🌊 Ocean Acidification Simulator

Watch CO2 dissolve into seawater, shift carbonate chemistry, and threaten marine life in real time

🤔 What Is Ocean Acidification?

The ocean absorbs about 30% of human CO2 emissions, making it Earth's largest carbon sink. When CO2 dissolves in seawater it forms carbonic acid (H2CO3), which releases hydrogen ions (H+) that lower the pH. Since the Industrial Revolution, ocean pH has dropped from 8.2 to 8.1 — a 26% increase in acidity. This threatens coral reefs, shellfish, and entire marine food chains that depend on calcium carbonate.

Why does this matter? Coral reefs support 25% of all marine species. When pH drops and aragonite saturation falls below 1.0, shell-building organisms can no longer form protective structures — their shells literally dissolve. At current emission rates, ocean pH could reach 7.8 by 2100, a level not seen in 14 million years. This simulator lets you explore the chemistry driving these changes.

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Coral Reefs
Bleaching and skeletal dissolution under acidic conditions
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Shell Organisms
Pteropods and mollusks losing protective shells
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Carbonate Chemistry
CO2 + H2O reactions shifting ocean equilibrium
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Temperature Coupling
Warming reduces CO2 solubility but accelerates reactions
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Food Chains
Disruption cascading from plankton to apex predators
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Human Impact
Fisheries, tourism, and coastal protection at risk

🚀 Quick Start

⚙️ Emission & Environment

📋 Event Log

Simulator ready. Press Start to begin ocean chemistry simulation...
pH Level: 8.10
CO2 (ppm): 420
Aragonite Sat. (Omega): 3.50
Coral Health: 100%
Shell Dissolution: 0.0%
DIC: 2050 umol/kg