Radioactivity
resides in UNSTABLE NUCLEUS.
Nucleus decays with EMISSION OF RADIATION.
Many elements have both:
stable isotopes (non-radioactive, eg 12C),
and
unstable isotopes (radioactive, eg 14C).
Different numbers of neutrons in nucleus.Electronic
configuration the same as that of non-radioactive isotope of same element, so chemical
properties are the same.
Hence use in chemistry and biology of
RADIOACTIVE TRACERS
Substitute radioactive for stable isotope, undergoes exactly same reactions but can be
detected and measured as required by radiation monitoring device.
Types of Radioactive Decay
a-emission
Nucleus disintegrates with emission of alpha particles (ionized He nuclei, He2+).
| eg |
226 |
Ra ---> |
222 |
Rn + |
4 |
He |
| 88 |
86 |
2 |
Only for elements of high atomic no. (>80), little used in biochemistry.
b-emission
Nucleus disintegrates with emission of electron (b-
particle), or less commonly a positron (b+
particle).
| eg |
14 |
C ---> |
14 |
N + b- |
| 6 |
7 |
g-emission
Disintegrating nucleus emits radiation (hn), high energy,
ionising cf X-rays.
Gamma ray emission can occur along with emission of beta particles, or as a result of
other processes eg electron capture, or sometimes without affecting atomic no. of
nucleus.
| eg |
125 |
I + e- (capture) ---> |
125 |
Te + g |
| 53 |
52 |
Detection and Measurement of Radioactivity
Geiger-Muller counter
Radiation causes ionization of gas in tube
---> current flow.
Portable, useful for monitoring of spillages.
Scintillation Counters
Preferred for most quantitative work:
Radiation from radio-isotope ---> excitation of electrons in a SCINTILLANT or FLUOR
---> emission of LUMINESCENCE, measure with photodetector.
- Solid scintillation counter
(gamma counter)
g-rays emerge from sample tube - impinge on external
scintillant crystal (NaI/T1I) --> emits light pulses to photomultiplier.
- Liquid scintillation counter
(beta counter)
b-particles often too weak to use external fluor.
Sample mixed in solution with "scintillation cocktail". Captures b-emission at source ---> photons. May be 2-stage process
involving primary and secondary fluors.
Units of Radioactivity
Fundamental (and SI) unit is the Becquerel (Bq) which is the number of
DISINTEGRATIONS PER SECOND (dps), ie. the number of nuclei that break down per second.
For historical reasons, radioactivity often measured in Curie (Ci) units.
1Ci = 3.7 x 1010 Bq
Because of the magnitudes, common derived units are :
- the microCurie (mCi)
- the megaBecquerel (MBq)
Measuring device reads counts per minute (cpm). In a scintillation counter each
"count" = pulse of light from fluor activated by radiation.
Counting efficiency < 100%, because of:
- radiation escaping without activating fluor
- fluors undergoing quenching
- hn from fluors not reaching photodetector
| Bq = |
cpm
60 |
x |
100
counting efficiency (%) |
Specific Radioactivity
This is radioactivity per gram
or
per mole of compound
Isotopically labelled compounds usually diluted with an excess of
unlabelled compound (carrier) in order to:
- use biologically relevant concentrations without excessive radiation hazard
- avoid excessive loss of isotope by adsorption etc.
| Specific activity increases as{ |
labelled species
|
} increases |
carrier |
Isotope dilution analysis depends on principle of adding labelled species of known
specific activity then measuring specific activity of a recovered sample, hence calculate
amount of unlabelled species in sample.
Decay Kinetics: Half-Life
Disintegrations of radioactive nuclei in sample are in proportion to number present
(1st order kinetics), so isotope decays exponentially. (Holme & Peck Ch 5).
Half-life (t0.5)= Time for no. of radioactive nuclei to decay by half
Important factor in planning experiments with isotopes.....
Long t0.5 (eg 14C, 5570 years):
- no complications due to loss of isotope over duration of experiment, but
- significant hazard if ingested (long-term exposure)
Shorter t0.5 (eg 32P, 14.2 days)
- plan purchase so delivery only when ready to use
- allow for decay during experiment (especially if measuring, eg metabolic
elimination)
Biochemical Aplications of Isotopes
Tracers
To observe metabolic fates of species. eg mechanism of photosynthesis:
CO2 + H2O ---> (CH2O) + O2
Reaction carried out using 18O labelled CO2 ---> No 18O
recovered as O2. Some in H2O.
If using 18O labelled H2O, all 18O recovered in O2.
So better representation of overall process is:
CO2 + 2H2O ---> (CH2O) + O2 + H2O
{ie CO2 + 2H2O ---> (CH2O)
+ O2 + H2O}
Enzyme assay
CH3CO.~SCoA + *CO2 -----> -OO*C-CH2CO.~SCoA
acetyl -CoA
malonyl-CoA
Measure fixation of *C (14C). (Becomes non-volatile)
Isotope Dilution Analysis
See 13.4,
also cf stable
isotope dilution analysis by mass spectrometry (5.4.1)
Radioautography (Autoradiography)
Detect position of specific labelled species on chromatogram or electrophoretogram
Into which protein has labelled glycine gone?
or
Which DNA fragment has bound labelled probe?
Place on top of photographic film. Incubate in light proof (& radiation proof)
container. Develop. Radiation produces an image.
Largely supplanted by luminescent probes.
Radioimmunoassay
The original form of competitive-binding immunoassay. Labelled (usually 125I)
and unlabelled antigen (Ag) compete for limited antibody (Ab).
Ag + Ab + Ag* <--> mixture of Ab-Ag & Ab-*Ag
Separate *Ag from Ab-*Ag (eg by precipitation with second antibody), and quantify
Ab-*Ag.
As Ag in test sample is increased, radioactive Ab-*Ag decreases.
Calibrate for quantitative assay.
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