Department of Chemistry
Radiochemistry
University of Helsinki
In this work, students are introduced to utilisation of 210Pb/210Po equilibrium in environmental samples and determination of 210Po for obtaining 210Pb concentration. This method is widely applied in radiolead dating of environmental samples. The radioanalytical techniques that will be learned via this exercise are sample digestion by concentrated acids and alpha sample preparation by spontaneous electrodeposition of Po.
Radium (226Ra) present in the ground produces continuously noble gas radon, part of which escapes into the atmosphere. As Rn decays, solid radioactive daughter nuclides (see the figure below) are formed in the atmosphere and attached to aerosol particles. The most important of these is the relatively long-lived 210Pb (T1/2 = 22.3 a).
The radioactive decay chain from 226Ra to 206Pb.
The daughters of radon in atmosphere will return to the ground surface with rain and dust and they are taken up by plants. Transfer to animals and humans can take place through grazing and consumption of radionuclide-bearing plant or meat products. 210Pb is a beta emitter, as well as its daughter nuclide 210Bi (T1/2 = 5 d). Instead, the daughter nuclide of 210Bi, 210Po (T1/2 = 138 d) is an alpha emitter (Eα = 5.3 MeV) and it can be easily separated and measured. In fresh vegetation and peat samples there are both deposited 210Po and ingrown 210Po due to decay of 210Pb. In the samples stored for at least two years, the deposited 210Po has decayed completely and there is practically only 210Po formed from the decay of 210Pb. Thus, the activity concentration measured for 210Po corresponds also the activity concentration of 210Pb.
(If the activity of 210Po initially in the plant is to be measured, the determination should be done well before its decay and the result should be corrected with respect to both decay of 210Po and its in-growth from 210Pb. This, however, is possible only if the activity concentration of 210Pb is also measured.)
The aim of this work is to determine the concentration of 210Po in a plant-based environmental sample. The used sample material can be vegetation, peat or lichen, depending on the availability and interest. Due to volatility of polonium, it is not possible to use hot temperature digestion for destroying organic matter and instead, a digestion with HNO3 and HCl is carried out. The insoluble residue (e.g. silicates) is removed by filtration and excess acid is evaporated. The remaining solution is kept in contact with a silver disc for two hours. Polonium is a more noble metal than silver and is electrodeposited on the surface of a silver disc. Hydrazine or other suitable reducing reagent (e.g. ascorbic acid) is added to reduce trivalent iron to divalent. Otherwise, precipitation of trivalent iron with polonium on a silver disc causes blackening of silver, increases mass on the surface of the alpha counting sample and further worsens the quality of the measured alpha spectrum. To speed up the deposition the temperature is raised to +65–75 oC by using a water bath.
For determination of chemical yield, a known amount of 209Po tracer is added to the sample solution before the acid digestion. Alpha energy of 209Po is 4.88 MeV. When the activity measurement is carried out by alpha spectrometry, the peak areas of both polonium isotopes (209Po and 210Po) are determined. The activity concentration of 210Po in the sample is calculated then from the peak areas of 209Po and 210Po and the activity amount of added 209Po.
1. 1–5 g of dry sample material (peat, lichen, moss, or vegetation) is weighed and the exact mass of the sample is recorded.
2. 0.2–0.5 Bq of 209Po tracer solution (T1/2 = 103 a) is added to the sample.
3. Wet ashing can be performed either using a microwave oven or by heating on a hot plate, or in a Kjeldahl digestion apparatus. In case of using a microwave oven, smaller acid volumes can be used and the digestion time is shorter than with heating on a hot plate. However, the sample mass should not exceed ~1 gram in the microwave digestion, or then the larger sample should be divided into subsamples for digestion.
Instructions for the microwave oven option (3a) and the hot plate/Kjeldahl apparatus option (3b):
3a) The sample is transferred to a Teflon tube. 20 ml of aqua regia (3:1 conc. HCl - HNO3) and 0.2-0.5 Bq of 209Po tracer solution (T1/2 = 103 a) are added to the tube. Write down the activity concentration, reference date for the activity, and the volume of the tracer. The sample is left to stand for overnight. Next day, the sample is digested according to the instructions given by microwave oven manufacturer. After digestion, the sample is moved into a beaker and the Teflon tube is rinsed with 3 x 2 ml of conc. HCl, which is added to the beaker. For continuing sample digestion further, 15 ml of conc. HCl is added to the beaker and the sample is evaporated to 2–3 ml with gentle heating on a hot plate. The sample is left to cool down.
3b) Alternatively, the digestion can be carried out in a glass beaker of 250–500 ml, depending on the size of the original sample, which can be 1–5 grams, larger sample mass requiring larger beaker due to excessive oxidation reaction. A Kjeldahl's flask of similar volume can be also used instead of beakers, if Kjeldahl apparatus will be used instead of a hot plate. First, 50 ml of conc. HNO3 and 0.2–0.5 Bq of 209Po tracer solution are added to sample in the beaker. Heating is started carefully, because vigorous foaming may appear in the beginning. The digestion is continued until the HNO3 solution is evaporated to ~10 ml. This will take several hours. (If there still is unburned fat etc., HNO3 can be added and the digestion continued.) The beaker or flask is let to cool well and 20 ml of conc. HCl is added. Then HNO3 is evaporated from the sample, so that brown gases disappear. Next, the sample is evaporated to 2–3 ml and left to cool down.
4. 10 ml of 0.5 M HCl is added to the digested sample and possible remaining solid residue (silicates) is removed by filtration (for example, using glass fibre filter paper in a glass funnel). The sample vessel is washed with 2 x 5 ml of 0.5 M HCl, which is also filtered and combined with the sample solution filtrate.
5. 3 ml of saturated hydrazine monohydrochloride solution is added. The solution is heated close to the boiling point, let to cool and another 0.5 ml of hydrazine monohydrochloride solution and 1 ml of 10% ascorbic acid is added. Alternatively, instead of using hydrazine and ascorbic acid solutions with sample heating, 200–300 mg of solid ascorbic acid can be added to the sample with no heating, and then proceed to step 6. Other reductants can also be used for reducing iron, instead of toxic hydrazine monohydrochloride.
6. A silver disc is washed with alcohol or toluene to remove fats. Mark the sample name to the bottom side (the side which will not be in contact with sample solution) of the disc with a permanent marker. An example of deposition vessel made of Teflon is presented in a figure below.
Install the deposition vessel so that the silver disc is attached in the bottom, a washed side up. The deposition vessel should be checked for leakages by filling it first with water, before the actual sample is poured in the vessel. Then the sample solution is poured into the empty deposition vessel, the beaker is washed with small amount of mQ-water and the rinsing solution is poured to the deposition vessel as well. mQ-water is added to the deposition vessel until a total volume of 50 ml is reached. The sample is deposited at 65–75 OC (water bath) for 2 hours using a mechanical stirrer.
7. The solution is removed from the deposition vessel. Wash the vessel once with a small amount of 0.5 M HCl. Remove the silver disc from deposition vessel and rinse well with water and ethyl alcohol. When the disc is dry, the radioactivity of 210Po is determined from the disc by alpha spectrometry.
The Lab Supervisor should study the MSDSs of the chemicals used in the work and search all supplies and reagents in advance. The volume calibration of the autopipette should be checked, if there has been a long time since the last check. It is good to get familiar with the microwave oven and alpha spectrometer before the exercise and ensure availability of the instruments.
209Po tracer
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This project has received funding from the Euratom research and training programme 2019–2020 under grant agreement No. 945301.