The growth of planets like Earth through the accretion of pebble-sized material may produce water as pebbles settle through a H2-rich atmosphere and FeO reduces to Fe-rich metal and water, according to experiments of mafic lithologies melted in H2…
Source: Nature Geoscience | Springer Nature Limited
Nature Geoscience | Springer Nature Limited
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- Microbial extracellular residues are a major source of mineral-associated soil carbon
- Contrasting aerosol–cloud feedbacks across a warming Arctic
- Author Correction: The dominant role of temperature in seasonal ozone sensitivity changes in China
- Persistent contribution of biogenic emissions to lower stratospheric aerosols via global monsoon convections
- Experimental simulation of water formation on Earth from dry pebble rain
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