A noncontact crucible method was used to investigate the process by which a Si 3 N 4 coating material forms Si 3 N 4 particles or precipitates on the surface of Si melts and ingots. Si ingots were grown using crucibles with and without a mixture of α-and β-Si 3 N 4 particles. The oxygen and nitrogen concentrations in the ingots were measured by Fourier transform infrared spectrometry analysis. The nitrogen concentration in the ingots grown using crucibles with a Si 3 N 4 coating was significantly higher than that in ingots grown using crucibles without a Si 3 N 4 coating because the nitrogen from the Si 3 N 4 coating material dissolved into the Si melt. From orientation image maps analyzed using electron backscattering diffraction patterns of Si x N y particles on the surface of the ingots, it was clarified that most of the Si x N y particles were β-Si 3 N 4. This was also confirmed by X-ray diffraction measurements. The Si 3 N 4 particles on the surface of the ingots had several morphologies such as needle-like, columnar, leaf-like, and hexagonal structures. There were two cases in which floating Si 3 N 4 particles were formed on the surface of the Si melts, i.e., the removal and dissolution of the Si 3 N 4 coating material. The removed or dissolved Si 3 N 4 coating materials, which consisted of a mixture of α-and β-Si 3 N 4 particles, are considered to have finally changed into β-Si 3 N 4 in the form of transformers or precipitates on the surface of the Si melt, and these β-Si 3 N 4 particles became attached to the surface of the ingots.