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Kinetics and mechanisms of the interaction between the calcite (10.4) surface and Cu~(2+)-bearing solutions

机译:方解石(10.4)表面与含Cu〜(2+)溶液相互作用的动力学和机理

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摘要

Calcite dissolution, occurring in rocks, soils and sediments, is essential to indicate element cycles and local environments in the lithosphere, biosphere, hydrosphere and atmosphere. Calcite dissolution strongly depends on metal ions in aqueous solutions. Previous studies showed that aquatic Cu2+, a typical bio-toxic metal ion, can alter the calcite dissolution behavior. However, wide concentration ranges of Cu(2+)coexisting with ubiquitous anions in local environments, such as waterways in the oxidation zones of copper deposits and soils near metal processing industry, was overlooked. When a considerable amount of aquatic Cu2+ ions are released into the environment, they migrate, diffuse, and hence become an environmental pollutant. Therefore, we focused on the interaction between calcite dissolution and wide concentration ranges of Cu2+-bearing solutions with different types of anions (SO42-, Cl- and NO3-). Comprehensive approaches including in situ atomic force microscopy (AFM), X-ray photoelectron spectroscopy (XPS), transmission electron microscope (TEM), and density functional theory (DFT) calculations were employed to investigate kinetics and mechanisms of the interaction between the calcite (10.4) surface and Cu2+-bearing solutions. Results demonstrated that both anion types and Cu2+ concentrations dramatically affect calcite dissolution. The morphology of etch pits generated in CuSO4 solutions can be fan-shaped but changed to Lear-shaped in Cu(NO3)(2) or CuCl2 solutions. Calcite dissolution kinetics is inhibited al C-C(u2+) = 0.1 mM, caused by the coverage of active sites on calcite surfaces. As the Cu2+ concentration increases (1 mM = CCu2+ = 10 mM), calcite dissolution kinetics is enhanced due to the coupling effect of Cu2+ incorporated surface structure and solution chemistry. These results revealed the interactive mechanism between calcite dissolution and the migration of toxic Cu2+ in waterways, provided a practical consideration in dealing with the local environment. (C) 2019 Elsevier B.V. All rights reserved.
机译:方解石溶解发生在岩石,土壤和沉积物中,对于指示岩石圈,生物圈,水圈和大气中的元素循环和局部环境至关重要。方解石的溶解在很大程度上取决于水溶液中的金属离子。先前的研究表明,水生Cu2 +是一种典型的具有生物毒性的金属离子,可以改变方解石的溶解行为。然而,人们忽略了铜(2+)的广泛浓度范围与局部环境中普遍存在的阴离子共存,例如铜沉积物的氧化区中的水路和金属加工工业附近的土壤。当大量的水生铜离子释放到环境中时,它们会迁移,扩散并因此成为环境污染物。因此,我们着眼于方解石溶解与具有不同类型阴离子(SO42-,Cl-和NO3-)的宽浓度范围的含Cu2 +的溶液之间的相互作用。利用包括原位原子力显微镜(AFM),X射线光电子能谱(XPS),透射电子显微镜(TEM)和密度泛函理论(DFT)计算在内的综合方法来研究方解石之间相互作用的动力学和机理10.4)表面和含Cu2 +的溶液。结果表明,阴离子类型和Cu2 +浓度均显着影响方解石的溶解。在CuSO4溶液中产生的腐蚀坑的形态可以呈扇形,但在Cu(NO3)(2)或CuCl2溶液中变为李尔形。方解石溶解动力学被抑制Al C-C(u2 +)<= 0.1 mM,这是由于方解石表面活性部位的覆盖所致。随着Cu2 +浓度的增加(1 mM <= CCu2 + <= 10 mM),由于结合了Cu2 +的表面结构和溶液化学的耦合作用,方解石溶解动力学得到增强。这些结果揭示了方解石溶解与水中有毒Cu2 +迁移之间的相互作用机制,为应对当地环境提供了实际考虑。 (C)2019 Elsevier B.V.保留所有权利。

著录项

  • 来源
    《The Science of the Total Environment》 |2019年第10期|602-616|共15页
  • 作者单位

    Chinese Acad Sci, CAS Key Lab Mineral & Metallogeny, Guangdong Prov Key Lab Mineral Phys & Mat, Guangzhou Inst Geochem, Guangzhou 510640, Guangdong, Peoples R China|Univ Chinese Acad Sci, Beijing 100049, Peoples R China|Chinese Acad Sci, Inst Earth Sci, Beijing 100029, Peoples R China;

    Chinese Acad Sci, CAS Key Lab Mineral & Metallogeny, Guangdong Prov Key Lab Mineral Phys & Mat, Guangzhou Inst Geochem, Guangzhou 510640, Guangdong, Peoples R China|Chinese Acad Sci, Inst Earth Sci, Beijing 100029, Peoples R China;

    Chinese Acad Sci, CAS Key Lab Mineral & Metallogeny, Guangdong Prov Key Lab Mineral Phys & Mat, Guangzhou Inst Geochem, Guangzhou 510640, Guangdong, Peoples R China|Univ Chinese Acad Sci, Beijing 100049, Peoples R China|Chinese Acad Sci, Inst Earth Sci, Beijing 100029, Peoples R China;

    Chinese Acad Sci, CAS Key Lab Mineral & Metallogeny, Guangdong Prov Key Lab Mineral Phys & Mat, Guangzhou Inst Geochem, Guangzhou 510640, Guangdong, Peoples R China|Univ Chinese Acad Sci, Beijing 100049, Peoples R China|Chinese Acad Sci, Inst Earth Sci, Beijing 100029, Peoples R China;

    Chinese Acad Sci, CAS Key Lab Mineral & Metallogeny, Guangdong Prov Key Lab Mineral Phys & Mat, Guangzhou Inst Geochem, Guangzhou 510640, Guangdong, Peoples R China|Univ Chinese Acad Sci, Beijing 100049, Peoples R China|Chinese Acad Sci, Inst Earth Sci, Beijing 100029, Peoples R China;

    Chinese Acad Sci, CAS Key Lab Mineral & Metallogeny, Guangdong Prov Key Lab Mineral Phys & Mat, Guangzhou Inst Geochem, Guangzhou 510640, Guangdong, Peoples R China|Univ Chinese Acad Sci, Beijing 100049, Peoples R China|Chinese Acad Sci, Inst Earth Sci, Beijing 100029, Peoples R China;

    Chinese Acad Sci, CAS Key Lab Mineral & Metallogeny, Guangdong Prov Key Lab Mineral Phys & Mat, Guangzhou Inst Geochem, Guangzhou 510640, Guangdong, Peoples R China|Univ Chinese Acad Sci, Beijing 100049, Peoples R China|Chinese Acad Sci, Inst Earth Sci, Beijing 100029, Peoples R China;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Calcite dissolution; Cu(2)(+)concentrations; Anion types; Coupling effect; Toxic element migration;

    机译:方解石溶解;Cu(2)(+)浓度;阴离子类型;耦合效应;有毒元素迁移;

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