Aqueous acidic ozone (O 3 )-containing solutions are increasingly used for silicon treatment in photovoltaic and semiconductor industries. We studied the behavior of aqueous hydrofluoric acid (HF)-containing solutions (i.e., HF−O 3 , HF−H 2 SO 4 −O 3 , and HF−HCl−O 3 mixtures) toward boron-doped solar-grade (100) silicon wafers. The solubility of O 3 and etching rates at 20 °C were investigated. The mixtures were analyzed for the potential oxidizing species by UV−vis and Raman spectroscopy. Concentrations of O 3 (aq) , O 3 (g) , and Cl 2 (aq) were determined by titrimetric volumetric analysis. F − , Cl − , and SO 4 2− ion contents were determined by ion chromatography. Model experiments were performed to investigate the oxidation of Hterminated silicon surfaces by H 2 O−O 2 , H 2 O−O 3 , H 2 O−H 2 SO 4 −O 3 , and H 2 O−HCl−O 3 mixtures. The oxidation was monitored by diffuse reflection infrared Fourier transformation (DRIFT) spectroscopy. The resulting surfaces were examined by scanning electron microscopy (SEM) and X-ray photoelectron spectroscopy (XPS). HF−H 2 O−O 3 mixtures show a polishing etching behavior, whereas HF−HCl−H 2 O−O 3 mixtures exhibit slight anisotropic etching. Formation of pyramidal-like morphologies on (100) silicon surfaces was observed. In all cases, cleaned and H-terminated silicon surfaces are obtained. The results were used to draw conclusions about the dissolution mechanism of silicon in the respective solutions. In HF−H 2 O−O 3 mixtures, silicon is dissolved by an O 3(aq) -diffusion-controlled tetravalent etching mechanism. Interestingly, in H 2 SO 4 -rich aqueous HF−H 2 SO 4 −O 3 solutions, only the native oxide is removed, whereas silicon is not attacked and dissolved. In HCl-containing solutions, Cl 2 or Cl 3− are responsible for silicon oxidation. HCl can be considered as a catalyst resulting in a divalent silicon dissolution mechanism similar to the etching in alkaline solutions.