Reimus Paul W, Haga Marc J, Adams Andrew I, Callahan Timothy J, Turin H J, Counce Dale A
Environmental Science and Waste Technology Division, Los Alamos National Laboratory, P.O. Box 1663, MS J534, NM 87545, USA.
J Contam Hydrol. 2003 Apr-May;62-63:613-36. doi: 10.1016/s0169-7722(02)00185-7.
Two cross-hole tracer tests involving the simultaneous injection of two nonsorbing solute tracers with different diffusion coefficients (bromide and pentafluorobenzoate) and one weakly sorbing solute tracer (lithium ion) were conducted in two different intervals at the C-wells complex near the site of a potential high-level nuclear waste repository at Yucca Mountain, NV. The tests were conducted to (1) test a conceptual radionuclide transport model for saturated, fractured tuffs near Yucca Mountain and (2) obtain transport parameter estimates for predictive modeling of radionuclide transport. The differences between the responses of the two nonsorbing tracers and the sorbing tracer (when normalized to injection masses) were consistent with a dual-porosity transport system in which matrix diffusion was occurring. The concentration attenuation of the sorbing tracer relative to the nonsorbing tracers suggested that diffusion occurred primarily into matrix pores, not simply into stagnant water within the fractures. The K(d) values deduced from the lithium responses were generally larger than K(d) values measured in laboratory batch sorption tests using crushed C-wells cores. This result supports the use of laboratory-derived K(d) values for predicting sorbing species transport at the site, as the laboratory K(d) values would result in underprediction of sorption and hence conservative transport predictions. The tracer tests also provided estimates of effective flow porosity and longitudinal dispersivity at the site. The tests clearly demonstrated the advantages of using multiple tracers of different physical and chemical characteristics to distinguish between alternative conceptual transport models and to obtain transport parameter estimates that are better constrained than can be obtained using only a single tracer or using multiple nonsorbing tracers without a sorbing tracer.
在内华达州尤卡山一个潜在的高放核废料储存库附近的C井场地,在两个不同层段进行了两次跨孔示踪剂试验,同时注入两种具有不同扩散系数的非吸附性溶质示踪剂(溴化物和五氟苯甲酸盐)和一种弱吸附性溶质示踪剂(锂离子)。进行这些试验的目的是:(1)测试尤卡山附近饱和裂隙凝灰岩的放射性核素迁移概念模型;(2)获取用于放射性核素迁移预测建模的迁移参数估计值。两种非吸附性示踪剂与吸附性示踪剂(按注入质量归一化后)响应之间的差异与存在基质扩散的双孔隙度迁移系统一致。吸附性示踪剂相对于非吸附性示踪剂的浓度衰减表明,扩散主要发生在基质孔隙中,而不仅仅是进入裂隙内的滞水中。从锂的响应推导出的K(d)值通常大于使用粉碎的C井岩芯在实验室批量吸附试验中测得的K(d)值。这一结果支持使用实验室得出的K(d)值来预测场地中吸附性物质的迁移,因为实验室K(d)值会导致吸附预测偏低,从而得出保守的迁移预测结果。示踪剂试验还提供了场地有效流动孔隙度和纵向弥散度的估计值。这些试验清楚地证明了使用具有不同物理和化学特性的多种示踪剂来区分不同的概念性迁移模型以及获取比仅使用单一示踪剂或使用多种非吸附性示踪剂而不使用吸附性示踪剂能得到更好约束的迁移参数估计值的优势。