Ancient blue-and-white porcelains exhibit wide color variations and ‘color dispersion’ due to the use of different cobalt-based blue pigment in different periods. Nowadays, it is difficult to date back due to cobalt ore raw material exhaustion. To clarifying the wide color variations and ‘color dispersion’, Field emission scanning electron microscopy (FE-SEM), X-ray absorption fine structure (XAFS), Optical Microscope (OM), etc, were used to study the color mechanism and ‘color dispersion’ behavior of blue-and-white porcelain by comparing cobalt speciation state and crystal structure stability. The blue tones of blue-and-white porcelain are mainly due to Co2 + ions located in the tetrahedron structure in the glaze, and thus the ‘color dispersion’ distance is large. when Co2+ is located in the tetrahedral structure of the spinel crystal, the blue-and-white porcelain appears dark blue and thus the ‘color dispersion’ distance is small.
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