Please use this identifier to cite or link to this item: http://library.iigm.res.in:8080/xmlui/handle/123456789/1645
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dc.contributor.authorKanu, M.O.
dc.contributor.authorMeludu, O.C.
dc.contributor.authorBasavaiah, N.
dc.contributor.authorOniku, A.S.
dc.date.accessioned2010-08-05T18:11:22Z
dc.date.accessioned2021-02-12T10:50:54Z-
dc.date.available2010-08-05T18:11:22Z
dc.date.available2021-02-12T10:50:54Z-
dc.date.issued2019
dc.identifier.citationActa Geophysica. 67, 517–532, doi: 10.1007/s11600-019-00248-8en_US
dc.identifier.urihttp://localhost:8080/xmlui/handle/123456789/1645-
dc.description.abstractThe study analyzed the relationship between mineral magnetic properties and particle size in order to determine the suitability of magnetic measurements to serve as particle size proxy for urban top soils samples collected from Jalingo, NE Nigeria. Pearson correlation analyses between mineral magnetic parameters (χlf, χfd%, χARM, SIRM, Soft IRM, ARM/SIRM) and particle size properties (PM2.5, PM10, clay, silt and sand) are reported. Results indicate that each particle size class shows diferent strength of correlation with magnetic parameters, implying that each particle class contains a proportion of magnetic minerals. For the whole data set (n=154), χfd%, χARM and ARM/SIRM show signifcant positive correlation with the fne size fractions (PM2.5, PM10, clay and silt) but negatively correlated with the sand proportion, while χlf, SIRM and Soft IRM exhibit contrasting relationship. Of all the magnetic parameters, the magnetic parameters indicating fne-grained ferrimagnetic minerals (ARM/SIRM and χARM) have the strongest and most signifcant correlations. The nature of the magneto-particle size relationship is diferent when examined in terms of land use. The fact that magnetic properties and textural parameters have strong relationship indicates that magnetic methods could be considered a potential particle size proxy in Jalingo. However, since the relationship does not follow predictable and consistent patterns of other studies in top soils and sedimentary settings, it brings to fore the non-universality of the method. Hence, the type of relationship existing between magnetic and particle size properties in an environmental setting must be determined before applying the magnetic method as particle size proxy.en_US
dc.language.isoen_USen_US
dc.subjectSoilen_US
dc.subjectMineral magnetic propertiesen_US
dc.subjectEnvironmentaen_US
dc.subjectSoil texture parametersen_US
dc.subjectParticle sizeen_US
dc.subjectParticulate matteren_US
dc.titleRelationship between mineral magnetic properties and soil textural parameters soil textural parametersen_US
dc.typeArticleen_US
dc.identifier.accession091815
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