🌋 Turning Volcanic Rock Into a Carbon Sink
Basalt and olivine naturally react with CO2 to form solid carbonate minerals over geological time — enhanced weathering and mineral carbonation aim to speed that reaction up into a genuine, permanent carbon removal technology.
Crushed volcanic rock is spread across a field while atmospheric CO₂ molecules drift down, dissolve onto grain surfaces, and slowly turn dark basalt or olivine into a pale carbonate crust — a speeded-up view of enhanced weathering.
🔬 What It Demonstrates
Mineral carbonation: silicate rock reacting with dissolved CO₂ to lock carbon away as solid carbonate minerals, and how grain size, temperature and moisture each accelerate that reaction.
🎮 How to Use
Choose a rock type, crush it finer, warm it up and add rainfall to speed the reaction. Watch the reaction-rate multiplier and cumulative CO₂-captured counter respond as grains whiten with carbonate.
💡 Did You Know?
Iceland's Carbfix project injects CO₂-charged water into basalt formations and finds over 95% mineralises into solid rock within about two years — remarkably fast for a process that normally takes millennia.
Basalt and olivine naturally react with CO2 to form solid carbonate minerals over geological time — enhanced weathering and mineral carbonation aim to speed that reaction up into a genuine, permanent carbon removal technology.
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