Introduction A more general title for this course might be “Radiation Detector Physics” Goals are to understand the physics, detection, and applications of ionizing radiation The emphasis for this course is on radiation detection and applications to radiological physics However there is much overlap with experimental astro-, particle and nuclear physics And examples will be drawn from all of these fields 1 Introduction While particle and medical radiation physics may seem unrelated, there is much commonality Interactions of radiation with matter is the same Detection principals of radiation are the same Some detectors are also the same, though possibly in different guises Advances in medical physics have often followed quickly from advances in particle physics 2 Introduction Roentgen discovered x-rays in 1895 (Nobel Prize in 1901) A few weeks later he was photographing his wife’s hand Less than a year later x-rays were becoming routine in diagnostic radiography in US, Europe, and Japan Today the applications are ubiquitous (CAT, angiography, fluoroscopy, …) 3 Introduction Ernest Lawrence invented the cyclotron accelerator in 1930 (Nobel Prize in 1939) Five years later, John Lawrence began studies on cancer treatment using radioisotopes and neutrons (produced with the cyclotron) Their mother saved from cancer using massive xray dose 4 Introduction Importance and relevance Radiation is often the only observable available in processes that occur on very short, very small, or very large scales Radiation detection is used in many diverse areas in science and engineering Often a detailed understanding of radiation detectors is needed to fully interpret and understand experimental results 5 Introduction Applications of particle detectors in science Particle physics ATLAS and CMS experiments at the CERN LHC Neutrino physics experiments throughout the world Nuclear physics ALICE experiment at the CERN LHC Understanding the structure of the nucleon at JLAB Astronomy/astrophysics CCD’s on Hubble, Keck, LSST, … , amateur telescopes HESS and GLAST gamma ray telescopes Antimatter measurements with PAMELA and AMS Condensed matter/material science/ chemistry/biology Variety of experiments using synchrotron light sources throughout the world 6 Introduction Applications of radiation/radiation detectors in industry Medical diagnosis, treatment, and sterilization Nuclear power (both fission and fusion) Semiconductor fabrication (lithography, doping) Food preservation through irradiation Density measurements (soil, oil, concrete) Gauging (thickness) measurements in manufacturing (steel, paper) and monitoring (corrosion in bridges and engines) Flow measurements (oil, gas) Insect control (fruit fly) Development of new crop varieties through genetic modification Curing (radiation curing of radial tires) Heat shrink tubing (electrical insulation, cable bundling) Huge number of applications with hundreds of billions of $ and millions of jobs 7 Introduction 8 Introduction Cargo scanning using linear accelerators 9 Radiation Directly ionizing radiation (energy is delivered directly to matter) Charged particles Electrons, protons, muons, alphas, charged pions and kaons, … Indirectly ionizing radiation (first transfer their energy to charged particles in matter) Photons Neutrons Biological systems are particularly sensitive to damage by ionizing radiation 10 Electromagnetic Spectrum Our interest will be primarily be in the region from 100 eV to 10 MeV 11 Electromagnetic Spectrum Note the fuzzy overlap between hard x-rays and gamma rays Sometimes the distinction is made by their source X-rays Produced in atomic transitions (characteristic x-rays) or in electron deacceleration (bremsstrahlung) Gamma rays Produced in nuclear transitions or electron-positron annihilation The physics is the same; they are both just photons 12 Nuclear Terminology Nuclear species == nuclide A nucleons (mass number), Z protons (atomic number) N neutrons (neutron number) A = Z+N Nuclides with the same Z == isotopes Nuclides with the same N == isotones Nuclides with the same A == isobars Identical nuclides with different energy states == isomers Metastable excited state (T1/2>10-9s) 13 Table of Nuclides Plot of Z vs N for all nuclides Detailed information for ~ 3000 nuclides 14 Table of Nuclides Here are some links to the Table of Nuclides which contain basic information about most known nuclides http://www.nndc.bnl.gov/nudat2 http://atom.kaeri.re.kr/ton/ http://ie.lbl.gov/education/isotopes.htm http://t2.lanl.gov/data/map.html http://yoyo.cc.monash.edu.au/~simcam/ton/ 15 Table of Nuclides ~3000 nuclides but only ~10% are stable No stable nuclei for Z > 83 (bismuth) Unstable nuclei on earth Naturally found if τ > 5x109 years (or decay products of these long-lived nuclides) 238U, 232Th, 