What are the main causes of seawater intrusion?
The main causes of seawater intrusion are the over-extraction of groundwater, which lowers the water table and allows seawater to move inland, and sea level rise due to climate change. Poorly managed coastal development and natural subsurface pathways can also contribute to this phenomenon.
What are the effects of seawater intrusion on freshwater aquifers?
Seawater intrusion results in increased salinity in freshwater aquifers, which can degrade water quality and render it unsuitable for drinking, agriculture, and industrial use. It disrupts ecosystems dependent on freshwater, reduces biodiversity, and can harm crops by increasing soil salinity. Additionally, it poses challenges to water management and infrastructure.
How can seawater intrusion be prevented?
Seawater intrusion can be prevented by controlling groundwater extraction, recharging aquifers with freshwater, creating physical barriers like subsurface dams, and implementing managed aquifer recharge through stormwater or treated wastewater. Land management practices and maintaining healthy coastal ecosystems also help prevent seawater from infiltrating freshwater reserves.
How does climate change influence seawater intrusion?
Climate change exacerbates seawater intrusion by rising sea levels and altering precipitation patterns. Higher sea levels increase groundwater salinity as ocean water infiltrates coastal aquifers. Additionally, changes in rainfall can reduce freshwater replenishment of aquifers, diminishing their capacity to counteract intrusion. This amplifies the risk of saltwater contamination in freshwater resources.
What are the signs of seawater intrusion in coastal areas?
Signs of seawater intrusion in coastal areas include increased salinity in groundwater, changes in vegetation composition, groundwater level fluctuations, and the presence of salt-tolerant species. Economic indicators may include reduced agricultural yields and corrosion of infrastructure due to salinity.