酸化作用对碳酸钙-铅共沉淀体稳定性的影响机制

Effective Mechanism of Acidification on the Stability of Calcium Carbonate-Lead Co-precipitates

  • 摘要:
    目的 探究酸化作用对石灰性土壤中碳酸钙共沉淀固定铅(Pb)的稳定性影响,为Pb的生物有效性调控提供理论依据。
    方法 本研究以重金属Pb为目标污染物,通过共沉淀实验系统探究不同pH、离子强度以及盐酸和有机酸介导的酸化强度对碳酸钙共沉淀及其结合态Pb稳定性的影响,并利用同步辐射X射线近边吸收结构光谱(XANES)阐明碳酸钙对Pb的固定机制。
    结果 土壤pH的增加有利于碳酸钙通过共沉淀作用对Pb的固定,而离子强度的增加不利于Pb的固定;随着体系pH降低程度的增加,碳酸钙-Pb共沉淀体的稳定性减弱;有机酸对Pb的提取率高于盐酸,其中柠檬酸整体上高于苹果酸,但是当体系pH为5.5时,苹果酸对Pb的提取能力较柠檬酸更强;X射线衍射和Ca的L边XANES结果表明,Pb的存在抑制球霰石向方解石转化,球霰石是Pb的主要固定相。
    结论 酸化作用不利于碳酸钙-Pb共沉淀体的稳定,其中柠檬酸的酸化强度最高,苹果酸次之,盐酸最低。此外,在共沉淀过程中Pb主要与球霰石结合。

     

    Abstract:
    Objective Calcium carbonate in calcareous soil can immobilize the heavy metal lead (Pb) by co-precipitation. However, soil acidification caused by fertilization and rhizosphere action inevitably affects the stability of calcium carbonate and its bound heavy metals.
    Method Pb was selected for the study. The effects of pH and ionic strength on the co-precipitation of calcium carbonate with Pb were quantitatively investigated and the stability of calcium carbonate-Pb co-precipitates was studied using hydrochloric acid and organic acids (citric and malic acid).
    Result The results showed that the increase of pH promoted the Pb immobilization by calcium carbonate, while the opposite was true for ionic strength. The stability of calcium carbonate-Pb coprecipitates was weaker with the increase of acidification pH. The extraction of Pb by organic acids was higher than that of hydrochloric acid, where citric acid was higher than malic acid. However, malic acid was more capable of extracting Pb under organic acid extraction at pH 5.5. XRD results indicated that the presence of Pb inhibited the transformation of vaterite to calcite. Ca L-edge XANES analysis revealed that vaterite was the primary phase responsible for Pb immobilization.
    Conclusion Citric and malic acids have different effects on the stability of lead immobilized by calcium carbonate and are closely related to pH. The results can be useful for the study of the chemical transport and transformation behavior of heavy metal elements in the rhizosphere of calcareous soils.

     

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