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Application of a liquid scintillation counter to the measurement of tracing radioactivity in experiments on suspended matter uptake in aquatic environments

El Mrabet, Rachid; Manjón Collado, Guillermo; Abril Hernández, José María; García-Tenorio García-Balmaseda, Rafael

Abstract

The experiments on the study of the kinetic transfer coefficients of conservative and non-conservative radionuclides, in aquatic environments, need to determine radionuclide activity in large number of samples. Different radioactivity measurement techniques can be selected for analyses, but the liquid scintillation technique is preferred due to its easy sample treatment and its low time consumption. Samples are initially traced with a known activity of a selected radionuclide (2 3 9Pu, M IAm or "Tc). The transference of radionuclides, from the water to the suspended matter, is studied through the determination of the residual activity in aliquots of water sample, which are successively collected with time. In this work, we present the experimental procedures used for the 2 3 9Pu, 2 4 1Am and "Tc activity measurement by liquid scintillation counting, using a Wallac Quantulus 1 2 2 0 spectrometer. Results of the application of this technique to traced water samples are also shown in this study.

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Radiop o ec ion - Collogues, olume 37, CI (2002) Cl-1015 Applica ion o a liquid scin illa ion coun e o he measu emen o acing adioac i i y in expe imen s on suspended ma e up ake in aqua ic en i onmen s R. El-M abe , G. Manjon1, J.M. Ab il2 and R. Ga cia-Teno io1 Depa amen o de Física A ómica, Molecula y Nuclea , Facul ad de Física, Uni e si y o Se ille, Apdo. 41060 Se illa, Spain 1 Depa amen o de Física 2, Uni e si y o Se ille, ETSA, A da. Reina Me cedes s/n, 41012 Se illa, Spain 2 Depa amen o de Física Aplicada 1, Uni e si y o Se ille, EUITA, Ca e e a de U e a km 1, 41013 Se illa, Spain Abs ac , The expe imen s on he s udy o he kine ic ans e coe icien s o conse a i e and non-conse a i e adionuclides, in aqua ic en i onmen s, need o de e mine adionuclide ac i i y in la ge numbe o samples. Di e en adioac i i y measu emen echniques can be selec ed o analyses, bu he liquid scin illa ion echnique is p e e ed due o i s easy sample ea men and i s low ime consump ion. Samples a e ini ially aced wi h a known ac i i y o a selec ed adionuclide (239Pu, MIAm o "Tc). The ans e ence o adionuclides, om he wa e o he suspended ma e , is s udied h ough he de e mina ion o he esidual ac i i y in aliquo s o wa e sample, which a e successi ely collec ed wi h ime. In his wo k, we p esen he expe imen al p ocedu es used o he 239Pu, 241Am and "Tc ac i i y measu emen by liquid scin illa ion coun ing, using a Wallac Quan ulus 1220 spec ome e . Resul s o he applica ion o his echnique o aced wa e samples a e also shown in his s udy. 1. INTRODUCTION The so p ion and elease kine ics o 239Pu, 241 Am and "Tc by eshwa e suspended pa icles we e in es iga ed o be e iden i y he biogeochemical p ocesses in ol ed and o unde es and he beha iou o hese elemen s in aqua ic en i onmen s. Time se ies da a can be ob ained om labo a o y s udies and can be analysed o s udy he ans e ence o adionuclides ac i i y om he wa e o he suspended ma e . T acing expe imen s we e pe o med du ing a la ge ime using na u al aqueous suspensions om h ee aqua ic sys ems (Ge gal ese oi , he Guadalqui i i e and he es ua y o he Tin o i e ). Scien i ic li e a u e lis s many examples o expe imen al s udies on up ake kine ics o dissol ed adionuclides by suspended loads [1, 2]. In his wo k we ca y ou a se ies o acing expe imen s wi h 239Pu, 241Am and "Tc by using en i onmen al samples o un il e ed wa e s om h ee aqua ic sys ems in he Sou h o Spain. The expe imen al p ocedu e ensu es he p ese a ion o en i onmen al condi ions. As he expe imen al me hod equi es he de e mina ion o Pu, Am and Tc ac i i ies in a la ge numbe o samples, i is impo an o selec a measu emen echnique wi h low ime consump ion. Recen