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^(85)Sr、^(134)Cs和^(60)Co在浅地层黄土与地下水间的分配系 被引量:10

DETETERMINATION OF DISTRIBUTION COEFFICENTS FOR ^(85)Sr,^(134)Cs AND ^(60)Co BETWEEN LOESS AND UNDERGROUND WATHER
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摘要 本文报道了 ̄(85)Sr、 ̄(134)Cs和 ̄(60)Co在采自本院野外试验场,从地表到地下2m深黄土与地下水间分配系数的测定结果,以及核素浓度、pH和温度对分配系数的影响。黄土采集的深度范围分别为:地表-0.5m,0.5-1m,1-1.5m,1.5-2m,共采集16个样品;地下水取自试验场的井水。实验采用静态法。实验结果表明,16个样品测定的 ̄(85)Sr、 ̄(134)Cs和 ̄(60)Co的分配系数的均值分别为82、7.4×10 ̄3和5.4×10 ̄3mL/g;在不同深度的黄土中测得的分配系数基本一致。pH值的变化对 ̄(134)Cs和 ̄(85)Sr的分配系数有较大影响,对 ̄(60)Co则影响不大。 Measurement results of distribution coefficients were reported for the radionu-clides  ̄(85)Sr、 ̄(134)Cs and ̄(60)Co between the loess and underground water taken from CIRP' s fieldtest site. In addition,the affection of carrier concentration of each radionuclide ,pH value andtemperature to the distribution coefficient was also declared. Sixteen loess samples were coLlected in the following depthes:surface-0.5m,0.5-1.0m,1.0-1.5 m and l.5-2.0m.The well water in the field test site was taken as underground water. Batch method was usedin the experiment. For each kind of radionuclides the distribution coefficients were almost thesame for loess samples taken from different depthes. Average K_d value of sixteen samples for ̄(85)Sr、 ̄(134)Cs and  ̄(60)Co was 82,7.4×10 ̄3 and 5.4 ×10 ̄3mL/g,respectively. Distribution coeffi-cients were greatly affected by pH value for these three radionuclides.
出处 《辐射防护》 CAS CSCD 北大核心 1995年第2期138-142,共5页 Radiation Protection
关键词 分配系数 ^(85)Sr ^(134)Cs ^(60)Co 黄土 地下水 核素迁移 ^(85)Sr ^(134)Cs ^(60)Co Underground Water Loess Distribution coefficient Nuclide Migration
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参考文献1

  • 1李祯堂,辐射防护,1987年,7卷,6期,414页

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