首页> 美国政府科技报告 >Waste Isolation Safety Assessment Program. Task 4. Collection and Generation of Transport Data Theoretical and Experimental Evaluation of Waste Transport in Selected Rocks. Annual Progress Report, October 1, 1978-September 30, 197
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Waste Isolation Safety Assessment Program. Task 4. Collection and Generation of Transport Data Theoretical and Experimental Evaluation of Waste Transport in Selected Rocks. Annual Progress Report, October 1, 1978-September 30, 197

机译:废物隔离安全评估计划。任务4.运输数据的收集和生成选定岩石中废物运输的理论和实验评估。年度进展报告,1978年10月1日至197年9月30日

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The objective of the program is to establish a basis for the prediction of radionuclide sorption in geologic environments. In FY 79, experimental and theoretical efforts were concentrated on a study of the sorption of cesium on the solid substrates Min-u-sil (quartz) and Belle Fourche clay (montmorillonite). Cesium sorption isotherms were obtained for the two substrates at 26 exp 0 C as a function of initial Cs concentration in solution (10 exp -3 M to 10 exp -9 M), pH (5 to 10) and supporting electrolyte concentration (0.002M, 0.01M, 0.1M, and 1M) NaCl and a simulated basalt groundwater in batch-type experiments using crushed material. Characterization of the solid phases included measurements of chemical compositions, particle sizes, surface areas, and cation-exchange capacities. In addition, potentiometric acid/base titrations of the solid phases were conducted in order to determine the acid dissociation and electrolyte exchange constants of the surfaces. Preliminary analysis of the sorption data indicate that while the clay data could be explained by simple mass-action expressions, the quartz data could not. Theoretical efforts were aimed at developing and testing an electrolyte binding electrical double-layer model to predict sorption isotherms. A computerized version of the model, MINEQL, which simultaneously considers surface and solution chemical equilibria, was brought to operational status. Input parameters required by MINEQL were determined and sorption isotherms for Cs on the Belle Fourche clay were calculated over the same range of parameters as the experimental measurements. Comparisons showed that the model was able to simulate the isotherms quite well except at the lowest pH values for the 0.002M and 0.01M NaCl solutions. (ERA citation 05:021898)

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