Please use this identifier to cite or link to this item: https://hdl.handle.net/10356/90322
Title: Analysis of magnetic properties rocks and soils around the Danau Diatas, West Sumatra
Authors: Fajri, R. N.
Putra, R.
De Maisonneuve, Caroline Bouvet
Fauzi, A.
Yohandri
Rifai, H.
Keywords: Science::Geology
Diamagnetic
Rock Material
Issue Date: 2019
Source: Fajri, R. N., Putra, R., De Maisonneuve, C. B., Fauzi, A., Yohandri., & Rifai, H. (2019). Analysis of magnetic properties rocks and soils around the Danau Diatas, West Sumatra. Journal of Physics: Conference Series, 1185, 012024-. doi:10.1088/1742-6596/1185/1/012024
Series/Report no.: Journal of Physics: Conference Series
Abstract: The magnetic characteristics of the rocks have different magnetic properties of each kind. If this rock experiences weathering, then the rock material will be carried around the area such as the lake, through the wind, the water is then sedimentated. These sediments can also come from dust from volcanic eruptions (volcanic ash) where the magnetic properties that come from surrounding rocks are different from the magnetic properties derived from dust from volcanic eruptions. This study was used to determine the magnetic characteristics of rocks and soil around the Danau Diatas West Sumatra, which is one source of sediment. This the magnetic properties can be determined using rocks magnetism method that are commonly used to determine the magnetic properties of a material nature. Characteristics magnetic determined through test susceptibility magnetic using Bartington MS2B (Magnetic Suceptibility sensor B) dual frequency of 470 Hz and 4.7 kHz. Results this study shows values χ LF (susceptibility low frequency), χ hf (susceptibility high frequency) and χ fd % (susceptibility frequency dependent ). Value of susceptibility of rocks and soil obtained variations in the range of 23.77 × 10−8 m3 / kg - 2791.6 × 10−8 m3 / kg and 17.4 × 10−8 m3 / kg - 2804.4 × 10−8 m3 / kg. The value of magnetic suceptibility of rock and soil is included in the ferromagnetic mineral group and the types of minerals contained there in are ilmenite (FeTiO3) and hematite (Fe2O3). The value of frequency-dependent magnetic susceptibility χ fd (%) ranges from 0.4% to 13.5%. For the value of χ fd (%) 0.4% - 1.1% means that there is no or contains less than 10% superparamagnetic grain, for the value of χ fd (%) 3.3% means the mixture of superparamagnetic grain and coarser non-superparamagnetic grain, or superparamagnetic grain measuring < 0.005μm, and for the value of χ fd (%) 13.5%, meaning that the whole or consists of more than 75% superparamagnetic grains.
URI: https://hdl.handle.net/10356/90322
http://hdl.handle.net/10220/49436
ISSN: 1742-6588
DOI: http://dx.doi.org/10.1088/1742-6596/1185/1/012024
Rights: © 2019 The Author(s). Published by IOP Publishing Ltd. Content from this work may be used under the terms of the Creative Commons Attribution 3.0 licence. Any further distribution of this work must maintain attribution to the author(s) and the title of the work, journal citation and DOI.
Fulltext Permission: open
Fulltext Availability: With Fulltext
Appears in Collections:ASE Journal Articles

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