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Frequency domain electromagnetic induction survey in the intertidal zone: Limitations of low-induction-number and depth of exploration

机译:潮间带频域电磁感应调查:低感应数和勘探深度的局限性

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摘要

Subsurface investigation in the Belgian intertidal zone is severely complicated due to high heterogeneity and tides. Near-surface geophysical techniques can offer assistance since they allow fast surveying and collection of high spatial density data and frequency domain electromagnetic induction (EMI) was chosen for archaeological prospection on the Belgian shore. However, in the intertidal zone the effects of extreme salinity compromise validity of low-induction-number (LIN) approximated EMI data. In this paper, the effects of incursion of seawater on multi-receiver EMI data are investigated by means of survey results, field observations, cone penetration tests and in-situ electrical conductivity measurements. The consequences of LIN approximation breakdown were researched. Reduced depth of investigation of the quadrature-phase (Qu) response and a complex interpretation of the in-phase responsewere confirmed. Nonetheless, a high signal-to-noise ratio of the Qu response and viable data with regard to shallow subsurface investigation were also evidenced, allowing subsurface investigation in the intertidal zone.
机译:由于高度的非均质性和潮汐,比利时潮间带的地下调查非常复杂。近地表地球物理技术可以提供帮助,因为它们可以快速调查和收集高空间密度数据,并且选择了频域电磁感应(EMI)进行比利时沿岸的考古勘探。但是,在潮间带,极端盐度的影响损害了低感应数(LIN)近似EMI数据的有效性。在本文中,通过调查结果,现场观察,锥形渗透测试和原位电导率测量,研究了海水入侵对多接收器EMI数据的影响。研究了LIN近似分解的后果。确认了减小的正交相(Qu)响应调查深度和同相响应的复杂解释。但是,还证实了Qu响应的高信噪比和浅层地下调查的可行数据,从而允许在潮间带进行地下调查。

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