Accurate classification of nickel laterite mineral resources is a crucial element in
supporting sustainable and efficient mining operations. This classification process
is typically conducted by experts who consider various factors, including
geological models, sampling density, and drill hole configurations. However, the
uncertainties associated with classification decisions are often inadequately
accounted for. This study aims to evaluate two geostatistical methods, namely
conditional simulation and specific area. Both techniques are applied for
classifying nickel laterite mineral resources in Central Halmahera, North Maluku,
Indonesia, focusing on both plateau and coastal deposit types.
The conditional simulation method is employed to capture spatial variability and
uncertainty, while the specific areamethod serves to assess the efficiency of drill
hole spacing in resource classification. The data utilized includes geological
characteristics, nickel accumulation, and other related variables obtained from two
deposit locations: plateau and coastal. Analysis is conducted using the
geostatistical software Isatis.neo for variography, estimation, and simulation.
This study compares various drilling configurations while considering
uncertainties related to nominal production as support. A dataset comprising 953
drill holes in the plateau deposit and 612 drill holes in the coastal deposit, spaced
at 50 meters, is used to investigate the performance of these methods. Infill drill
holes (grade control data) is added as well with drill hole mesh of 25m and 12.5m
for plateau and coastal deposit, respectively.
The results indicate that the conditional simulation method provides more accurate
estimates at closer drill hole spacings, as indicated by the increase in the
probability of the simulation over the estimated, while the specific area method
offers a more conservative view of resource classification. For plateau deposits, an
optimal drill hole spacing of 25m × 25m is required for measured resource
classifications in both limonite and saprolite layers. In contrast, for coastal
deposits, a tighter spacing of 12.5m × 12.5m is recommended for measured
classifications in the limonite and fine saprolite layers, while 25m × 25m is
sufficient for the saprolite layer.
Findings demonstrate that both methods can be synergistically employed to classify
mineral resources within a two-dimensional context. The specific area method
functions as a routine to obtain a good order of magnitude and to determine drill
holes that delineate the boundaries between Mineral Resource classifications.
Meanwhile, conditional simulation can be utilized to validate these boundaries.
This research significantly contributes to the development of more accurate and
effective mineral resource classification methods, which has implications for
improved decision-making in the mining industry.
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