RESISTIVITY MEASUREMENTS IN VALLEYS WITH ELLIPTIC CROSS-SECTION
In this paper an idealized valley of a semi-elliptic cross-section is considered. For a Schlumberger configuration on the axis, sets of master curves are calculated for the ratio of semi-axis a/b= 1, 2, 3, 4, 5 in corresponding to various resistivity ratios of surrounding rocks and valley sediments....
Full description
| Author: |
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| Format: |
Electronic Article |
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| Published: |
Oxford, UK: Blackwell Publishing Ltd ; 1972 |
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| Physical Description: |
Online-Ressource |
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| Secondary Edition: |
Online edition ; 2006 ; Blackwell Publishing Journal Backfiles 1879-2005 ; 041108-5 |
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| Containing Work: |
In: Geophysical prospecting - Oxford [u.a.] : Wiley-Blackwell, Vol. 20, No. 2 (1972), p. 0 |
| Links: |
Volltext [NL] |
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| DOI / URN: |
10.1111/j.1365-2478.1972.tb00638.x |
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| Catalog id: |
NLEJ239619099 |
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| 100 | 1 | |a MUNDRY, E. | |
| 245 | 1 | 0 | |a RESISTIVITY MEASUREMENTS IN VALLEYS WITH ELLIPTIC CROSS-SECTION |h Elektronische Ressource |
| 264 | 3 | 1 | |a Oxford, UK |b Blackwell Publishing Ltd |c 1972 |
| 300 | |a Online-Ressource | ||
| 520 | |a In this paper an idealized valley of a semi-elliptic cross-section is considered. For a Schlumberger configuration on the axis, sets of master curves are calculated for the ratio of semi-axis a/b= 1, 2, 3, 4, 5 in corresponding to various resistivity ratios of surrounding rocks and valley sediments. For small resistivity ratios, these model curves have the shape of three-layer curves for horizontal bedding and are often equivalent to them within the accuracy of measurements. The axial ratio a/b considerably affects the depth determination of valley sediments. In the special case of a circular cross-section (a/b= 1) the influence of the position of the electrodes on the sounding curve is studied in more detail.The application of the master curves in practice shows that the influence of the specific shape of the valley on soundings should not be neglected. In general, the valleys have a greater “true” depth than can be seen from the interpretation of a sounding by master curves corresponding to the horizontal bedding. | ||
| 533 | |a Online edition |d 2006 |f Blackwell Publishing Journal Backfiles 1879-2005 ; 041108-5 |7 |2006|||||||||| | ||
| 700 | 1 | |a HOMILIUS, J. | |
| 773 | 0 | 8 | |i In |t Geophysical prospecting |d Oxford [u.a.] : Wiley-Blackwell |g Vol. 20, No. 2 (1972), p. 0 |q 20:2<0 |w (DE-601)NLEJ243927630 |x 1365-2478 |
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