Erosion — 浸食
Erosion begins not with disappearance, but with penetration. Something enters matter and gradually changes the structure from within. In this work, light seems to move through the mineral surface as water might pass through stone, loosening density and weakening the boundary between solid and fluid states. The darker upper field retains weight, pressure, and resistance, while the pale area below appears increasingly permeable, as though the material has begun to yield to an internal force.
The transformation is slow rather than violent. Cracks, abrasions, and granular traces remain visible, preserving the memory of the original surface even as its solidity starts to dissolve. The work focuses on this intermediate condition: matter is still present, but no longer completely stable. Erosion here is not simply the wearing away of a surface. It is a process in which an unseen presence enters, spreads, and quietly reorganizes the material from inside over time.
