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方解石(10.4)表面与含铜溶液相互作用的动力学和机制。

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

机构信息

CAS Key Laboratory of Mineralogy and Metallogeny/Guangdong Provincial Key Laboratory of Mineral Physics and Materials, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China; University of Chinese Academy of Sciences, Beijing 100049, China; Institutions of Earth Science, Chinese Academy of Sciences, Beijing 100029, China.

CAS Key Laboratory of Mineralogy and Metallogeny/Guangdong Provincial Key Laboratory of Mineral Physics and Materials, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China; Institutions of Earth Science, Chinese Academy of Sciences, Beijing 100029, China.

出版信息

Sci Total Environ. 2019 Jun 10;668:602-616. doi: 10.1016/j.scitotenv.2019.02.232. Epub 2019 Feb 28.

Abstract

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 Cu, a typical bio-toxic metal ion, can alter the calcite dissolution behavior. However, wide concentration ranges of Cu 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 Cu 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 Cu-bearing solutions with different types of anions (SO, Cl and NO). 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 Cu-bearing solutions. Results demonstrated that both anion types and Cu concentrations dramatically affect calcite dissolution. The morphology of etch pits generated in CuSO solutions can be fan-shaped but changed to tear-shaped in Cu(NO) or CuCl solutions. Calcite dissolution kinetics is inhibited at c ≤ 0.1 mM, caused by the coverage of active sites on calcite surfaces. As the Cu concentration increases (1 mM ≤ c ≤ 10 mM), calcite dissolution kinetics is enhanced due to the coupling effect of Cu-incorporated surface structure and solution chemistry. These results revealed the interactive mechanism between calcite dissolution and the migration of toxic Cu in waterways, provided a practical consideration in dealing with the local environment.

摘要

方解石溶解发生于岩石、土壤和沉积物中,对指示岩石圈、生物圈、水圈和大气圈中的元素循环和局部环境至关重要。方解石溶解强烈依赖于水溶液中的金属离子。先前的研究表明,水生 Cu(一种典型的生物毒性金属离子)可以改变方解石的溶解行为。然而,广泛浓度范围的 Cu 与局部环境中普遍存在的阴离子共存,如铜矿床氧化带中的水道和金属加工业附近的土壤,这一点被忽视了。当相当数量的水生 Cu 离子被释放到环境中时,它们会迁移、扩散,从而成为环境污染物。因此,我们专注于方解石溶解与不同类型阴离子(SO、Cl 和 NO)的含 Cu 溶液之间的相互作用。综合运用原位原子力显微镜(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)计算等方法,研究了方解石(10.4)表面与含 Cu 溶液相互作用的动力学和机制。结果表明,阴离子类型和 Cu 浓度都对方解石溶解有显著影响。在 CuSO 溶液中生成的侵蚀坑的形态可以是扇形的,但在 Cu(NO)或 CuCl 溶液中则变成撕裂状。在 c≤0.1mM 时,由于方解石表面活性位点的覆盖,抑制了方解石的溶解动力学。随着 Cu 浓度的增加(1mM≤c≤10mM),由于掺入表面结构和溶液化学的 Cu 的耦合效应,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有毒 Cu 在水道中迁移的相互作用机制,为处理局部环境提供了实际考虑。

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