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Improved accuracy of plane-wave electromagnetic modelling by application of the total and scattered field decomposition and perfectly matched layers

Buntin, Laura M. (författare)
Uppsala universitet,Geofysik
Kalscheuer, Thomas, 1975- (författare)
Uppsala universitet,Geofysik
Kreiss, Gunilla (författare)
Uppsala universitet,Institutionen för informationsteknologi
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Ren, Z (författare)
School of Geo-science and Info-Physics, Central South University , Changsha, Hunan 410017 China.
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 (creator_code:org_t)
2023
2023
Engelska.
Ingår i: Geophysical Journal International. - : Oxford University Press (OUP). - 0956-540X .- 1365-246X. ; 235:2, s. 1201-1217
  • Tidskriftsartikel (refereegranskat)
Abstract Ämnesord
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  • In 2-D magnetotelluric modelling, the standard application of Dirichlet boundary conditions (BC) may severely diminish the solution accuracy, because the unknown scattered part of the electromagnetic field is erroneously reflected at the domain boundary. Therefore, we adapt the total and scattered field decomposition (TSFD) to geophysical modelling, enabling the application of fully absorbing boundary methods, here perfectly matched layers (PML), to the scattered field. Our novel TSFD divides the modelling domain into two regions. In the total-field region containing the area of interest, the solution is computed for the total field. In the scattered-field region containing the boundaries, the solution is obtained for the scattered field, which is fully absorbed by PML at the boundaries. The plane-wave source is excited at the TSFD interface between both regions. Thus, boundary reflections are eradicated leading to superior solution accuracy, and boundaries can be placed closer to the receivers, shrinking the computational problem. Especially for challenging models with strong lateral changes, the solution accuracy of the TSFD is superior to that of the standard Dirichlet approach. Owing to the linearity of Maxwell's equations, the inaccuracy introduced to the electric and magnetic fields by using Dirichlet BC can be expected to partly cancel out in the magnetotelluric transfer functions, for example the impedance tensor. In this work, we quantify this cancellation effect. The inaccuracy is less than typical measurement errors in the vast majority of apparent resistivity and phase data, even, when the primary fields are strongly inaccurate.

Ämnesord

NATURVETENSKAP  -- Geovetenskap och miljövetenskap -- Geofysik (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences -- Geophysics (hsv//eng)

Nyckelord

Magnetotellurics
Numerical modelling
Numerical solutions
Total and scattered field decomposition
Perfectly matched layers
Scientific Computing
Beräkningsvetenskap
Geofysik med inriktning mot seismologi
Geophysics with specialization in Seismology

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Buntin, Laura M.
Kalscheuer, Thom ...
Kreiss, Gunilla
Ren, Z
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NATURVETENSKAP
NATURVETENSKAP
och Geovetenskap och ...
och Geofysik
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Uppsala universitet

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