ly, liquid scin illa ion coun ing has been applied o Pu, Am and Tc-iso opes. In wo ks epo ed by [3], 239+240pu we e simul aneously measu ed using a liquid scin illa ion coun e PERALS™ and wo ex ac i e scin illa o s. Liquid scin illa ion echnique is p e e ed because he edious sample ea men equi ed, e.g. o alpha spec ome y, is no necessa y. The poo esolu ion o his echnique (abou 300 keV) will be no ele an in ou measu emen s because a single alpha emi e , adio ace , will be p esen in ou samples. This echnique allows us o in es iga e newe and in e es ing aspec s o he kine ic o he elec oly ic eac ions o Pu, Am and Tc in esh wa e ecosys ems. I MATERIAL AND METHODS 21 Sampling Wa e samples we e collec ed om h ee di e en aqua ic scena ios om he Sou h o Spain. The i s s a ion was loca ed he Ge gal ese oi (NW om Se ille). The second sample was collec ed in he Guadalqui i i e , nea he own o Se ille. Wa e s we e da k g ey colou ed by he e luen s om ac o ies and u ban sewage in he su oundings. Finally a hi d sample was collec ed in he Tin o es ua y, dose o he A lan ic Ocean, du ing he low ide. A icle published by EDP Sciences and a ailable a h p://www. adiop o ec ion.o g o h p://dx.doi.o g/10.1051/ adiop o/2002118 Cl-1016 RADIOPROTECTION - COLLOQUES A each sample si e, we illed ou 25 1 plas ic bo les. Tempe a u e, pH and elec ical conduc i i y we e measu ed jus a e collec ion. Samples we e hen ca ied o ou labo a o y and s o ed in da k du ing ew hou s. The acing expe imen s gene ally begun a he ollowing mo ning. We used a nephelome e o measu e he suspended ma e con en . To con e NTU in o mg/1 we weigh ed he d y ma e ob ained a e il e ing 50 1 o wa e by using a 0.45 um NUCLEOPORE il e . This calib a ion was epea ed o each new en i onmen . In Table 1 we show he empe a u e, pH, he elec ical conduc i i y, and he suspended ma e con en o collec ed samples, co esponding wi h na u al condi ions p e ailing du ing he sampling. Table 1. Tempe a u e, pH, elec ical conduc i i y and suspended ma e con en in wa e samples measu ed jus a e collec ion. Da a can be conside ed as en i onmen al condi ions. En i onmen Tempe a u e PH Conduc i i y Suspended ma e (°C) (mS) (mg/1) Ge gal ese oi 27.1 8.35 0.46 7.37 Guadalqui i i e 20.4 7.84 1.37 12.6 T in o es ua y 19.4 7.86 66.25 7.62 He ea e he solid ac ion will be conside ed ha o med by suspended pa icles wi h a diame e la ge han 0.45 um. The dissol ed (mo e p ope ly he il e ed) ac ion is o med by he wa e , dissol ed elemen s and pa icles wi h smalle sizes. This is a p ac ical assump ion, since in mos o he expe imen al s udies his po e size is used o sepa a e bo h ac ions. 2.2 Expe imen al p ocedu e The objec i e o his wo k was o e alua e he up ake o 239Pu,241 Am and "Tc by suspended ma e in en i onmen al esh wa e s. In each expe ience, a ypical olume o 1.0 1 o wa e was ans e ed in o a glass beake . The e, he sample was spiked wi h 239Pu, 241 Am o "Tc and con inuously s i ed in o a oid any decan a ion o he suspended ma e . We ollowed he ime e olu ion o he ac i i y concen a ion in he dissol ed phase by aking aliquo s a di e en imes a e spiking. A ypical olume o 45 ml was selec ed o e e y aliquo . Suspended ma e was emo ed by cen i uga ion (20 minu es a 4000 pm). Then, 35 ml o supe na an we e ans e ed in o aplas ic con aine and acidula ed wi h 1ml o HN03 o a oid loses o plu oniumby adso p ion on o he con aine walls. Finally, 5 ml o acidula ed sample was ans e ed in o a plas ic ial and mixed wi h 15 ml o liquid scin illa ion cock ail Pha macia Op iphase 3. Nephelome ic measu emen s p o ed ha he u bidi y o he supe na an wa e s a e cen i uga ion we e simila o he measu ed ones in he il a ed ac ion. Consequen ly, cen i uga ion is an e icien p ocess o sepa a e almos he same ac ion ha we could ob ain by il a ion. Fil a ion canno be used as al e na i e echnique o sepa a e bo h ac ions om each aliquo e, since app oxima ely some 10% in he case o he Pu was e ained by he il e i sel , as p o ed by il a ing dis illa e wa e spiked wi h Pi Al hough cen i uga ion is ou bes choice, i is no a pe ec p ocess, and in some samples we go an incomple e sepa a ion, p o oking some o e -es ima ions o he speci ic ac i i y in he dissol ed ( il e ed) phase. 