Water management in West Flanders is under pressure as the flow from the Leie to the IJzer river decreases significantly. Governor Carl Decaluwé recently described this water movement as the “infusion” that keeps the IJzer alive. However, persistent dry weather and falling water levels in the Leie and Bovenschelde rivers are causing concern.
- Water moves from Leie to IJzer
- Governor Decaluwé calls it "infuus"
- Leie and Bovenschelde flow rates drop
- Reduced flow limits water transfer ability
- Current flow below 30 cubic meters/second
- Temporary halt in water transfer occurs
On 2025-05-21 16:37:00, officials reported that the flow rate from the Leie and Bovenschelde had dropped from 50 to 60 cubic meters per second just ten days ago to around 30 cubic meters per second or less. This reduction means that the essential water supply to the IJzer can no longer be maintained consistently.
What does this mean for local communities relying on these waterways? And how long can the current situation last without impacting the region’s water balance? The answers lie in how authorities manage the shrinking water flow.
Is the drop in water flow a sign of a worsening drought, or a temporary fluctuation? The current situation highlights several key points:
- The minimum flow of 30 cubic meters per second is critical to maintain water transfer to the IJzer.
- Below this threshold, water flow to the IJzer stops, risking ecological and supply issues.
- Ongoing dry conditions reduce river levels, emphasizing the need for sustainable water management.
Looking ahead, it is vital for policymakers and communities to support measures that safeguard river flows and water quality. Could improved water conservation and infrastructure investments help prevent future disruptions? Staying informed and proactive will be key to managing West Flanders’ water resources effectively.
