Formation of Hydrocarbons in the Presence of Native Iron under Upper Mantle Conditions: Experimental Constraints

Formation of Hydrocarbons in the Presence of Native Iron under Upper Mantle Conditions: Experimental Constraints Full article

Journal

Minerals
ISSN: 2075-163X

Output data

Year: 2020, Volume: 10, Number: 2, Article number : 88, Pages count : DOI: 10.3390/min10020088

Tags

mantle; fluid; hydrocarbons; subduction; experiment; native iron; gas chromatography-mass spectrometry

Authors

Sokol Alexander ^1,2 , Tomilenko Anatoly ¹ , Sokol Ivan ¹ , Zaikin Pavel ³ , Bul'bak Taras ¹

Affiliations

1	(Данные Web of science) RAS, IGM SB, Siberian Branch, VS Sobolev Inst Geol & Mineral, 3 Koptyug Ave, Novosibirsk, Russia
2	(Данные Web of science) Novosibirsk State Univ, 2 Pirogov Str, Novosibirsk, Russia
3	(Данные Web of science) RAS, NIOCh SB, Siberian Branch, NN Vorozhtsov Novosibirsk Inst Organ Chem, Novosibirsk, Russia

The formation of hydrocarbons (HCs) upon interaction of metal and metal-carbon phases (solid Fe, Fe3C, Fe7C3, Ni, and liquid Fe-Ni alloys) with or without additional sources of carbon (graphite, diamond, carbonate, and H2O-CO2 fluids) was investigated in quenching experiments at 6.3 GPa and 1000-1400 degrees C, wherein hydrogen fugacity (fH(2)) was controlled by the Fe-FeO + H2O or Mo-MoO2 + H2O equilibria. The aim of the study was to investigate abiotic generation of hydrocarbons and to characterize the diversity of HC species that form in the presence of Fe/Ni metal phases at P-T-fH(2) conditions typical of the upper mantle. The carbon donors were not fully depleted at experimental conditions. The ratio of H-2 ingress and consumption rates depended on hydrogen permeability of the capsule material: runs with low-permeable Au capsules and/or high hydrogenation rates (H2O-CO2 fluid) yielded fluids equilibrated with the final assemblage of solid phases at fH(2)(sample) <= fH(2)(buffer). The synthesized quenched fluids contained diverse HC species, predominantly light alkanes. The relative percentages of light alkane species were greater in higher temperature runs. At 1200 degrees C, light alkanes (C-1 approximate to C-2 > C-3 > C-4) formed either by direct hydrogenation of Fe3C or Fe7C3, or by hydrogenation of graphite/diamond in the presence of Fe3C, Fe7C3, and a liquid Fe-Ni alloy. The CH4/C2H6 ratio in the fluids decreased from 5 to 0.5 with decreasing iron activity and the C fraction increased in the series: Fe-Fe3C -> Fe3C-Fe7C3 -> Fe7C3-graphite -> graphite. Fe3C-magnesite and Fe3C-H2O-CO2 systems at 1200 degrees C yielded magnesiowustite and wustite, respectively, and both produced C-enriched carbide Fe7C3 and mainly light alkanes (C-1 approximate to C-2 > C-3 > C-4). Thus, reactions of metal phases that simulate the composition of native iron with various carbon donors (graphite, diamond, carbonate, or H2O-CO2 fluid) at the upper mantle P-T conditions and enhanced fH(2) can provide abiotic generation of complex hydrocarbon systems that predominantly contain light alkanes. The conditions favorable for HC formation exist in mantle zones, where slab-derived H2O-, CO2- and carbonate-bearing fluids interact with metal-saturated mantle.

Sokol A. , Tomilenko A. , Sokol I. , Zaikin P. , Bul'bak T.
Formation of Hydrocarbons in the Presence of Native Iron under Upper Mantle Conditions: Experimental Constraints

Minerals. 2020. V.10. N2. 88 . DOI: 10.3390/min10020088 WOS Scopus РИНЦ OpenAlex

Full text from publisher

Published online:

Jan 21, 2020

Web of science:	WOS:000522452900003
Scopus:	2-s2.0-85078801667
Elibrary:	43235211
OpenAlex:	W3003091961

DB	Citing
Web of science	2
Scopus	2
OpenAlex	5