What Happens When Fertilizer Gets in Water?

Fertilizer that reaches rivers, lakes, or coastal waters triggers a cascade of biological and chemical changes that can turn a healthy waterway into something unrecognizable. Nitrogen and phosphorus, the same nutrients that make crops grow, fuel explosive growth of algae and aquatic plants when they enter water. That overgrowth depletes oxygen, poisons wildlife, degrades drinking water, and can produce toxins dangerous to people and animals. The process is well-documented and intensifying globally, but the full picture involves more than just green scum on a pond.

How Fertilizer Gets Into Water in the First Place

Crops use less of the fertilizer applied to them than most people assume. Research indicates that no more than about half of the nitrogen in fertilizer is directly taken up by the crops it is applied to. A portion leaches downward toward groundwater, while a large share ends up bound in the soil, where it slowly breaks down and releases nitrogen over the course of decades, continuing to feed into water long after the original application.1SN Applied Sciences. Fertilizers and nitrate pollution of surface and ground water: an increasingly pervasive global problem That means even if a farmer stopped fertilizing a field today, the soil beneath it would keep releasing nitrogen for years.

The two main routes into waterways are surface runoff and subsurface leaching. During heavy rain, water flowing over fields picks up dissolved nutrients and carries them into streams, rivers, and eventually lakes or the ocean. Subsurface drainage tiles, installed widely in agricultural regions to keep fields from waterlogging, act as express lanes for dissolved nitrate into streams. Erosion compounds the problem by carrying phosphorus attached to soil particles directly into surface water.

Farming is the dominant source, but it is not the only one. In urban and suburban areas, lawn fertilizer and pet waste are major nutrient contributors. A U.S. Geological Survey study of lakeshore properties in Wisconsin found that runoff from lawns carried high concentrations of nitrogen and phosphorus, and that the cumulative effect of many individual lawns could represent a large share of a lake’s total nutrient load.2U.S. Geological Survey Water-Resources Investigations Report. Effects of lawn fertilizer on nutrient concentration in runoff from lakeshore lawns, Lauderdale Lakes, Wisconsin Research on residential neighborhoods confirmed that nitrogen and phosphorus in irrigation-driven runoff from lawns is a meaningful contributor to nutrient loading in nearby surface waters.3PubMed Central. Managing urban runoff in residential neighborhoods: Nitrogen and phosphorus in lawn irrigation driven runoff

An important wrinkle in cities is that nitrogen and phosphorus travel by different pathways. A study of urban watersheds found that phosphorus moves primarily through stormwater runoff into surface water, while nitrogen additionally pollutes groundwater. That difference means managing the two nutrients requires different strategies: reducing nitrogen calls for cutting back on how much enters the watershed, while phosphorus management also needs to keep the nutrient from washing off lawns and into storm drains.4PubMed Central. Contrasting nitrogen and phosphorus budgets in urban watersheds and implications for managing urban water pollution

The Algal Bloom Sequence

Once nitrogen and phosphorus reach a body of water, they do exactly what they were designed to do on a farm: feed growth. Microscopic algae and cyanobacteria (sometimes called blue-green algae) respond to the nutrient influx by multiplying rapidly. During warm months especially, these nutrients fuel eutrophication, a state of high biological production that causes large algal blooms.5PubMed Central. The dead zones: oxygen-starved coastal waters The water turns green or brown, visibility drops, and a thick mat of organic material forms at or near the surface.

Which nutrient matters most depends on where you are. In freshwater lakes and rivers, phosphorus is generally the nutrient that limits how much algae can grow, so adding phosphorus has the biggest effect. In estuaries and coastal waters, nitrogen tends to be the primary driver of algal growth, though the picture is more complex: limitations can shift among nitrogen, phosphorus, and silicon depending on the salinity and the season.6AMBIO: A Journal of the Human Environment. Nitrogen in Aquatic Ecosystems This is why blanket solutions are tricky. Controlling phosphorus alone might clean up a lake but do little for a coastal bay, and vice versa.

