Title: Physics Applied to Radiology RADI R250 Fall 2003
1Physics Applied to RadiologyRADI R250 -- Fall
2003
2(No Transcript)
3Atomic Models
4Matters Fundamental Particles
- electron proton neutron
- MASS SI (absolute value) 9.1 x 10-31 kg
1.7x10-27 kg 1.7x10-27 kg - relative (to e-) 1 1836 1838
- relative (to p) 1/2000 1 1
- atomic mass number 0 1 1
- atomic mass unit .000549 1.00728
1.00867 - CHARGE SI (absolute value) -1.6x10-19 C
1.6x10-19 C 0 - relative -1 1 0
- LOCATION orbit nucleus nucleus
- SYMBOL e- p no
5Term Atomic Number (Z)
- identifies an element
- every element has a different atomic number
- of protons in the nucleus
- electrically neutral atom p e
- abbreviation Z
6Electron Orbits
Shell Numbers n
Shell Letter Designations
- Bohr's model too simplified but useful concept
- energy levels or shells that contain e-
- each shell has specific binding energy (Eb)
- e- must gain energy to move outward
- e- loses energy to move inward
7Binding Energy (Eb)
- strength of the nuclear pull on the e-
- inner shells higher Eb
- outer shells lower Eb
- each element has unique set of Eb
- ground state all e- as close to nucleus as
possible
8Eb (cont.)
Ground State
Excited State
1 or more e- above ground
12C 2k 4l
9Eb Atomic Number
High Z atom
Low Z atom
- greater of p in high Z
- higher Eb for all shells
10Quantum Numbers
- more precise location to individual e- of an atom
- 1st principle main energy level (shell) n
- 2nd orbital subshells shape of orbit l
- 3rd spatial orientation to nucleus ml
- 4th spin magnetic orientation ms
- Pauli exclusion principle -- no 2 e- may have the
same 4 quantum numbers - Maximum of e- in an inner shell 2n²
- Maximum of e- in an outer shell 8 (except k
2)
11Shell e- Capacity
k shell
n 1 2n2 2 outer shell 2
12Shell e- Capacity (cont.)
13Electronic Transitions
- movement of e- between shells
- e- at lowest (ground) E state
- e- needs E to move to a higher shell
- E to D Eb
- E released when e- returns to ground state
- characteristic xray
14Orbital Transitions
- Determine the energy gain that the electron
receives in the example to the right. - Ee D Eb En - Eo
- -50 eV - (-900 eV)
- 850 eV
- Determine the characteristic x-ray energy emitted
in the example to the right. - Ex D Eb Eo - En
- -40 eV - (-1000 eV)
- 960 eV
Eb
Ee
n -35 eV
m -50 eV
l -300 eV
k -900 eV
15Neutral vs. Ionized Atoms
- Neutral atom
- p e-
- electrically uncharged
- Ionization
- any process that or - e- from an atom p ¹
e- - ion -- electrically charged atom
- ion pair -- charged atom charged particle
16Periodic Law
- chemical physical properties of elements repeat
at regular intervals - enables classification of elements
- inert gasses
- metals
- based on
- elements Z
- of outer shell orbital e-
17Periodic Table (Bushong figure 4-4, page 40)
- chart of all known elements
- illustrates the Periodic Law
18The Periodic Table Atomic
- elements listed by increasing Z
19Groups (columns)
- represents of electrons in the outer shell of
element - element in the same group will react similarly
Outer shell e- I 1 e- II 2 e- III 3 e-
20Periods (rows)
- represents the principle quantum number (n) of
the outermost electron shell of the element
ç n 3 è
21Periodic Table -- example of use
- For the shaded box on the table, determine the Z,
total of e-, of orbital shells, of e- in
each shell? - Z 17
- e- 17
- shells 3
- e- in sh. k 2 l 8 m7
22Structure of the Nucleus
- central core of the atom
- contains p n0 ( other particles)
- identifies the atom as a specific element
- held together by fundamental force ("strong")
23Nucleon(s)
- generic term for the particles found in the
nucleus - reference to protons neutrons in the nucleus
without being specific
24NUCLEUS
- complex arrangement of nucleons empty space
- of p in nucleus defines an element (Z)
- p n are in all elements except hydrogen
- many other subatomic particles (50)
25Protons
- of p in nucleus defines the element
- called the atomic number (Z)
- 1 p hydrogen
- 2 p helium
- 3 p lithium
- neutral atom e- p
26Neutrons
- element (specific p) may exist with differing
numbers of neutrons - example p n0
- hydrogen 1 0
- hydrogen 1 1
- hydrogen 1 2
- neutron number (N) n0 in the nucleus
27Nuclear Nomenclature
- atomic mass number (A) total number of nucleons
- A Z N
- symbolic notation
28Nuclide
- generic term
- helps identify nuclear configuration
- p n
- gt100 elements but gt1500 nuclides
- classification of nuclides by similarities
- isotope p Z same element
- isobar nucleons A
- isotone n N
- isomer p n Z N excess energy
29Isotope Example
30Isotopes
- varies for each Z
- 3 for hydrogen, 26 for tin
- some are man-made
- isotopic configurations of nuclides
- stable (at ground state)
- unstable (excited state) radionuclide
