Fertiliser runs off. The water turns green.
Algal blooms are a global water crisis and they start on a farm. Here is why it happens, what it costs the world, and what breaks the chain.
Every summer, coastlines and lakes across the world turn green. The Gulf of Mexico. Lake Erie. The Chinese coast. The Baltic, the Black Sea, the Adriatic. These aren't isolated incidents, they are the same problem, repeating globally, driven by the same cause: nutrients from agriculture entering water they were never supposed to reach.
A global problem, not a regional one
In many of the world's large lakes, summer algal blooms have grown more intense since the 1980s.² Research published in Nature Communications found that human nutrient inputs almost double the river catchment area with elevated algal growth, compared with a world without them — an area home to around 40% of the world's population.¹
This is not a problem contained to one sea or one continent. It follows the food system wherever it operates.
The mechanism is the same everywhere: nitrogen and phosphorus from agricultural fertilisers escape the fields they're applied to, enter waterways through rain and runoff, and arrive in rivers, lakes, and coastal waters where they act as a second fertiliser, feeding algae instead of crops.
Why fertiliser is necessary and why it escapes
Synthetic fertiliser isn't applied carelessly. Nitrogen and phosphorus are the core nutrients crops need to grow at the volumes modern agriculture requires, and in most soils, they can't be supplied naturally at that scale. Fertiliser fills the gap, and has been doing so since the Industrial Revolution, when reactive nitrogen production began to accelerate. By 2005, human activity was creating about 187 million tonnes of reactive nitrogen a year, from fertiliser, fossil fuels and farming combined.³
The problem is physical: nutrients applied to open fields don't stay where they're placed. Rain carries them. Irrigation systems distribute them beyond the root zone. They enter drainage channels, groundwater, streams, rivers, and eventually coastlines and lakes, arriving in water bodies where they behave exactly as they do on land, as a growth stimulus. For algae, an excess of nitrogen and phosphorus is an invitation to bloom.
From field to dead water, the chain
- Fertiliser applied to open fields worldwide
Nitrogen and phosphorus added to soil to grow crops at scale. Essential for modern food production volumes, and applied across hundreds of millions of hectares globally.
- Rain and runoff carry nutrients into waterways
Excess nutrients not absorbed by crops drain into streams, rivers, and groundwater. Agriculture is the dominant source of this nutrient pollution globally.
- Nutrients accumulate in lakes and coastal waters
Rivers deliver nitrogen and phosphorus into enclosed and semi-enclosed bodies of water worldwide, from Lake Erie to the Baltic to Chinese coastal seas. Many of these systems have slow water turnover, meaning nutrients accumulate over decades.
- Algae and cyanobacteria explode
Excess nutrients fuel rapid algal growth. In warm summer conditions, blooms develop within days, covering vast surface areas, turning water opaque, and producing toxins in many species.
- Oxygen disappears. Ecosystems collapse.
When blooms die and decompose, they strip oxygen from the water. The result: hypoxic and anoxic dead zones where almost nothing survives, a pattern now documented across the world's most productive coastal waters.
Why this is serious, three levels
Algal blooms are routinely described as an aesthetic problem, green water, closed beaches. The consequences run considerably deeper.
Human health — Toxic cyanobacteria produce compounds harmful to people and animals. Lake Erie alone supplies drinking water to 11 million people⁵, and its annual blooms require costly treatment and carry real health risks when untreated water is consumed.
Marine & freshwater ecosystems — Dead zones eliminate fish, invertebrates, and the food chains that depend on them. Biodiversity collapses. Fisheries that communities depend on contract or disappear entirely. The damage compounds year on year.
Economic & social cost — Fishing industries, tourism, property values, and drinking water treatment costs are all directly hit. In the United States alone, potential damages from freshwater eutrophication were estimated at about SEK 23 billion (US$2.2 billion) a year⁴, costs borne by communities, not the agricultural sector that generates the runoff.
Why reduction alone isn't enough
Many countries have made genuine progress reducing agricultural nutrient inputs over recent decades. And yet in many lakes the blooms keep coming. The reason is accumulation. Nutrients from past loading build up in sediments, and even where inputs have fallen they can keep feeding algae for years.
This is what makes the source so important. Reduction slows the loading rate. Elimination of the runoff pathway is structurally different, it stops the accumulation from continuing at all.
Where Freshborne sits in this picture
In our sealed hydroponic system, plants grow with their roots in a closed-loop nutrient solution, water and dissolved minerals circulating inside the pod, reused rather than discharged. There is no soil. There is no outdoor exposure. There is no runoff pathway. The nutrients that go in are either absorbed by the plant or remain in the system. They don't drain into a stream.
The mechanism that carries fertiliser into the world's water bodies simply isn't present in a closed hydroponic system. The chain has no first link to start from. That's not a marginal improvement on open-field agriculture, it's the structural removal of the problem's origin.
What it looks like if this model scales
The hypothesis is straightforward: if more of the world's fresh produce was grown in closed hydroponic systems, the nutrient load reaching waterways from that portion of agriculture would approach zero. Not reduced. Removed. The chain breaks at its first link, not by managing the runoff better, but by eliminating the conditions that create it.
Every growing system that moves indoors and into a closed loop is one more source of agricultural runoff that stops. The lakes and coastlines get more time to recover. The 40% of the world's population living near bloom-affected water gets cleaner water to live beside.
This is the synergy effect. Zero distance from harvest to your hand, no pesticides, closed-loop water, each of these is independently valuable. Together, they describe a model of food production that doesn't leak. And a food system that doesn't leak is the prerequisite for water that stops turning green.
Sources
- WWF: Övergödning
- WWF: Övergödning och algblomning i Östersjön
- Havs- och vattenmyndigheten: Övergödning
- Sveriges vattenmiljö
- Nature Communications (2025)
- Anderson et al., Estuaries (2002)
- American Scientist: The increasing problem of nutrient runoff on the coast
Footnotes
- Nature Communications (2025): https://www.nature.com/articles/s41467-025-57054-8 ↩
- Ho, Michalak & Pahlevan, Nature (2019) ↩
- Galloway et al., Science (2008) ↩
- Dodds et al., Environmental Science & Technology (2009) ↩
- US EPA, Lake Erie ↩