Silicon single crystals are prepared from molten granules, by producing a first volume of molten silicon between a growing single crystal and the lower end of a silicon conical tube which is closed at its lower end, and encloses a central opening of a rotating silicon plate below which the tube extends, by means of a first induction heating coil arranged below the plate; producing a second volume of molten silicon by a second induction heating coil arranged above the plate; melting the lower end of the tube to form a passage for the second volume of molten silicon, the passage produced at a point in time when the second volume is not yet present or is less than double the volume of the first volume; and crystallizing monocrystalline silicon on the growing single crystal with consumption of molten silicon from the first and the second volume.