Page 3: Research news on carbon mineralization

Carbon mineralization, in the context of carbon sequestration topics, refers to the suite of geochemical and geomicrobiological processes by which inorganic carbon, typically as dissolved CO₂ or bicarbonate, is transformed into stable carbonate minerals such as calcite, magnesite, or siderite. It proceeds via reactions between CO₂-bearing fluids and metal cations (e.g., Ca²⁺, Mg²⁺, Fe²⁺) derived from silicate or oxide minerals, often involving dissolution–precipitation mechanisms controlled by pH, alkalinity, temperature, and fluid–rock ratios. Carbon mineralization is studied as a thermodynamically favorable, long-term CO₂ storage pathway in natural and engineered subsurface systems.

Fig trees convert atmospheric CO₂ to stone, research reveals

Some species of fig trees store calcium carbonate in their trunks—essentially turning themselves (partially) into stone, new research has found. The team of Kenyan, U.S., Austrian, and Swiss scientists found that the trees ...

Proposed experiment could clarify origin of Martian methane

Over the past decade, the Curiosity rover has repeatedly detected methane on the surface of Mars. This gas is often produced by microbes, so it could herald the presence of life on the red planet. But skeptics have postulated ...

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