On July 8, 2026, a study by the Institute of Environmental Science and Technology at the Universitat Autònoma de Barcelona revealed that over 90% of key nutrients degrading the Mar Menor lagoon originate from recirculated underground flows. This finding challenges current restoration strategies that overlook this significant contamination pathway.
Understanding Nutrient Sources in Mar Menor
The Mar Menor, located in southeastern Spain, has faced severe ecological degradation, notably since 2016. The lagoon, once a popular tourist spot, has increasingly become known for episodes of eutrophication, which depletes oxygen in the water and leads to massive species mortality, such as the fish die-off in 2019.
Traditionally, pollution was attributed to agricultural fertilizers rich in phosphates and nitrates entering through the Albujón stream, the lagoon's only surface watercourse. However, the recent study utilized radium isotopes to trace groundwater types entering the lagoon and identified three main groundwater discharge processes:
- Freshwater groundwater discharge from irrigation.
- Continuous recirculation of saline lagoon water through the aquifer.
- Porewater exchange at the lagoon's sediment bottom.
The Role of Recirculated Flows
The study highlights that the latter two processes are the primary sources of ammonium, dissolved organic nitrogen, dissolved inorganic phosphorus, and dissolved silica in the Mar Menor. These processes operate on two temporal scales:





