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Modelling of Electromagnetic (EM) field yield from analytical procedure which is developed to obtain the exact evaluation of the complete integral that representation EM field components generated by a Vertical Magnetic Dipole (VMD) lying on the surface of a flat and homogeneous half-space earth. Th...
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id-itb.:157722017-09-27T11:45:07Z#TITLE_ALTERNATIVE# KAMILA (NIM: 10210043); Tim Pembimbing : Dr. Eng. Alamta Singarimbun; Wahyu Srigutomo Ph.D, GHINA Indonesia Final Project INSTITUT TEKNOLOGI BANDUNG https://digilib.itb.ac.id/gdl/view/15772 Modelling of Electromagnetic (EM) field yield from analytical procedure which is developed to obtain the exact evaluation of the complete integral that representation EM field components generated by a Vertical Magnetic Dipole (VMD) lying on the surface of a flat and homogeneous half-space earth. The model of electromagnetic fields build both for homogeneous and layered earth assumption to proof and compare <br /> <br /> <br /> the output at the same resistivity value. At first, models are built in frequency domain formulation. Quasi-static approximation take occasion, which only valid in the low- <br /> <br /> <br /> frequency range, while build forward modelling data. Furthermore, these data will be transformed on to time domain by inverse Fourier transform using quadrature Gauss-Kronrod numerical method. text |
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Modelling of Electromagnetic (EM) field yield from analytical procedure which is developed to obtain the exact evaluation of the complete integral that representation EM field components generated by a Vertical Magnetic Dipole (VMD) lying on the surface of a flat and homogeneous half-space earth. The model of electromagnetic fields build both for homogeneous and layered earth assumption to proof and compare <br />
<br />
<br />
the output at the same resistivity value. At first, models are built in frequency domain formulation. Quasi-static approximation take occasion, which only valid in the low- <br />
<br />
<br />
frequency range, while build forward modelling data. Furthermore, these data will be transformed on to time domain by inverse Fourier transform using quadrature Gauss-Kronrod numerical method. |
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Final Project |
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KAMILA (NIM: 10210043); Tim Pembimbing : Dr. Eng. Alamta Singarimbun; Wahyu Srigutomo Ph.D, GHINA |
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KAMILA (NIM: 10210043); Tim Pembimbing : Dr. Eng. Alamta Singarimbun; Wahyu Srigutomo Ph.D, GHINA #TITLE_ALTERNATIVE# |
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KAMILA (NIM: 10210043); Tim Pembimbing : Dr. Eng. Alamta Singarimbun; Wahyu Srigutomo Ph.D, GHINA |
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KAMILA (NIM: 10210043); Tim Pembimbing : Dr. Eng. Alamta Singarimbun; Wahyu Srigutomo Ph.D, GHINA |
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https://digilib.itb.ac.id/gdl/view/15772 |
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