The Aqueous Solubility and Speciation Analysis for Uranium, Neptunium and Selenium by the Geochemical Code (Eq3/6)

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The Aqueous Solubility and Speciation Analysis for Uranium, Neptunium and Selenium by the Geochemical Code (Eq3/6) JAERI-Research--95-069 JAERI-Research JP9512224 95-069 THE AQUEOUS SOLUBILITY AND SPECIATION ANALYSIS FOR URANIUM, NEPTUNIUM AND SELENIUM BY THE GEOCHEMICAL CODE (EQ3/6) November 1995 Seiji TAKEDA, Shigeki SHIMA, Hideo KIMURA and Hideo MATSUZURU Japan Atomic Energy Research Institute 2 7 Ife 0 7 *v ,t:- I- 12, tl \^M-1)W9ir)\iy^'&M~'hPJ L "C^SWF'ft&-;lnl WfAT-ftWft^Mittf ffiOT/ffiftftiS (=p3l9-ll (T319-11 "^JteicW-fflSWfflrjIuf/iWB AVftf-iiWKmH) t-Wylz i h'MV&.M*• Hz. This report is issued irregularly. Inquiries about availability of the reports should be addressed to Information Division. Department of Technical Information, Japan Atomic Energy Research Institute, To1' li- mura, Naka-gun, Ibaraki-ken 319-11, Japan. ©Japan Atomic Energy Research Institute, 1995 4:)fii /• )} Wf % JAERI-Research 95-069 The Aqueous Solubility and Speciation Analysis for Uranium, Neptunium and Selenium by the Geochemical Code(EQ3/6) Seiji TAKEDA, Shigeki SHIMA, Hideo KIMURA and Hideo MATSUZURU Department of Environmental Safety Research Tokai Research Establishment Japan Atomic Energy Research Institute Tokai-mura, Naka-gun, Ibaraki-ken (Received October 2, 1995) The geochemical condition of a geologic disposal system of HLW controls the solubility and physicochemical forms of dominant aqueous species for elements, which are one of essential information required for safety assessment. Based on the measured compositions of groundwater, the compositions of groundwater in the disposal system were calculated. The solubility and speciation analyses for the polyvalent elements, uranium, neptunium, and selenium, were performed by the geochemical code EQ3/6. The results obtained were compared with the data appeared in the literatures on the solubilities and speciations. The geochemical behaviors of the elements with respect to the solubility and speciation could quantitatively be elucidated for the compositions of the interstitial waters in an engineered barrier and ground water in a natural barrier. In the pH range of neutral to alkali, the solubilities of U and Np tend to increase with an increase of the carbonate concentration in groundwater. This carbonate concentration dependence of the solubility was also estimated. In the engineered barrier the predominant aqueous species were specified, and in the natural barrier the change of aqueous species was also predicted while the chemical compositions changed from the reducing to oxidizing conditions. The dominant aqueous species for the elements, which migrate in and through the disposal system, were determined by the speciation analysis. JAERI- Research 95-069 Keywords: Geochemical Model, Geochemistry, Solubility and Speciation Analysis, Chemical Composition, Eh-pH Condition, Thermodynamic Data, Groundwater, Uranium, Neptunium, Selenium, Radioactive Waste Disposal, High-level Radioactive Waste, Safety Assessment JAERI- Research 95-069 CHLW) , Np, S : T319-11 -4 JAERI-Research 95-069 Contents 1. Introduction 1 2. Geochemical Model 3 2.1 Geochemical Code 3 2.2 Methodology of Analysis 5 2.3 Chemical Composition of Groundwater 7 2.4 Thermodynamic Data 10 2.5 Solid Phase in Natural Groundwater 15 3. Results of Analysis 17 3.1 Uranium 17 3.2 Neptunium 24 3.3 Selenium 29 4. Conclusion 33 4.1 Solubility and Speciation in the Engineered Barrier 34 4.2 Solubility and Speciation in the Natural Barrier 34 Reference 37 Appendix Thermodynamics Data for Uranium, Neptunium, and Selenium 40 V JAERI-Research 95-069 a 1 [^ gA 1 1. rr Htm l 2. fife^-ft^^x;!/ 3 2. 1 ft&I£fl^3- K 3 2. 2 B?fff¥& 5 2. 3 «lT7J<©{(:^#f4 7 2. 4 miJ^T-? 10 2. 5 ifeTTKS^Cfclt^Sffi 15 3. JS¥«fig% 17 3. 1 Uranium 17 3. 2 Neptunium 24 3. 3 Selenium 29 4. %a m 33 4. 1 AX'OjTCtettSjgJB&fcftSMi 34 4.2 ^&'<y TiztstfzfeftBtkftsm 34 i 37 U, Np, Se©fi^^«]r-^ 40 Vi JAERI-Research 95-069 1. INTRODUCTION In the safety assessment for deep geologic disposal of high-level radioactive waste (HLW), the geochemical condition of the disposal system is one of important factors, which govern the performance of the multibarrier system consisting of engineered and natural barriers. The geochemical condition controls the corrosion of metallic containers (canister and overpack) by an interstitial water in the engineered barrier, determine the dissolution of radionuclides from in a waste form, and also govern a chemical form of radionuclides which migrate through the multibarrier. Figure 1 shows the relation between the chemical condition of groundwater and parameters involved in radionuclide transport models to be used in the long-term safety assessment. Such parameters as the solubility and the distribution coefficient of elements depend