The spatial distribution of electrolyte ions at water interfaces remains a topic of considerable interest to the atmospheric, geochemical and physical sciences communities. Here, the depthresolved spatial distributions of K + and CO 3 2− from 0.5 M and 1.1 M aqueous solutions of potassium carbonate (K 2 CO 3 ) are measured by synchrotron based X-ray photoelectron spectroscopy (XPS) in combination with a liquid microjet. The ion distributions determined from the intensities of the K 2p and C 1s orbitals are consistent with the K + cation residing on average slightly closer to the interface than the CO 3 2− anion. The interface of this solution is the broadest yet reported for an electrolyte solution by depth-resolved XPS, consistent with earlier molecular dynamics simulations of aqueous Na 2 CO 3 that showed a large (>1 nm) ion depletion layer at the interface. Results are compared, where possible, between liquid jets running in vacuum (1 × 10 −4 mbar) and jets in an equilibrated background vapor pressure that is determined by the temperature of the solution (6 mbar in this case). The ion spatial distributions and the molecular level pictures of the air-and vacuum-aqueous electrolyte interfaces as derived by XPS are identical.