Growth of Nanosized Calcite through Gas−Solid Carbonation of Nanosized Portlandite under Anisobaric Conditions

G. Montes-Hernandez; D. Daval; R. Chiriac; F. Renard

doi:10.1021/cg100714m

Journal articles

Growth of Nanosized Calcite through Gas−Solid Carbonation of Nanosized Portlandite under Anisobaric Conditions

G. Montes-Hernandez ¹ D. Daval ^{2, 3, 4} R. Chiriac ⁵ F. Renard ^{1, 6}

1 LGCA - Laboratoire de Géodynamique des Chaines Alpines

2 LGIT - Laboratoire de Géophysique Interne et Tectonophysique

3 LGE - Laboratoire de géologie de l'ENS

4 IPGP - Institut de Physique du Globe de Paris

5 LMI - Laboratoire des Multimatériaux et Interfaces

6 PGP - Physics of Geological Processes [Oslo]

Abstract : The gas−solid carbonation of nanosized portlandite was experimentally investigated using a static bed reactor under anisobaric conditions. The effects of initial CO2 pressure (10−40 bar), reaction temperature (30 and 60 °C), and relative humidity were investigated. Three steps of the carbonation process were determined: (1) instantaneous CO2 mineralization during CO2 injection period. From 25 to 40 wt % of initial portlandite grains were transformed into calcite during the CO2 injection period (from 0.9 to 2 min). (2) Fast CO2 mineralization after gas injection period (<5 h) followed by (3) a slow CO2 mineralization until an equilibrium state (<24 h). The results revealed high efficiency from portlandite-to-calcite transformation (>95%). For this case, the mineralization of CO2 does not form a protective carbonate layer around the reacting particles of portlandite as typically observed by other gas−solid carbonation methods. This method could be efficiently performed to produce nanosized calcite. Moreover, the separation of calcite particles from the fluid phase is most simple compared with precipitation methods. A kinetic pseudo-second-order model was satisfactorily used to describe the three CO2 mineralization steps except for the carbonation reaction initiated at 40 bar. In this latter case, a kinetic pseudo-first-order model was satisfactorily used; indicating that the slow CO2 mineralization step appears less significant during the carbonation process.

Document type :

Journal articles

Domain :

Sciences of the Universe [physics] / Earth Sciences / Geochemistry

Environmental Sciences / Global Changes

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https://hal-insu.archives-ouvertes.fr/insu-00549812
Contributor : Pascale Talour <>
Submitted on : Wednesday, December 22, 2010 - 5:21:19 PM
Last modification on : Friday, September 25, 2020 - 3:13:47 AM

Growth of Nanosized Calcite through Gas−Solid Carbonation of Nanosized Portlandite under Anisobaric Conditions

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Growth of Nanosized Calcite through Gas−Solid Carbonation of Nanosized Portlandite under Anisobaric Conditions

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