significantly on the groundwater chemical condition. The distribution coefficient of a specific element, which is an equilibrium parameter to define partitioning of a solute between a solid and a liquid phase, will vary with possible chemical forms of the element in an aqueous solution, e.g., cationic, anionic and nonionic forms. Solubility and thermodynamic data have been obtained from the experiments with solutions of relatively simple compositions compared with natural groundwater. It might be difficult to make the direct estimation, based on these experimental measurements, of their solubilities in solutions containing many kinds of co-ions. The effects of many kinds of aqueous species coexisting in solutions are not negligible to determine the solubility of a specific species. Therefore aqueous solubility and speciation in geochemical environments are subjected to calculations by using geochemical models, based on reliable thermodynamic data obtained from the experiments with solutions of relatively simple compositions. The time durations of these experiments are at the longest a few years. The time scale to consider in the safety assessment is of the orders of at least a few thousand years or more. The change in the long-term chemical compositions in groundwater must be predicted. Considering the circumstances mentioned above, based on the measured characteristics of the deep groundwater, the solubility and speciation analyses for some kinds of the groundwater have been undertaken by SKI (Swedish Nuclear Power Inspectorate, Sweden)(1) and SKB (Swedish Nuclear Fuel and Waste Management Co., Sweden)(2). Chemical interactions between solutions and minerals under physical and chemical conditions of a deep geologic environment can be modeled by the geochemical code, e.g., PHREEQE(3) and EQ3/6(4). The geochemical code must be supported by thermodynamic data, and the reliability of the analyzed results of solubility and speciation thereby depends on the credibility of the thermodynamic data. The thermodynamic data of some kinds of elements have been collected by OECD/NEA. Most of the thermodynamic data used here were obtained from OECD/NEA, and were selected by the criterion of thereliable data used in many literatures. Reacent literatures concerning thermodynamic data of elements - 1 - JAERI-Research 95-069 were also cited. In this report, the aqueous solubility and speciation of several polyvalent elements were analyzed by the geochemical code rystem EQ3/6 by assuming the thermodynamic equilibrium, under some chemical conditions of the groundwater, which are expected in near and far fields. Considering the space- and time-varying chemical characteristic of the groundwater, two types of models for the groundwater were assumed. For the first model (Model 1), the chemical compositions of the interstitial water in the engineered barrier under the reducing conditions were assumed, and for the second model (Model 2), the granitic groundwater in the natural barrier. These chemical compositions were calculateded by the geochemical code by assuming the thermodynamic equilibrium, based on the measured compositions of groundwater. The results obtained here were compared with the literatures on solubility and speciation. < Chemical condition > •pH • redox potential (Eh) • compositon of aqueous solution Experimental data: I Solubility, Speciation, Solubility and speciatbn Equilibrium constants, analysis by geochemical Thermodynamics, etc. code I I Radionuclide transport models used for long-term safety assessment Engineered barrier < Parameters > Transport/ • Solubility I migration • Distribution coefficient Natural barrier etc. Fig. 1 Relation between chemical conditions in groundwater and radonuclide transport models used for long-term safety assessment 2 - JAERI-Research 95-069 2. GEOCHEMICAL MODEL 2.1 Geochemical Code The geochemical software package EQ3/6 (version 3245) (4)(5)(6> consists of main two kinds of the geochemical codes, the EQ3NR code and the EQ6 code, and is supported by the thermodynamic data base and the conversion programs for this data base. It is possible for EQ3/6 to model geochemical processes such as chemical interactions between water-solid or water- mineral. The geochemical code EQ3/6 has been used in the solubility and speciation analyses for many aqueous environments, and known as the code with a high reliability. The flow of information between data files and codes for the EQ3/6 package is shown in Fig. 2. The MCRT code builds the equilibrium constants for aqueous species, minerals, and gases from the thermodynamic data base, and the output file is given as a text form. The EQPT is the preprocessor for the EQ3/6 data base, and the input of the EQPT code is the output of MCRT. Based on the thermodynamic data, concentrations and abundances of individual aqueous species are calculated by the Newton-Raphson method.
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