- non-existent
31Isobar Example
32Isotone Example
33Isomer Example
34Nuclide Set Selection Example
- From the following set of nuclides, select sets
of isotopes, isotones and isobars - A
- Z
- N 32 33 33 33 32
- isotope Z 60Ni, 61Ni 59Fe, 58Fe
- isotone N 59Fe, 60Co, 61Ni 58Fe, 60Ni
- isobar A 60Ni, 60Co
60
60
59
61
58
Ni
Co
Fe
Ni
Fe
28
27
26
28
26
35Radioactivity
- definition see notes
- property of unstable nuclei
- spontaneous break up of nucleus
- forms other nuclide and emits radiation
- many factors that determine radioactivity
- N/P ratio
- too many or too few neutrons
- nuclear energy state
- above its ground energy state (excited)
36N/P Ratio Thompson figure 3-9, page 68
37Radionuclide
- nuclear configuration that is unstable and
exhibits radioactivity - activity
- quantity that measures amount of radioactive
material - indicates rate that radiation is emitted
- units
- common Curie (Ci) 3.7 x 1010 d/s
- SI Bequerel (Bq) 1 d/s
- d/s disintegrations/s
38Radioactive Decay (disintegration)
- process used by atom
- original radionuclide is unstable
- it ejects energy /or particles
- and changes into a different nucleus
- new nuclide may be stable or unstable
- If stable, nuclide exists and persists
- If unstable, it will decay continuing the process
until stability is reached - Decay series (or chain) formed
39Radioactivity Flow Chart
40Radioactivity
- definition see notes
- property of unstable nuclei
- spontaneous break up of nucleus
- forms other nuclide and emits radiation
- many factors that determine radioactivity
- N/P ratio
- too many or too few neutrons
- nuclear energy state
- above its ground energy state (excited)
41NP Ratio
- Plot of p (Z) vs. n (N) for all stable nuclides
- any nuclide combination that exists off of the
line of stability is unstable - unstable nuclides will emit radioactive energy
/or particles to move closer to line of
stability
42Physical Half-Life (T½)
- time required to reduce the activity of a
radionuclide to ½ of its original value - rate of decay of the radionuclide
- each radionuclide has a specific T½
- no 2 radionuclides have the same T½.
43T½ Example
T½ 3.8 d
start
after 1T½ 3.8 d
after 2T½ 7.6 d
44Using T½ to determine activity
- Need T½ for radionuclide
- Find the T½ that have passed since know A
- T½ time / T½
- Example
- How many half-lives occur in 32 days for a
radionuclide with a T½ of 13.2 days? - T½ ?? Time 32 days T½ 13.2 days
- T½ time / T½
- 32 days / 13.2 d/T 1/2
- 2.42424242 T1/2
- 2.4 T1/2
45Using T½ to determine activity
- Find of original that will remain (3 ways)
- 1. Formula .5T½ use yx calculator key
- 2. Read from graph (see page 51) (estimate)
- 3. Make chart estimate if between whole T½
- T½ decimal
- 0 100 1.00
- 1 50 .50
- 2 25 .25
- 3 12.5 .125
46Using T½ (cont.)
- Find remaining activity
- Multiply starting activity by
- A Ao A0original activity
- Combining Equations
- .5T½ A Ao
- A .5T½A0
47T½ Example
- 82 µCi of radon gas is contained in a closed
beaker. How much will remain after 9.5 days? (T½
of Rn 3.8days) - A?? 82 µCi A0 9.5delapsed t 3.8d T½
- T½ time / T½ 9.5d / 3.8d 2.5
- .5T½ .52.5 0.1767766952966
- A A0
- 0.1767766952966 82 µCi
- 14.49568901432 µCi
- 14 µCi
48Alpha Decay a
Process
49Alpha Decay a
- Description 2p 2n0 (helium nucleus)
- Origin high Z nucleus (Zgt82)
- Effect on nucleus Z 2
- N 2
- A 4
- Charge 2
- Mass Number 4
- Ionization high
- Penetration low
- After KE lost captures 2 e- becomes He gas
50Beta- Decay b-
Process
Decay Equation
Decay Schematic
5730 yr
b- ( .156 MeV)
51Beta- Decay b-
- Description negatron (electron)
- Origin neutron rich nucleus
- Effect on nucleus Z 1
- N 1
- A (isobar) n0 D p
- Charge -1
- Mass Number 0
- Ionization low
- Penetration moderate
- After KE lost becomes free e-
52Beta Decay b
Process
Decay Equation
Decay Schematic
53Beta Decay b
- Description positron (positive electron)
- Origin neutron deficient nucleus
- Effect on nucleus Z 1
- N 1
- A (isobar) p D n0
- Charge 1
- Mass Number 0
- Ionization low
- Penetration moderate
- After KE lost attracts e- annihilates
54Annihilation Radiation
b e- Þ M
55Gamma Ray Emission g
Decay Equation
Process
Decay Schematic
56Gamma Ray Emission g
- Description electromagnetic radiation
- Origin nucleus with excess energy
- Effect on nucleus energy (isomeric transition)
- No D in Z, A or N
- Charge none
- Mass Number none
- Ionization very low
- Penetration high
- After E lost ceases to exist
57Other Radiation Processes
- Neutron emission
- Proton emission
- electron capture e
- fission
- fusion
- others
58Combination Emissions
- many radionuclides decay in multiple modes
- example
59NP Graph
b- -- n D p (isobar) b -- p D n (isobar)
D N -- isotope
D p -- isotone