In
the more than 100 years since the Liesegang phenomenon was discovered,
intensive studies have been conducted to understand and control the
characteristics of the periodic precipitation patterns in which the
outer electrolyte diffuses into a hydrogel containing the inner electrolyte.
Between fields of physics and chemistry, the periodicity of the precipitate
has been investigated restrictively by spatial analyses and numerical
simulations at macroscopic scales and it has been considered as a
result of simple precipitation. In this work, calcium ion diffusion
into gelatin hydrogels containing phosphate ions, a biomimetic system
for bone formation, resulted in typical Liesegang patterns at macroscopic
scales, but the asymmetric growth of the crystal was found in every
single band at microscopic scales, which has not been observed or
overlooked in the previous reports. The pattern consists of three
characteristic bands: a continuous band, a split-fin band, and an
intact-fin band. While the continuous band has a uniform crystal density,
the split-fin and intact-fin bands have asymmetric crystal densities
along the single band. We investigate the formation process of individual
bands as well as the whole pattern by combining microscopic and spatiotemporal
analyses based on the nucleation theory. Formation processes of asymmetric
bands are explained by the unique stability and the diffusive property
of amorphous precursors depending on the rate of calcium ion delivery.
This is the first study to focus on the inhomogeneity of a single
band in Liesegang patterns and the time-dependent mechanism of its
growth.