Laboratory work has shown that common cyanobacteria can readily use agricultural fertilizer as a nitrogen source. In experiments with Microcystis aeruginosa, a species responsible for toxic blooms worldwide, the organism grew and photosynthesized just as well on urea (the most widely applied nitrogen fertilizer) as it did on standard nitrate.7PubMed. Effects of fertilizer-urea on growth, photosynthetic activity and microcystins production of Microcystis aeruginosa isolated from Dianchi Lake In other words, there is no buffer between what farmers spread on fields and what feeds toxic algae in a lake downstream. The fertilizer is the food.

Dead Zones and Oxygen Collapse

The real destruction begins not when algae bloom, but when they die. As the mass of organic material decays, bacteria that break it down consume enormous amounts of dissolved oxygen from the water. This accumulation of decaying matter encourages intense microbial activity that strips oxygen from bottom waters.8PubMed. Spreading dead zones and consequences for marine ecosystems When dissolved oxygen drops below the level that fish and shellfish need to survive, the area becomes what scientists call a hypoxic zone and the public calls a dead zone.

Dead zones are not a metaphor. Fish, crabs, shrimp, and bottom-dwelling organisms either flee the area or suffocate. Mobile species like adult fish can sometimes swim away, but larvae, eggs, and slow-moving creatures like mussels and worms cannot. The Gulf of Mexico dead zone, driven largely by fertilizer runoff from the Mississippi River basin, regularly spans thousands of square miles each summer. Similar zones exist in the Baltic Sea, the Chesapeake Bay, and hundreds of other coastal systems worldwide. The number of these zones has been growing for decades.

When the Bloom Is Toxic

Not all algal blooms are merely ugly and oxygen-depleting. Certain species of cyanobacteria produce potent toxins, and these harmful algal blooms (HABs) present a direct threat to anyone who comes in contact with contaminated water. Microcystins, produced by Microcystis and related genera, can damage the liver and are dangerous to humans, pets, and livestock. Dogs have died after swimming in water with active cyanobacterial blooms. Municipal water treatment plants sometimes struggle to remove these toxins, leading to drinking water advisories.

The same experiments that showed Microcystis grows well on urea also measured toxin production at different fertilizer concentrations, confirming that fertilizer-fed blooms are not merely cosmetic problems but potential public health hazards.7PubMed. Effects of fertilizer-urea on growth, photosynthetic activity and microcystins production of Microcystis aeruginosa isolated from Dianchi Lake Climate change is expected to make this worse. Projections for U.S. freshwaters indicate that harmful cyanobacterial bloom concentrations will increase, driven primarily by rising water temperatures, with additional contributions from changing nutrient transport patterns as hydrology shifts.9PubMed. Climate Change Impacts on Harmful Algal Blooms in U.S. Freshwaters: A Screening-Level Assessment Warmer water favors cyanobacteria over the less harmful green algae, so the blooms of the future may be more toxic, not just more frequent.

Nitrate in Drinking Water and Human Health

Fertilizer contamination of water creates direct health risks beyond toxic algae. Nitrate, the form of nitrogen most soluble in water, leaches readily through soil into groundwater, which is the drinking water source for millions of households, particularly in rural areas. When infants consume water high in nitrate, or formula prepared with that water, they can develop methemoglobinemia, sometimes called blue baby syndrome. The condition interferes with the blood’s ability to carry oxygen, causing a distinctive blue-gray skin color, lethargy, and, in severe cases, coma and death.10PubMed Central. Blue babies and nitrate-contaminated well water

The science here is real but more nuanced than the standard telling. A review of historical cases found that gastrointestinal infections in infants may have played a bigger role in many methemoglobinemia cases than previously thought, because gut inflammation independently triggers overproduction of nitric oxide, which can also cause the condition.11PubMed Central. Infantile methemoglobinemia: reexamining the role of drinking water nitrates That does not mean nitrate in water is safe; it means that in some cases attributed to well water, the real culprit may have been bacterial contamination working alongside the nitrate. For adults, chronic exposure to elevated nitrate in drinking water has been linked in epidemiological studies to increased risks of certain cancers, though the evidence is still debated. Regulatory limits for nitrate in public water supplies exist in most countries specifically because of these concerns.

Heavy Metals Along for the Ride

Nitrogen and phosphorus get the headlines, but fertilizers can carry unwanted passengers. Phosphate fertilizers are manufactured from mined phosphate rock, and that rock naturally contains cadmium, a toxic heavy metal. Repeated application of phosphate fertilizers over years can elevate cadmium concentrations in soil, and from there cadmium can migrate into groundwater.12PubMed Central. Cadmium in soils and groundwater: A review Cadmium is a known carcinogen and accumulates in the body over time, so even low-level chronic exposure matters. Some countries regulate the cadmium content of fertilizers, but standards vary widely.

