Influence of microstructure and atomic-scale chemistry on iron ore reduction with hydrogen at 700{\deg}C

TL;DR

This paper investigates how microstructure and atomic-scale chemistry influence hydrogen reduction of iron ore at 700°C, aiming to optimize processes for greener steel production and reduce CO2 emissions.

Contribution

It provides a detailed multi-scale analysis of iron ore reduction with hydrogen, highlighting microstructural and chemical factors affecting reaction kinetics.

Findings

Microstructure significantly impacts reduction rates.

Atomic-scale chemistry influences reaction pathways.

Insights enable improved ore processing for sustainable steel manufacturing.

Abstract

With 1.85 billion tons produced per year, steel is the most important material class in terms of volume and environmental impact. While steel is a sustainability enabler, for instance through lightweight design, magnetic devices, and efficient turbines, its primary production is not. For 3000 years, iron has been reduced from ores using carbon. Today 2.1 tons CO2 are produced per ton of steel, causing 30% of the global CO2 emissions in the manufacturing sector, which translates to 6.5% of the global CO2 emissions. These numbers qualify iron- and steel-making as the largest single industrial greenhouse gas emission source. The envisaged future industrial route to mitigate these CO2 emissions targets green hydrogen as a reductant. Although this reaction has been studied for decades, its kinetics is not well understood, particularly during the wustite reduction step which is dramatically slower than the hematite reduction. Many rate-limiting factors of this reaction are set by the micro- and nanostructure as well as the local chemistry of the ores. Their quantification allows knowledge-driven ore preparation and process optimization to make the hydrogen-based reduction of iron ores commercially viable, enabling the required massive CO2 mitigation to ease global warming. Here, we report on a multi-scale structure and composition analysis of iron reduced from hematite with pure H2, reaching down to near-atomic scale.