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Distribution Coefficients of Polonium Between 0.75 M HDEHP in Cyclo- Hexane and Aqueous Hydrochloric and Nitric Acids Guogang Jia* and Giancarlo Torri

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Distribution Coefficients of Polonium Between 0.75 M HDEHP in Cyclo- Hexane and Aqueous Hydrochloric and Nitric Acids Guogang Jia* and Giancarlo Torri 18 The Open Inorganic Chemistry Journal, 2008, 2, 18-21 Distribution Coefficients of Polonium Between 0.75 M HDEHP in Cyclo- hexane and Aqueous Hydrochloric and Nitric Acids Guogang Jia* and Giancarlo Torri Agency for Environmental Protection and for Technical Services, Via V. Brancati 48, 00144 Roma, Italy Abstract: The distribution coefficients (D) of polonium between 0.75 M di(2-ethyhexyl)phosphoric acid (HDEHP) in cy- clohexane and aqueous hydrochloric and nitric acids have been studied. Results indicate that: (1) D values are ranged from 32.7 to 0.00048 when the HCl acidities vary from 0.10 to 10.0 M, showing that polonium can well be extracted by 0.75 M HDEHP in cyclohexane if the aqueous HCl acidities are 0.050 M and it will not be extracted if 0.10 M HCl; (2) D values are ranged from 47.1 to 0.0117 when the HNO3 acidities vary from 0.10 to 10.0 M, showing that polonium can be extractable by 0.75 M HDEHP in cyclohexane and in a wide range acidity of 4 M HNO3. The different extraction behaviours of polonium in 0.75 M HDEHP in cyclohexane and different acidities of HCl and HNO3 were found. The find- ings will be very helpful to improve the methods involving polonium decontamination for determination and separation of americium, curium as well as other radioelements in environmental soil, water and biological samples. Keywords: Polonium, HDEHP, distribution coefficients. 1. INTRODUCTION on its oxidation state. Therefore, question is raised: which oxidation state is responsible for major polonium volatility, The element polonium (210Po) was discovered by Marie valences of +2, +4, and probably +6? Curie as the first element separated from pitchblende, and named after her home country, Poland [1, 2]. It has 25 As the second evidence, there is a lack of information known radioactive isotopes with mass numbers of 192–218, about the chemical extraction behaviours of polonium with of which only the 208Po, 209Po and 210Po have half-lives many popular used organic extractants [4], such as: Tri- longer than days. Of these three, 208Po and 209Po, being arti- octyl-phosphine oxide (TOPO), di(2-ethyhexyl)phosphoric ficial isotopes are often be used as tracers in the analytical acid (HDEHP), tri-n-octylamine (TNOA), and tri-n-butyl procedures for the determination of natural polonium iso- phosphate (TBP) etc. Uranium and transuranium nuclides, tope. However, it is 210Po, which lends itself well to indus- such as 238U, 234U, 235U, 239+240Pu, 238Pu, 241Am etc, represent trial applications, particularly in static elimination and con- the highly radiotoxic and/or chemical toxic, long-lived and trol, in neutron generation, and also as a heat source for sat- worldwidely dispersed -emitting radionuclides in the envi- ellite power supplies etc. Therefore, 210Po is of the most in- ronment [5, 6]. The activity concentration studies of these terested polonium isotope from health physics and environ- radionuclides in the environmental matrices can provide ba- mental impact viewpoints due to its radiation exposure. sic information on the contamination levels, sources, distri- butions, inventory estimation and ecological processes of the Not like many other elements, studies on the physical radionuclides in the environment. Due to the complexity of properties and chemical behaviours of polonium is relatively the matrices and the very low level of radioactivity in it, for difficult and less extent due to the facts that (1) there is no most common determination techniques extensive sample any stable isotope, and (2) a measurable mass of polonium preparation, separation and purification procedures are re- compounds always contains very high specific radioactivity. quired to achieve accurate results [6-9]. TOPO, HDEHP, As the first evidence, it has long been said that polonium TNOA and TBP etc are very popularly used as extractants to is volatile at high temperature (< 190 °C). But which valence separate actinides from the interfering elements in environ- or compound of polonium is volatile is not well known. mental samples. Interference of 210Po was observed and is Some researchers [3] studied the volatility of polonium in also very critical in the determination of actinides in envi- soil by fusion method (0.1 g soil sample containing 210Po, ronmental samples due to the widespread occurrence of 210Po mixed well with 2.0 g of Na2CO3 and Na2O2, and fused at as a natural radionuclide. For instance: (1) For the determi- 600 °C for different time periods of 10 - 120 min). The ob- nation of uranium isotope composition in lichen and soil 232 tained average volatility of polonium