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Titlebook: Electromagnetic Depth Soundings; L. L. Vanyan,L. Z. Bobrovnikov,E. I. Terekhin Book 1967 Consultants Bureau 1967 ETA.Matching.behavior.bou

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發(fā)表于 2025-3-21 16:27:22 | 只看該作者 |倒序?yàn)g覽 |閱讀模式
書目名稱Electromagnetic Depth Soundings
編輯L. L. Vanyan,L. Z. Bobrovnikov,E. I. Terekhin
視頻videohttp://file.papertrans.cn/306/305980/305980.mp4
圖書封面Titlebook: Electromagnetic Depth Soundings;  L. L. Vanyan,L. Z. Bobrovnikov,E. I. Terekhin Book 1967 Consultants Bureau 1967 ETA.Matching.behavior.bou
描述10.------------------------, 10.------------------------. N ::IE ~ w ~ ‘" "‘0.1 ~ 0 M z SIDE VIEW PLAN VIEW 0.01 LI --‘---‘---LLL-‘---LLLlI ~-L---"---LLL..ll..L.LJ‘-‘:‘;;‘ 0.01 1 100 10 100 fr Fig. 1. The behavior of the magnetic and electric fields from a vertical magnetic dipole source at the surface of the earth (after Wait [1951,1955]). earth, the experimental curve so plotted should have the same shape as a portion of the ap- propriate theoretical curve, but with the ordinates and abscissas shifted by an amount dependent on the resistivity. The conductivity can be determined from the amount of shift between the field data and the theoretical curve. A detailed description of the curve matching procedure is found in a text by Keller and Frischknecht (1966). The curve matching procedure, though used, has several disadvantages. Measurements must be made over a diagnostic portion of the theoretical curve, one in which there is some curvature, so that the amount of shift required to make a match can be determined uniquely. This means that the approximate conductivity of the earth must be known when measurements are made. Secondly, determination of a single value of conductivity requ
出版日期Book 1967
關(guān)鍵詞ETA; Matching; behavior; boundary element method; earth; electromagnetic; equation; experiment; field; fields
版次1
doihttps://doi.org/10.1007/978-1-4684-0670-2
isbn_softcover978-1-4684-0672-6
isbn_ebook978-1-4684-0670-2
copyrightConsultants Bureau 1967
The information of publication is updating

書目名稱Electromagnetic Depth Soundings影響因子(影響力)




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Concerning Some Causes for the Distortion of Transient Sounding Curves,haracter. These distortions are most severe in the left-hand segments of the curves, and may substantially increase or decrease the value of ρ. computed for small times. In extreme cases, the value for ρ. computed for the left-most segment of the transient coupling curve may be negative (this part o
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Four-Layer Master Curves for Frequency Electromagnetic Sounding,. L. Vanyan and G. M. Morozova at the Computer Center of the Siberian Department of the Academy of Sciences of the USSR, and prepared for publication by E. I. Terekhin and A.I. Shtimmer at the All-Union Research Institute for Applied Petroleum Geophysics.
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on of the theoretical curve, one in which there is some curvature, so that the amount of shift required to make a match can be determined uniquely. This means that the approximate conductivity of the earth must be known when measurements are made. Secondly, determination of a single value of conductivity requ978-1-4684-0672-6978-1-4684-0670-2
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