Acid Rain Risk Calculator

Enter your SO₂ emissions, NOₓ emissions, stack height, distance from source, and precipitation pH to estimate your acid deposition risk level. The calculator returns a Risk Index, projected soil acidification rate, ecosystem impact score, and a breakdown chart showing relative contributions of sulfur and nitrogen deposition.

kg/day

Daily sulfur dioxide emissions from the source (industrial plant, power station, etc.)

kg/day

Daily nitrogen oxides emissions from the source

m

Height of the emission stack in metres. Taller stacks disperse pollutants over a wider area.

km

Distance of the area of concern from the emission source

m/s

Mean wind speed in the region. Higher wind speeds disperse pollutants further.

mm/yr

Average annual rainfall in the region. Higher rainfall increases wet deposition.

Natural (unpolluted) rain pH is ~5.6. Values below 5.6 indicate existing acidification.

Type of ecosystem in the area of concern. Forests and wetlands are most sensitive to acid deposition.

Soils with high buffering capacity (e.g. calcareous) neutralise acid more effectively.

Results

Acid Rain Risk Index

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Risk Category

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Estimated SO₂ Deposition

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Estimated NOₓ Deposition

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Projected Precipitation pH

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Ecosystem Impact Score

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Soil Acidification Rate

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Deposition Contribution: SO₂ vs NOₓ

Frequently Asked Questions

What pH level defines acid rain?

Normal rainfall is slightly acidic at around pH 5.6 due to dissolved CO₂ forming carbonic acid. Rain is considered 'acid rain' when its pH falls below 5.0. Severely acidic rain can reach pH 4.0 or lower in heavily industrialised regions.

How do SO₂ and NOₓ contribute to acid rain?

Sulfur dioxide (SO₂) and nitrogen oxides (NOₓ) released from burning fossil fuels and industrial processes react with water vapour and oxygen in the atmosphere to form sulfuric acid (H₂SO₄) and nitric acid (HNO₃). These acids dissolve in precipitation, lowering its pH and causing acid deposition.

What is the difference between wet and dry acid deposition?

Wet deposition includes acid rain, sleet, fog, and snow that carry SO₂ and NOₓ acids to the ground. Dry deposition occurs when acidic particles and gases settle directly onto surfaces without precipitation. Both types damage ecosystems, though wet deposition typically accounts for a larger share of total acid load in high-rainfall regions.

Why does soil buffering capacity matter for acid rain risk?

Soils with high buffering capacity — such as those rich in calcium carbonate (limestone or chalk) — can neutralise incoming acid through chemical reactions, protecting plant roots and water quality. Sandy or granite-derived soils have little buffering ability, so they acidify faster and cause more severe ecological damage.

What ecosystems are most sensitive to acid deposition?

Forests, freshwater lakes, streams, and wetlands are most sensitive. Acid rain leaches essential nutrients like calcium and magnesium from soils, impairs root function, and mobilises toxic aluminium ions. Aquatic ecosystems are particularly vulnerable because many fish and amphibians cannot survive below pH 5.0.

How does stack height affect acid rain risk at ground level?

Taller stacks disperse pollutants higher into the atmosphere, spreading them over a larger geographic area rather than concentrating deposition near the source. While this reduces local risk, it can transport acid precursors across long distances and national borders — a key reason acid rain is considered a transboundary pollution problem.

What does the Risk Index score mean in this calculator?

The Risk Index is a composite score combining estimated SO₂ and NOₓ deposition rates, terrain sensitivity, soil buffering capacity, and projected pH change. Scores below 2 indicate low risk, 2–5 moderate risk, 5–8 high risk, and above 8 indicate critical risk requiring immediate mitigation measures.

What actions can reduce acid rain risk?

Effective measures include installing flue-gas desulfurisation (scrubbers) on industrial stacks to reduce SO₂, using catalytic converters and low-NOₓ burners to cut NOₓ emissions, switching to low-sulfur fuels or renewables, and applying agricultural lime to acidified soils to restore buffering capacity.

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