235U (Actinium) series Laboratory produced Most stable nuclei have N=Z True for small N and Z For heavier nuclei, N>Z 16 Valley of Stability 17 Valley of Stability Table also contains information on decays of unstable nuclides Alpha decay 238 234 4 U Th Beta (minus or plus) decay 92 90 2 He 137 Cs Ba e v(IT) e Isomeric transitions 56 4 U 234 90Th 2 He 238 92 137 55 Tc Tc fission (SF) 99 m 99 43 43 Spontaneous 256 100 112 Fm140 Xe 54 46 Pd 4n 18 Valley of Stability 19 Binding Energy The binding energy B is the amount of energy it takes to remove all Z protons and N neutrons from the nucleus B(Z,N) = {ZMH + NMn - M(Z,N)} M(Z,N) is the mass of the neutral atom MH is the mass of the hydrogen atom One can also define proton, neutron, and alpha separation energies Sp = B(Z,N) - B(Z-1,N) Sn = B(Z,N) - B(Z,N-1) Sα = B(Z,N) - B(Z-2,N-2) - B(4He) Similar to atomic ionization energies 20 Binding Energy Separation energies can also be calculated as Sn M AZ1 X M n M ZA X S p M ZA11 X M 1H M ZA X Note these are atomic masses S M ZA22 X M 4 He M ZA X Q, the energy released, is just the negative of the separation energy S Q>0 => energy released as kinetic energy Q<0 => kinetic energy converted to nuclear mass or binding energy Sometimes the tables of nuclides give the mass excess (defect) Δ = {M (in u) – A} x 931.5 MeV 21 Example Is 238U stable wrt to α decay? Sα = B(238U) - B(234Th) - B(4He) Sα = 1801694 – 1777668 – 28295 (keV) Sα = -4.27 MeV => Unstable and will decay 22 Radioactivity Radioactive decay law dN Ndt N t N 0e t where N t is thenumber at timet 1 t / N t N 0e where is themean lifetime Nomenclature λ in 1/s = decay rate λ in MeV = decay width (h-bar λ) τ in sec = lifetime You’ll also see Γ = λ 23 Radioactivity t1/2 = time for ½ the nuclei to decay N0 t / N t N 0e 2 1 t ln 2 ln 2 t1 / 2 ln 2 24 Radioactivity It’s easier to measure the number of nuclei that have decayed rather than the number that haven’t decayed (N(t)) The activity is the rate at which decays occur dN t t At N t A0e dt A0 N 0 Measuring the activity of a sample must be done in a time interval Δt << t1/2 Consider t1/2=1s, measurements of A at 1 minute and 1 hour give the same number of counts 25 Radioactivity Activity units bequerel (Bq) 1 Bq = 1 disintegration / s Common unit is MBq curie (C) 1 C = 3.7 x 1010 disintegrations / s Originally defined as the activity of 1 g of radium Common unit is mC or μC 26 Radioactivity Often a nucleus or particle can decay into different states and/or through different interactions The branching fraction or ratio tells you what fraction of time a nucleus or particle decays into that channel A decaying particle has a decay width Γ Γ = ∑Γi where Γi are called the partial widths The branching fraction or ratio for channel or state i is simply Γi/Γ 27 Radioactivity Sometimes we have the situation where 1 2 1 2 3 226 Ra Rn Po 222 218 The daughter is both being created and removed 28 Radioactivity We have (assuming N1(0)=N0 and N2(0)=0) dN1 1 N1dt dN2 1 N1dt 2 N 2dt then N 2 t N 0 2 1 e 1t e 2t 1 A2 t 2 N 2 t A0 2 2 e and maximumactivityat ln2 / 1 tmax 2 1 1t e 2t 1 29 Radioactivity Case 1 (parent half-life > daughter half-life) This is called transient equilibrium 1 2 N1 t N 0e 1t N 2 t N 0 1 2 1 e 1t e 2t becomes 2 N 2 2 1 e 2 1 t 1 N1 2 1 A2 2 A1 2 1 30 Radioactivity Transient equilibrium A2/A1=2/(2-1) Example is 99Mo decay (67h) to 99mTc decay (6h) Daughter nuclei effectively decay with the decay constant of the parent 31 Radioactivity Case 2 (parent half-life >> daughter half-life) This is called secular equilibrium Example is 226Ra decay 1 2 N 2 t N 0 1 2 1 e 1t e 2t becomes 1 N 2 t N 0 1 e t 2 2 N 2 t N 01 2 A2 A1 32 Radioactivity Secular equilibrium A1=A2 Daughter nuclei are decaying at the same rate they are formed 33 Radioactivity Case 3 (parent half-life < daughter half-life) What happens? 34 Units Sometimes I will slide into natural units used in particle physics c 1 Then at the end of the calculation or whatever we’ll insert h-bar’s and c’s to make the answer dimensionally correct And while it might not come up so often e 2 1 4 0c 137 35 Electromagnetic Spectrum What part of the EM spectrum has a physiological effect on the human body? 36 Radioactivity Case 3 (parent half-life < daughter half-life) What happens? Parent decays quickly away, daughter activity rises to a maximum and then decays with its characteristic decay constant 37 Electromagnetic Spectrum What part of the EM spectrum has a physiological effect on the human body? 38 Electromagnetic Spectrum Photon energy is given by E h hc 1.240 106 E eV m h 1.051034 Js 6.5810 22 MeVs 2 -19 1 eV 1.60210 J c 197 MeVfm 200 MeVfm 39 Constants and Conversions 34 1.05 10 22 Js 6.58 10 MeVs 1eV 1.6 1019 J c 3 10 m / s 8 15 1F (fermi) 1 10 m c 197.3MeVF e2 1 4 0c 137 1b (barn) 1028 m 2 40