Geraedts K, Maes A
Centre for Surface Chemistry and Catalysis, Department of Microbial and Molecular Systems, Catholic University of Leuven, Kasteelpark Arenberg 23, B-3001 Heverlee, Belgium.
Chemosphere. 2008 Sep;73(4):491-7. doi: 10.1016/j.chemosphere.2008.06.042. Epub 2008 Aug 15.
The interaction between colloidal Tc(IV) species and colloidal Gorleben humic substances (HS) was quantified after application of the La-precipitation method on supernatant solutions obtained under various experimental conditions but at constant ionic strength of the Gorleben groundwater (0.04M). The determined interaction constant LogKHS (2.3+/-0.3) remained unchanged over a large range of Tc(IV) and HS concentrations and was independent of the pH of the original supernatant solution (pH range 6-10), Tc(IV)-HS loading (10(-3)-10(-6)molTcg(-1) HS) and the nature of the reducing surface (Magnetite, Pyrite and Gorleben sand) used for the pertechnetate reduction. The LogKHS value determined by the La-precipitation method is lower than the LogK value obtained from a previous study where the interaction between colloidal Tc(IV) species and Gorleben humic substances was quantified using a modified Schubert approach (2.6+/-0.3). The La-precipitation method allows to accurately determine the amount of Tc(IV) associated with HS but leads to a (small) overestimation of the free inorganic Tc(IV) species.
在对不同实验条件下但戈尔莱本地下水离子强度恒定(0.04M)时获得的上清液应用镧沉淀法后,对胶体态四价锝物种与胶体态戈尔莱本腐殖质(HS)之间的相互作用进行了定量。所确定的相互作用常数LogKHS(2.3±0.3)在四价锝和腐殖质的较大浓度范围内保持不变,并且与原始上清液的pH值(pH范围6 - 10)、四价锝 - 腐殖质负载量(10⁻³ - 10⁻⁶molTc g⁻¹ HS)以及用于高锝酸盐还原的还原表面(磁铁矿、黄铁矿和戈尔莱本砂)的性质无关。通过镧沉淀法确定的LogKHS值低于先前一项研究中使用改良舒伯特方法(2.6±0.3)对胶体态四价锝物种与戈尔莱本腐殖质之间的相互作用进行定量时获得的LogK值。镧沉淀法能够准确确定与腐殖质结合的四价锝的量,但会导致对游离无机四价锝物种的(少量)高估。