Partition of Elements Between Solid and Liquid Phases in Aquatic Environments
  • 【DOI】

    10.1007/s10498-011-9121-8

  • 【摘要】

    The average composition of natural waters such as rivers, lakes, ocean, and hydrothermal vents and corresponding solids in equilibrium (e.g., river-suspended particles or shale; lake sedim... 展开>>The average composition of natural waters such as rivers, lakes, ocean, and hydrothermal vents and corresponding solids in equilibrium (e.g., river-suspended particles or shale; lake sediments; oceanic pelagic clay, organisms, and manganese nodules; and the mid-ocean ridge basalts) do not change randomly. The observed positive correlation between the electron binding energy (I z [*I z ]) and logarithms of bulk distribution coefficient (log K d ) for cations with charge of 1–4, and the negative correlation between I z [*I z ] and log K d for anions in various aquatic systems are consistent with the prediction from the surface comp 收起<<

  • 【作者】

  • 【刊期】

    Aquatic Geochemistry 2011年4-5期

  • 【语种】

    eng