Eutrophication
Eutrophication refers to the phenomenon of increased production of organic matter, primarily nitrogen and phosphorus, in aquatic systems (Nixon, 1995). Eutrophication can be caused by human activities (e.g. sewage outfall, agricultural runoff, aquaculture) and may result in secondary environmental effects such as algal blooms and fish kills (NOAA, 2007; UNEP, 2015). Given the complex structure and functioning of ecosystems, and the multitude of pressures they face (Cloern, 2001), the precise definition of eutrophication remains to be established (Pannard et al., 2024).
Primary reference(s)
Cloern, J., 2001. Our evolving conceptual model of the coastal eutrophication problem. Marine Ecology Progress Series, 210, 223–253.
Nixon, S. W., 1995. Coastal marine eutrophication: A definition, social causes, and future concerns. Ophelia, 41(1), 199–219.
NOAA, 2007. National Estuarine Eutrophication Assessment: Update. National Centers for Coastal Ocean Science, National Oceanic and Atmospheric Administration (NOAA). Accessed 21 January 2025.
Pannard, A., Souchu, P., Chauvin, C., Delabuis, M., Gascuel‐Odoux, C., Jeppesen, E., Le Moal, M., Ménesguen, A., Pinay, G., Rabalais, N. N., and Souchon, Y., 2024. Why are there so many definitions of eutrophication? Ecological Monographs, p.e1616.
UNEP, 2015. Mediterranean Action Plan. Report of the Online Groups on Eutrophication, Contaminants and Marine Litter. United Nations Environment Programme (UNEP). Accessed 21 January 2025.
Annotations
Additional scientific description
Eutrophication results from the overabundance of nutrients, primarily nitrogen and phosphorus, introduced into aquatic environments from sources such as sewage outfalls and agricultural runoff (Akinnawo, 2023). This nutrient loading accelerates the growth of algae and other aquatic vegetation. The subsequent degradation of organic matter depletes dissolved oxygen, leading to oxygen deficiency. This hypoxia has multiple cascading effects on the ecosystem, including the death of aquatic species, toxin production, and changes in aquatic community structure (Chrislock et al., 2013).
Where there are narrow continental shelves, certain wind conditions can bring nutrient-rich, oxygen-poor water into coastal zones, producing hypoxic (low-oxygen) or even anoxic (no-oxygen) conditions in which eutrophication can develop (Altieri, 2019). Such conditions have been observed on the western coasts of the American continent immediately north and south of the equator, the western coast of sub-Saharan Africa, and the western coast of the Indian subcontinent (United Nations, 2021). Dead zones and low-oxygen areas caused by eutrophication and climate change can have severe environmental, economic, and social consequences (United Nations, 2021).
Metrics and numeric limits
There is currently no single, universal set of numeric limits for eutrophication. However, a combination of metrics, together with an understanding of local ecosystem characteristics, can facilitate the assessment of eutrophication risk and inform appropriate management strategies. Key indicators include:
- Chlorophyll-a concentration (µg L⁻¹): used as a proxy for phytoplankton biomass.
- Dissolved oxygen percentage saturation: used to determine whether water is supersaturated or undersaturated in oxygen; as oxygen solubility depends on temperature and salinity, these parameters should also be measured.
- Nutrient concentrations (µM dm⁻³) and nutrient (atomic) ratios: deviations from the 'Redfield' nitrogen-to-phosphorus (N:P) ratio and shortages of silicate relative to nitrogen and phosphorus can provide critical insights.
Key relevant UN convention / multilateral treaty
The UNECE Convention on Long-range Transboundary Air Pollution adopted the Protocol to Abate Acidification, Eutrophication and Ground-level Ozone in Gothenburg, Sweden, on 30 November 1999. The Protocol sets national emission ceilings from 2010 to 2020 for four pollutants: sulphur (SO₂), nitrogen oxides (NOₓ), volatile organic compounds (VOCs), and ammonia (NH3).
Sustainable Development Goal (SDG) Target 6.3 (water quality) and SDG Target 14.1 (marine pollution) directly address nutrient pollution from land-based sources, aligning eutrophication with the broader global sustainability agenda. (https://sdgs.un.org/2030agenda). Although these are not binding, they provide useful guidance.
