Difficulty: Easy
Correct Answer: Cobalt oxide
Explanation:
Introduction / Context:
Hematite iron ore primarily contains iron(III) oxide with various gangue minerals. Understanding typical impurities helps in beneficiation route selection and slag design in ironmaking.
Given Data / Assumptions:
Concept / Approach:
Titanium oxide and manganese oxide can occur as trace impurities; calcium oxide appears from carbonate gangue (e.g., calcite/dolomite) or flux addition, though not intrinsic to the hematite lattice. Cobalt oxide is not a typical component or common impurity associated with iron ore bodies on an appreciable level.
Step-by-Step Solution:
List likely impurities from geology: TiO2, MnO, SiO2, Al2O3, carbonates.Note that CoO occurrence is rare/negligible in iron ores.Select cobalt oxide as “not present.”
Verification / Alternative check:
Typical assay tables of hematite ores seldom record cobalt oxides; processing does not account for cobalt removal in iron ore circuits.
Why Other Options Are Wrong:
TiO2/MnO: observed in some ores.CaO: may occur via carbonates or be considered in gangue/flux context.SiO2: classic gangue mineral.
Common Pitfalls:
Assuming any listed oxide cannot occur; geology varies, but CoO is distinctly uncommon.
Final Answer:
Cobalt oxide
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