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Analisis Suseptibilitas Magnetik Tanah dan Laju Evapotranspirasi di Desa Ranooha, Kecamatan Ranomeeto, Kabupaten Konawe Selatan

Jurnal Penelitian Pendidikan Fisika · Vol. 5 No. 3 (2020) · pp. 227–232

DOI
10.36709/jipfi.v5i3.13444
ISSN
2715-551X, 2502-3861
Published
2020-08-27
Publisher
Universitas Halu Oleo
Language
eng
License
creativecommons.org/licenses/by-nc/4.0

Abstract

The problem in this research is how the magnetic susceptibility of the soil and the rate of evapotranspiration in Ranooha Village, Ranomeeto District, Konawe Selatan District. Soil magnetic susceptibility was measured using Bartington Susceptibility MS2B meter while evapotranspiration rate was measured using Lycimeter. Soil magnetic susceptibility analyzed consisted of three sampling points, each consisting of vegetation (grass) and non-vegetation (without grass) sites, with the same depth variations namely 0 cm, 10 cm, 20 cm, 30 cm, 40 cm and 50 cm. Each sample is coded V00, V10, V20, V30, V40, V50 for sampling at vegetation (grass) sites, and NV00, NV10, NV20, NV30, NV40, and NV50 for sampling at non-vegetation (without grass) sites. The measurement results show that variations in values of χLF range from a minimum value of 0.8 x 10-8 m3/ kg toa maximum value of 3.8 x 10-8 m3/ kg at point 1, minimum value of 0.8 x 10-8 m3/ kg up to a maximum value of 3.9 x 10-8 m3/ kg at point 2, and a minimum value of 0.9 x 10-8 m3/ kg up to a maximum value of 2.6 x 10-8 m3/ kg at point 3 for vegetation (grass). While variations in values of χLF rangefrom a minimum value of 1.7 x 10-8 m3/ kg to a maximum value of 2.4 x 10-8 m3/ kg at point 1, a minimum value of 1.6 x 10-8 m3/ kg up to a maximum value of 2.9 x 10-8 m3/ kg at point 2, and a minimum value of 1.6 x 10-8 m3/ kg up to a maximum value of 2.9 x 10-8 m3/ kg at point 3 for non vegetation (without grass). While the maximum rate of evapotranspiration occurs in November for 2018 which is 5.3 mm / day, while the maximum rate of evapotranspiration in 2019 also occurs in November which is 6.1 mm / day for vegetation (grass) sites. While the maximum rate of evapotranspiration occurs in October for 2018 which is 4.3 mm / day, while the maximum rate of evapotranspiration in 2019 occurs in November which is 5.7 mm / day for non-vegetation (without grass) sites

Keywords

Collaboration network of the authors

40 authors · 92 co-authorship links · showing the 40 most connected

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  • Universitas Halu Oleo
  • Jenderal Soedirman University
  • Affiliation unknown
  • Different organisations
  • Same organisation
  • Affiliation unknown
  • Thicker line = more joint articles · bigger circle = more articles
Show as table
Co-authorOrganisationJoint articles
Tahir TahirAffiliation unknown4
Amiruddin TakdaUniversitas Halu Oleo4
Arman ArmanUniversitas Halu Oleo3
Fahyuddin FahyuddinAffiliation unknown2
La SaharaAffiliation unknown2
La Ode RusmanAffiliation unknown2
Laode SafiuddinAffiliation unknown1
Saras SarasAffiliation unknown1
Vivi HastutiAffiliation unknown1
Suci Kris LukmanaAffiliation unknown1
Vivi Hastuti RMAffiliation unknown1
Rusdiman BuheraAffiliation unknown1
Nur Hasiyatin HamunduAffiliation unknown1
Mardi YunusAffiliation unknown1
Muhammad YasinUniversitas Halu Oleo1
Jahidin JahidinAffiliation unknown1
Sitti AsrianiAffiliation unknown1
Amran AmranJenderal Soedirman University1
I Nyoman SudianaAffiliation unknown1
Sitti KasmiatiAffiliation unknown1
HUSEIN HUSEINUniversitas Halu Oleo1
La Ode SaifuddinAffiliation unknown1
Mardiana NAffiliation unknown1
Mustari MustariAffiliation unknown1
Erniwati ErniwatiAffiliation unknown1
Agus TrisnawatiAffiliation unknown1
Halima HalimaAffiliation unknown1
Roliana EsoAffiliation unknown1
Muhammad AnasAffiliation unknown1
Nuri YantiAffiliation unknown1
La HusonoAffiliation unknown1
Nilawati UteUniversitas Halu Oleo1
Sri Hasriani HasranAffiliation unknown1
Wayan MurtayasaAffiliation unknown1
Hasmina Tari MokuiUniversitas Halu Oleo1
La Ode SaidmanAffiliation unknown1
Kasman KasmanAffiliation unknown1

Affiliations come from OpenAlex; journal OAI-PMH metadata carries none. Authors without an OpenAlex ID are matched by name, which can merge or split people.

