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239Pu(Ⅳ)在花岗岩裂隙介质中迁移的数值模拟

刘君 刘春雨 江宇

核化学与放射化学2013,Vol.35Issue(4):252-256,5.
核化学与放射化学2013,Vol.35Issue(4):252-256,5.DOI:10.7538/hhx.2013.35.04.0252

239Pu(Ⅳ)在花岗岩裂隙介质中迁移的数值模拟

Numerical Simulation of 239Pu(Ⅳ) Transport in Granite Fissure

刘君 1刘春雨 2江宇1

作者信息

  • 1. 哈尔滨工程大学 核科学与技术学院,黑龙江哈尔滨150001
  • 2. 西北核技术研究所,陕西西安710049
  • 折叠

摘要

Abstract

According to the dual continuous medium model,the nuclide transport equations of fissure and matrix are derived in parallel plate single fractured granite based on the nuclide migration rule in this paper,the relative concentrations of nuclide are obtained in fissure and matrix.The 239Pu(Ⅳ) is selected as the simulation subject,the distributions of relative concentration are analyzed in granite fissure and matrix of the study region,combined with the permeability coefficient,the partition coefficient and other parameters of the study region,and the developing trend and migration of 239Pu(Ⅳ) are predicted in fissure and matrix.The simulation shows that this diffusion velocity of 239Pu(Ⅳ) is very slow,the range of diffusion is only millimeter level after 0.5 × 105 a in matrix,but it is 3 m in fissure.The result shows that this area of the granite meets the condition of radioactive waste disposal containing 239Pu(Ⅳ) etc.At the same time,the rule of the nuclides migration is discussed due to the variation of some parameters in the fissure,including the average speed of fissure water,gap width,permeability coefficient,radionuclide half-life,retardation factor in matrix and fissure etc.

关键词

239Pu(Ⅳ)/花岗岩裂隙/核素迁移/数值模拟

Key words

239Pu(Ⅳ)/granite fissure/ radionuclide migration/ numerical simulation

分类

能源科技

引用本文复制引用

刘君,刘春雨,江宇..239Pu(Ⅳ)在花岗岩裂隙介质中迁移的数值模拟[J].核化学与放射化学,2013,35(4):252-256,5.

核化学与放射化学

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