was 13.9 ± 3.2%, and samples [10, 11], U [E=5.2635 MeV (31%) and 5.3203 210 the effect of the fusion time at 600 °C seems not significant. MeV (69%)], which has a similar E to Po [E=5.304 It means that most of the polonium remains not volatile. The MeV (100%)], is often used as a yield tracer. Due to the less observation of many experiments during polonium determi- effective separation of uranium from 210Po in the Microth- nation for some biological samples concluded that oxidation- ene-TOPO chromatographic column under the experimental reduction process can cause a significant lost of polonium. It conditions and the limited resolution of the -spectrometry means that the volatility of polonium signifi-cantly depends (the best FWHM is about 20-30 keV), trace amounts of 210Po can remain in the uranium fraction in the prepared disks of the samples. Owing to the interference of 210Po, yield correc- *Address correspondence to this author at the Agency for Environmental 232 Protection and for Technical Services, Via V. Brancati 48, 00144 Roma, tion from the U counts can lead to inaccurate results and Italy; E-mail: [email protected] can make the uranium concentrations of the samples much 1874-0987/08 2008 Bentham Science Publishers Ltd. Distribution Coefficients of Polonium Between 0.75 M HDEHP The Open Inorganic Chemistry Journal, 2008, Volume 2 19 lower than the real values [11]. (2) A similar interference of ml with benzene and washed with 4.5 ml of distilled water to 210Po can also happen in americium analyses where Microth- lower the acidity of the solution. Finally, the polonium in the ene-HDEHP chromatographic column was used, as the peaks organic phase was back-extracted twice with same volume of 210 243 of Po and Am (E=5.2766 MeV) as an americium tracer 0.025 M (NH4)2C2O4 solution. All the washing and back- are in the nearly same energy region and can not be resolved extracting solutions were combined in another 150 ml by -spectrometry [8]. (3) If compared with the 210Po con- beaker. In order to destroy the residue organic matters, the centration, plutonium nuclides only exist in extra-trace extracting and back-extracting solutions were evaporated to amount in environmental samples. The interference of 210Po dryness. 1 ml of concentrated HCl was added and the residue to the plutonium determinations by Microthene-TNOA was boiled at 100 °C for some minutes with addition some chromatographic column can also be possible [6], because drops of 30% H2O2. After cooling, the pH of the solution the peak of 210Po appears just in the region between the dou- was adjusted to 1.5 with 1:5 (v/v) ammonia. The solution 239 240 blet peak of Pu [E=5.155 MeV (73.2%)], Pu was diluted to 50 ml, heated and stirred on a hot-plate mag- 238 [E=5.1681 MeV (73.5%)] and the peak of Pu [E=5.465 netic stirrer. A Perspex holder with a silver disk was placed MeV (28.3%) and 5.4992 MeV (71.6%)]. Good resolution on the beaker and the silver disk was immersed into the solu- sources for -spectrometry measurement are needed in order tion. Any air bubbles trapped beneath the disk were removed to reduce the interference of 210Po for plutonium nuclide de- by manipulation of the stirrer bar. The polonium deposition termination as less as possible. was continued for 5-6 h at 85-90 °C, then the disk was re- moved, washed with distilled water and acetone, dried and Therefore, in order to improve the analytical techniques assayed by -spectrometry. For detailed analytical proce- for actinides and some other interested elements it is cer- dure, please refer to literature 14 . tainly necessary and important to study the extraction behav- [ ] iours of polonium in different organic phases (toluene, cy- 2.3. Distribution Coefficients clohexane, xylene etc) of TOPO, HDEHP, TNOA and TBP The distribution coefficient (D) was calculated as fol- etc, and aqueous phases (HCl, HNO3, H2SO4 etc). For this purpose, the distribution coefficients of polonium between lows: 5% TOPO in toluene and aqueous hydrochloric and nitric AoVw acids have been studied previously [12]. The objective of D = this paper is to study the distribution coefficients of polo- AwVo 209 nium between 0.75 M HDEHP in cyclohexane and aqueous Where, Ao and Aw are the Po activities in the organic hydrochloric and nitric acids in detail. These data are needed and aquatic solutions; Vo and Vw are the volumes of the or- to develop more accurate method for determination of am- ganic and aquatic solutions. ericium and curium isotopes by -spectrometry, and are also helpful to improve the methods involving polonium separa- 3. RESULTS AND DISCUSSION tion for other element determination. It was reported that some polonium compounds are vola- 2. MATERIALS AND METHOD tile, possibly in its pure and chloride forms [2]. Therefore, the studies on the polonium extraction by HDEHP in cyclo- 2.1. Apparatus and Reagents hexane and acidified aqueous phases are not easily achiev- able due to its volatility.
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