In-situ abiogenic methane synthesis from diamond and graphite under geologically relevant conditions

Diamond and graphite are fundamental sources of carbon in the upper mantle, and their reactivity with H 2 -rich fluids present at these depths may represent the key to unravelling deep abiotic hydrocarbon formation. We demonstrate an unexpected high reactivity between carbons’ most common allotropes...

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Published inNature communications Vol. 12; no. 1; pp. 6387 - 5
Main Authors Peña-Alvarez, Miriam, Brovarone, Alberto Vitale, Donnelly, Mary-Ellen, Wang, Mengnan, Dalladay-Simpson, Philip, Howie, Ross, Gregoryanz, Eugene
Format Journal Article
LanguageEnglish
Published London Nature Publishing Group UK 04.11.2021
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Abstract Diamond and graphite are fundamental sources of carbon in the upper mantle, and their reactivity with H 2 -rich fluids present at these depths may represent the key to unravelling deep abiotic hydrocarbon formation. We demonstrate an unexpected high reactivity between carbons’ most common allotropes, diamond and graphite, with hydrogen at conditions comparable with those in the Earth’s upper mantle along subduction zone thermal gradients. Between 0.5-3 GPa and at temperatures as low as 300 °C, carbon reacts readily with H 2 yielding methane (CH 4 ), whilst at higher temperatures (500 °C and above), additional light hydrocarbons such as ethane (C 2 H 6 ) emerge. These results suggest that the interaction between deep H 2 -rich fluids and reduced carbon minerals may be an efficient mechanism for producing abiotic hydrocarbons at the upper mantle. Using diamond anvil cell and high temperature experiments, this work proves that the interaction between deep hydrogen rich fluids and reduced carbon minerals may be an efficient mechanism for producing abiotic hydrocarbons at the upper mantle’s pressures and temperatures.
AbstractList Using diamond anvil cell and high temperature experiments, this work proves that the interaction between deep hydrogen rich fluids and reduced carbon minerals may be an efficient mechanism for producing abiotic hydrocarbons at the upper mantle’s pressures and temperatures.
Diamond and graphite are fundamental sources of carbon in the upper mantle, and their reactivity with H2-rich fluids present at these depths may represent the key to unravelling deep abiotic hydrocarbon formation. We demonstrate an unexpected high reactivity between carbons' most common allotropes, diamond and graphite, with hydrogen at conditions comparable with those in the Earth's upper mantle along subduction zone thermal gradients. Between 0.5-3 GPa and at temperatures as low as 300 °C, carbon reacts readily with H2 yielding methane (CH4), whilst at higher temperatures (500 °C and above), additional light hydrocarbons such as ethane (C2H6) emerge. These results suggest that the interaction between deep H2-rich fluids and reduced carbon minerals may be an efficient mechanism for producing abiotic hydrocarbons at the upper mantle.Diamond and graphite are fundamental sources of carbon in the upper mantle, and their reactivity with H2-rich fluids present at these depths may represent the key to unravelling deep abiotic hydrocarbon formation. We demonstrate an unexpected high reactivity between carbons' most common allotropes, diamond and graphite, with hydrogen at conditions comparable with those in the Earth's upper mantle along subduction zone thermal gradients. Between 0.5-3 GPa and at temperatures as low as 300 °C, carbon reacts readily with H2 yielding methane (CH4), whilst at higher temperatures (500 °C and above), additional light hydrocarbons such as ethane (C2H6) emerge. These results suggest that the interaction between deep H2-rich fluids and reduced carbon minerals may be an efficient mechanism for producing abiotic hydrocarbons at the upper mantle.
Diamond and graphite are fundamental sources of carbon in the upper mantle, and their reactivity with H2-rich fluids present at these depths may represent the key to unravelling deep abiotic hydrocarbon formation. We demonstrate an unexpected high reactivity between carbons’ most common allotropes, diamond and graphite, with hydrogen at conditions comparable with those in the Earth’s upper mantle along subduction zone thermal gradients. Between 0.5-3 GPa and at temperatures as low as 300 °C, carbon reacts readily with H2 yielding methane (CH4), whilst at higher temperatures (500 °C and above), additional light hydrocarbons such as ethane (C2H6) emerge. These results suggest that the interaction between deep H2-rich fluids and reduced carbon minerals may be an efficient mechanism for producing abiotic hydrocarbons at the upper mantle.Using diamond anvil cell and high temperature experiments, this work proves that the interaction between deep hydrogen rich fluids and reduced carbon minerals may be an efficient mechanism for producing abiotic hydrocarbons at the upper mantle’s pressures and temperatures.
Diamond and graphite are fundamental sources of carbon in the upper mantle, and their reactivity with H 2 -rich fluids present at these depths may represent the key to unravelling deep abiotic hydrocarbon formation. We demonstrate an unexpected high reactivity between carbons’ most common allotropes, diamond and graphite, with hydrogen at conditions comparable with those in the Earth’s upper mantle along subduction zone thermal gradients. Between 0.5-3 GPa and at temperatures as low as 300 °C, carbon reacts readily with H 2 yielding methane (CH 4 ), whilst at higher temperatures (500 °C and above), additional light hydrocarbons such as ethane (C 2 H 6 ) emerge. These results suggest that the interaction between deep H 2 -rich fluids and reduced carbon minerals may be an efficient mechanism for producing abiotic hydrocarbons at the upper mantle. Using diamond anvil cell and high temperature experiments, this work proves that the interaction between deep hydrogen rich fluids and reduced carbon minerals may be an efficient mechanism for producing abiotic hydrocarbons at the upper mantle’s pressures and temperatures.
