### Abstract

Original language | English |
---|---|

Place of Publication | Espoo |

Publisher | VTT Technical Research Centre of Finland |

Number of pages | 50 |

ISBN (Print) | 951-38-2630-9 |

Publication status | Published - 1986 |

MoE publication type | D4 Published development or research report or study |

### Publication series

Name | Tiedotteita / Valtion teknillinen tutkimuskeskus |
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Publisher | VTT |

Volume | 597 |

### Fingerprint

### Keywords

- geophysics
- environmental surveys
- municipal engineering
- landfills
- leachate
- monitoring

### Cite this

*Calculation of electromagnetic field components in frequency and time domain using dipole source excitation and layered earth model: Documentation of software development*. Espoo: VTT Technical Research Centre of Finland. Valtion teknillinen tutkimuskeskus. Tiedotteita, No. 597

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*Calculation of electromagnetic field components in frequency and time domain using dipole source excitation and layered earth model: Documentation of software development*. Valtion teknillinen tutkimuskeskus. Tiedotteita, no. 597, VTT Technical Research Centre of Finland, Espoo.

**Calculation of electromagnetic field components in frequency and time domain using dipole source excitation and layered earth model : Documentation of software development.** / Korkealaakso, Juhani; Saksa, Pauli.

Research output: Book/Report › Report › Professional

TY - BOOK

T1 - Calculation of electromagnetic field components in frequency and time domain using dipole source excitation and layered earth model

T2 - Documentation of software development

AU - Korkealaakso, Juhani

AU - Saksa, Pauli

PY - 1986

Y1 - 1986

N2 - The completely generalized program that calculates the mutual coupling ratios of two loops over an n-layer earth model in four coil configuration (horizontal coplanar, perpendicular, vertical coplanar and ver-tical coaxial) systems has been modified to take advantage of a digital linear filter method. This method rapidly evaluates the many Hankel transform integrals encountered in layered earth electromagnetic modelling. The program is valid for any frequency, coil separation or coil altitude and any resistivities, dielectric constants and relative magnetic permeabilities of the layers. Applying this rapid and thus inexpensive method it has also been possible to develop a computer program that calculates the time domain electromagnetic response of a multilayered earth for the Crone PEM dipole system. The conversion into the time domain involves Fourier series summation of the matched complex mutual coupling ratios of the layered earth models computed by the digital linear filter method.

AB - The completely generalized program that calculates the mutual coupling ratios of two loops over an n-layer earth model in four coil configuration (horizontal coplanar, perpendicular, vertical coplanar and ver-tical coaxial) systems has been modified to take advantage of a digital linear filter method. This method rapidly evaluates the many Hankel transform integrals encountered in layered earth electromagnetic modelling. The program is valid for any frequency, coil separation or coil altitude and any resistivities, dielectric constants and relative magnetic permeabilities of the layers. Applying this rapid and thus inexpensive method it has also been possible to develop a computer program that calculates the time domain electromagnetic response of a multilayered earth for the Crone PEM dipole system. The conversion into the time domain involves Fourier series summation of the matched complex mutual coupling ratios of the layered earth models computed by the digital linear filter method.

KW - geophysics

KW - environmental surveys

KW - municipal engineering

KW - landfills

KW - leachate

KW - monitoring

M3 - Report

SN - 951-38-2630-9

T3 - Tiedotteita / Valtion teknillinen tutkimuskeskus

BT - Calculation of electromagnetic field components in frequency and time domain using dipole source excitation and layered earth model

PB - VTT Technical Research Centre of Finland

CY - Espoo

ER -