scholarly journals On finding the surface admittance of an obstacle via the time domain enclosure method

2019 ◽  
Vol 13 (2) ◽  
pp. 263-284
Author(s):  
Masaru Ikehata ◽  
Keyword(s):  
Time Domain ◽  
Enclosure Method ◽  
The Time Domain ◽  
Surface Admittance

scholarly journals Prescribing a heat flux coming from a wave equation

2019 ◽  
Vol 27 (5) ◽  
pp. 731-744 ◽  
Author(s):  
Masaru Ikehata
Keyword(s):  
Heat Flux ◽  
Asymptotic Behavior ◽  
Wave Equation ◽  
Time Domain ◽  
Indicator Function ◽  
The Body ◽  
Enclosure Method ◽  
Whole Space ◽  
The Time Domain ◽  
Recent Version

Abstract What happens when one prescribes a heat flux which is proportional to the Neumann data of a solution of the wave equation in the whole space on the surface of a heat conductive body? It is shown that there is a difference in the asymptotic behavior of the indicator function in the most recent version of the time domain enclosure method, which aims at extracting information about an unknown cavity embedded in the body.

scholarly journals On finding a buried obstacle in a layered medium via the time domain enclosure method

2018 ◽  
Vol 12 (5) ◽  
pp. 1173-1198
Author(s):  
Masaru Ikehata ◽  
◽  
Mishio Kawashita ◽  
Keyword(s):  
Time Domain ◽  
Layered Medium ◽  
Enclosure Method ◽  
The Time Domain

Apodisation in the time domain

1992 ◽  
Vol 2 (4) ◽  
pp. 615-620
Author(s):  
G. W. Series
Keyword(s):  
Time Domain ◽  
The Time Domain

JOINT INTERPRETATION OF AIRBORNE ELECTROMAGNETIC DATA IN THE TIME DOMAIN AND FREQUENCY DOMAIN

2018 ◽  
Vol 12 (7-8) ◽  
pp. 76-83
Author(s):  
E. V. KARSHAKOV ◽  
J. MOILANEN
Keyword(s):  
Fourier Transform ◽  
Frequency Domain ◽  
Time Domain ◽  
Frequency Interval ◽  
Single Spectrum ◽  
Simultaneous Inversion ◽  
Homogeneous Half Space ◽  
Time Domain Data ◽  
The Time Domain

Тhe advantage of combine processing of frequency domain and time domain data provided by the EQUATOR system is discussed. The heliborne complex has a towed transmitter, and, raised above it on the same cable a towed receiver. The excitation signal contains both pulsed and harmonic components. In fact, there are two independent transmitters operate in the system: one of them is a normal pulsed domain transmitter, with a half-sinusoidal pulse and a small "cut" on the falling edge, and the other one is a classical frequency domain transmitter at several specially selected frequencies. The received signal is first processed to a direct Fourier transform with high Q-factor detection at all significant frequencies. After that, in the spectral region, operations of converting the spectra of two sounding signals to a single spectrum of an ideal transmitter are performed. Than we do an inverse Fourier transform and return to the time domain. The detection of spectral components is done at a frequency band of several Hz, the receiver has the ability to perfectly suppress all sorts of extra-band noise. The detection bandwidth is several dozen times less the frequency interval between the harmonics, it turns out thatto achieve the same measurement quality of ground response without using out-of-band suppression you need several dozen times higher moment of airborne transmitting system. The data obtained from the model of a homogeneous half-space, a two-layered model, and a model of a horizontally layered medium is considered. A time-domain data makes it easier to detect a conductor in a relative insulator at greater depths. The data in the frequency domain gives more detailed information about subsurface. These conclusions are illustrated by the example of processing the survey data of the Republic of Rwanda in 2017. The simultaneous inversion of data in frequency domain and time domain can significantly improve the quality of interpretation.

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