Bauxite is the world’s principal source of aluminium and can vary from very soft earth to very hard rock. It can occur as red-yellow compacted earth (both friable and re-cemented), small red round pebbles (pisolites), or large pale (pink, white, buff) hard stones. Bauxite is a mixture of aluminium minerals, clay minerals, and insoluble materials. Three aluminium minerals principally occur in bauxite: gibbsite, boehmite and diaspore.
Once at the laboratory, sample preparation for DSO bauxites is usually limited to drying, weighing, crushing, sub-sampling and grinding the sample to less than 75 microns. For bauxites that are subject to beneficiation, sample preparation includes a screening step, additional drying and weighing steps, and the calculation of a percentage yield.
ALS offers routine multi-element geochemistry with high precision and accuracy necessary for bauxite ore analysis. Bauxite ore is mainly composed of aluminium hydroxide, gibbsite, boehmite and diaspore but may also contain iron oxides, goethite and hematite, kaolinite, anatase (TiO2), ilmenite (FeTiO3 or FeO.TiO2 ) and other minor or trace level impurities which can affect processing.
Although bauxite comprises a mixture of minerals, the industry standard analytical method for reporting the composition is by elemental analysis, expressed as metal oxides. This analysis is usually determined by X-Ray Fluorescence Spectrometry (XRF) available by ALS methods ME-XRF13u/n (unnormalised and normalised options). In addition, Loss on Ignition (LOI) is also measured by furnace or Thermogravimetric Analyser (TGA). This determines the loss of mass due to volatiles that are driven off when the sample is heated from 105°C to 1,000°C (i.e., after the removal of free moisture).
|Code||Analytes & ranges (%)||Description|
|Al2O3||0.01-100||MgO||0.01-40||SrO||0.01-1.5||Fused disc XRF. 0.7g sample.
as part of this
|Loss on Ignition.
|Furnace or Thermo-gravimetric Analyser (TGA)|
Analysis of bauxite by automated fusion/ loss on ignition system, HAG, is also available.
Impurities are often more important to consider than the alumina grade because of their detrimental effect. Silica is the most commercially important impurity in bauxite as generally the more silica in the bauxite, the higher the amount of caustic soda consumed in the refining process, and the higher the loss of alumina to the red mud tailings in the desilication product (DSP).
ALS offers methods for analysing available alumina and reactive silica at 145ᵒC by method ME-LICP01 and at 235ᵒC with method ME-LICP02. The temperature, caustic strength and sample/caustic weight ratio maybe requested for these methods.
|ME-LICP01||Reactive Silica and Available Alumina, 0.1-100%. Standard digestion temperature 145°C. Alternative temperatures, caustic strength and sample/caustic weight ratio may be requested.||1g sample. Microwave digestion, chemical separation and ICP-AES analysis.|
|ME-LICP02||Reactive Silica and Available Alumina, 0.1-100%. Standard digestion temperature 235°C. Alternative temperatures, caustic strength and sample/caustic weight ratio may be requested.||1g sample. Microwave digestion, chemical separation and ICP-AES analysis.|
Mineralogy is very important as it dictates the refining conditions that must be used and has a large bearing on the economics of processing bauxite. Alumina refineries are usually classified as either high temperature (>240°C) or low temperature (~143°C -150°C). Pure gibbsite or mixed gibbsite and boehmite deposits with a low boehmite content are usually sent to low temperature refineries. However, once the deposit has more than about 6% boehmite, then it must be sent to a high temperature refinery due to economics.
Fourier Transform-Near Infrared Spectroscopy (FT-NIR) can be used to determine the kaolinitic content of samples. The method requires a project specific calibration using multiple samples that have been analysed by an alternative technique. This information is used to set up a chemometric algorithm which is used to quantify kaolinite in subsequent samples.
|Code||Analytes & ranges||Description|
|Si-NIR07*||Kaolinitic Silica, 0.4%-100%.||2g sample Fourier Transform infrared (FT-NIR).|
Gibbsite - Al(OH)3 or Al2O3.3H2O: Commonly referred to as tri-hydrate due to the three lots of water. The three OH bonds are relatively weak and require the lowest refining temperature to break them, typically 143°C -150°C.
Boehmite - AlO(OH) or Al2O3.H2O: Commonly referred to as monohydrate due to the single water. The single OH bond is much stronger than the three bonds in gibbsite and requires a higher refining temperature to break it, typically 240-260°C
Diaspore - AlO(OH) or Al2O3.H2O: Has the same composition as boehmite but is denser and harder due to a different crystal form. Diaspore requires the highest refining temperatures to process, typically +260°C.
Please contact your local client services group who will in turn contact the laboratory that will be preforming the analysis to make the requested change. It is worth indicating all variations required on the sample submittal form.
The sample submittal form can be downloaded from this web page or obtained from your local client services group.
ALS has expert teams for mineralogy studies for all stages of exploration and mining.MORE INFORMATION