An integrated toolkit using multiple methods for determining the potential sources of iron and manganese in groundwater: a case study from the lower Kelantan River Basin, Malaysia

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dc.contributor.authorUsman Abdullahi Usman
dc.contributor.authorIsmail Yusof
dc.contributor.authorMuggundha Raoov
dc.contributor.authorYatimah Alias
dc.contributor.authorJonathan Hodgkinson
dc.contributor.authorNurzaidi Abdullah
dc.coverage.publicationMalaysia
dc.date.accessioned2024-05-20T04:01:13Z
dc.date.available2024-05-20T04:01:13Z
dc.date.issued2021
dc.description.abstractThe application of thin-section petrography, field emission scanning electron microscopy and energy dispersive X-ray analysis (FESEM–EDX), Fourier transform infrared spectroscopy (FTIR), X-ray diffraction (XRD), thermo-analysis, and laser Raman spectral analysis methods can be combined to characterize iron-ores and distinguish clay minerals in alluvial soils. The integrated methodology developed for this work provides the basis for a generic mineral characterization toolkit. Five main alluvial soil types have been defined in the upper layer of the lower Kelantan Basin, Malaysia: sand with low clay content, clay sand, sandy clay, mottled clay, and mud-sand.
dc.identifier.citationUsman, U. A., Yusoff, I., Raoov, M., Alias, Y., Hodgkinson, J., & Abdullah, N. (2021). An integrated toolkit using multiple methods for determining the potential sources of iron and manganese in groundwater: a case study from the lower Kelantan river basin, Malaysia. Environmental Earth Sciences, 80, 1-17.
dc.identifier.urihttps://repoemc.ukm.my/handle/123456789/1398
dc.language.isoen
dc.publisherSpringer
dc.publisher.alternativeEnvironmental Earth Sciences
dc.subjectIron-oxyhydroxide
dc.subjectClay
dc.subjectQuaternary
dc.subjectSoil
dc.subjectGoethite
dc.subjectHematite
dc.subjectAlluvial
dc.titleAn integrated toolkit using multiple methods for determining the potential sources of iron and manganese in groundwater: a case study from the lower Kelantan River Basin, Malaysia
dc.typeJournal

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