地球化学技术在尼日利亚的地震预报

Lungfa Collins Wuyep, U. Kadiri, Isogun Adeyemi Monday, N. Nansak, Lumi Zakka, Habila Yusuf Thomas, Ezisi Pius Ogugua
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摘要

尽管人们对地震预报的不可能性产生了几轮怀疑,但越来越多的国家,甚至是政府最高层,都意识到,在建立一个真正的预报系统所面临的真正困难面前,无所作为是一种恐惧的鸵鸟姿态。尼日利亚在过去被认为是地震频发的国家。然而,尼日利亚从1933年到2021年的地震记录表明,与这种想法相反,尼日利亚多年来记录了许多地震。近年来,随着观测技术和地球化学理论知识的发展,断层气体地球化学观测再次成为研究的热点。Rn、Hg、H2等用于地球化学观测。222Rn的半衰期为3.825天,在不超过142公里的距离内,通过前兆现象可以探测到5.0级地震。汞等元素是地震预报的重要探测器,在揭示断裂带流体与地震发生的关系方面发挥着重要作用,5.0级地震的探测范围限制在200 km以内。在许多断层系统中,氢气浓度已经被监测到前兆变化,要么使用离散采样和实验室分析,要么使用氢敏感燃料电池对地面气体进行连续监测。地下水化学的前兆变化通常归因于来自两个或两个以上化学性质不同的含水层的流体混合,然而,流体混合的物理机制尚未得到很好的确定。
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Geo-Chemical Techniques for Earthquake Forecasting in Nigeria
Regardless of the doubt caused by some rounds on the impossibility of earthquake forecast, more and more countries, even at the highest governmental levels, realize that doing nothing is the ostrich position of dread before the real difficulties associated with the creation of a real forecasting system. Nigeria in times past was believed to be aseismic. However, the seismic record of Nigeria from 1933-2021 have demonstrated in contrast to the idea, numerous quakes have been recorded in Nigeria throughout the years. With the development of observation techniques and theoretical knowledge of geochemistry, geochemical observation of faults gas has become a hotspot once more in recent years. Rn, Hg, H2, etc., are used for geochemical observations. 222Rn has a half-life of 3.825 days, a magnitude 5.0 earthquake will be detected through precursory phenomena at a distance not greater than 142 km. Mercury and other elements are used as important detectors for earthquake prediction and they play an important role in revealing the relationship between fluid in the fault zone and the occurrence of earthquakes, the range for a magnitude 5.0 earthquake is limited to 200 km. Hydrogen concentrations have been monitored for precursory variations in many fault systems, using either discrete sampling and laboratory analysis or continuous monitoring of ground gas, using hydrogen-sensitive fuel cells. Precursory changes in groundwater chemistry are often attributed to the mixing of fluids from two or more chemically distinct aquifers, the physical mechanism responsible for the mixing of fluids is, however, not well established.
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