Metadata source: OAI-PMH (metadata jurnal) https://ojs.uho.ac.id/index.php/JIPFI/oai, first harvested 31 Okt 2026, last seen 1 Nov 2026.
Original metadata (oai_dc) 
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	<dc:title xml:lang="en-US">Analisis Suseptibilitas Magnetik Tanah dan Laju Evapotranspirasi di Desa Ranooha, Kecamatan Ranomeeto, Kabupaten Konawe Selatan</dc:title>
	<dc:creator>Khairani, Miftah</dc:creator>
	<dc:creator>Eso, Rosliana</dc:creator>
	<dc:creator>Safiuddin, La Ode</dc:creator>
	<dc:subject xml:lang="en-US">Soil Magnetic Susceptibility, Evapotranspiration Rate, Bartington MS2B Susceptibility Method, Lycimeter Method</dc:subject>
	<dc:description xml:lang="en-US">The problem in this research is how the magnetic susceptibility of the soil and the rate of evapotranspiration in Ranooha Village, Ranomeeto District, Konawe Selatan District. Soil magnetic susceptibility was measured using Bartington Susceptibility MS2B meter while evapotranspiration rate was measured using Lycimeter. Soil magnetic susceptibility analyzed consisted of three sampling points, each consisting of vegetation (grass) and non-vegetation (without grass) sites, with the same depth variations namely 0 cm, 10 cm, 20 cm, 30 cm, 40 cm and 50 cm. Each sample is coded V00, V10, V20, V30, V40, V50 for sampling at vegetation (grass) sites, and NV00, NV10, NV20, NV30, NV40, and NV50 for sampling at non-vegetation (without grass) sites. The measurement results show that variations in values of χLF range from a minimum value of 0.8 x 10-8 m3/ kg toa maximum value of 3.8 x 10-8 m3/ kg at point 1, minimum value of 0.8 x 10-8 m3/ kg up to a maximum value of 3.9 x 10-8 m3/ kg at point 2, and a minimum value of 0.9 x 10-8 m3/ kg up to a maximum value of 2.6 x 10-8 m3/ kg at point 3 for vegetation (grass). While variations in values of χLF rangefrom a minimum value of 1.7 x 10-8 m3/ kg to a maximum value of 2.4 x 10-8 m3/ kg at point 1, a minimum value of 1.6 x 10-8 m3/ kg up to a maximum value of 2.9 x 10-8 m3/ kg at point 2, and a minimum value of 1.6 x 10-8 m3/ kg up to a maximum value of 2.9 x 10-8 m3/ kg at point 3 for non vegetation (without grass). While the maximum rate of evapotranspiration occurs in November for 2018 which is 5.3 mm / day, while the maximum rate of evapotranspiration in 2019 also occurs in November which is 6.1 mm / day for vegetation (grass) sites. While the maximum rate of evapotranspiration occurs in October for 2018 which is 4.3 mm / day, while the maximum rate of evapotranspiration in 2019 occurs in November which is 5.7 mm / day for non-vegetation (without grass)  sites</dc:description>
	<dc:publisher xml:lang="en-US">Universitas Halu Oleo</dc:publisher>
	<dc:contributor xml:lang="en-US"></dc:contributor>
	<dc:date>2020-08-27</dc:date>
	<dc:type>info:eu-repo/semantics/article</dc:type>
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	<dc:identifier>https://ojs.uho.ac.id/index.php/JIPFI/article/view/13444</dc:identifier>
	<dc:identifier>10.36709/jipfi.v5i3.13444</dc:identifier>
	<dc:source xml:lang="en-US">Jurnal Penelitian Pendidikan Fisika; Vol 5, No 3 (2020): Jurnal Penelitian Pendidikan Fisika; 227-232</dc:source>
	<dc:source>2715-551X</dc:source>
	<dc:source>2502-3861</dc:source>
	<dc:language>eng</dc:language>
	<dc:relation>https://ojs.uho.ac.id/index.php/JIPFI/article/view/13444/9656</dc:relation>
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	<dc:rights xml:lang="en-US">Copyright (c) 2020 Jurnal Penelitian Pendidikan Fisika</dc:rights>
	<dc:rights xml:lang="en-US">http://creativecommons.org/licenses/by-nc/4.0</dc:rights>
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