摘要： Introduction. There are two main mechanisms of stone ablation with long‐pulsed infrared lasers: photothermal and photomechanical. Which of them is primary in stone destruction is still a matter of discussion. Water holds importance in both mechanisms but plays a major role in the latter. We sought to identify the prevailing mechanism of stone ablation by evaluating the stone mass‐loss after lithotripsy in different media. Material and methods. We tested a Ho:YAG laser (100W, Lumenis, USA), a Tm‐fiber laser U1 (TFL U1), (120W, NTO IRE‐Polus, Russia) and a Superpulse Tm‐fiber laser U2 (TFL U2) (500W, NTO IRE‐Polus, Russia). A single set of laser parameters (15 W = 0.5 J × 30 Hz) was used. Contact lithotripsy was performed in phantoms (BegoStones) in different settings: a) hydrated phantoms in water; b) hydrated phantoms in air; с) dehydrated phantoms in water; d) dehydrated phantoms in air. Laser ablation was performed with total energy of 0.3 kJ. Phantom mass‐loss was defined as the difference between the initial phantom mass and the final phantom mass of the ablated phantoms. Results. All lasers demonstrated effective ablation in hydrated phantoms ablated in water, no visual differences between the lasers were detected. The ablation of dehydrated phantoms in air was also effective with visible vapor during ablation and condensation on the cuvette wall. Dehydrated phantoms in water and in air shown minimal to no ablation accompanied with formation of white crust on phantoms surface. Among laser types, TFL U2 had the highest phantom mass‐loss in all groups except for dehydrated phantoms ablated in air. Conclusions. Our results suggest that both photothermal and thermomechanical ablation mechanisms (explosive vaporization) occur in parallel during laser lithotripsy. In Ho:YAG and TFL U2 stone ablation, explosive vaporization prevail, while in TFL U1 ablation, photothermal mechanism appear to predominate.