2.3 G anulome ic analysis and mine al composi ion s udy I is known [4, 5] ha he kine ic ans e coe icien o di ec so p ion depends on he o al a ail su ace o pa icles pe uni olume o solu ion, and on he concen a ion o ac i e si es in he sui ECORAD 2001 Cl-1017 laye o solids. This las depends on he mine al composi ion, ee edges, po es, coa ings, e c. Thus, i is necessa y o handle he pa icle size spec a and he mine al composi ion o na u al occu ing suspended loads o compa e esul s om di e en en i onmen s and o ix he condi ions o applicabili y o he de i ed coe icien s. A g anulome ic analysis o all he samples was ca ied ou by using a Ma e Size ins umen wi h 100 size bands, om 0.01 o 1000 um. A Scanning elec on mic oscope (SEM) was used o s udy he mo phology o na u al pa icles om all he samples. The SEM mic og aph o he ou samples e ealed ha he mos common shape is he sphe ical one. We can app ecia e some agg ega ion o pa icles owing o he p epa a ion p ocedu e. Sal - c ys als a e p een in mos o he samples. Finally, he mine al composi ion was de e mined by X- ay di ac ion (XRD). Some esul s a e summa ised in Table 2. Table 2.- Resul s om g anulome ic and miné alogie analysis. Diame e in (im, co esponds o he mos equen diame e , and d)2 is he diame e co esponding o pa icles wi h he highes pe cen age o olume. The speci ic su ace a ea (S.S.A.) is compu ed assuming a densi y o 2.10 g cm-3 o all he solids. En i onmen Diame e dp. Diame e <b2 S.S.A. Main mine alogical (u n) (um) (m2/g) composi ion Ge gal ese oi 0.30 19 0.28 CaC03 Calci e, Musco i e Guadalqui i i e 0.22 15 1.63 CaC03 Calci e T in o es ua y 0.18 28 0.78 CaS042H20, Bassani e 2.4 Liquid scin illa ion coun e A liquid scin illa ion spec ome e Wallac Quan ulus 1220™ was used o 239Pu, 241 Am and "Tc ac i i y measu emen s. The low backg ound o he de ec o allows he measu emen o low-le el ac i i ies. Mo eo e , alpha and be a ac i i y om he same sample can be measu ed simul aneous and sepa a ely (alpha and be a spec a) by using i s pulse shape analyse (PSA) [6]. The PSA was op imised by measu ing a 239Pu and 241 Am s anda d samples, unde he ypical measu emen condi ions, a di e en alues o he PSA h eshold le el. Resul s a e shown in Fig.l, whe e alpha in e e ence is plo ed e sus PSA le el. Taking in o accoun ha alpha in e e ence is de ined as he ac ion o alpha coun s measu ed in he be a spec um, a A PSA le el o 55 was selec ed in ou wo king condi ions, because using highe alues he alpha in e e ence canno be conside ed negligible and he coun ing e iciency dec eases. In he "Tc ac i i y measu emen s, i is no necessa y o use he PSA. PSA " e 1.- Op imisa ion o he PSA o he Wallac Quan ulus 1220™. Bes esul s do Pu and Am co esponds o PSA = 55 Cl-1018 RADIOPROTECTION - COLLOQUES When PSA is selec ed on, backg ound coun s a e acqui ed in he be a spec um, because 40K (a be a emi e ) o ial walls is he main con ibu o o backg ound o de ec o . We ha e o no e ha alpha / be a sepa a ion is no o ally e icien , and a pa o he be a emissions can be coun ed in he alpha spec um, This ac ion is known as he be a in e e ence and can be conside ed as he main con ibu ion o he alpha backg ound. Ob iously, his be a in e e ence dec eases when inc easing he PSA alue. Fo his eason he PSA alue was selec ed as he maximum alue a which he alpha in e e ence is s ill negligible. On he o he hand, we also s udied he dependence o he alpha backg ound wi h he olume o he sample. Always he dis illed wa e /scin illa o olume a io was 1:1, and he sample olume anged om 8 up o 20 ml. When he op imum PSA le el was selec ed, he alpha backg ound was simila in all cases. Fo ha eason, he sample accep ance o he scin illa o was conside ed as he main pa ame e o selec ing he sample olume. Fo example, he scin illa o used, he Wallac Op iphase Hisa e3, has a sample accep ance o 4 ml o 2M F£N03 in 10 ml o scin illa o . The samples ob ained in ou expe imen s can be conside ed as a 0.4M HN03 solu ion, bu