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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Cu〜(2 +)轴承溶液相互作用的动力学和机制

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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:在岩石,土壤和沉积物中发生的方解石溶解对于指示岩性圈,生物圈,水圈和大气中的元素周期和局部环境至关重要。方解石溶解强烈取决于水溶液中的金属离子。以前的研究表明,水生Cu2 +,典型的生物毒性金属离子,可以改变方解石溶出行为。然而,忽视了众所周境的Cu(2+)与普遍存在的阴离子(例如金属加工业附近的铜沉积物和土壤氧化区)中普遍存在的阴离子共存的宽浓度范围。当释放到环境中的大量水生Cu2 +离子时,它们迁移,弥散,并因此成为环境污染物。因此,我们专注于具有不同类型的阴离子(SO 42,Cl-和NO 3-)的Caircate溶解和Cu2 + - 布线溶液之间的宽浓度范围之间的相互作用。包括在原位原子力显微镜(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)计算的综合方法,用于调查方解石之间相互作用的动力学和机制( 10.4)表面和Cu2 +八件解决方案。结果表明阴离子类型和Cu2 +浓度显着影响方解石溶解。 CusO4溶液中产生的蚀刻坑的形态可以是风扇形的,但在Cu(NO 3)(2)(2)或CUCl2溶液中改变为Lear。通过在方解石表面上的活性位点的覆盖率引起的钙化物溶解动力学被抑制Al C-C(U2 +)<= 0.1mm。由于Cu2 +浓度增加(1mm + CCU2 + <= 10mm),因此由于Cu2 +掺入的表面结构和溶液化学的偶联效应,方解石溶解动力学增强了。这些结果揭示了方解石溶解与水道中有毒CU2 +的迁移之间的互动机制,提供了处理当地环境的实际考虑。 (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;偶联效果;有毒元素迁移;

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