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Simulation of weathered profiles coupled with multivariate block-support simulation of the Puma nickel laterite deposit, Brazil

机译:仿真型材耦合,加上巴西美洲乳镍红土矿床的多变量阻滞仿真

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Modelling and assessing spatial variability and uncertainty of mineral deposits is critical for both capital investments in mining projects as well as operational issues once a mine is developed. However, traditional approaches for modelling geological domains and geostatistical estimation provide smoothed representations of the pertinent deposit attributes, ignore spatial variability and, thereby, can mislead downstream decisions. Spatial variability and related uncertainty in modelling mineral deposit characteristics of interest, ranging from metal content and geological boundaries to geomechanical-geotechnical rock properties, can be modelled and quantified by stochastic spatial simulations. This is demonstrated through a detailed, step-by-step application to the Puma deposit, a major nickel lateritic asset in Brazil, part of the Onca-Puma mining complex. To integrate the variability of the regolith profiles of the deposit, their thicknesses are calculated after an unwrinkling process is applied and the deposit is then jointly simulated using min/max autocorrelation factors (MAF). The realizations serve as geological boundaries within which Ni, Co, Fe, SiO2, MgO and Dry-tonnage factor (DTF) are subsequently jointly simulated directly at block support scale. The final result is a series of equally probable representations of the Puma deposit, which are used to quantify and assess the uncertainty about key aspects of the project at the Puma,deposit, such as the uncertainty of the in-situ resources documented herein, and the strict control of the ore's quality that feeds the ferronickel processing plant. The framework presented shows the advantages of the MAF and direct block simulation approaches for the efficient joint simulation of spatially variant geological attributes of large deposits for industrial environments. The methods presented are general, new in the context of geotechnical and geomechanical engineering, and can assist in the modelling of spatial variability and quantification of uncertainty linked to geotechnical rock properties and pertinent lithological boundaries. (C) 2016 Elsevier B.V. All rights reserved.
机译:矿产矿床的模型和评估空间变异性和不确定度对于矿业项目的资本投资以及开发矿井后的业务问题至关重要。然而,用于建模地质域和地质统计估算的传统方法提供了相关的存款属性的平滑表示,忽略了空间变异性,从而可以误导下游决策。利用矿物质沉积特性的空间变异性和相关的不确定度,从金属含量和地质边界到地质力学 - 岩土岩石性能的范围,通过随机空间模拟建模和量化。这是通过详细的,逐步申请来证明Puma矿床,巴西的主要镍蛋白矿产资产,部分ONCA-Puma采矿复合物。为了整合沉积物的可变性型材的可变性,在施加不包装过程之后计算它们的厚度,然后使用Min / MAX自相关因子(MAF)联合模拟沉积物。该实现用作地质边界,随后在嵌段支撑秤上直接连续模拟Ni,Co,Fe,SiO 2,MgO和干吨吨(DTF)。最终结果是Puma矿床的一系列同样可能的Puma押金表示,用于量化和评估PUMA,押金的项目的关键方面的不确定性,例如本文记录的原位资源的不确定性,以及严格控制矿石的质量,供铸造铁合金加工厂。提出的框架显示了MAF和直接块模拟方法的优点,用于工业环境大沉积的空间变体地质属性的有效联合模拟。所提出的方法是普遍的,在岩土和地质力学工程的背景下新的,并且可以帮助建模空间变异性和与岩土岩石特性相关的不确定性的量化和相关的岩性边界。 (c)2016年Elsevier B.v.保留所有权利。

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