Drivers
While there are some causes of natural eutrophication (Knight, 2021), the primary drivers stem from human activity. Untreated or inadequately treated sewage remains a major source of nitrogen and phosphorus, often originating from municipal wastewater or agricultural runoff containing human waste (Akinnawo, 2023). Biomass processing industries such as food processing, animal feed production, and pulp and paper mills also contribute organic matter and nutrient-rich wastewater when not properly managed (Tusseau-Vuillemin, 2001).
Intensive agricultural practices, particularly overuse of fertilisers and manure, as well as soil erosion due to cultivation techniques, contribute to nutrient runoff into water bodies (Akinnawo, 2023). Aquaculture can also contribute to eutrophication through nutrient-rich feed and fish waste (Talbot, 1994). Atmospheric deposition of nitrogen oxides (NOₓ) from fossil fuel combustion may increase nutrient enrichment in water bodies via precipitation (Paerl, 1995).
Land-use changes-including urbanisation, deforestation, drainage of wetlands, removal of riparian vegetation, and damming of rivers-disrupt natural nutrient cycling and filtration, increasing nutrient loads in aquatic systems (Rodríguez-Gallego et al., 2017).
Environmental stressors such as rising sea surface temperatures and increased salinity can intensify stratification, limiting vertical mixing and promoting algal growth (Coffey et al., 2018). Flooding can flush fertilisers and sewage into water bodies, increasing nutrient loads (Nazari-Sharabian et al., 2018). Forest fires also contribute to eutrophication by releasing nitrogen oxides into the atmosphere, which are later deposited over water bodies (Paerl, 1995).
Impacts
Eutrophication causes cascading effects on aquatic ecosystems. Nutrient enrichment favours fast-growing phytoplankton, leading to shifts in phytoplankton community structure (Chrislock et al., 2013). Reduced light penetration and algal overgrowth result in the loss of seagrass habitats essential for marine biodiversity (Pick, 1991). Oxygen depletion from decaying biomass leads to hypoxic or anoxic conditions, causing fish kills and harming benthic organisms (Akinnawo, 2023).
These changes disrupt food webs, reduce biodiversity, and compromise the overall health and resilience of aquatic ecosystems (Chrislock et al., 2013).
Eutrophication acts as a trigger point for a series of secondary hazards, further exacerbating the problem. As organic matter from algal blooms decomposes under anoxic conditions, it releases toxic gases such as hydrogen sulfide, which can affect aquatic life and pose a serious threat to human health (Dunnette et al., 1985). Additionally, eutrophication creates ideal conditions for the accumulation of persistent organic pollutants (POPs) and heavy metals. These pollutants, originating from various sources including industrial waste, bind to organic particles in the water and become incorporated into the food web. As they move up the food chain through a process known as biomagnification, their concentrations increase, posing long-term ecological and human health risks (Larsson et al., 2000).
The consequences of eutrophication extend beyond ecological damage. Certain algal blooms can produce toxins such as microcystins and saxitoxins that pose a public health risk to humans (Gody et al., 2019; Brooks et al., 2016). These toxins can also sicken or kill animals within the aquatic ecosystem and threaten human health through contaminated drinking water or seafood consumption (Brooks et al., 2016). Additionally, fish kills and decreased fishery productivity can lead to economic losses for commercial and recreational fisheries (Kerr et al., 1992). Finally, eutrophication can render water bodies unsuitable for recreational activities such as swimming and boating due to the unpleasant aesthetics associated with algal blooms (Priskin, 2008).
Multi-hazard context
The figure below summarises common interactions between eutrophication and other hazards. This information should be used with caution and not be solely relied upon in disaster risk management, particularly as some interactions may not have been included. Note that hazardous events occurring together or locally in space or time may not necessarily cause, amplify, or be otherwise related to each other. Specific examples of the multi-hazard context can be found in the ‘Hazard drivers’ and ‘Impacts’ sections above.
Multi-hazard diagram
Risk Management
Risk management combines source control (e.g. wastewater treatment), in-system measures (e.g. biomanipulation), and policy (e.g. effluent standards). Context-specific approaches are essential (UNESCO, 2015).
