Effect of grain size on the 85Sr2+ sorption and desorption in columns of crushed granite and infill materials from granitic water under dynamic conditions

被引:9
|
作者
Palagyi, S. [1 ,2 ]
Stamberg, K. [2 ]
Havlova, V. [1 ]
Vodickova, H. [1 ]
机构
[1] Nucl Res Inst Rez Plc, Chem Fuel Cycle & Waste Management Div, Waste Disposal Dept, Husinec Rez 25068, Czech Republic
[2] Czech Tech Univ, Fac Nucl Sci & Phys Engn, Dept Nucl Chem, CR-11519 Prague, Czech Republic
关键词
Crystalline rocks; Groundwater; Sorption; Desorption; Sr-85; Dynamic conditions; Grain size; Breakthrough curve; Linear and non-linear isotherm; Erfc-function model; SAND COLUMN; TRANSPORT; SOILS; RADIONUCLIDES; MIGRATION; CS-137(+);
D O I
10.1007/s10967-012-2311-z
中图分类号
O65 [分析化学];
学科分类号
070302 ; 081704 ;
摘要
The sorption of Sr-85(2+) in the form of 10(-6) M Sr(NO3)(2) in synthetic granitic water (SGW), and its desorption using the same radiotracer-free solution, were investigated under dynamic conditions in columns loaded with crushed granitic materials. The goal of study was to evaluate the influence of grain size on the retardation (R) and distribution (K (d)) coefficients of the soluble Sr-85(2+), as well as on the other transport parameters type of Peclet number (Pe) and hydrodynamic dispersion coefficient (D (d)). Pure granitic sample and granitic fissure infill samples were used, crushed and sieved into 4 different grain size from 0.063 to1.25 mm were used. In order to determine migration parameters, the model based on erfc-function was used, assuming reversible equilibrium linear or non-linear (Freundlich) sorption/desorption isotherms. By means of both model approaches, the experimental breakthrough curves were fitted using non-linear regression procedure according to Newton-Raphson method. The obtained results also validated the applicability of the linear equilibrium isotherms of the Sr-85(2+) sorption/desorption in the studied systems. It was found that in the case of linear isotherm approach, both retardation and distribution coefficients increased with decreasing grain size. Moreover, their values for fracture infill samples are higher than comparing to granite. Depending on the grain size, the retardation coefficient R varied between 11 and 25 for pure granite and 33-58 between for fissure infill material. These values correspond to distribution coefficients K (d) of 2-7 and 9-24 cm(3)/g, respectively. Consequently, the sorption capacity of crushed rocks also increases with decreasing grain size and are about 2.5-times higher for fracture infill than in pure granite. The values of D (d) increase with increasing grain size. Due to inverse proportion, values of Pe number are decreasing.
引用
收藏
页码:33 / 39
页数:7
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