TY - JOUR
T1 - Groundwater-driven nutrient inputs to coastal lagoons
T2 - The relevance of lagoon water recirculation as a conveyor of dissolved nutrients
AU - Rodellas, Valentí
AU - Stieglitz, Thomas C.
AU - Andrisoa, Aladin
AU - Cook, Peter G.
AU - Raimbault, Patrick
AU - Tamborski, Joseph J.
AU - van Beek, Pieter
AU - Radakovitch, Olivier
PY - 2018/11/15
Y1 - 2018/11/15
N2 - Evaluating the sources of nutrient inputs to coastal lagoons is required to understand the functioning of these ecosystems and their vulnerability to eutrophication. Whereas terrestrial groundwater processes are increasingly recognized as relevant sources of nutrients to coastal lagoons, there are still limited studies evaluating separately nutrient fluxes driven by terrestrial groundwater discharge and lagoon water recirculation through sediments. In this study, we assess the relative significance of these sources in conveying dissolved inorganic nutrients (NO3 −, NH4 + and PO4 3−) to a coastal lagoon (La Palme lagoon; France, Mediterranean Sea) using concurrent water and radon mass balances. The recirculation of lagoon water through sediments represents a source of NH4 + (1900–5500 mol d−1) and PO4 3− (22–71 mol d−1), but acts as a sink of NO3 −. Estimated karstic groundwater-driven inputs of NO3 −, NH4 + and PO4 3− to the lagoon are on the order of 200–1200, 1–12 and 1.5–8.7 mol d−1, respectively. A comparison between the main nutrient sources to the lagoon (karstic groundwater, recirculation, diffusion from sediments, inputs from a sewage treatment plant and atmospheric deposition) reveals that the recirculation of lagoon water through sediments is the main source of both dissolved inorganic nitrogen (DIN) and phosphorous (DIP) to La Palme lagoon. These results are in contrast with several studies conducted in systems influenced by terrestrial groundwater inputs, where groundwater is often assumed to be the main pathway for dissolved inorganic nutrient loads. This work highlights the important role of lagoon water recirculation through permeable sediments as a major conveyor of dissolved nutrients to coastal lagoons and, thus, the need for a sound understanding of the recirculation-driven nutrient fluxes and their ecological implications to sustainably manage lagoonal ecosystems.
AB - Evaluating the sources of nutrient inputs to coastal lagoons is required to understand the functioning of these ecosystems and their vulnerability to eutrophication. Whereas terrestrial groundwater processes are increasingly recognized as relevant sources of nutrients to coastal lagoons, there are still limited studies evaluating separately nutrient fluxes driven by terrestrial groundwater discharge and lagoon water recirculation through sediments. In this study, we assess the relative significance of these sources in conveying dissolved inorganic nutrients (NO3 −, NH4 + and PO4 3−) to a coastal lagoon (La Palme lagoon; France, Mediterranean Sea) using concurrent water and radon mass balances. The recirculation of lagoon water through sediments represents a source of NH4 + (1900–5500 mol d−1) and PO4 3− (22–71 mol d−1), but acts as a sink of NO3 −. Estimated karstic groundwater-driven inputs of NO3 −, NH4 + and PO4 3− to the lagoon are on the order of 200–1200, 1–12 and 1.5–8.7 mol d−1, respectively. A comparison between the main nutrient sources to the lagoon (karstic groundwater, recirculation, diffusion from sediments, inputs from a sewage treatment plant and atmospheric deposition) reveals that the recirculation of lagoon water through sediments is the main source of both dissolved inorganic nitrogen (DIN) and phosphorous (DIP) to La Palme lagoon. These results are in contrast with several studies conducted in systems influenced by terrestrial groundwater inputs, where groundwater is often assumed to be the main pathway for dissolved inorganic nutrient loads. This work highlights the important role of lagoon water recirculation through permeable sediments as a major conveyor of dissolved nutrients to coastal lagoons and, thus, the need for a sound understanding of the recirculation-driven nutrient fluxes and their ecological implications to sustainably manage lagoonal ecosystems.
KW - Coastal lagoons
KW - Eutrophication
KW - Groundwater
KW - Nutrients
KW - Radon
KW - Recirculation
UR - http://www.scopus.com/inward/record.url?scp=85048537627&partnerID=8YFLogxK
U2 - 10.1016/j.scitotenv.2018.06.095
DO - 10.1016/j.scitotenv.2018.06.095
M3 - Article
C2 - 29920463
AN - SCOPUS:85048537627
VL - 642
SP - 764
EP - 780
JO - Science of The Total Environment
JF - Science of The Total Environment
SN - 0048-9697
ER -