ma e ial o iginally dissol ed in he en i onmen al wa e could be p esen also in he sample o be measu ed and could educe he sample accep ance o scin illa o . This is he case o he Guadalqui i sample, whe e i is possible o app ecia e he p esence o colloids. Fo his eason, a olume o 5 ml was selec ed o he aqueous phase, which was mixed wi h 15 ml o scin illa o . In hese condi ions, alpha backg ound and alpha e iciency we e de e mined in he di e en collec ed wa e samples. Alpha e iciency was de e mined spiking he 5 ml o he wa e samples wi h known amoun s o 239Pu, 241 Am o "Tc. Resul s a e lis ed in Table 3 o Pu measu emen s. Alpha coun ing e iciency anged om 0.67 up o 0.89 being no uni o m, p obably due o a di e en chemical quenching o he sample. Backg ound le el anged om 0.4 cpm in he ese oi wa e s, o 0.8 cpm o he Guadalqui i wa e . A highe le el o 2.4 cpm was measu ed in wa e collec ed om he Tin o es ua y. This esul can be a ibu ed o he p esence o na u al alpha emi e s in he sample [7]. Table 3. Coun ing cha ac e is ics o a Wallac Quan ulus 1220™ in he case o "'Pu, using wa e samples collec ed in di e en en i onmen al scena ios. LID is de de ec ion limi , and MDA is he minimum de ec able ac i i y; coun ing ime was 600 min in all he cases. En i onmen E iciency Backg ound MDA LID (cpm) (Bq li e 1) (cpm) Ge gal 0.67 ± 0.01 0.66 ± 0.03 0.23 0.047 Guadalqui i 0.89 ± 0.03 0.79 + 0.04 0.19 0.051 Tin o 0.67 ± 0.02 2.36 ± 0.06 0.44 0.089 3. RESULTS AND DISCUSSION In igu es 2, 3, 4, 5 and 6 we show he ime e olu ion o 239Pu, 241 Am and "Tc ac i i ies in he dissol ed phase co esponding o he ou se ies o expe imen s. Measu ed alues a e ep esen ed wi h e o ba s. F om Fig. 2, 3, 4 and 5, in loga i hmic scale, h ee di e en egions cha ac e ised by di e en slopes can be dis inguished: i s egion co esponds o a as eac ion, las ing o ew minu es, du ing which ime up o 30% o dissol ed Pu o Am is ans e ed on o suspended solids. This co esponds o a as physical-adso p ion eac ion (Pu o Am is ixed by coulombian o ces on o he ex e nal ee su ace o pa icles); in second egion, o he eac ion go e ns he Pu o Am up ake du ing 10-20 hou s ime, ans e ing up o 30% o emaining Pu in dissol ed o m. This eac ion co esponds o physical adso p ion on o he inne su ace o po es and ee-edges, and o he o ma ion o e e sible unions o a di e en na u e and/o s eng h. In hi d egion, he up ake (up o 50% o he emaining Pu o Am in solu ion) con inues du ing se e al days ( he du a ion o he expe imen s was oo sho o allow a conclusion conce ning he inal cou se o he eac ion). This eac ion may co espond o a slowe p ocess in which p e iously adso bed Pu o Am is ans e ed in o he inne ma ix o he pa icles o o ms o he non- e e sible unions. ECORAD 2001 CT-1019 2.5 2 1.5 1 0.5 0 2.4 2.2 2 1.8 1.6 1.4 1.2 1 0.8 0.6 2.4 2.2 2 1.8 1.6 1.4 1.2 1 0.8 0.6 200 Fig.2 Ri e ~—• * I • 0 5 10 15 20 25 30 Time (hou s) 35 40 45 50 ; Fig.3 Es ua y -•—« I J I 0 5 10 15 20 25 30 Time (hou s) 35 40 45 50 • Fig. 4 Rese oi . I I 10 15 20 25 30 Time (hou s) 35 40 45 50 20 80 100 40 60 j. Time (hou s) '?'*'..'3'4.' Time e olu ion o 239-Pu and 241 -Am ac i i ies (in cpm and mBq) in he dissol ed phase co esponding o e ou senes o expe imen s on 239-Pu and 241-Am up ake (non-conse a i e adio ace s) in na u al aqueous suspensions. Cl-1020 RADIOPROTECTION - COLLOQUES Fig. 6 Ri e ¡ i l i I l 0 50 100 150 200 250 Time (hou s) Fig. 6: Time e olu ion o 99-Tc ac i i ies (in mBq) in he dissol ed phase co esponding o he se ie o expe imen s on conse a i e adio ace (99-Tc) up ake in na u al aqueous suspensions o un il e ed wa e s om Guadalqui i i e . F om Fig.6, he 99-Tc is conside ed as conse a i e adionuclide, he ac ion o he 99-Tc abso bed by he suspended ma e is negligible. 4. CONCLUSIONS In his wo k we applied a use ul expe imen al p ocedu e o s udy he up ake o Pu, Am and Tc by na u al aqueous suspensions, based on he use o liquid scin illa ion echnique. Acknowledgemen s This wo k has been pa ially suppo ed by I+D con ac wi h ENRESA, Spain. Re e ences 1. 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