Salty Groundwater and Concrete Foundations: A Rising Concern
Introduction
As sea levels rise, coastal areas worldwide are facing an unexpected adversary: salty groundwater12. This phenomenon, largely driven by climate change, is causing significant damage to concrete foundations, particularly in regions like South Maui12.
The Saltwater Threat
Concrete, while robust and widely used in construction, is porous3. When exposed to saltwater, the salt can penetrate these pores and cause substantial damage3. Additional signs of salt-damaged concrete include chips, cracks, discoloration, surface erosion, and scaling3.
Rising Saltwater Tables
In coastal areas, the saltwater table, which is the boundary layer where fresh groundwater and saltwater meet, is typically located near the coast or far below the land surface2. However, due to sea-level rise and over-extraction of groundwater, the saltwater table is rising, bringing it closer to the surface and further inland12. This rising saltwater table can have devastating effects on urban infrastructure12.
As the saltwater table rises, it comes into contact with concrete foundations67. The saltwater isclimate.mit.edu/…/how-will-coastal-residents-first-experience-effects-sea-level-rise drawn up into the concrete through capillary action67. Over time, this saltwater can degrade the materials that hold a foundation together, further damaging a home with the added stress of the ebb and flow of groundwater67.
Mitigating the Effects
Fortunately, there are steps that can be taken to prevent salt damage to concrete surfaces3. Using a sealer that prevents salt intrusion is one such measure3. Regular cleaning of the concrete surface to remove salt residue is another crucial step3.
Conclusion
The rising saltwater table in coastal areas is a pressing issue that requires immediate attention and action. By understanding the impacts and implementing effective mitigation strategies, it is possible to safeguard our communities and the environment from the detrimental effects of salty groundwater.