Geological and Mineralogical Sequestration of CO<sub>2</sub>

The rapid increasing of concentrations of anthropologically generated greenhouse gases (primarily CO2) in the atmosphere is responsible for global warming and ocean acidification. The International Panel on Climate Change (IPCC) indicates that carbon capture and storage (CCS) techniques are a necess...

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Other Authors: Ruggieri, Giovanni (Editor), Gherardi, Fabrizio (Editor)
Format: Book Chapter
Published: Basel, Switzerland MDPI - Multidisciplinary Digital Publishing Institute 2020
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Online Access:Get Fullteks
DOAB: description of the publication
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042 |a dc 
072 7 |a GP  |2 bicssc 
072 7 |a R  |2 bicssc 
100 1 |a Ruggieri, Giovanni  |4 edt 
700 1 |a Gherardi, Fabrizio  |4 edt 
700 1 |a Ruggieri, Giovanni  |4 oth 
700 1 |a Gherardi, Fabrizio  |4 oth 
245 1 0 |a Geological and Mineralogical Sequestration of CO<sub>2</sub> 
260 |a Basel, Switzerland  |b MDPI - Multidisciplinary Digital Publishing Institute  |c 2020 
300 |a 1 electronic resource (198 p.) 
506 0 |a Open Access  |2 star  |f Unrestricted online access 
520 |a The rapid increasing of concentrations of anthropologically generated greenhouse gases (primarily CO2) in the atmosphere is responsible for global warming and ocean acidification. The International Panel on Climate Change (IPCC) indicates that carbon capture and storage (CCS) techniques are a necessary measure to reduce greenhouse gas emissions in the short-to-medium term. One of the technological solutions is the long-term storage of CO2 in appropriate geological formations, such as deep saline formations and depleted oil and gas reservoirs. Promising alternative options that guarantee the permanent capture of CO2, although on a smaller scale, are the in-situ and ex-situ fixation of CO2 in the form of inorganic carbonates via the carbonation of mafic and ultramafic rocks and of Mg/Ca-rich fly ash, iron and steel slags, cement waste, and mine tailings. According to this general framework, this Special Issue collects articles covering various aspects of recent scientific advances in the geological and mineralogical sequestration of CO2. In particular, it includes the assessment of the storage potential of candidate injection sites in Croatia, Greece, and Norway; numerical modelling of geochemical-mineralogical reactions and CO2 flow; studies of natural analogues providing information on the processes and the physical-chemical conditions characterizing serpentinite carbonation; and experimental investigations to better understand the effectiveness and mechanisms of geological and mineralogical CO2 sequestration. 
540 |a Creative Commons  |f https://creativecommons.org/licenses/by/4.0/  |2 cc  |4 https://creativecommons.org/licenses/by/4.0/ 
546 |a English 
650 7 |a Research & information: general  |2 bicssc 
650 7 |a Earth sciences, geography, environment, planning  |2 bicssc 
653 |a CO2 reservoir rock 
653 |a CO2 sealing capacity 
653 |a CO2 sequestration 
653 |a CO2 storage capacity 
653 |a CO2 storage ratio 
653 |a supercritical CO2 
653 |a CO2 geological storage 
653 |a depleted gas fields 
653 |a deep saline aquifers 
653 |a Adriatic offshore 
653 |a Croatia 
653 |a CO2 geological sequestration 
653 |a unconsolidated sediments 
653 |a gas hydrates 
653 |a suitable methodology for mineral carbonation 
653 |a construction and demolition waste 
653 |a basalts 
653 |a carbonation 
653 |a CO2 storage 
653 |a hydrochemistry 
653 |a regional heat flow 
653 |a CO2 leakage 
653 |a cement 
653 |a well integrity 
653 |a leakage remediation 
653 |a TOUGHREACT 
653 |a reactive transport modelling 
653 |a CCS 
653 |a mineralization 
653 |a carbonatization 
653 |a mineral trapping 
653 |a mineral sequestration 
653 |a Johansen Formation 
653 |a North Sea 
653 |a sedimentary facies 
653 |a serpentinite 
653 |a X-ray diffraction 
653 |a rietveld refinement 
653 |a magnesium leaching 
653 |a thermal activation 
653 |a meta-serpentine 
653 |a heat activation optimization 
653 |a CO2 mineral sequestration 
653 |a hydromagnesite 
653 |a kerolite 
653 |a Cu mine 
653 |a Montecastelli 
653 |a underground microclimate 
653 |a replacement process 
653 |a low temperature carbonate precipitation 
653 |a Secondary Ion Mass Spectrometer 
653 |a seawater influx 
653 |a hydrothermal circulation 
653 |a ophicalcite 
653 |a n/a 
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856 4 0 |a www.oapen.org  |u https://directory.doabooks.org/handle/20.500.12854/69043  |7 0  |z DOAB: description of the publication