PENGARUH TINGKAT PELAPUKAN TERHADAP KADAR NIKEL LATERIT PADA DAERAH USSU, KEC. MALILI KAB. LUWU TIMUR PROV. SULAWESI SELATAN

Authors

  • Muhamad Hardin Wakila Department of Mining Engineering, Faculty of Industrial Technology, Universitas Muslim Indonesia
  • Andi Fahdli Heriansyah Jurusan Teknik Pertambangan, Universitas Muslim Indonesia
  • Firdaus Jurusan Teknik Pertambangan, Universitas Muslim Indonesia
  • Sitti Ratmi Nurhawaisyah Jurusan Teknik Pertambangan, Universitas Muslim Indonesia

DOI:

https://doi.org/10.33536/jg.v7i01.1302

Keywords:

logging, nikel laterit, pelapukan, pemboran

Abstract

The impact of seasonal changes will affect the level of weathering, and the grade of laterite  nickel. The purpose of this study was to determine the effect of weathering levels on the grade  of laterite nickel. The method used is direct observation and description of core samples from  drill holes that represent sloping areas and steep areas. The results of the description will be analyzed so that the grade values in each drill hole are known, both drill holes in sloping areas and drill holes in steep areas. The results obtained showed that the drill holes representing the sloping areas of DH-016, DH-015, DH-014, and DH-O13, had relatively high limonite thicknesses ranging from 8 to 17 meters, and the thickness of the saprolite zone ranged from 8 to 16 meters, and has Ni limonite zone grades ranging from 0.85% to 1.01%, and Ni saprolite zone grades ranging from 1.88% to 2.01%. This is inversely proportional to the drill hole which represents a steep area where the thickness of the limonite zone only reaches 1 meters, and the thickness of the saprolite zone is only 2 to 5 meters, and the Ni grade of the limonite zone ranges from 0.49% to 0.71%, and the grades value the saprolite zone Ni ranged from 1.43% to 1.54%, and bedrock zones were also found with a range of Ni grades ranging from 0.94% to 1.06%. From the results above it can be concluded that weathering affects the Ni content, because the higher the level of weathering in an area, the higher the Ni content in the area.

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References

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Nahon, D., 1986. Evolution of iron crusts in tropical landscapes. In: Rates of Chemical Weathering of Rocks and Minerals (pp. 169-191). Academic Press, London.

Sufriadin. 2013. Mineralogi, Geokimia Dan Perilaku “Leaching” Pada Endapan Laterit Nikel Soroako, Sulawesi Selatan, Indonesia. Disertasi. Universitas Gadjah Mada.

Syafrizal., Heriawan MN., Notosiswoyo S., Anggayana K. 2009. Morphology and Geologic Structure Control of Nickel Laterite Depositian: Case Study Nickel Laterite Deposit in the Gee Island and Pakal Island, East Halmahera, North Maluku. International ConferenceEarth Science and Technology (Volume 1). Yogyakarta, Indonesia Department ofGeological Engineering, Gadjah Mada University.Tim Geologi PT. PUL. 2010 “Laporan Teknis Izin Usaha Pertambangan” PT.PUL, Malili.

Waheed, Ahmad., 2001. Nickel Laterites-A Trainning Manual: Chemistry, Mineralogy, and Formation of Ni Laterites, INCO, tidak dipublikasikan.

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Published

30-04-2019

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Section

Articles

How to Cite

PENGARUH TINGKAT PELAPUKAN TERHADAP KADAR NIKEL LATERIT PADA DAERAH USSU, KEC. MALILI KAB. LUWU TIMUR PROV. SULAWESI SELATAN. (2019). Jurnal Geomine, 7(01), 30-35. https://doi.org/10.33536/jg.v7i01.1302

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