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Palabras clave – provistas por la editorial

CO2 reservoir rock; CO2 sealing capacity; CO2 sequestration; CO2 storage capacity; CO2 storage ratio; supercritical CO2; CO2 geological storage; depleted gas fields; deep saline aquifers; Adriatic offshore; Croatia; CO2 geological sequestration; unconsolidated sediments; gas hydrates; suitable methodology for mineral carbonation; construction and demolition waste; basalts; carbonation; CO2 storage; hydrochemistry; regional heat flow; CO2 leakage; cement; well integrity; leakage remediation; TOUGHREACT; reactive transport modelling; CCS; mineralization; carbonatization; mineral trapping; mineral sequestration; Johansen Formation; North Sea; sedimentary facies; serpentinite; X-ray diffraction; rietveld refinement; magnesium leaching; thermal activation; meta-serpentine; heat activation optimization; CO2 mineral sequestration; hydromagnesite; kerolite; Cu mine; Montecastelli; underground microclimate; replacement process; low temperature carbonate precipitation; Secondary Ion Mass Spectrometer; seawater influx; hydrothermal circulation; ophicalcite; n/a