Column and batch experiments were performed to study the migration behaviour of Ba and Sr in colemanite matrix. 133Ba. 90Sr and 3H were used as tracers. The retardation factors and the distribution ratios of Ba and Sr in column experiments were found to be smaller than those obtained in batch experiments. Sorption Ra values of Ba were higher than those of Sr determined by both techniques. Sorption energies calculated from batch experiments are in good agreement with the literature values

Erten H.N.

Göktürk H.

Hatipoǧlu, S.

Radiochimica Acta

Column and batch experiments were performed to study the migration behaviour of Ba and Sr in colemanite matrix. Ba-133, Sr-90 and H-3 were used as tracers. The retardation factors and the distribution ratios of Ba and Sr in column experiments were found to be smaller than those obtained in batch experiments. Sorption R(d) values of Ba were higher than those of Sr determined by both techniques. Sorption energies calculated from batch experiments are in good agreement with the literature values

Hatipoglu, S

Gokturk, H

Erten, HN

OpenMETU (Middle East Technical University)

Migration behaviour of barium and strontium through colemanite

Bilkent University Institutional Repository

Radiochimica Acta 72, 105-108 (1996) © R. Oldenbourg Verlag, München 1996 Migration Behaviour of Barium and Strontium through Colemanite By S. Hatipoglu1, H. Göktürk1 and Η. N. Erten2 1 Department of Chemistry, Middle East Technical University, Ankara, Türkey 2 Department of Chemistry, Bilkent University, Ankara, 1\irkey (Received March 1, 1995; revised July 17, 1995) Colemanite / Sorption / Distribution ratios / Batch method / Column method Summary Column and batch experiments were performed to study the mi-gration behaviour of Ba and Sr in colemanite matrix. ' "Ba, *°Sr and 3H were used as tracers. The retardation factors and the distribution ratios of Ba and Sr in column experiments were found to be smaller than those obtained in batch experiments. Sorption Rd values of Ba were higher than those of Sr deter-mined by both techniques. Sorption energies calculated from batch experiments are in good agreement with the literature values. Introduction The management and disposal of nuclear waste is a burden accepted along with the benefits from the use of radioactive materials. Among a number of disposal options "underground disposal" of radioactive waste seems to be the most realistic way of providing the necessary protection for humans and the environment. Colemanite (Ca2B601t · 5 H20), with its highly vitrous crystalline characteristics is a potential candidate for geological matrices considered [1], provided that it significantly sorbs the radionuclides important in waste considerations. Information on the sorption characteristics of colemanite can be obtained via batch and column experiments. In batch experiments, the distribution ratio Rd is obtained [2], In column experiments, migration of a radionuclide is characterized by a retardation factor, Rf, which describes the average radionuclide velocity (Vr) - migration rate — in the matrix with respect to the average water velocity (Vw) in the same medium. Rd and Rf are related by Ä ^ l + Ä , ^ (2) Vv where gs = Density of the solid matrix Ac = Cross sectional area of the column W = Volumetric flow rate of water Batch and column experiments provide informa-tion on the type of the sorption process, sorption ener-gies, the kinetic order of the reactions and other pa-rameters affecting retardation. Among the several fission products discharged into the environment, ^Sr is important because of its high fission yield and long half-life. Another important safety hazard in radioactive waste considerations is Ra. Β a, a member of group IIA elements was chosen along with Sr as a suitable homolog of Ra. In this work the migration behaviour of Β a and Sr through colemanite has been extensively studied. Experimental The radionuclides l33Ba, 90Sr and 3H obtained from the Radiochemical Center Amersham, were used as radio-tracers. Colemanite was obtained from a deposit in the Emet-Kütahya region of Turkey. Fourier transform in-frared and X-ray diffraction spectrometry, differential thermal gravimetric analysis, particle size fractionation and surface area measurements were carried out to elucidate the structure and properties of colemanite. All solutions were prepared using synthetic groundwater with similar composition as the ground-waters found in Kütahya region (Table 1). In column experiments, the retardation of radio-nuclides were determined by measuring the effluent activities collected from the bottom of a mini-column system (0.32 cm in diameter and length of 28.7 cm). The column was packed with a weighed amount of colemanite having 90 μηι average particle size. After four