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Mapping the Chemical Composition of Nickel Laterites with Reflectance Spectroscopy at Koniambo, New Caledonia

机译:在新喀里多尼亚科尼亚博用反射光谱法绘制镍红土的化学成分图

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Reflectance spectroscopywas applied as a sampling tool for deriving compositional data of nickel laterites in the Koniambo deposits of New Caledonia. The aim of the work was to test the feasibility of acquiring spectral reflectance data for retrieving quantitative compositional information on nickel laterites exposed in mine bench walls as a routine sampling method for ore-grade control in a mining operation. The spectral reflectance data record complex variations in mineralogical and chemical compositions of nickel laterites. A key method tested in this work is a calibration procedure for converting spectral reflectance to weight percentage of chemical components. A partial least squares (PLS) analysis method was used for this purpose. The abundances of Ni, Fe, MgO, and SiO_2, the four most important chemical components collectively determining the economical value and the metallurgical behaviors of lateritic nickel ores, were modeled by the spectral reflectance data of a set of reference samples. The models were then validated by an independent set of samples with known chemical compositions. The validated models were applied to spectral reflectance data acquired on mine bench walls to derive the chemical compositions of lateritic ores. The results have confirmed that the chemical compositions of nickel laterites can be modeled and predicted with confidence by use of spectral reflectance data. Parameters used for modeling were selected based on the considerations of (1) simplicity of data processing, and (2) relationships between chemistry and mineralogy. Smoothed and background-removed spectral reflectance data of the 400 to 2,500 nm wavelengths were used for modeling Ni, Fe, MgO, and SiO_2. This work demonstrates that reflectance spectroscopy provides an efficient and effective sampling tool for deriving high density compositional data of nickel laterites. An approach combining reflectance spectroscopy with conventional sampling techniques will result in significant improvement on ore-grade control sampling in terms of representation and precision of data and savings on cost for sampling.
机译:反射光谱法被用作取样工具,以推导新喀里多尼亚科尼亚博矿床中镍红土的成分数据。该工作的目的是测试获取光谱反射率数据以检索矿山工作台壁中暴露的镍红土的定量组成信息的可行性,以此作为采矿作业中矿石品位控制的常规采样方法。光谱反射率数据记录了镍红土的矿物学和化学组成的复杂变化。在这项工作中测试的关键方法是将光谱反射率转换为化学成分重量百分比的校准程序。为此使用了偏最小二乘(PLS)分析方法。通过一组参考样品的光谱反射率数据对镍,铁,氧化镁和SiO_2的丰度(这四个最重要的化学成分共同决定红土镍矿的经济价值和冶金行为)进行了建模。然后通过一组独立的具有已知化学成分的样品对模型进行验证。将经过验证的模型应用于在矿井工作台壁上获得的光谱反射率数据,以得出红土矿石的化学成分。结果证实,可以通过使用光谱反射率数据对镍红土的化学成分进行建模和预测。基于以下考虑因素选择用于建模的参数:(1)数据处理的简便性,以及(2)化学与矿物学之间的关系。使用平滑和去除背景的400至2500 nm波长的光谱反射率数据对Ni,Fe,MgO和SiO_2进行建模。这项工作表明,反射光谱法提供了一种有效且有效的采样工具,用于导出镍红土的高密度成分数据。将反射光谱法与常规采样技术相结合的方法将在数据表示和精度方面显着改善矿石级控制采样,并节省采样成本。

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