Monitoring
The section and the table below offer an overview of monitoring for eutrophication. This information can be used for forecasting within a national early warning system (EWS). Since EWS capacities and processes differ across countries, the most current and specific information regarding EWS should be obtained from the appropriate national or regional agency/authority responsible for disaster management.
| Which institution(s) produce(s) disaster risk data/information? | Environmental agencies.
|
| How is the hazard monitored/observed/forecast? | Monitoring the concentrations of nitrogen and phosphorus in water bodies is a critical early warning tool for eutrophication, despite the lack of universally standardised thresholds across different regions. Thresholds can vary depending on factors such as water depth, flow, and natural background levels. Significant and sustained increases in nutrient levels can serve as a red flag, prompting further investigation (Yang et al., 2008). A decline in water clarity suggests an increase in suspended algae and organic matter, a hallmark of eutrophication (Pick, 1991). Technological advancements can facilitate this assessment; for example, ocean colour remote sensing allows for the monitoring of algal blooms over vast areas, providing a large-scale perspective on potential eutrophication risks (Banks et al., 2012). A sudden drop in dissolved oxygen levels at night can serve as a critical early warning. This 'night-time oxygen sag' indicates an intensified imbalance between oxygen production and consumption, potentially leading to hypoxic or anoxic events where aquatic life struggles to survive. This imbalance can be further exacerbated by the decomposition of organic matter from algal blooms (Miranda et al., 2001). Biodiversity loss is another crucial early warning sign. Eutrophication can favour certain species, particularly nuisance or invasive algae, while displacing others that are more sensitive to nutrient enrichment (Rosset et al., 2014). In some cases, ecosystems may exhibit multiple critical mutation points, indicating that degradation and collapse due to eutrophication can occur rapidly (Wang et al., 2012). |
References
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Altieri, A.H., Diaz, R.J., 2019. Dead zones: oxygen depletion in coastal ecosystems. In World seas: An environmental evaluation (pp. 453-473). Academic Press. DOI: 10.1016/B978-0-12-805052-1.00021-8. Accessed 21 January 2025.
Banks, A.C., Prunet, P., Chimot, J., Pina, P., Donnadille, J., Jeansou, E., Lux, M., et al., 2012. A satellite ocean color observation operator system for eutrophication assessment in coastal waters. Journal of Marine Systems 94 (2012): S2-S15. DOI: 10.1016/j.jmarsys.2011.11.001. Accessed 21 January 2025.
Brooks, B.W., Lazorchak, J.M., Howard, M.D., et al., 2016. Are harmful algal blooms becoming the greatest inland water quality threat to public health and aquatic ecosystems? Environ Toxicol Chem. 35(1):6-13. DOI: 10.1002/etc.3220. Accessed 21 January 2025.
Chislock, M.F., Doster, E., Zitomer, R.A., Wilson, A.E., 2013. Eutrophication: Causes, Consequences, and Controls in Aquatic Ecosystems. Nature Education Knowledge 4(4):10. Accessed 21 January 2025.
Coffey R., Paul M., Stamp J., Hamilton A., Johnson T., 2018. A Review of Water Quality Responses to Air Temperature and Precipitation Changes 2: Nutrients, Algal Blooms, Sediment, Pathogens. J Am Water Resour Assoc. 20;55(4):844-868. DOI: 10.1111%2F1752-1688.12711. Accessed 21 January 2025.
Dunnette, D.A. et al., 1985. The source of hydrogen sulfide in anoxic sediment. Water Research, 19(7), 875-884. DOI: 10.1016/0043-1354(85)90146-0. Accessed 21 January 2025.
FAO, 2018. Nutrient flows and associated environmental impacts in livestock supply chains: Guidelines for assessment (Version 1). Livestock Environmental Assessment and Performance (LEAP) Partnership. Rome, FAO. 196 pp. Accessed 21 January 2025.
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Kerr, S.R., Ryder, R.A., 1992. Effects of cultural eutrophication on coastal marine fisheries: a comparative approach. In Marine Coastal Eutrophication (pp. 599-614). Elsevier. DOI: 10.1016/B978-0-444-89990-3.50054-7. Accessed 21 January 2025.
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Nazari-Sharabian, M., Ahmad, S., Karakouzian, M., 2018. Climate Change and Eutrophication: A Short Review. Engineering, Technology and Applied Science Research, 8(6), 3668-3672. Accessed 21 January 2025.
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Pannard, A., Souchu, P., Chauvin, C., Delabuis, M., Gascuel‐Odoux, C., Jeppesen, E., Le Moal, M., Ménesguen, A., Pinay, G., Rabalais, N.N., Souchon, Y., 2024. Why are there so many definitions of eutrophication?. Ecological monographs, p.e1616.
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