Re()在铜改性膨润土中的吸附与扩散行为

    Adsorption and Diffusion Behavior of Re() in Cu-Bentonite

    • 摘要: 通过批式实验研究了Re(Ⅶ)在铜改性膨润土中的吸附行为,并确定了Re(Ⅶ)的吸附规律。采用贯穿扩散法,研究了不同压实密度的铜改性膨润土中Re(Ⅶ)的扩散行为,并与未经改性的高庙子膨润土、钠基膨润土、钙基膨润土以及中国浙江安吉膨润土中的Re(Ⅶ)扩散行为进行了比较。研究发现,在铜改性膨润土中,Re(Ⅶ)的吸附能力和分配系数随着温度的升高而降低。随着铜改性膨润土的压实密度从1300 kg/m3增加到1800 kg/m3,Re(Ⅶ)的有效扩散系数De从约2.15×10−11 m2/s下降到约0.55×10−11 m2/s,这与Re(Ⅶ)在高庙子、钠基、钙基以及浙江安吉膨润土中的扩散系数随膨润土压实密度变化情况相一致。随着压实密度逐渐增加,岩石容量因子α呈现下降趋势,从约0.23减少到约0.11;表观扩散系数Da从约9.35×10−11 m2/s下降到约5.00×10−11 m2/s,这主要是由于压实密度的改变所引起的扩散空间层结构的变化导致的。

       

      Abstract: This work aims to evaluate the potential of copper-modified bentonite(Cu-bentonite) as a barrier material for deep geological nuclear waste repositories. It specifically focuses on its capability to adsorb and impede the migration of rhenium(Re(Ⅶ)), which serves as an experiment alternative for the long-lived fission product technetium-99(99Tc). Comprehending the adsorption behavior and diffusion mechanisms of Re(Ⅶ) in modified bentonites is crucial for assessing the long-term safety of repositories. The chemical composition and surface characteristics of bentonite were analyzed using scanning electron microscope-energy dispersive spectroscopy(SEM-EDS), X-ray fluorescence spectroscopy(XRF), multi-angle particle size and high-sensitivity zeta potential analyzer, and X-ray photoelectron spectroscopy(XPS). First, batch experiments were conducted to investigate the adsorption behavior of Re(Ⅶ) on Cu-bentonite. Then, the diffusion behavior of Re(Ⅶ) through compacted Cu-bentonite samples was studied using the through-diffusion method. To establish a baseline and evaluate the modification effect, the diffusion behavior of Re(Ⅶ) was also studied in various unmodified bentonites: Gaomiaozi bentonite(GMZ), Na-bentonite, Ca-bentonite, and Anji bentonite(from Zhejiang province, China). This study examined the influence of key parameters, such as temperature on adsorption and compaction density on diffusion, on the performance metrics. Adsorption studies reveal that the adsorption capacity and distribution coefficient(Kd) of Re(Ⅶ) on Cu-bentonite decrease with increasing temperature. Diffusion experiments demonstrate that both the effective diffusion coefficient(De) and the apparent diffusion coefficient(Da) of Re(Ⅶ) decrease significantly as the compaction density of the compacted Cu-bentonite increases from 1 300 kg/m3 to 1 800 kg/m3. Specifically, De droppes from about 2.15×10−11 m2/s to 0.55×10−11 m2/s, and Da decreases from about 9.35×10−11 m2/s to 5.00×10−11 m2/s. Concurrently, the rock capacity factor(α) decreases from about 0.23 to 0.11 with increasing compaction density. This decreasing trend of diffusion coefficients with increasing compaction density is consistent and observes not only in Cu-bentonite but also in all the tested unmodified bentonites(GMZ, Na-, Ca-, Anji). Analysis indicates that the reduction in diffusion coefficients is primarily attributed to changes in the interlayer pore structure and diffusion pathways resulting from increased compaction density. Crucially, under identical density conditions, the mobility of Re(Ⅶ) in Cu-bentonite remains consistently low. Copper modification significantly enhances the capability of bentonite to retard Re(Ⅶ) migration. The increased adsorption capacity at higher temperatures and the significant reduction in diffusion rates associated with higher compaction densities are favorable properties for barrier materials. The dominant mechanism for reduced diffusion appears to be the alteration of the pore structure limiting diffusion pathways as density increases.

       

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