Thermal poling processes can be used to form modified surface layers on glass that, under ion‐blocking electrode conditions, are depleted of virtually all network‐modifying cations relative to the network‐forming species. During this process, many outstanding questions remain as to the structure of these layers and how it may vary between glasses of different “parent” composition, with important implications for resultant surface properties and industrial applications of this technology. This phenomenon of depleting modifiers is particularly difficult to rationalize in aluminosilicate glass compositions, where—in the parent glass—aluminum ions are predominantly present as cation‐charge‐compensated [AlO4]− tetrahedra prior to poling. Here, we present results of a detailed investigation into the surface depletion layers formed across a wide range of ternary sodium aluminosilicate (NAS) glasses, applying a host of surface‐sensitive spectroscopy methods to directly interrogate the resulting composition and structure within the Na‐depleted, anode‐side surface layers. The desired depletion layers were successfully formed on all of the NAS glasses attempted, all showing (a) near‐complete depletion of alkali within 300‐500 nm‐thick layers on the anode‐side surfaces, (b) thin zones of Al depletion with the Na‐depleted layer, and (c) the absence of injected H+ ions that could serve as an alternative charge‐compensation mechanism. These data essentially confirmed a true binary Al2O3–SiO2 composition inside the depletion layers. However, no significant structural dependence was found as a function of parent glass, where initial compositions ranged from peralkaline to charge‐balanced. Importantly, TEM imaging showed the depletion layers to be fully amorphous and homogeneous (not phase‐separated) at the nanoscale, despite final compositions in the range of 5‐33 mol% Al2O3—a composition space notoriously prone to phase‐separation if prepared by conventional melting. Within the depletion layers, ELNES and TEY‐XANES evidence is shown for retention of Al in a 4‐coordinated state, along with XPS data indicating elimination of non‐bridging oxygen. Taken as a whole, our results indicate a highly‐connected aluminosilicate network, most likely with a relatively high concentration of 3‐coordinated oxygen—or O “triclusters”—as a plausible means of charge‐compensating 4‐coordinated Al in the absence of Na+ or H+. The combined results of this work provide convincing new evidence for unique glass structures within the depletion layers not achievable through analogous melt pathways, with important implications for surface properties.
