Colloidal self-assembly is a process in which dispersed matter spontaneously form higher-order structures without external intervention. During self-assembly, packed particles are subject to solvent-evaporation induced dynamic structuring phases, which leads to microscale defects called the grain boundaries. While it is imperative to precisely control detailed grain boundaries to fabricate well-defined self-assembled crystals, the understanding of the colloidal physics that govern grain boundaries remains a challenge due to limited resolutions of current visualization approaches. In this work, we experimentally report in situ interparticle interactions during evaporative colloidal assembly by studying a novel microscale laser induced fluorescence technique. The fluorescence microscopy measures the saturation levels with high fidelity to identify distinct colloidal structuring regimes during self-assembly as well as cracking mechanics. The techniques discussed in this work not only enables unprecedented levels of colloidal self-assembly analysis but also have potential to be used for various sensing applications with microscopic resolutions.
Main Findings
We employ a novel μLIF technique that overcomes extant resolution barriers to experimentally characterizes real-time interparticle interactions in colloidal assemblies that decide grain boundary formation mechanisms with up to 300 nm spatial resolution. Our method identifies three distinctive saturation level-dictated structuring phases called the saturated, the wet, and the dry regime. The fluorescence intensity increases by 44% and 153% during saturated to wet regime and wet to dry regime transition, respectively. The saturation level jumps indicate discrete saturation level reductions during the self-assembly process. The quick transition (~15 s) from saturated to wet regime suggest a rapid structuring of nanospheres. In addition, grain boundaries form in the wet regime where the local saturation level measurements shows that the near-crack domain has 25% lower normalized dryness than the opal domain, suggesting the existence of microscale evaporation rate misbalances between the two domains. The evaporation rate misbalances in turn can cause auxiliary tensile forces that especially promote longitudinal cracks. Furthermore, in situ saturation level monitoring shows that transverse cracks function as hydraulic barriers that trigger local grain dry-out, which eventuate in non-simultaneous film dry-out. The findings in this study provides foundational grounds for engineering novel micro/nanostructures and promises innovational advances in large scale fabrication of self-assembled structures.