The first step is to excavate a fixed-form river channel, allowing water to naturally flow and take on an initial winding state. Once the water system for the site is established, silvoarable, silvopasture and windbreak systems are introduced.

After the site is re-excavated for water channels, the land types are reorganised. Three years later, the waterways gradually develop a winding natural flow pattern. A decade later, the riverbank green buffer zone naturally takes shape.

As the ecosystem on the site gradually recovers and the agricultural model takes shape, a portion of the local wildlife species return due to abundant and natural habitats.