AI Article Synopsis

  • The study uses x-ray photon correlation spectroscopy (XPCS) and in situ rheology to explore the dynamics and properties of Laponite clay suspensions, which change from fluid to soft glass over time.
  • The research finds that the number of localized particles increases quickly during initial formation, while the size of localized areas decreases steadily, but both metrics are linked to the material's elastic shear modulus regardless of concentration.
  • Observations suggest that dynamic heterogeneity plays a significant role in the early stages of aging, indicating that soft solids may form through the development of localized clusters.

Article Abstract

We report a study combining x-ray photon correlation spectroscopy (XPCS) with in situ rheology to investigate the microscopic dynamics and mechanical properties of aqueous suspensions of the synthetic hectorite clay Laponite, which is composed of charged, nanometer-scale, disk-shaped particles. The suspensions, with particle concentrations ranging from 3.25 to 3.75 wt %, evolve over time from a fluid to a soft glass that displays aging behavior. The XPCS measurements characterize the localization of the particles during the formation and aging of the soft-glass state. The fraction of localized particles, f_{0}, increases rapidly during the early formation stage and grows more slowly during subsequent aging, while the characteristic localization length r_{loc} steadily decreases. Despite the strongly varying rates of aging at different concentrations, both f_{0} and r_{loc} scale with the elastic shear modulus G^{'} in a manner independent of concentration. During the later aging stage, the scaling between r_{loc} and G^{'} agrees quantitatively with a prediction of naive mode coupling theory. Breakdown of agreement with the theory during the early formation stage indicates the prevalence of dynamic heterogeneity, suggesting the soft solid forms through precursors of dynamically localized clusters.

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Source
http://dx.doi.org/10.1103/PhysRevE.102.042619DOI Listing

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