The Min River on the Chengdu Plain
During the third century BCE, Qin developed agriculture and administration in Shu. The Min River carried seasonally changing flows and sediment onto the Chengdu Plain. Both floods and shortages affected cultivation. Construction of Dujiangyan is traditionally associated with Li Bing and dated to around 256 BCE. Its works directed river water toward irrigation while managing flood and sediment problems, connecting regional farming with Qin’s broader administration of the territory.
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Diversion, sediment and maintenance
The Fish Mouth diversion embankment, Flying Sand Weir and Bottle Neck intake work together to direct flows. Diversion separates channels, overflow and sediment handling reduce accumulation, and the intake regulates water entering the irrigation network. Structures were repeatedly repaired and adapted to river conditions. Reliable operation required observation, dredging and embankment maintenance. Hydraulic knowledge therefore included both physical works and the continuing organization of people responsible for their upkeep.
References: [1]
Fields and regional life
Later Tang, Song, Yuan and Ming administrations modified and enlarged the irrigation system. Water supported fields, settlements and urban activity, while maintenance required coordination between users. Continued operation reflects centuries of repair and adaptation, as successive workers renewed materials and adjusted structures to changing rivers and local requirements. Dredging, rebuilding and allocation joined farming to public engineering. Communities used the river while repeatedly organizing the work required to manage shortages, flooding and competing demands.
References: [1]