地球物理环境中长期电场测量的电极系统研究

F. Perrier, G. Petiau, G. Clerc, V. Bogorodsky, E. Erkul, L. Jouniaux, D. Lesmes, J. Macnae, J. Meunier, D. Morgan, Darcy Nascimento, G. Oettinger, G. Schwarz, H. Toh, M. Valiant, K. Vozoff, O. Yazici-čakin
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引用次数: 71

摘要

在法国Garchy进行的一项为期一年的实验中,对设计用于测量土壤或海水中超过一分钟的电场的各种类型的电极进行了比较。实验包括50多个具有液体或吸收电解质的电极对以及Pb/PbCl2、Ag/AgCl、Cu/CuSO4和Cd/CdCl2金属离子对。在实验室系统测量电极参数,并将电极安装在现场,形成50米长,间隔2米的平行偶极子。在盐水容器中监测用于海洋测量的成对电极。在1995年5月至1996年4月期间,以1分钟的抽样间隔记录了42个电位差。当电极比较时,在长期稳定性以及对日变化、降雨和土壤饱和度的敏感性方面观察到很大的差异。对于土壤中的测量,电极的安装方法起着重要的作用。在盐水中,表现最好的电极对具有每年0.1 mV量级的漂移。在土壤中,最佳传感器的典型漂移在干土中为0.2 mV /月,在湿土中为0.5 mV /月。根据外部条件或地球物理测量类型,优选电极设计和安装方法。除了大地磁场之外,还观察到非电极或装置效应的电位变化,并将其归因于土壤中的电源。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
A One-Year Systematic Study of Electrodes for Long Period Measurements of the Electric Field in Geophysical Environments
Various types of electrodes designed for the measurement of the electric field in the soil or in sea water at periods larger than one minute have been compared in a one-year experiment in Garchy, France. The experiment included more than fifty electrode pairs with liquid or absorbed electrolytes and Pb/PbCl2, Ag/AgCl, Cu/CuSO4 and Cd/CdCl2 metal-ion couples. The electrode parameters were systematically measured in the laboratory and the electrodes were installed in the field to constitute 50-meter long parallel dipoles separated by 2 meters. Pairs of electrodes used for sea measurements were monitored in a salted water vessel. Fourty-two potential differences were recorded with a sampling interval of 1 minute between May 1995 and April 1996. When electrodes are compared, large differences are observed in the long term stability as well as in the sensitivity to diurnal variations, rainfall and soil saturation. For measurements in soil, the installation method of the electrodes plays an important role. In salted water, the best performing electrode pair has a drift of the order of 0.1 mV per year. In soil, typical drifts for the best sensors are of the order of 0.2 mV per month in dry soil and 0.5 mV per month in soaked soil. Preferred electrode designs and installation methods, depending on the external conditions or the type of geophysical measurement, emerge from this experiment. In addition to the magneto-telluric field, potential variations which are not electrode or installation effects are observed and attributed to electrical sources in the soil.
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