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~(99)TcO_4~-,HTO在花岗岩中的扩散研究

~(99)TcO_4~-,HTO在花岗岩中的扩散研究[J]. 核化学与放射化学, 2003, 25(4): 204-204.
引用本文: ~(99)TcO_4~-,HTO在花岗岩中的扩散研究[J]. 核化学与放射化学, 2003, 25(4): 204-204.
DIFFUSION BEHAVIOR OF SOME WEAKLY ABSORBED NUCLIDE SPECIES IN GRANITE[J]. Journal of Nuclear and Radiochemistry, 2003, 25(4): 204-204.
Citation: DIFFUSION BEHAVIOR OF SOME WEAKLY ABSORBED NUCLIDE SPECIES IN GRANITE[J]. Journal of Nuclear and Radiochemistry, 2003, 25(4): 204-204.

~(99)TcO_4~-,HTO在花岗岩中的扩散研究

详细信息
  • 中图分类号: O614712

DIFFUSION BEHAVIOR OF SOME WEAKLY ABSORBED NUCLIDE SPECIES IN GRANITE

  • 摘要: 采用实验室模拟方法研究了99TcO-4和HTO在某花岗岩中的扩散行为,获得了扩散系数。并对99TcO-4,HTO以及文献中报道的一些弱吸附性放射性物种在花岗岩中的扩散系数与分子量的关系进行了初步分析。分析表明,在花岗岩中,99TcO-4,HTO,125I-,36Cl-等弱吸附性放射性物种的扩散系数与相应物种的分子量的平方根近似成反比关系。
    Abstract: The diffusion behavior of))~99)TcO~-4 and HTO in granite slice samples is investigated by laboratory simulation method. The apparent diffusion coefficients of))~99)TcO~-4 and HTO in the granite are obtained. In comparison, the relation of the apparent diffusion coefficients of))~99)TcO~-4 and HTO in the granite and the diffusion coefficients of some other nuclide species in granites reported by other scientists to the inverse ratio of the square root of their molecular mass is analyzed. The analysis indicates that for the main species of some wealky absorbed nuclide species, such as))~99)TcO~-4,HTO,~125)I~-,~36) Cl~- et al., the ratio of the apparent diffusion coefficient seems to be inversely related to the ratio of the square root of the molecular mass.
  • [1] 刘元方.当前核素迁移研究的若干进展[J].核化学与放射化学,1990,12(1):1~6.
    [2] PARKCK,RYUBH,HAHNPS.MigrationCharacteristicsofSomeChemicalSpeciesinaGraniteFractureAccordingtoTheirChemicalProperties[J].KoreanJChemEng,2002,19(5):765~772.
    [3] SZANTOZ,SVINGORE,MOLNARM,etal.DiffusionofH 3,Tc 99,I 125,Cl 36andSr 85inGranite,ConcreteandBentonite[J].JRadioanalNuclChem,2002,252(1):133~138.
    [4] LIUChun li,WANGXiang yun,LIShu shen,etal.DiffusionofTc 99inGranite:ASmallScaleLaboratorySimulationExperiment[J].RadiochimActa,2001,89(10):639~642.
    [5] YAMAGUCHIT,NAKAYAMAS.DiffusivityofU,PuandAmCarbonateComplexesinaGraniteFromInada,Ibaraki,JapanStudiedbyThroughDiffusion[J].JContamHydrol,1998,35(1~3):55~65.
    [6] CUIDQ,ERIKSENT.ReactiveTransportofSr,CsandTcThroughaColumnPackedWithFracturefillingMaterial[J].RadiochimActa,1998,82:287~292.
    [7] YAMAGUCHIT,SAKAMOTOY,NAKAYAMAS,etal.EffectiveDiffusivityoftheUranylIoninaGraniteFromInada,Ibaraki,Japan[J].JContamHydrol,1997,26(1~4):109~117.
    [8] LEEJO,LEEKJ,CHOWJ.SorptionandDiffusionofI 125andSr 90inaMixtureofBentoniteandCrushedGraniteBackfillofaRadioactiveWasteRepository[J].RadiochimActa,1997,76(3):143~151.
    [9] WENRui yuan,GAOHong cheng,WANGXiangyun,etal.DiffusionofFissionFragmentNuclidesinGranite[J].RadiochimActa,1997,76(3):137~142.
    [10] 温瑞媛,高宏成,蒋成华,等.裂片核素在岩石中的迁移研究I 核素75Se在花岗岩和石灰岩中的扩散行为[J].核化学与放射化学,1991,13(4):214.
    [11] LIESERKH.TechnetiumintheNuclearFuelCycle,inMedicineandintheEnvironment[J].RadiochimActa,1993,63:5.
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出版历程
  • 收稿日期:  2002-12-12
  • 刊出日期:  2003-11-19

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