Biodiversity Loss Beyond the Dead Zone

The ecological damage from fertilizer in water extends well beyond the oxygen-depleted areas that make the news. A global assessment of how nitrogen and phosphorus fertilizer used for major crops affects aquatic biodiversity found high spatial variability, with significant biodiversity losses occurring outside of the highest production regions.13The International Journal of Life Cycle Assessment. Global impacts of nitrogen and phosphorus fertiliser use for major crops on aquatic biodiversity In other words, you do not have to live next to an industrial farm belt to see the effects. Nutrients travel long distances through river networks, and the damage they cause can show up hundreds of miles downstream from the source.

Even in seemingly pristine environments, fertilizer-derived nutrients leave fingerprints. Research on alpine ponds found that although adding nitrogen and phosphorus elevated ambient nutrient concentrations several times over, the expected algal explosion did not always materialize because intense grazing by resident invertebrates and competition from bottom-growing algae kept phytoplankton in check. However, isotopic tracers confirmed that the added nitrogen was being incorporated into the food web, moving from algae up into herbivores, demonstrating that even where blooms are suppressed, the nutrient signal still enters the ecosystem.

When blooms do shift the species composition of the base of the food web, the consequences ripple upward. Cyanobacteria and certain green algae that thrive under high-nutrient conditions are poor producers of the highly unsaturated fatty acids that fish and other aquatic animals need.14PubMed Central. Fatty Acid Profiles and Production in Marine Phytoplankton So even when total biological production increases, the nutritional quality of that production for the rest of the food web goes down. More food, but worse food, which translates into poorer growth and reproduction for the animals that depend on it.

The Legacy Phosphorus Problem

One of the most frustrating aspects of fertilizer pollution is its persistence. Phosphorus that accumulates in lake and river sediments over decades of runoff does not simply disappear when you reduce the amount entering from the outside. This legacy phosphorus creates a persistent challenge for water quality restoration, because sediments can release stored phosphorus back into the water column, undermining nutrient reduction efforts.15PubMed. Legacy phosphorus dynamics in subtropical river sediments: Impacts of dredging and water column aeration status

The release is especially pronounced when dissolved oxygen at the sediment surface drops, a condition common during summer stratification in lakes or during low-flow conditions in rivers. Under low-oxygen conditions, chemical changes in the sediment liberate stored phosphorus into the water, feeding algal blooms from below even when surface runoff has been controlled.16PubMed. Internal Loading and Redox Cycling of Sediment Iron Explain Reactive Phosphorus Concentrations in Lowland Rivers This is why some lakes that have seen dramatic reductions in external phosphorus loading still suffer algal blooms for years or decades afterward. The sediment has become a reservoir that keeps paying out its stored nutrients. Managers have tried approaches like dredging contaminated sediments or injecting oxygen into bottom waters, but these are expensive and not always effective at the scale needed.

Fertilizer, Water, and Greenhouse Gases

A less obvious consequence of fertilizer in water is its contribution to climate change. When nitrogen-rich water flows through soils, groundwater, and into rivers and lakes, microbial processes convert some of that nitrogen into nitrous oxide, a greenhouse gas roughly 300 times more potent than carbon dioxide per molecule over a century. Global nitrous oxide emissions from inland waters roughly tripled between 1900 and 2010, climbing from about 0.4 to 1.3 teragrams of nitrogen per year. The increase was slow before 1950 and accelerated sharply afterward, tracking the explosion in synthetic fertilizer use. About half of total inland-water nitrous oxide emissions over that period came from nitrogen carried in by groundwater, with the remainder produced within the water bodies themselves, particularly in reservoirs.17PubMed Central. Inland Waters Increasingly Produce and Emit Nitrous Oxide

This creates an unpleasant feedback loop. Fertilizer-driven nutrient loading worsens algal blooms. Warming temperatures from greenhouse gas emissions make those blooms more frequent and more toxic. And the nutrient pollution itself generates additional greenhouse gases, nudging temperatures higher still.

