In a method for producing a silicon single by pulling the silicon single crystal from a silicon melt contained in a crucible, a magnetic field is applied to the silicon melt in a radial direction of the silicon single crystal, and a vertical level of a center of the magnetic field relative to a surface of the silicon melt is controlled such that a thermal gradient in an axial direction of the crystal is maintained at a constant value in respective portions along a radial direction of the silicon single crystal.