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Updated: Apr 10, 2026

Dynamic Pore-scale Reservoir-condition Imaging of Reaction in Carbonates Using Synchrotron Fast Tomography
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Dynamic Pore-scale Reservoir-condition Imaging of Reaction in Carbonates Using Synchrotron Fast Tomography

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二酸化硫化物と炭酸塩溶解は,地質学的時間尺度におけるCO2の源として存在しています

Mark A Torres1, A Joshua West1, Gaojun Li2

  • 1Department of Earth Sciences, University of Southern California, Los Angeles, California 90089, USA.

Nature
|March 21, 2014
PubMed
まとめ

地球の長期の炭素循環の安定性は,これまで認識されていない二酸化炭素 (CO2) 源によって説明されうる:炭酸溶解と結合した硫化物の酸化が強化された. このプロセスは,潜在的に地質上昇によって引き起こされ,地質学的時間尺度におけるシリケート気象によるCO2消費のバランスをとるのに役立ちます.

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