In-situ oxidation of solid phase was considered to investigate adsorption behavior under different geochemical parameters like pH, initial concentration and ionic strength. Pumice tuff, a potential host rock for low a...In-situ oxidation of solid phase was considered to investigate adsorption behavior under different geochemical parameters like pH, initial concentration and ionic strength. Pumice tuff, a potential host rock for low and intermediate radioactive wastes, has been affected by the redox zone. The characterization of the fresh and oxidized tuff was performed by X-ray diffractometer, scanning electron microscope and mercury intrusion porosimetry. In order to compare the difference of distribution coefficient (K<sub>d</sub>) in fresh and oxidized pumice tuffs, a batch adsorption study was carried out at the range of pH (4 - 12), ionic strength (0.003, 0.1, 1.0 and 3.0 mol/dm<sup>3</sup>) and initial cesium concentration (10<sup>dž</sup>, 10<sup>LJ</sup>, 10<sup>Lj</sup> and 10<sup>lj</sup> mol/dm<sup>3</sup>). Based on experimental K<sub>d</sub> values, ionic strength was found to be the most influential factor, whereas the effects of pH, initial Cs concentration and weathering condition of pumice tuff were negligible. The recalculated K<sub>d</sub> values suggest that the existing surface complexation model is applicable to explain the sorption coefficients through the wide range of solution conditions.展开更多
文摘In-situ oxidation of solid phase was considered to investigate adsorption behavior under different geochemical parameters like pH, initial concentration and ionic strength. Pumice tuff, a potential host rock for low and intermediate radioactive wastes, has been affected by the redox zone. The characterization of the fresh and oxidized tuff was performed by X-ray diffractometer, scanning electron microscope and mercury intrusion porosimetry. In order to compare the difference of distribution coefficient (K<sub>d</sub>) in fresh and oxidized pumice tuffs, a batch adsorption study was carried out at the range of pH (4 - 12), ionic strength (0.003, 0.1, 1.0 and 3.0 mol/dm<sup>3</sup>) and initial cesium concentration (10<sup>dž</sup>, 10<sup>LJ</sup>, 10<sup>Lj</sup> and 10<sup>lj</sup> mol/dm<sup>3</sup>). Based on experimental K<sub>d</sub> values, ionic strength was found to be the most influential factor, whereas the effects of pH, initial Cs concentration and weathering condition of pumice tuff were negligible. The recalculated K<sub>d</sub> values suggest that the existing surface complexation model is applicable to explain the sorption coefficients through the wide range of solution conditions.
