About: Effect of grain size on the Sr-85(2+) sorption and desorption in columns of crushed granite and infill materials from granitic water under dynamic conditions     Goto   Sponge   NotDistinct   Permalink

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  • 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.
  • 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. (en)
Title
  • Effect of grain size on the Sr-85(2+) sorption and desorption in columns of crushed granite and infill materials from granitic water under dynamic conditions
  • Effect of grain size on the Sr-85(2+) sorption and desorption in columns of crushed granite and infill materials from granitic water under dynamic conditions (en)
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  • Effect of grain size on the Sr-85(2+) sorption and desorption in columns of crushed granite and infill materials from granitic water under dynamic conditions
  • Effect of grain size on the Sr-85(2+) sorption and desorption in columns of crushed granite and infill materials from granitic water under dynamic conditions (en)
skos:notation
  • RIV/46356088:_____/13:#0001366!RIV14-MPO-46356088
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  • P(FR-TI1/362)
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  • 1
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  • 71529
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  • RIV/46356088:_____/13:#0001366
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  • Crystalline rocks; Groundwater Sorption; Desorption; Dynamic conditions; Linear and non-linear isotherm (en)
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  • NL - Nizozemsko
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  • [A18B83A28CD0]
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  • Journal of Radioanalytical and Nuclear Chemistry
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  • 297
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  • Havlová, Václava
  • Palágyi, Štefan
  • Vodičková, Hana
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  • 000320284200005
issn
  • 0236-5731
number of pages
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  • 10.1007/s10967-012-2311-z
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