted; having value 3-4 for thesuperallowed decays.

    Below is a table of decays to 147 N7, and the parents which decay to it, and with their correspondingdata.

    14C log ft = 9.03 0+ 1+ Q = 0.156MeV14O(0.6%) + log ft = 7.3 0+ 1 Q = 5.144MeV14O(99.3%) + log ft = 3.4 0+ 0+ Q = 2.83MeV

    The table shows that the last entry is of the type superallowed.

    It turns out that:

    f t= 23h ln(2(hc)6)

    (mec2)5G2Vm2 1

    G2V

    WhereGVis the weak interaction coupling constant; and is thus a fundamental test of the StandardModel.

    5.3 Angular Momentum Rules for -decay

    Remember that for -decay, involving h, we had an emitted a distance:

    r= h2mE

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    From the centre. Since me, m

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    5.3.2 First Forbidden Decay

    Here, we have = 1, and hence a parity change of1. We have:

    Ii= If+S+

    The Fermi-first forbidden has s= 0, and hence I= 0, 1.The GT-first forbidden has s= 1, and thus that I= 0, 1, 2.Considering an example:

    115In(9/2+) 115 SN(1/2+)We see that I= 9/2 1/2 = 4. And that = 0. Hence, we deduce that must be even. Now,as I= + s, we see thats can either be 0 or 1 (for = 4, 3). However, we also saw that must beeven . Therefore, we conclude that it must be of Fermi-type (i.e. s = 0), and the fourth forbiddendecay (as = 4). Infact, such a reaction has t1/2 1014yrs!Another example:

    9/2 1/2+So, I= 4, and = 1. Thus, we see that must be odd. s can be either 0 (Fermi) or 1 (GT).If 0, then must be 4 (which is even, which we have discounted); or 1, then must be 3, and weconclude that this must be the case.Hence, it is the third forbidden GT decay.

    5.4 Parity Violation in -decay Process

    Most laws of nature are parity invariant; they dont change under r r, a reflection through theorigin. Examples are the strong force and EM: they all conserve parity.

    If the Hamiltonian conserves parity, then the eigenstates are said to have good parity. Note:(r) = (r); if the -, then even, and if +, then odd.In 1957, Madame Wu (et al) discovered the -decay (weak int) process violated parity:

    Vnuclear =Vstrong+ VEM+ Vweak

    WhereVweak is the parity violating part of nuclear potential, and is of the order 107.

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    6 -RAY EMISSION 46

    6 -ray Emission

    6.1 Angular Momentum Considerations

    Photons carry an intrinsic spin ofs= 1, with a component of either sz =1 (but not zero) alongthe direction of propogation. Like -particles,-rays have difficulty in carrying away orbital angularmomentumh.

    If a-ray is emitted from postionrfrom the centre of a nucleus, carrying energy E, and momentump= hk, where E=pc = hkc; with the useful relation:

    hc= 197M e Vf m

    Thus, we have that h= r p. Hence:

    r=h

    p =

    hc

    E= 100f m

    Where we have computed for E= 2MeV. That is, for a photon to carry away angular momentum, it must have been emitted from a distance 100fm from the centre. This is way out in the tail ofthe nuclear wavefunction.Also, via h= r pand p = hk, we can see that:

    h= r hk

    That is:= kr

    But, kR

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    6 -RAY EMISSION 47

    L Transition Type Comments

    E1 Electric Dipole Must be = 0 ass= 1. Therefore, not hindered,and thus fast.

    M1 Magnetic Dipole Must be= 0 ass= 1. Therefore, not hindered,

    and thus fast, but slower than E1.E2 Electric Quadrupole Must be = 1, as s = 1. It is hinderd via

    (kR)2 = (kR)2; and parity change w.r.t dipole.M2 Magentic Quadrupole Same as E2.

    E3, M3 Electric/Magnetic Octupole = 2, s = 1. Hindered via (kR)2 = (kR)4,compared to dipole.

    E4, M4 Electric/Magnetic Hexadecupole Hindered by (kR)6 (= 3).

    Experimentally, we see the lowest order most of the time, as it is least hindered.

    We use DCO (directional correlation from orientated states) to distinguish between states.

    6.2 Parity Rules

    Now, we mentioned that parity changes for different transitions, but we did not say from what towhat.

    Suppose we have a transition Iii Iff . We have the following rules:

    EL Parity Change Example,Iii Iff .

    E1 Yes 1 0+E2 No 2+ 0+E3 Yes 3 0+E4 No 4+ 0+

    And, for magnetic:

    M L Parity Change Example,Iii Iff .

