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Hard water is a well-known issue in Belgium. In some regions, homeowners deal with visible limescale buildup almost daily, while in others the problem is noticeably less severe.
But why does water hardness vary so much from one area to another?
The reason for it lies in geology, groundwater composition, and regional infrastructure. Knowing and understanding these differences helps explain why certain cities, especially in parts of Flanders and Wallonia, are more impacted by limescale than others.
Hard water contains higher concentrations of dissolved minerals, primarily calcium and magnesium. These minerals are absorbed naturally as groundwater flows through layers of rock underground.
The more limestone or chalk there is in the soil and bedrock, the more minerals the water collects before it reaches homes and buildings. When heated, these minerals form limescale deposits in pipes, boilers, water heaters and household appliances.
Hard water is not harmful to health. Over time, however, it can have a significant impact on sanitary facilities, heating performance and maintenance costs.
Belgium has very diverse geological formations over relatively short distances. Some areas are characterised by limestone-rich bedrock, while others have sandier or clayier subsoil.
Regions with a high limestone content tend to produce harder water. This explains why certain provinces consistently have higher water hardness levels.
Groundwater extraction methods and local water treatment processes can also influence the final mineral concentration delivered to households, but geology remains the most important factor.
Average water hardness in Belgium varies significantly by region:
(For reference, water above 25 °fH is already classified as hard and can lead to significant limescale buildup over time.)
These differences may seem abstract, but they directly impact how quickly limescale forms inside your plumbing system.
If you want to know the exact hardness level in your municipality, you can use the SoluCalc Water Hardness Calculator on our Homepage to check your region and understand what it means for your home.
In Flanders, several areas are known for elevated water hardness levels.
Cities such as Ghent, parts of the province of Antwerp and areas in Limburg often have higher mineral concentrations due to the underlying limestone structures and the composition of the groundwater. Homeowners in these regions often report:
Since these minerals occur naturally, they cannot simply be ‘filtered out’ using standard water treatment systems.
In Wallonia, too, there are differences in water hardness depending on the geological profile of the individual areas.
The regions around Namur, Charleroi and parts of Hainaut are known for their high lime content due to the lime-rich subsoil formations. Even within relatively short geographical distances, water hardness can change noticeably.
Although municipalities use certain treatment processes, the mineral content often remains high enough to cause visible limescale deposits in households.
The key point is that regional differences are natural and have a direct impact on household plumbing systems over time.
If you live in a region with hard water, the effects are cumulative rather than immediate. Limescale gradually builds up in heating systems, pipes and appliances.
Over several years, this can lead to the following problems:
The harder the water, the more pronounced these long-term effects are.
Knowing the water quality in your area will help you decide whether preventive treatment is a structural necessity rather than a cosmetic measure.
As water hardness varies across Belgium, treatment solutions must be adapted to local conditions.
SoluCalc converts limescale into soluble bicarbonate through controlled CO₂ injection. Rather than removing calcium from the water, it prevents it from forming limescale deposits in pipes and appliances.
This approach:
For homeowners in regions such as Ghent, Antwerp, Limburg, Namur or Hainaut, where mineral concentrations are structurally higher, a salt-free CO₂ system offers long-term protection without complex infrastructure.
Regional differences in water hardness in Belgium are primarily due to geological factors. In areas with limestone-rich subsoil formations, the groundwater naturally has a higher mineral concentration.
Although hard water is safe for human consumption, its long-term effects on sanitary and heating systems should not be underestimated. Especially in regions with consistently high hardness levels.