2020
DOI: 10.1080/25726838.2020.1863013
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Geometallurgical characterisation of Mn ores

Abstract: This article details two geometallurgical case studies using classification schemes developed for Mn fine and lump ores. For the first, the relative abundance of 15 material types was compared to chemistry by size fraction. Positive correlations were evident between the proportion of aluminosilicate-bearing ore groups and Al 2 O 3 content, the ratio of Mn oxide/ Fe oxide ore groups and the Mn/Fe content, the proportion of cryptomelane-bearing groups and the K 2 O and BaO contents, and the ratio of hard to mode… Show more

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Cited by 3 publications
(3 citation statements)
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“…Assmang is a Wessels-type ore, which contains both braunite-I and braunite-II minerals (MnOÁ3Mn 2 O 3 ÁSiO 2 ), bixbyite ((Mn,Fe) 2 O 3 ), hematite (Fe 2 O 3 ) and carbonates ((Mg,Ca)CO 3 ), whereas Comilog is mineralogically dominated by pyrolusite (MnO 2 ), nsutite (Mn 4þ 1Àx Mn 2þ 2À2x OH ð Þ 2x ) and cryptomelane (KMn 8 O 16 ) and exhibits a relatively high level of microporosity. [29] The ores were ground and sieved into particle size fractions of 9.5 to 16 mm. The ores were chemically analyzed by SINTEF Norlab using X-ray fluorescence, while the oxygen amount connected to Mn-oxides was obtained by titration for ore, whereas Eltra (combustion-IR) was used to determine the amount of carbon, which was recalculated to CO 2 in the carbonate minerals.…”
Section: A Charge Materialsmentioning
confidence: 99%
“…Assmang is a Wessels-type ore, which contains both braunite-I and braunite-II minerals (MnOÁ3Mn 2 O 3 ÁSiO 2 ), bixbyite ((Mn,Fe) 2 O 3 ), hematite (Fe 2 O 3 ) and carbonates ((Mg,Ca)CO 3 ), whereas Comilog is mineralogically dominated by pyrolusite (MnO 2 ), nsutite (Mn 4þ 1Àx Mn 2þ 2À2x OH ð Þ 2x ) and cryptomelane (KMn 8 O 16 ) and exhibits a relatively high level of microporosity. [29] The ores were ground and sieved into particle size fractions of 9.5 to 16 mm. The ores were chemically analyzed by SINTEF Norlab using X-ray fluorescence, while the oxygen amount connected to Mn-oxides was obtained by titration for ore, whereas Eltra (combustion-IR) was used to determine the amount of carbon, which was recalculated to CO 2 in the carbonate minerals.…”
Section: A Charge Materialsmentioning
confidence: 99%
“…This is mainly because manganese ores used by industry in the production of FeMn alloys have different origins and therefore differ in mineralogy, chemical and physical properties. Typically, metallurgical grade ores contain more than 35 pct Mn and literature [8][9][10][11][12][13][14] covers properties of ores with Comilog, CVRD, Groote Eylandt, Wessels and Mamatwan type ores as examples. Several studies [10,11,[15][16][17][18][19][20][21][22] have been conducted on the prereduction of manganese ores by either CO gas or solid carbon.…”
Section: ½8mentioning
confidence: 99%
“…Comilog exhibit high level of microporosity and is mainly composed of pyrolusite (b-MnO 2 ), nsutite ((Mn 4+ ) (1Àx) (Mn 2+ )O (2À2x) (OH) 2x (x = 0.06 to 0.07)) and cryptomelane (K(Mn 4+ 7 ,Mn 3+ )O 16 ) minerals. UMK and Nchwaning contains both braunite-I ((Mn 2+ ,Mn 3+ )6(SiO 4 )O 8 ) and braunite-II (Ca(Mn 3+ ,Fe 3+ )6(SiO 4 )O 8 ) minerals, Nchwaning contains more bixbyite ((Mn 3+ ,Fe 3+ ) 2 O 3 ) and hematite (Fe 2 O 3 ) and less carbonate minerals compared to UMK ore. [12] Characterization of ores and products of prereduction was for porosity and chemical compositions. Techniques used for characterization include pycnometry, X-ray fluorescence (XRF), permanganometric titration, thermogravimetric and combustion-IR methods.…”
Section: A Characterization Of Raw Materials and Prereduced Productsmentioning
confidence: 99%