    M1 No 1+ 0+M2 Yes 2 0+M3 No 3+

    0+

    M4 Yes 4 0+

    So, notice that E and M are opposite. We will derive E1 later. Experimentally, we can distinguishbetween these EL & ML by measuring -ray polarisation.

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    6 -RAY EMISSION 48

    6.2.1 Angular Momentum Considerations

    Radiation carries away Lh of angular momentum:

    Ii= If+L

    Under the usual vector addition rules. That is, the possible L values:

    |Ii If| L |Ii+If|Note, L = 0 is not possible. Transition proceed by least hindered process, usually the one withlowest L. However, there is a common exception: an enhanced E2 can often compete with M1,as they have the same parity change. When more than one L contribute, we call it a mixedtransition.

    Figure 32: Some possible transitions. (a) We have that|20| L |2 + 0| as the possiblevalues. Hence, L = 2 only, and must be E2 as no parity change. (b) Same reasoning as for (a). (c)Again, the only possible value ofL is 2, and there is no parity change, hence E2. (d) We have that|2 2| L |2 + 2|, hence possibleL = 0, 1, 2, 3, 4. We exclude 0. Hence possible are M1, E2, M3,E4 (by parity considerations: not changing). The higherL values are hindered; hence we get themixed transition of both M1 & E2. (e) Possible|4 2| L |4 + 2|, i.e. L= 2, 3, 4, 5, 6. However,lower L favoured. Hence E2 or M3 mixed transition.

    6.3 Parity Rule for E1 & Transition Rates

    Now, the electric dipole moment is charge times the distance between the two charges: ez. Hence,the E1 transition rate goes like:

    fezid

    2

    Via the Fermi Golden rule.

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    6 -RAY EMISSION 49

    Sincez is an odd function, then the integrand is zero ifi,

    fhave the same parity.

    The rule is that E1 transitions connect states of opposite parity. Transition rates are given by theFermi Golden rule:

    =2

    h fM(L)id

    2 dN

    dEWhere M(L) is the operator for a L-type transition, having the form:

    M(L) 1k

    (kr)LPL(cos )

    Notice the (kr)L dependance coming in. The factor ofdN/dE is just the density of final states foremitted photon, and is E3.

    6.4 Single Particle Weiskopf Estimates

    Now, we calculate:

    fM(L)id

    2For a single proton making a simple transition between two shell-model states. We shall say thati, f are known wavestates. We are able to calculate (but not actually do) rates for varioustransitions:

    (E1) = 1 1014A2/3E3(E2) = 7.3 107A4/2E5(E3) = 34A2E7

    (E4) = 1.1

    105A8/3E9

    With a set for magnetic transitions:

    (M1) = 5.6 1013E3(M2) = 3.5 107A2/3E5(M3) = 16A4/3E7

    (M4) = 4.5 106A2E9

    Where the transition rate is ins1; andE in MeV. So, for example, a 152keV transition in142Tb

    has:

    (E1) = 1

    (E1)

    = 1.04

    1013secs (M1) = 5.08

    1012secs

    We have used that the lifetime of a L-decay is:

    = 1

    (L)

    And also, its half-life:

    t1/2= ln 2

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    6 -RAY EMISSION 50

    Now, a state may decay via different modes: 4+ 2+, via E2, or 4+ 3+ via M1. The total decayrate is:

    total = (E2) + (M1)

    And hence the lifetime of the state is:

    (4+) = 1total

    The experimental data can be compared with these single particle rates.; to determine wetherenhanced rate or hindered rate.

    For example, in rotational nuclei, where large number of nucleons Nare coherently involved in themotion, then the E2 rate would be enhanced.

    fM(E2)id N single particle value

    Thus, the decay rate:

    2 N2(single particle)

    This is why E2 transitions can compete with single particle M1 transitions (note, M1, as sameparity change). For example, superdeformed E2s may have 2000 times single particle values.

    6.5 Internal Conversion

    This is a process which competes with -decay. The nucleus makes the transition by giving theenergy to one of the orbiting electrons. So, the total decay rate is the sum of-decay and internaldecay rate:

    total = + e

    Then, is shortened. We define the internal conversion coefficient:

    e

    So, if = 1, then the decay rate is doubled by internal conversion, and thus the lifetime is halved.Also, the coefficient is the sum for contributions from different electron shells.

    Also,L= 0 transitions are not allowed, via -decay. However, they can occur by internal conver-sion.