Natural H2 exploration: tools and workflows to characterize a play

IF 2.7
Dan Lévy, Vincent Roche, Gabriel Pasquet, Valentine Combaudon, Ugo Geymond, Keanu Loiseau, Isabelle Moretti
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引用次数: 1

Abstract

Natural dihydrogen (H 2 ) exploration is now active in various countries, but tools and workflows that help to characterize prospective zones are still poorly defined. This review paper is dedicated to share our experience in characterizing H 2 plays based on exploration efforts carried out in many countries in Europe, North and South America, Africa, and Oceania between 2017 and 2023. We decided to focus on onshore exploration where three main reactions are generating H 2 : (i) redox reactions between Fe 2+ and H 2 O, (ii) radiolysis of water and, (iii) organic late maturation where H 2 comes from hydrocarbons. This leads to classify the H 2 generating rocks (H 2 _GR) into four types that seem us the more likely to be of economic interest: basic and ultrabasic rocks of oceanic/mantellic affinity (H 2 _GR1), iron-rich bearing sedimentary and intrusive rocks, (H 2 _GR2), radioactive continental rocks (H 2 _GR3) and organic matter-rich rocks (H 2 _GR4). For the pre-fieldwork, the workflow aims to target new promising areas for H 2 exploration. Cross-referencing the presence of H 2 _GR in the basement, classical geological-hydrodynamic features (fault, water source), and already-known H 2 occurrences at the surface remain essential but should be accompanied by remote sensing analyses to detect possible H 2 occurrences. For the fieldwork, the focus is made on gas and rocks. A discussion is led concerning the importance of punctual measurements and long-term monitoring of gas seepages, that allow to conclude on dynamics of H 2 leakage from depth through space and time. For the post-fieldwork, we present the most useful analytical tools to characterize H 2 gas seepages and the suspected H 2 _GR. The critical parameters to estimate the H 2 potential of a rock are the content in Fe 2+ /Fe tot (H 2 _GR1 and H 2 _GR2), the content of radioactive elements U, Th, K (H 2 _GR3), and the total organic content (H 2 _GR4). The hydrogen exploration is in its infancy and all the profession is attempting to define an automated and fast workflow. We are still far away from it due to a lack of data, yet this review presents a practical guide based on the current knowledge.
天然氢气勘探:表征油气藏的工具和工作流程
天然二氢(h2)勘探目前在许多国家都很活跃,但用于描述远景区的工具和工作流程仍然不明确。这篇综述文章致力于分享我们在2017年至2023年期间在欧洲、北美和南美、非洲和大洋洲许多国家开展的勘探工作的基础上,对h2油气藏进行特征描述的经验。我们决定将重点放在陆上勘探上,其中有三种主要反应产生h2:(i) Fe 2+和h2o之间的氧化还原反应,(ii)水的辐射分解,(iii)有机晚成熟,其中h2来自碳氢化合物。由此将生氢岩(h2 _GR)划分为四种最有经济价值的类型:具有海洋/地幔亲和作用的基性和超基性岩(h2 _GR1)、富铁沉积和侵入岩(h2 _GR2)、放射性陆相岩(h2 _GR3)和富有机质岩(h2 _GR4)。对于现场前的工作,工作流程旨在针对新的有前途的h2勘探区域。交叉参考基底中h2 _GR的存在、经典的地质-水动力特征(断层、水源)和地表已知的h2赋存仍然是必要的,但应辅以遥感分析,以探测可能的h2赋存。野外工作的重点是气体和岩石。讨论了气体渗漏的准时测量和长期监测的重要性,从而得出了从深度到空间和时间的氢气泄漏动力学的结论。在野外工作后,我们提出了最有用的分析工具来表征h2气体渗漏和可疑的h2 _GR。岩石中fe2 + / fet的含量(h2_gr1和h2_gr2)、放射性元素U、Th、K的含量(h2_gr3)和有机质的总含量(h2_gr4)是评价岩石氢电位的关键参数。氢勘探还处于起步阶段,所有的专业人士都试图定义一个自动化和快速的工作流程。由于缺乏数据,我们离它还很远,但这篇综述提出了一个基于现有知识的实用指南。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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