Adi Maulana

Adi Maulana


Research Focus & Metrics

Academic Career Length

14Years (2013-Present)

(Calculated once Scilit publication data is synced: current year − year of first publication + 1)

Representative Publications

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18 June 2014 in Journal of Earth Science
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AMAdi Maulana
Adi Maulana
KYKotaro Yonezu
Kotaro Yonezu
KWKoichiro Watanabe
Koichiro Watanabe

12 May 2021 in Resource Geology
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AIAkane Ito
Akane Ito
TOTsubasa Otake
Tsubasa Otake
AMAdi Maulana
Adi Maulana
KSKenzo Sanematsu
Kenzo Sanematsu
SUSufriadin
Sufriadin
Tsutomu SatoTsutomu Sato
Tsutomu Sato
Indonesia is one of the largest Ni ore producers in the world and is also expected to be an important potential source of some critical metals (e.g., Co, Sc, rare‐earth elements, and platinum‐group elements). However, few studies have examined Ni laterite deposits in this country. In this study, we investigate Ni enrichment and the potential accumulation of critical metals in four laterite profiles with varying degrees of serpentinization and weathering intensity in the Soroako and Pomalaa mining areas of Sulawesi, Indonesia. We integrate geochemical evaluation with a mass‐balance approach and mineralogical analysis to better constrain the geochemical factors influencing the mobilization of Ni during lateritization. Nickel contents in the saprolite horizon of the profiles that are strongly weathered and developed over serpentinized peridotite are higher than those that are weakly weathered and developed over unserpentinized harzburgite. The bulk Ni contents of saprolite horizons are related to Ni contents of Ni‐bearing Mg‐phyllosilicates, which suggests that Ni remobilization is the main control on Ni enrichment in the profiles. Mass‐balance calculations reveal that the amounts of gained Fe and Ni in the profiles are positively correlated. This relationship indicates that the redistribution of Ni is likely controlled by the aging of Ni‐bearing goethite (dissolution/recrystallization) involving ligand‐promoted dissolution by organic matter and/or reductive dissolution by microbial activity near the surface. Critical metals show enrichment in specific horizons. Enrichments in Co and rare‐earth elements are strongly influenced by the formation of Mn‐oxyhydroxides in the oxide zone of the profiles. In contrast, Sc, Pt, and Pd show residual enrichment patterns, with grades influenced mainly by their initial contents in bedrock. The profiles show a positive correlation between Sc and Fe, as reported for other Ni laterite deposits. Among the critical metals, Sc, Pt, and Pd contents in the studied profiles are comparable with values reported from other Ni laterite deposits worldwide.

1 March 2015 in Geochemistry
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Journal Article
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AMAdi Maulana
Adi Maulana
ACAndrew G. Christy
Andrew G. Christy
DEDavid J. Ellis
David J. Ellis

21 October 2013 in Island Arc
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Journal Article
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AMAdi Maulana
Adi Maulana
ACAndrew G. Christy
Andrew G. Christy
DEDavid J. Ellis
David J. Ellis
AIAkira Imai
Akira Imai
KWKoichiro Watanabe
Koichiro Watanabe

1 July 2016 in Journal of Asian Earth Sciences
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Journal Article
Closed access
AMAdi Maulana
Adi Maulana
AIAkira Imai
Akira Imai
TLTheo Van Leeuwen
Theo Van Leeuwen
KWKoichiro Watanabe
Koichiro Watanabe
KYKotaro Yonezu
Kotaro Yonezu
ASAnders Schersten
Anders Schersten

1 April 2019 in Journal of Asian Earth Sciences
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Journal Article
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AMAdi Maulana
Adi Maulana
ACAndrew G. Christy
Andrew G. Christy
DEDavid J. Ellis
David J. Ellis
MBMichael Bröcker
Michael Bröcker