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ELECTRICAL SOUNDINGS BY THE METHOD OF PURE ANOMALIES WITH THE COMBINED THREE-ELECTRODE ARRAY AMN+NMA

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Выполнено физическое моделирование электрических зондирований с комбинированной установкой AMN+NМА по методике чистых аномалий над проводящей и непроводящей неоднород- ностью. На разрезе аномальной разности потенциалов вертикальные границы объекта с вмещающей средой выделяются знакопеременными экстремумами. Приводится экспериментальное исследование, которое показывает, что по затуханию аномальной разности потенциалов возможно определение ниж- ней границы геоэлектрической неоднородности. Physical modeling of electrical soundings with the combined array AMN+NMA was performed by the method of pure anomalies over conducting and non -conductive heterogeneity. On the section of an abnormal potential difference the vertical boundaries of the object with the host environment are distinguished by alternating extremes. An experimental study is given, which shows that determining the lower boundary of geoelectrical heterogeneity it is possible by attenuation of the abnormal potential difference.
Y. P. Bulashevich Institute of Geophysics, Ural Branch of the Russian Academy of Sciences
Title: ELECTRICAL SOUNDINGS BY THE METHOD OF PURE ANOMALIES WITH THE COMBINED THREE-ELECTRODE ARRAY AMN+NMA
Description:
Выполнено физическое моделирование электрических зондирований с комбинированной установкой AMN+NМА по методике чистых аномалий над проводящей и непроводящей неоднород- ностью.
На разрезе аномальной разности потенциалов вертикальные границы объекта с вмещающей средой выделяются знакопеременными экстремумами.
Приводится экспериментальное исследование, которое показывает, что по затуханию аномальной разности потенциалов возможно определение ниж- ней границы геоэлектрической неоднородности.
Physical modeling of electrical soundings with the combined array AMN+NMA was performed by the method of pure anomalies over conducting and non -conductive heterogeneity.
On the section of an abnormal potential difference the vertical boundaries of the object with the host environment are distinguished by alternating extremes.
An experimental study is given, which shows that determining the lower boundary of geoelectrical heterogeneity it is possible by attenuation of the abnormal potential difference.

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