Number of the records: 1  

Magnetic mapping of distribution of wood ash used for fertilization of forest soil

  1. 1.
    SYSNO ASEP0486295
    Document TypeJ - Journal Article
    R&D Document TypeJournal Article
    Subsidiary JČlánek ve WOS
    TitleMagnetic mapping of distribution of wood ash used for fertilization of forest soil
    Author(s) Petrovský, Eduard (GFU-E) ORCID, RID
    Remeš, J. (CZ)
    Kapička, Aleš (GFU-E) ORCID, RID
    Podrázský, V. (CZ)
    Grison, Hana (GFU-E) RID, ORCID, SAI
    Borůvka, L. (CZ)
    Source TitleScience of the Total Environment. - : Elsevier - ISSN 0048-9697
    Roč. 626, June (2018), s. 228-234
    Number of pages7 s.
    Publication formPrint - P
    Languageeng - English
    CountryNL - Netherlands
    Keywordsforest soil ; wood ash ; fertilizing ; tree plants ; iron oxides ; rock magnetism
    Subject RIVDE - Earth Magnetism, Geodesy, Geography
    OECD categoryPhysical geography
    Institutional supportGFU-E - RVO:67985530
    UT WOS000428194000024
    EID SCOPUS85040690515
    DOI10.1016/j.scitotenv.2018.01.095
    AnnotationThe effect of wood-ash fertilization on forest soils has been assessed mainly through geochemical methods (e.g., content of soil organic matter or nutrients). However, a simple and fastmethod of determining the distribution of the ash and the extent of affected soil is missing. In this studywe present the use of magnetic susceptibility, which is controlled by Fe-oxides, in comparing the fertilized soil in the forest plantation of pine and oakwith intact forest soil. Spatial and vertical distribution of magnetic susceptibility was measured in an oak and pine plantation next to stems of young plants, where wood ash was applied as fertilizer. Pattern of the susceptibility distribution was compared with that in non-fertilized part of the plantation as well as with a spot of intact natural forest soil nearby. Our results showthat the wood-ash samples contain significant amount of ferrimagnetic magnetite with susceptibility higher than that of typical forest soil. Clear differences were observed between magnetic susceptibility of furrows and ridges. Moreover, the dispersed ash remains practically on the surface, does not penetrate to deeper layers. Finally, our data suggest significant differences in surface values between the pine and oak plants. Based on this study we may conclude that magnetic susceptibility may represent a simple and approximate method of assessing the extent of soil affected by wood-ash.
    WorkplaceGeophysical Institute
    ContactHana Krejzlíková, kniha@ig.cas.cz, Tel.: 267 103 028
    Year of Publishing2019
Number of the records: 1  

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