Morphological Study of Surface Magnetic Minerals, Case Study of North Banjarmasin Settlement Areas

We have conducted research to identify the morphology of magnetic minerals from the land in the Banjarmasin regional settlement area. We used scanning electron microscopy and energy dispersive X-ray spectroscopy (SEM EDS) on the soil sample to look at the shape of its magnetic minerals. In nature, magnetic minerals can indicate the presence of heavy metals. The shape of a magnetic mineral can reveal its origin in either the litogenic or anthropogenic processes. There were mostly pseudo-single domain grains (3.29–10 m) and multidomain grains (> 10–134.69 m) in the study area. The multidomain grains came in the shapes of sperules, irregulars, angles, and prisms. These results indicate that in the residential land location there are magnetic mineral grains originating from litogenic and anthropogenic processes.

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Publication Details

Journal
Jurnal Fisika Flux Jurnal Ilmiah Fisika FMIPA Universitas Lambung Mangkurat
Published
2024-12-28
DOI
https://doi.org/10.20527/flux.v21i3.20532
Primary Topic
Geological and Geophysical Studies
Type
article
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article

Morphological Study of Surface Magnetic Minerals, Case Study of North Banjarmasin Settlement Areas

Sudarningsih Sudarningsih, Tetti Novalina Manik, Fahruddin Fahruddin, Dzikri Dzikri
Jurnal Fisika Flux Jurnal Ilmiah Fisika FMIPA Universitas Lambung Mangkurat
Geological and Geophysical Studies
article

Morphological Study of Surface Magnetic Minerals, Case Study of North Banjarmasin Settlement Areas

Sudarningsih Sudarningsih, Tetti Novalina Manik, Fahruddin Fahruddin, Dzikri Dzikri
article en

Abstract

We have conducted research to identify the morphology of magnetic minerals from the land in the Banjarmasin regional settlement area. We used scanning electron microscopy and energy dispersive X-ray spectroscopy (SEM EDS) on the soil sample to look at the shape of its magnetic minerals. In nature, magnetic minerals can indicate the presence of heavy metals. The shape of a magnetic mineral can reveal its origin in either the litogenic or anthropogenic processes. There were mostly pseudo-single domain grains (3.29–10 m) and multidomain grains (> 10–134.69 m) in the study area. The multidomain grains came in the shapes of sperules, irregulars, angles, and prisms. These results indicate that in the residential land location there are magnetic mineral grains originating from litogenic and anthropogenic processes.

Jurnal Fisika Flux Jurnal Ilmiah Fisika FMIPA Universitas Lambung MangkuratVol. 21(3)
Lambung Mangkurat University (ID)
Openalex Percentile: Top 49%
Geological and Geophysical Studies
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