days of pre-equilibration with groundwater, a spike of radionuclide solution (0.3 ml, 5.5 · 104 Bq [Ba2+] = 1.6 X 10~8 mmol/ml, [Sr2*] = 5.7 X10"8 mmol/ml) was introduced from the top by injection. Then migration through colemanite was initiated with a continuous water flow through the column and frac-tions of effluent were collected by a fractional collec-tor at certain time intervals. The activities of the solu-tions were determined by y-rays spectrometry (,33Ba), Table 1. Composition of synthetic groundwater used in the sorp-tion experiments Ion concentration (meq/L) PH N a + + K + Ca2+ Mg2+ CO!" NO-r c r s o r 0.89 4.70 3.15 0.17 3.14 0.84 0.18 7.80 Brought to you by | Hacettepe UeniversitesiAuthenticatedDownload Date | 11/27/18 10:26 PM106 S. Hatipoglu, Η. Göktürk and Η. Ν. Erten 0.06 100 · ο ro 73 Φ 4—· φ φ > Ε Ο ξ 0.09 > > ο (0 "D Φ Ν 0.15 0.12 3 0 .06 -0.03 0.00 0 40 80 120 160 200 50 100 150 200 250 Fig. 1. A typical breakthrough curve of Ba2+-colemanite interac-tions. A: Normalized activity versus time. Ο: Cumulative eluted activity, %. liquid scintillation counting (3H) or /^-counting ('"Sr). Experiments were done using columns of varying length. The activities of the effluents collected were normalized as fraction of the total initial activity. The breakthrough curve of each column experi-ment was obtained by plotting normalized activities per ml of effluent as a function of time. The travelling times obtained from such curves were used to calcu-late the transport velocity of the radionuclide in that matrix. The average water velocity in the same matrix was obtained by performing similar experiments with triti-ated water. Cumulative eluted Τ activities were close to 100% in all cases, indicating no significant ex-change of T. Using the water velocity one can determine both the retardation factor, Rf, (Eq. (1)) and the distribution ratios, Rd, (Eq. (2)) in such column experiments. In the batch technique, weighed amount of solid samples were kept in contact with known volumes of radioactive solutions of Ba and Sr for certain times. The initial concentrations ranged from 10"8 mol · l"1 to 10"3 mol · 1"'. After separation of the two phases by centrifugation and filtration, the change of the ad-sorbate concentration in the aqueous phase was meas-ured and the distribution ratio was calculated [2]. Results and discussion A typical experimental breakthrough curve for Ba mi-gration in colemanite is shown in Fig. 1. The tailing observed indicates partially reversible adsorption [3]. The variation of the breakthrough curve with column Fig. 2. Breakthrough curve of Ba2+-colemanite interactions at various column depths. Δ : 3.8 cm. O: 8.0 cm. + : 13.5 cm. length is shown in Fig. 2. The percent cumulative elut-ed activities are found to be 80 percent, 60 percent and 40 percent for 3.5 cm, 8.0 and 13.5 cm columns, respectively. Similar behaviour was observed in Sr-colemanite interactions. The velocities of Ba and Sr migration, and tritiated water were obtained by dividing the matrix depths with retention times in each column experiment. The retardation factors, Rf, were calculated accordingly. The results obtained are given in Table 2. Assuming that a column system represents a radio-active leakage from a repository, the breakthrough curves obtained during leaching processes are treated in two different regions reflecting steady state (after the maximum activity is reached) and nonsteady state (before the maximum activity is reached) cases. The steady state equations are obtained using plots of Af versus time curves. Here, Af is the fraction of activity leached per unit time per unit volume. Then, the log ( — d A / d f ) versus log Af (Fig. 3) plots were used to calculate the leaching rate constant, k, and the leaching dAf rate order, n. Using these values = kA" type dt equations were obtained for Ba and Sr migration in colemanite (Table 2). Using such empirical equations, the fate of Ba, and Sr ions moving through colemanite matrix, under flowing steady state conditions, can be predicted. In the non-steady state region, assuming that Ba ions leach through colemanite according to first order kinetics and using the percent cumulative eluted ac-tivity information in the non-steady state region, after appropriate mathematical treatment, an empirical equation can be proposed for Β a ion migration as fol-lows : Brought to you by | Hacettepe UeniversitesiAuthenticatedDownload Date | 11/27/18 10:26 PMMigration Behaviour of Barium and Strontium through Colemanite 107 1000 5 £ 100 10"7 10~6 10"5 10~4 10"3 10'2 10_1 10° Log A, Fig. 3. Plots of l og (—dA/d t ) versus log Af for steady state flow of Ba2+ through colemanite matrix. Δ : Matrix depth 3.5 cm. A: Matrix depth 8.0 cm. O: Matrix depth 13.5 cm. χ (mmol/g) Fig. 4. Change of Rd values as a function of cation loading in colemanite. Δ : Ba2+. A: Sr2". Table 2. Results of column experiments for Ba2+ and Sr2+ inter-actions Rf R„ (ml/g) -dA/dt{\) (C.E.A.