4.6 Article

Time, pH, and size dependency of silver nanoparticle dissolution: the road to equilibrium

Journal

ENVIRONMENTAL SCIENCE-NANO
Volume 4, Issue 6, Pages 1314-1327

Publisher

ROYAL SOC CHEMISTRY
DOI: 10.1039/c6en00564k

Keywords

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Funding

  1. NanoNextNL [FES 5120756-02]

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Oxidative dissolution has large implications for the environmental fate and toxicity of silver nanoparticles (AgNPs). In this study, we quantify the kinetics, pH, and size dependency of silver ion (Ag+) release from AgNPs and explain our results in a consistent manner with a mechanistic view. Pristine AgNPs are covered by partially oxidized silver present in a single layer of subvalent. Ag3OH groups that will be released by oxidative dissolution via two different pathways. Undersaturation of a solution, created by acidification, will initiate a fast oxidative dissolution process in which a pristine surface can be opened at particular points that grow laterally until a full layer of Ag is stripped off. At the newly exposed surface,. equivalent to Ag3OH is reformed. The opening of new spots stops due to increasing Ag+ concentrations. Via another pathway, the initial equivalent to Ag3OH can be released by oxidative dissolution while simultaneously a new stable surface state is built with subvalent silver in two layers. This process is initiated by dilution and is visible around neutral pH values and may release a maximum of 30 +/- 1 mu mol Ag+ m(-2). Its equilibration can be well described with a formulated thermodynamic model. The equilibrium constant (logK) is linearly related to the specific surface area of the AgNPs used, but can be shifted by the type of capping agent. The particle size dependency of the log K can be attributed to a surface Gibbs free energy contribution of 0.7 +/- 0.1 J m(-2). Ag+ release by stripping is relatively fast (similar to 1 day) in contrast to the process that leads to equilibration of two types of surface species that differ in the amount of subvalent silver. For this process, a kinetic Langmuir model has been developed in which the rate of Ag+ release is governed by adsorbed molecular oxygen that can be activated via a proton, while adsorption of molecular oxygen by itself can become rate limiting in the initial stage of dissolution with high rates of release. In our study with data of different kinds, the overall release and equilibration by AgNPs has been interpreted successfully with a coherent, overarching mechanistic view.

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