Diamond and graphite are fundamental sources of carbon in the upper mantle, and their reactivity with H 2 -rich fluids present at these depths may represent the key to unravelling deep abiotic hydrocarbon formation. We demonstrate an unexpected high reactivity between carbons’ most common allotropes, diamond and graphite, with hydrogen at conditions comparable with those in the Earth’s upper mantle along subduction zone thermal gradients. Between 0.5-3 GPa and at temperatures as low as 300 °C, carbon reacts readily with H 2 yielding methane (CH 4 ), whilst at higher temperatures (500 °C and above), additional light hydrocarbons such as ethane (C 2 H 6 ) emerge. These results suggest that the interaction between deep H 2 -rich fluids and reduced carbon minerals may be an efficient mechanism for producing abiotic hydrocarbons at the upper mantle.
Diamond and graphite are fundamental sources of carbon in the upper mantle, and their reactivity with H 2 -rich fluids present at these depths may represent the key to unravelling deep abiotic hydrocarbon formation. We demonstrate an unexpected high reactivity between carbons’ most common allotropes, diamond and graphite, with hydrogen at conditions comparable with those in the Earth’s upper mantle along subduction zone thermal gradients. Between 0.5-3 GPa and at temperatures as low as 300 °C, carbon reacts readily with H 2 yielding methane (CH 4 ), whilst at higher temperatures (500 °C and above), additional light hydrocarbons such as ethane (C 2 H 6 ) emerge. These results suggest that the interaction between deep H 2 -rich fluids and reduced carbon minerals may be an efficient mechanism for producing abiotic hydrocarbons at the upper mantle.
Diamond and graphite are fundamental sources of carbon in the upper mantle, and their reactivity with H -rich fluids present at these depths may represent the key to unravelling deep abiotic hydrocarbon formation. We demonstrate an unexpected high reactivity between carbons' most common allotropes, diamond and graphite, with hydrogen at conditions comparable with those in the Earth's upper mantle along subduction zone thermal gradients. Between 0.5-3 GPa and at temperatures as low as 300 °C, carbon reacts readily with H yielding methane (CH ), whilst at higher temperatures (500 °C and above), additional light hydrocarbons such as ethane (C H ) emerge. These results suggest that the interaction between deep H -rich fluids and reduced carbon minerals may be an efficient mechanism for producing abiotic hydrocarbons at the upper mantle.
ArticleNumber 6387
Author Donnelly, Mary-Ellen
Howie, Ross
Peña-Alvarez, Miriam
Dalladay-Simpson, Philip
Brovarone, Alberto Vitale
Gregoryanz, Eugene
Wang, Mengnan
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  organization: Centre for Science at Extreme Conditions and School of Physics and Astronomy, University of Edinburgh, Center for High Pressure Science and Technology Advanced Research (HPSTAR), Key Laboratory of Materials Physics, Institute of Solid State Physics, Chinese Academy of Sciences
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Keywords Geochemistry
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Snippet Diamond and graphite are fundamental sources of carbon in the upper mantle, and their reactivity with H 2 -rich fluids present at these depths may represent...
Diamond and graphite are fundamental sources of carbon in the upper mantle, and their reactivity with H -rich fluids present at these depths may represent the...
Diamond and graphite are fundamental sources of carbon in the upper mantle, and their reactivity with H2-rich fluids present at these depths may represent the...
Diamond and graphite are fundamental sources of carbon in the upper mantle, and their reactivity with H 2 -rich fluids present at these depths may represent...
Using diamond anvil cell and high temperature experiments, this work proves that the interaction between deep hydrogen rich fluids and reduced carbon minerals...
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SubjectTerms 704/2151/209
704/2151/330
Allotropy
Carbon
Carbon sources
Diamond anvil cells
Earth mantle
Earth Sciences
Ethane
Geochemistry
Graphite
High temperature
High temperature effects
Humanities and Social Sciences
Hydrocarbons
Methane
Mineralogy
Minerals
multidisciplinary
Science
Science (multidisciplinary)
Sciences of the Universe
Subduction (geology)
Upper mantle
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Title In-situ abiogenic methane synthesis from diamond and graphite under geologically relevant conditions
URI https://link.springer.com/article/10.1038/s41467-021-26664-3
https://www.ncbi.nlm.nih.gov/pubmed/34737292
https://www.proquest.com/docview/2593361115
https://www.proquest.com/docview/2594293396
https://hal.sorbonne-universite.fr/hal-03449139
https://pubmed.ncbi.nlm.nih.gov/PMC8569197
https://doaj.org/article/265ddb38d697452d810facb738dc6690
Volume 12
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