Vaux-en-Bugey(法国艾因):法国第一个天然气田,为地下天然氢提供了经验教训。

Jean-François Deronzier, H. Giouse
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引用次数: 5

摘要

前Vaux-en-Bugey油田是20世纪初法国第一个生产甲烷的油田,作为一个案例研究,重新审视了氢和氦等气体的生成和聚集理论。最初的天然气储量估计为2200万立方米。根据5%的氢和0.096%的氦的组成,这些气体在该领域的体积分别约为110万立方米的氢和24000立方米的氦。综述了不同的氢源假说:蛇纹石化、菱铁矿氢氧化、水辐射分解、生物发酵、机械生成、深度断层脱气、钢腐蚀。对于氦的生成,研究了不同来源的放射性矿物和中间聚集物。最可能的情况是,在基底或基底附近,通过水的放射性分解产生氢,通过放射性衰变产生氦,通过深断层迁移,储存并集中在含热源甲烷的含水层中,然后在侏罗逆冲期间被甲烷冲入气田。在1906年的发现一个多世纪后,用便携式气体探测器进行了新的测量,虽然不完整,但包括氢,在一个以前的勘探井上有可能获得气体通量,这给了我们评论气体饱和度演变的机会。自发现该油田以来,氢含量的下降可能是由于硫酸盐还原菌的活性。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Vaux-en-Bugey (Ain, France): the first gas field produced in France, providing learning lessons for natural hydrogen in the sub-surface?
The former Vaux-en-Bugey field, first French methane production from early 20th century, is revisited as a case study to address the present generation and accumulation theories for gases like hydrogen and helium. The volume of the initial gas in place is estimated to be 22 million m3. Based on a composition of 5% of hydrogen and 0.096% of helium, the volumes of these gases in the field were respectively around 1.1 million m3 for hydrogen and 24 000 m3 for helium. The different hypotheses of hydrogen sources are reviewed: serpentinization, hydro-oxidation of siderite, water radiolysis, bio-fermentation, mechanical generation, degassing from depth trough faults, steel corrosion. For helium generation, the different sources of radioactive minerals and intermediate accumulations are examined. The most probable scenario is the hydrogen production by water radiolysis and helium production by radioactive decay in or near the basement, migrating trough deep faults, stored and concentrating in an aquifer with thermogenic methane, then flushed by methane into the gas field, during Jura thrusting. New measurements with portable gas detector, incomplete but including hydrogen, on a former exploration well with accessible flux of gas, give the opportunity to comment gas saturation evolution more than a century after the 1906 discovery. The decreasing of hydrogen content since the discovery of the field is probably due to Sulphate-Reducing Bacteria activity.
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