The Economic Toll

Eutrophication is not just an ecological problem; it carries substantial financial costs. In the United States alone, the loss in property values near eutrophic waterways has been estimated at roughly $1.6 billion annually, making it the single largest economic impact. Recreational losses from degraded freshwaters add hundreds of millions per year. In Florida, harmful algal blooms have caused monthly revenue losses in the range of several million dollars from restaurants and lodging in affected coastal counties, and the healthcare costs of respiratory illnesses associated with toxic blooms add further burdens.18Resources, Conservation and Recycling. Valuing economic impact reductions of nutrient pollution from livestock waste Every excess kilogram of phosphorus runoff from livestock waste was calculated to cause about $74.50 in total economic losses. For context, millions of kilograms of excess phosphorus enter U.S. waters every year.

What Actually Helps

Solving fertilizer pollution in water requires working at every stage of the chain, from reducing what gets applied to fields and lawns, to intercepting nutrients before they reach water, to managing what is already there.

On the farm, precision agriculture technologies allow variable-rate application of fertilizers, adjusting the amount delivered to different parts of a field based on real-time data about soil conditions and crop needs. This reduces over-application and the nutrient runoff that follows.19PubMed Central. Application of Precision Agriculture Technologies for Sustainable Crop Production and Environmental Sustainability: A Systematic Review Cover crops, planted between cash crop seasons, are another proven tool. By keeping living roots in the soil year-round, they take up residual nitrogen that would otherwise leach into drainage water. Field studies have shown cover crops reducing nitrate losses through tile drains by roughly 27 to 72 percent, with more variable but still meaningful reductions in phosphorus.20Agriculture, Ecosystems & Environment. Cover crops control nitrogen and phosphorus transport from two agricultural watersheds at multiple measurement scales Legume cover crops carry the added benefit of fixing atmospheric nitrogen, which can partially replace synthetic fertilizer inputs without sacrificing yield.21Field Crops Research. Cover crops as a tool to reduce reliance on intensive tillage and nitrogen fertilization in conventional arable cropping systems

Between fields and waterways, riparian buffer zones, strips of vegetation along streams and rivers, act as filters. A European study estimated that buffer zones retain about a third of nitrogen and roughly two-thirds of phosphorus from surface runoff before it reaches rivers.22Knowledge and Management of Aquatic Ecosystems. Reduction of nitrogen and phosphorus loads to European rivers by riparian buffer zones The type of vegetation matters: multi-year monitoring in the UK found that willow buffer strips reduced total runoff by about 49 percent and suspended sediment loss by 44 percent, outperforming both deciduous woodland and grass strips, though all three were effective compared to no buffer.23PubMed Central. Impacts of different vegetation in riparian buffer strips on runoff and sediment loss

For homeowners, the implications are straightforward. Fertilizing your lawn less, or not at all, especially near any body of water, makes a measurable difference. Keeping grass clippings and leaves off hard surfaces like driveways and sidewalks prevents them from washing into storm drains. And if you live near a lake, the strip of natural vegetation between your yard and the shoreline might be the single most important feature protecting water quality.

Why Not All Waters Respond the Same Way

The textbook sequence of nutrients-to-blooms-to-dead-zones plays out dramatically in warm, slow-moving, nutrient-poor waters. But not every water body responds the same way. Fast-flowing rivers flush nutrients downstream before blooms can establish. Deep, cold lakes may resist surface blooms because their thermal structure keeps nutrients from concentrating in the sunlit zone. In alpine ponds, heavy grazing pressure from resident invertebrates can suppress the expected algal explosion even when nutrient concentrations are elevated several-fold, though the nutrients still enter the food web through other pathways.

Seasonal patterns also matter. In temperate regions, algal blooms tend to peak in summer, when warm water, long days, and low flow combine to create ideal conditions. In tropical systems, eutrophication can be a year-round phenomenon. And in estuaries, the limiting nutrient can shift from nitrogen to phosphorus and back depending on the season and the mix of freshwater and saltwater, making management especially complex.6AMBIO: A Journal of the Human Environment. Nitrogen in Aquatic Ecosystems

These differences explain why a policy that works beautifully for one lake may fail completely for a river delta or a coastal estuary. There is no one-size-fits-all fix because the underlying chemistry and biology are not one-size-fits-all either. The nutrient is the same; the receiving water is not.