Legacy
iron (Fe) and steel wastes have been identified as a significant
source of silicate minerals, which can undergo carbonation reactions
and thus sequester carbon dioxide (CO
2
). In reactor experiments,
i.e., at elevated temperatures, pressures, or CO
2
concentrations,
these wastes have high silicate to carbonate conversion rates. However,
what is less understood is whether a more “passive”
approach to carbonation can work, i.e., whether a traditional slag
emplacement method (heaped and then buried) promotes or hinders CO
2
sequestration. In this paper, the results of characterization
of material retrieved from a first of its kind drilling program on
a historical blast furnace slag heap at Consett, U.K., are reported.
The mineralogy of the slag material was near uniform, consisting mainly
of melilite group minerals with only minor amounts of carbonate minerals
detected. Further analysis established that total carbon levels were
on average only 0.4% while average calcium (Ca) levels exceeded 30%.
It was calculated that only ∼3% of the CO
2
sequestration
potential of the >30 Mt slag heap has been utilized. It is suggested
that limited water and gas interaction and the mineralogy and particle
size of the slag are the main factors that have hindered carbonation
reactions in the slag heap.