裂片核素在岩石中的迁移研究Ⅲ.纵向弥散系数的测定和核素~(129)Ⅰ的迁移模型

    • 摘要: 研究了 ̄(125)Ⅰ(模拟裂片核素 ̄(129)Ⅰ)在花岗岩中的吸附动力学,结果表明在实验条件下 ̄(125)Ⅰ吸附极少。由测得的渗透曲线和流量曲线经物料衡算,求得岩石输出浓度与时间的关系曲线。利用分布函数性质,求得纵向弥散系数D、孔隙流速v和有效孔隙率ε_e。提出了 ̄(129)Ⅰ在花岗岩中迁移的数学模型方程,并求解得到核素浓度随时空变化的分析解和数值解。

       

      Abstract: MIGRATION STUDIES ON FISSION PKODUCTS NUCLIDES IN ROCKS Ⅲ.DETERMINATION OF THE LONGITUDINAL DISPERSION COEFFICIENT AND A MODEL EQUATION OF MIGRATION OF~(129)Ⅰ IN GRANITEWEN RUIYUAN;ANG XIANGYUN;AO HONGCHENG(Department of Technical Physics ,Peking University,Beijing,100871)ABSTRACT The adsorption kinetics of ~(129)Ⅰ in granite is studied with ~(125)Ⅰcomcentration in the effluxsorption is found to be negligibly small.The time dependence of ~(125)Ⅰcomcentration in the effluxfrom a granite layer is deduced from the measured penetration and flow curves by materialbalance calculation.Using the property of the distribution function,the longitudinal dispersioncoefficient,the interstitial flow velocity nd the effective interstice fraction are obtained.Adiffer-ential equation describing the migration of ~(129)Ⅰin granite is suggested,and both analytical andnumerical solutions to the eguation are given.Key words~(129)ⅠDispersion coefficient Interstitial flow velocity

       

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