This remarkable discovery was not the objective of the project, called Regalor. Instead, it aimed to determine the feasibility of methane production in the Lorraine region and to record the presence of traces of other gases. “Our original research was related to the study of carboniferous sediments in northeast France. This was important as Lorraine was one of France’s largest coal-producing regions,” Pironon said. […] Soon, the researchers will start taking measurements in three other boreholes at similar depths to understand if the hydrogen concentration remains high as you move laterally from the site of the original borehole. “If the concentration is similar, the next step, which is being discussed with the authorities, would be to drill a hole 3,000 meters deep to validate the evolution of the hydrogen concentration with depth,” he said. The deeper borehole could also throw up another surprise. “Besides knowing the level of hydrogen concentration, we will also know if hydrogen is present in dissolved form or in gaseous state at these depths,” Pironon said.
This study could also shed light on the source of this hydrogen. According to Pironon, there are two hypotheses, one of which is related to the presence of the mineral siderite. “Hydrogen could be produced by the reaction between water and siderite, which is made of iron carbonates. We consider that the siderite could be oxidized by water molecules to produce hydrogen. The oxygen then combines with iron to produce iron oxide.” According to Pironon, the other hypothesis relates its presence to the chemical processes that form coal, which, along with the release of methane, can also produce hydrogen.