%)ss(2) Ba2+ 24±4 19+3 2.1 A;·4 (2.6(W/VJ-0.4)i 1 -exp (—0.05 (W/Vm/1)) Sr2+ 7 ± 2 5±2 10 A}2 -(1) Change of normalized activity flux of outflowing solution (2) % cumulative eluted activity at steady state for 0 < t < 22 (VJW). (C.E.A.%) [2.6 (W/Vm) - 0.4] t 1 — exp(—0.05 (W/Vm) t) where (C.E.A.%)SS: Percent cumulative eluted activity at steady state W/Vm: Volumetric Flowrate/Matrix Volume. (Vm This equation is valid within 0 < t < 22 I limits (the non-steady state region) and may be useful in predicting the maximum leachable activity of the Ba ion in colemanite environment. The effect of presence of clay on the sorption characteristics of colemanite was also investigated us-ing 75% colemanite + 25% kaolinite clay mixtures (w/w). It was observed that Rd values increased in the presence of kaolinite from 19 to 55 ml/g in Ba sorp-tion and from 5 to 9 ml/g in Sr sorption. In batch experiments, kinetic studies indicated that the distribution ratio Rd reached saturation in about seven days in Ba-colemanite and in about two days in Sr-colemanite interactions. The effect of changes in initial cation concen-trations on Rd were investigated in the 10"8 M— ΙΟ"5 Μ interval for Ba2+ and in ΙΟ"8 M - 1 0 " 2 Μ inter-val for Sr2+. The resulting loading curves are given in Fig. 4. In the case of Ba it is apparent that the Rd values are not a function of initial cation concen-tration. This suggests that probably one type of sorp-tion site is dominating, with an average Rd value of 140 ml/g. In Sr sorption, the Rd values were found to vary slightly with the cation loading up to about 10 - 3 M. At higher concentrations, an apparent decrease in Rd values may probably mean that energetically less fa-vorable sites become involved in the sorption process. The experimental data obtained in batch experi-ments were fitted to various sorption isotherms and are found to be well described by Freundlich [4] and Dubinin-Radushkevich [5] type isotherms. The re-sulting parameters obtained are given in Table 3. Us-ing these parameters, the corresponding Freundlich empirical isotherm for Ba-colemanite interaction can be expressed as Rd = 95 [Ba]"002. Here [Ba] is the concentration of Ba in the solution following sorption. The corresponding expression for Sr-colemanite interactions is Rd = 30 [Sr]"0 06. Using the Dubinin-Radushkevich type isotherms similar empirical relations can be expressed: Rd = 6.5 Χ10"5 [Ba]- 'e 1 ^[-5.2xl0-3(/?rln(l+[Ba]-'))2] Brought to you by | Hacettepe UeniversitesiAuthenticatedDownload Date | 11/27/18 10:26 PM108 S. Hatipoglu, Η. Göktürk and Η. Ν. Erten Table 3. Various parameters obtained in isotherm fittings Isotherm model Parameter Ba2 Freundlich Dubinin-Radushkevich k Ν Xm (mol/g) Κ (mol2/kJ2) Ε (kJ/mol) 95 0.98 6.5 X10" 5.19X10" 9.8 Sr2"· 30 0.94 3.19X10" 6.52X10" 8.8 that colemanite is a suitable host matrix both for radio-active Sr and Ra storage and/or disposal. Acknowledgements Financial supports of METU through AFP 88-01-03-02 and AFP 90-01-03-05 are gratefully acknowledged. and Rd = 3.19 ΧΙΟ" 4 ^]" 1 £ΐ-6.52Χ10-'(«Π„<1+[5Γ]>Λ for Ba and Sr sorption on colemanite, respectively. The sorption energies (the free energy change when one mole of ions is transferred to the surface of the solid from infinity in solution), related to the Dubi-nin-Radushkevich isotherm constant Κ (Table 3) by Ε = (2 K)"1/2 were found to be 9.8 kJ/mol for Ba and 8.8 kJ/mol for Sr-colemanite sorption. These are in good agreement with the literature values of 8—16 kJ/ mol for ion exchange type interactions [6-8] . To conclude, the following statement can be made: From the waste management point of view, it seems References 1. Simon and Schuster's Rocks and Minerals, Simon and Schus-ter Inc. New York (1990). 2. Erten, Η. N., Aksoyoglu, §., Göktürk, Η.: Sei. Total. Environ. 69, 269 (1988). 3. Vine, E. N„ Bayhuest, B. P., Daniels, W. R., Devilliers, S. J., Erdal, B. R., Lawrance, F. O., Wolfsberg, Κ.: Los Alamos Scientific Laboratory Report, Los Alamos NM 87545 (1980). 4. Freundlich, Η.: Colloid and Capillary Chemistry, Methuen, London (1926). 5. Dubinin, Μ. M., Radushkevich, L. V.: Proc. Acad. Sei. Phys. Chem. Sec., USSR (1947) 331. 6. Cerofolini, G. F.: Surf. Sei. 24, 391 (1971). 7. Hobson, J. P.: J. Phys. Chem. 81, 2720 (1969). 8. Aksoyoglu, §.: J. Radioanal. Nucl. Chem. 134, 393 (1989). Brought to you by | Hacettepe UeniversitesiAuthenticatedDownload Date | 11/27/18 10:26 PM

Migration Behaviour of Barium and Strontium through Colemanite

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Migration Behaviour of Barium and Strontium through Colemanite

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