Natural hydrogen potential and basaltic alteration in the Asal–Ghoubbet rift, Republic of Djibouti

Abstract

The Asal–Ghoubbet active rift in the Republic of Djibouti is a site of interest for geothermal energy and natural hydrogen, and previous studies have indicated that dihydrogen (H2) emanates from this rift. However, the well-known serpentinization reaction does not appear to be the main mechanism generating H2 at this site. Rather, the H2 is generated as follows: (1) by alteration of basaltic lava at depth via reaction with seawater flowing from Ghoubbet Bay towards Lake Asal; (2) by simple degassing of the volcanic chamber located a few kilometers below the Fiale Caldera in the rift axis; or (3) as a result of pyritization processes via the oxidation of H2S. Analysis of microorganisms did not indicate any production or consumption of H2, CO2, or CH4; therefore, it is unlikely that microorganisms affected H2 gas contents measured at the surface. However, air contamination at fumaroles is typically considerable and may limit interpretation of such processes. 
 Drill cuttings from the Fiale 1 (F1) and Gale le Goma 1 (Glc1) wells (located on the inner and outer rift margins, respectively) were analyzed to determine where H2 is generated. Total rock analyses indicated distinct zones at depths of 464 m and 280 m for F1 and Glc1, respectively, representing the boundary between the Asal and Stratoïd Basalts. 57Fe Mössbauer analyses show a decrease in the percentage of Fe3+ at depth, indicating that Fe2+-rich material, particularly in the Stratoïd Basalts, may be a source of H2.
 Based on well data from the rift center and the outer rift margin, it is evident that H2 is present at the surface in the rift axis and that this area offers good remnant potential because of the presence of Fe-rich chlorite. Conversely, few H2 emissions were measured at the surface on the outer rift margins, although well data showed some H2 (~0.25%) at depth. The presence of a cap rock in the rift axis has not yet been proven; however, the high loss on ignition and the mineralogy in well Glc1 may indicate that the rocks are sufficiently altered to offer potential as a seal. If so, the rift margins would offer greater exploration potential than the rift center. 

Geothermal ecosystems on Mt. Erebus, Antarctica, support diverse and taxonomically novel biota

“…Erebus (11,67). However, at the Asal-Ghoubbet site, no consumption of CO2 or H2 in aerobic or anaerobic incubations of the soils was observed (66). Even though we observed an enrichment in predicted aerobic ammonia oxidation at Exposed sites, (Fig 7), ASV_1 was not one of the 40 ASVs predicted to be involved in this functional category (all predicted ammonia oxidisers were from the classes Nitrososphaera or Nitrocosmicus of phylum Crenarchaeota).…”

“…This class is common in marine habitats (62), with members known for being autotrophic ammonia oxidizers (AOA); some deep-branching, thermophilic members lack the genes needed for ammonia oxidation (63)(64)(65). In particular, the order SCGC AB-179-E04, although under-studied, was recently found in high abundances (up to 79% of the prokaryotic community) in CO2 and H2-rich fumarolic vents from Asal-Ghoubbet rift, Republic of Djibouti (66). This is striking because CO2 and H2 have both been reported to be produced in high concentrations by Mt.…”

Natural H2 exploration: tools and workflows to characterize a play

“…In addition to the outcrops, some countries (e.g., Australia and the USA) provide free access to their core libraries for both researchers and operators, particularly for the cores from previous drilling programs. When well data are available, cores or cuttings are ideal for obtaining a complete description of the generating interval, like the description of the cuttings in the Asal Rift and the identification of an H 2 system (Pasquet et al, 2023). They also avoid the effects of nearsurface weathering, which can affect the Fe 2+ /Fe 3+ ratio (Fig.…”