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Physical, Biological, Effective
Types of half-life
Physical half-life
The time required for a quantity of radioactivity to be reduced to one-half its original value
Every radioactive material has its own unique half life value
All radioactivity never disappears
Quantity decreases but never reaches zero
T1/2 = 0.693/ lambda
formula for physical half-life
3.3 half-lives
1 tenth life
Biological Half-life
The time required for the body to eliminate one-half of the dose of any substances by biological processes
Determined by the clearance of the radionuclides from the organ, tissue or body
Perspiration, urine, feces, exhalation
sample of biological half-life
Biological half-life
Most radiopharmaceuticals are also cleared from organs by various physiologic processes
Effective half-life
A combination of both T1/2 and Tb
The time required for half of initial radioactivity to disappear from an organ or body by combination of excretion and physical decay
Must always shorter than T1/2 or T
1/Te = 1/T1/2 + 1/Tb
formula for effective half-life
Alpha Decay, Beta Decay, Electron Capture, Isomeric Transition, Internal Conversion, Isobaric Transition
Decay Modes
Alpha Decay
Spontaneous decay emission of an alpha particle
Not used in medical imaging
Most common in A > 150 and Z > 82
Z - 2, A - 4, N - 2
Result of Alpha Decay
Alpha Particle
Identical to a helium nucleus
Consists of 2 protons and 2 neutrons
Heaviest and least penetrating form of radiation
Emitted from the atomic nucleus
Carries an electronic charge twice that of the proton
High LET
a
Symbol of Alpha particle
4
A of Alpha particle
+2
Charge of alpha particle
Little risk
external source of alpha particle
High risk
internal source
Ingestion, inhalation, wound
types of internal source
Paper
Alpha particles can be absorbed by?
Beta Decay
Occurs in allradionuclides
Occurs much more frequently than alpha particle
Emits beta particles
Beta minus, beta plus
Types of beta decay
Beta minus
Results:
Z + 1
A = no change
N – 1
Emits negatron and antineutrino (v)
Beta plus
Results:
Z - 1
A = no change
N + 1
Emits positron and neutrino (v)
Positron
Positively charge
Polyenergetic
Causes ionization
React violently with electron causing annihilation
Negatron
Negatively charge
Causes ionization
Antiparticle of positron
Antineutrino, Neutrino
Subatomic particle
Neutral charge
Lighter than electron
Electron Capture
K-capture
Method of radioactive decay that involves the capture of an orbital electron most likely in the K or L-shell by its nucleus
Similar to positron decay
Occurs in proton rich (neutron deficient) nuclei
Electron Capture
Most common in heavy proton rich nuclei
1 e- + 1 p+ ⟶ 1 n + neutrino
<1.02 MeV
common threshold for e- capture
≥1.02 MeV
both e- capture or beta plus decay may occur
Same as beta plus decay, characteristic xrays, gamma rays, auger electron
results of electron capture
Auger Process
The process of removing electron by a characteristic x-rays within an atom
Isomeric Transition
A decay process occurs when a nuclei in the excited state goes to ground state by emission of gamma radiation to attain stability
Isomeric State
Metastable state
Exists for >10^-9 s
Always unstable
No change in Z,A,N, Emission of gamma radiation, characteristic radiation, Auger electron
results of isomeric transition
Internal Conversion
Multipole electric fields of the nucleus interact with the orbital e
Causes ionization of electron
Not the same as gamma decay
Excess Electromagnetic Transition Energy
The surplus energy stored within a nucleus when its protons and neutrons are in an excited, unstable arrangement
Unstable configuration
After a nucleus undergoes alpha or beta decay, its protons and neutrons (nucleons) are often left rearranged in a high-energy "excited state."
EM Force (279keV), Ionized atom, Inner-shell vacancy, Internal conversion electron, stable nucleus, characterostic xrays, auger electrons
Results of internal conversion
Isobaric Transition
Modes of decay in which the mass number remains constant
Negatron decay, Positron decay, Electron Capture
isobaric transition occur in?