马里卡(巴西),改变氢勘探模式的新天然氢矿

IF 8.3 2区 工程技术 Q1 CHEMISTRY, PHYSICAL
Alain Prinzhofer , Christophe Rigollet , Nicolas Lefeuvre , Joao Françolin , Paulo Emilio Valadão de Miranda
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引用次数: 0

摘要

马里卡市(巴西里约热内卢州)的氢气勘探表明,重新激活的断层释放出大量氢气和氦气。土壤中的气体浓度和模拟气体通量是迄今为止世界上测量到的最密集的气体通量之一。这次勘探显示了氢微渗的新地表表现形式,沿着重新激活的大型构造事故观察到了氢微渗,而不是 "仙女圈","仙女圈 "是地壳形成中氢系统最常见的代表。马里卡的地质由新近纪变质岩组成,没有任何关于易产生氢的地层的文献记载,因此是研究天然氢的一个非常新的领域。研究结果表明,在 80 厘米深处插入的普通探测器存在系统性的氢饱和现象,而且随着时间的推移,氢不断补充,没有弛豫时间。此外,正氦异常与土壤氢气有关,证明存在来自地下深层的气体通量。这降低了地表氢气测量结果被误读的风险,因为钻头变质或表层生物活动诱发氢气伪影的可能性始终存在。这些氢气和氦气微渗出与正钍浓度表层异常有关,这在其他与氢渗出有关的地方已经观察到。我们提出了一个土壤气体行为模型,每个气体化合物(N2、O2、Ne、H2 和 He)的吸附/解吸过程不同,与氢和氦的深层通量有关。氢通量的量化值为 0.32 立方米/立方米-2.天-1。表面通量比 He/H2 远高于任何已公布的生成通量值。这可能是由于地表下的积累造成的,在地表下,氢发生了严重的变化,而氦却保留了下来,从而增加了氦与氢的相对比例。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Maricá (Brazil), the new natural hydrogen play which changes the paradigm of hydrogen exploration

Maricá (Brazil), the new natural hydrogen play which changes the paradigm of hydrogen exploration

Hydrogen exploration in the municipality of Maricá (Rio de Janeiro State, Brazil) indicates that important hydrogen and helium gas fluxes are emitted through reactivated faults. The gas concentrations in the soils, and the modelled gas fluxes, are among the most intense measured so far in the world. This exploration has shown new surface expression of hydrogen micro-seeps, observed along reactivated large tectonic accidents instead of “fairy circles”, most common proxy for hydrogen systems in cratonic formation. The geology of Maricá, consisting in Neoproterozoic metamorphic rocks without any already documented evidence of hydrogen-prone formations, appears as a very new field of investigation for natural hydrogen. Results indicate the presence of systematic hydrogen saturation of the usual detectors plugged at 80 cm depth, as well as a permanent recharge of hydrogen through time, without relaxation time. Moreover, positive helium anomalies are associated with this hydrogen soil gas, proving the existence of a gas flux coming from deep horizons of the subsurface. This reduces the risk of misinterpretation of surface hydrogen measurement, since the fear of drill bit metamorphism or superficial biological activity inducing hydrogen artefacts is always a possibility. These hydrogen and helium micro-seeps are associated with positive thorium concentration superficial anomalies, as it was already observed in other places associated with hydrogen exudations. We present a model of soil gas behavior, with a differential process of adsorption/desorption of each gas compound (N2, O2, Ne, H2 and He), associated with a deep flux of hydrogen and helium. It is possible to assess a quantification of hydrogen flux of 0.32 m3 m−2.day−1. The surface flux ratio He/H2 is much higher than any published value of generative flux. This may be explained by a subsurface accumulation, where hydrogen is severely altered whereas helium is preserved, increasing the relative proportion of helium versus hydrogen.

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来源期刊
International Journal of Hydrogen Energy
International Journal of Hydrogen Energy 工程技术-环境科学
CiteScore
13.50
自引率
25.00%
发文量
3502
审稿时长
60 days
期刊介绍: The objective of the International Journal of Hydrogen Energy is to facilitate the exchange of new ideas, technological advancements, and research findings in the field of Hydrogen Energy among scientists and engineers worldwide. This journal showcases original research, both analytical and experimental, covering various aspects of Hydrogen Energy. These include production, storage, transmission, utilization, enabling technologies, environmental impact, economic considerations, and global perspectives on hydrogen and its carriers such as NH3, CH4, alcohols, etc. The utilization aspect encompasses various methods such as thermochemical (combustion), photochemical, electrochemical (fuel cells), and nuclear conversion of hydrogen, hydrogen isotopes, and hydrogen carriers into thermal, mechanical, and electrical energies. The applications of these energies can be found in transportation (including aerospace), industrial, commercial, and residential sectors.
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