Response of a current loop antenna in an invaded borehole

Geophysics ◽  
1984 ◽  
Vol 49 (1) ◽  
pp. 81-91 ◽  
Author(s):  
W. C. Chew

The problem of the radiation of a current loop antenna in a multicylindrical medium is formulated exactly in terms of an integral. The integrand is calculated using an iterative scheme making the integral more tenable to approximation. This closely approximates the response of a dielectric logging tool such as the deep propagation tool (DPT) or an induction tool in invaded boreholes. To gain more physical insight into the waves, an asymptotic approximation of the integral is derived. The large parameter for the validity of this approximation is the ratio of the transmitter‐receiver separation to the diameter of the invasion around the borehole. An iterative scheme is devised to compute systematically the approximation for an arbitrary number of cylindrical layers. The multicylindrical layer model is a good model of the invasion zone, borehole, and tool housing. The final approximation to the azimuthal electric field contains three terms. The first term resembles the response of a current loop in a homogeneous medium with electrical properties of the outermost medium or the formation. The higher order terms are improvements. The approximation is better at lower frequencies, implying that it is also good for the induction logging tool.

1988 ◽  
Vol 31 (4) ◽  
pp. 299-308 ◽  
Author(s):  
V. I. Karpman ◽  
A. I. Osin ◽  
O. F. Pogrebnyak

Author(s):  
C. Le Cunff ◽  
E. Fontaine ◽  
F. Biolley

Fatigue due to environmental conditions is studied on a top-tensioned riser. The fatigue is due to two factors. First, the waves produce a displacement of the top of the riser, which excites the structure. Secondly, currents create vortices behind the structures. The phenomenon is then referred to as vortex-induced vibrations (VIV), whereby the vortices can lock onto a structural mode through the shedding frequency. In the present paper, we have two objectives. The first is to compare the fatigue estimates given either by a modal analysis or by Navier-Stokes calculations for a riser in a current. The second is to determine if studying the wave and current effects separately produces conservative results or if they must be studied together.


Author(s):  
Berthold F. Kriegshäuser ◽  
André Santos ◽  
Liming Yu

Geophysics ◽  
1982 ◽  
Vol 47 (7) ◽  
pp. 1068-1077 ◽  
Author(s):  
G. M. Hoversten ◽  
H. F. Morrison

The electric field induced within four layered models by a repetitive current wave form in a circular loop transmitter is presented along with the resulting magnetic fields observed on the surface. The behavior of the induced electric field as a function of time explains the observed sign reversal of the vertical magnetic field on the surface. In addition, the differences between magnetic field responses for different models are explained by the behavior of the induced electric fields. The pattern of the induced electric field is shown to be that of a single “smoke ring,” as described by Nabighian (1979), which is distorted by layering but which remains a single ring system rather than forming separate smoke rings in each layer.


Geophysics ◽  
1981 ◽  
Vol 46 (9) ◽  
pp. 1291-1300 ◽  
Author(s):  
W. C. Chew ◽  
S. Gianzero ◽  
K. J. Kaplin

The long time transient response is developed for a point coil transmitter (vertical magnetic dipole) located in a wellbore surrounded by a homogeneous formation. A simple algorithm is derived for the apparent conductivity signal based on the difference between the voltage nulls in a pair of receiver coils which are displaced vertically from the transmitter along the axis of the wellbore. A justification of these results is provided by means of a direct numerical integration (double Fourier transform) and also two separate approximate approaches.


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