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Magnetotelluric power line noise removal using temporally varying sinusoidal subtraction of the grid utility frequency

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985530%3A_____%2F23%3A00574381" target="_blank" >RIV/67985530:_____/23:00574381 - isvavai.cz</a>

  • Result on the web

    <a href="https://link.springer.com/article/10.1007/s00024-023-03323-w" target="_blank" >https://link.springer.com/article/10.1007/s00024-023-03323-w</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1007/s00024-023-03323-w" target="_blank" >10.1007/s00024-023-03323-w</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Magnetotelluric power line noise removal using temporally varying sinusoidal subtraction of the grid utility frequency

  • Original language description

    The magnetotelluric method relies on variations of natural electromagnetic fields, which in the vicinity of human settlements are persistently distorted by anthropogenic electromagnetic noise. A large source of noise to the magnetotelluric response is caused by the harmonic oscillations of the power network utility frequency centered on 50/60 Hz along with the associated higher harmonics. Removing this type of noise is essential for high frequency magnetotelluric measurements used for shallow surveys. There are a large number of approaches for how to treat power line noise in magnetotelluric signals, however, commonly used methods do not take into account time variations/instabilities of the utility frequency. That is not serious problem in vicinity of well balanced grid networks, but can cause issues in regions with larger utility frequency variations. Under such conditions, commonly used methods loose more of the natural signal, which is undesirable especially in case of very noisy datasets. Hence, we adopted approach for removing of power line noise with respect to time variations of the utility frequency and applied it to magnetotelluric signals to preserve more of natural signal. The method is based on modelling of the grid network harmonic oscillations by the optimum utility frequency and its integer multiples. The resulting sum of sinusoidal signals is subsequently subtracted from recorded data and only particular noise frequencies are removed from the original signal with high precision, while frequency ranges around power line harmonics are cleaned.

  • Czech name

  • Czech description

Classification

  • Type

    J<sub>imp</sub> - Article in a specialist periodical, which is included in the Web of Science database

  • CEP classification

  • OECD FORD branch

    10508 - Physical geography

Result continuities

  • Project

  • Continuities

    I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Others

  • Publication year

    2023

  • Confidentiality

    S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Data specific for result type

  • Name of the periodical

    Pure and Applied Geophysics

  • ISSN

    0033-4553

  • e-ISSN

    1420-9136

  • Volume of the periodical

    180

  • Issue of the periodical within the volume

    9

  • Country of publishing house

    DE - GERMANY

  • Number of pages

    15

  • Pages from-to

    3303-3317

  • UT code for WoS article

    001021371600001

  • EID of the result in the Scopus database

    2-s2.0-85163795043