Nickel mobilization during single-stage aqueous mineral carbonation of serpentinized peridotite at 185 °C and PCO₂ of 100 bar

Forsterite-rich ultramafic rocks, such as serpentinized peridotites, are considered highly promising natural materials for mineral carbonation – a carbon capture and storage (CCS) technique aimed at reducing atmospheric carbon dioxide (CO 2 ) by sequestering carbon as carbonate minerals. These rocks are commonly characterized by a high content of divalent cations, including nickel (Ni 2 + ), whose behavior and mobility during mineral carbonation remain insufficiently understood. This issue is critical, as the large-scale application of mineral carbonation may pose ecotoxicological risks by mobilizing specific metallic elements naturally occurring in ultramafic rocks. To elucidate possible Ni mobility during single-stage aqueous mineral carbonation, 15 g of powdered serpentinized peridotite was carbonated in a batch-type reactor for 96 hours at 185°C and a P CO₂ of 100 bar. The experiment resulted in the dissolution of forsterite and the extensive crystallization of magnesite, demonstrating that the serpentinized peridotite is a highly effective natural material for permanent CO 2 storage in the single-stage carbonation processes. Nickel released during the dissolution of forsterite (approximately 50 % of the whole Ni budget) was mainly incorporated in newly formed Ni-rich phyllosilicates (more than 98 %) and a small portion was mobilized into the post-carbonation fluid (less than 2 %), reaching a concentration of approximately18 mg/kg after 96 hours. The presence of Ni in newly crystallized magnesite crystals has not been detected. These results suggest that the behavior of Ni during single-stage mineral carbonation is complex and requires careful monitoring to prevent potential negative impacts on the natural environment. • Serpentinized peridotite was carbonated to investigate Ni mobilization. • Forsterite was identified as the primary source of Ni²⁺ release. • Magnesite constituted 46 wt% of post-carbonation solid products. • More than 98 % of the mobilized Ni was incorporated into Ni-phyllosilicates. • After 96 h of carbonation, the Ni content in the fluid reached 18 mg/kg.

Authors

Institutions

Publication Details

Journal
Journal of CO2 Utilization
Published
2025-05-19
DOI
https://doi.org/10.1016/j.jcou.2025.103119
Citations
3
Primary Topic
CO2 Sequestration and Geologic Interactions
Type
article
Field-Weighted Citation Impact
2.40
Controls
|||
ALL TIME
JAN
FEB
MAR
APR
MAY
JUN
JUL
AUG
SEP
OCT
article

Nickel mobilization during single-stage aqueous mineral carbonation of serpentinized peridotite at 185 °C and PCO₂ of 100 bar

Artur Pędziwiatr, Krzysztof Turniak, Maciej Róziewicz, Alicja Lacinska et al.
3 citations
Journal of CO2 Utilization
CO2 Sequestration and Geologic Interactions
2.40
article

Nickel mobilization during single-stage aqueous mineral carbonation of serpentinized peridotite at 185 °C and PCO₂ of 100 bar

Artur Pędziwiatr, Krzysztof Turniak, Maciej Róziewicz, Alicja Lacinska, Agata Łamacz, Błażej Cieślik, Anna Pietranik, Jakub Kierczak
article en
3 citations

Abstract

Forsterite-rich ultramafic rocks, such as serpentinized peridotites, are considered highly promising natural materials for mineral carbonation – a carbon capture and storage (CCS) technique aimed at reducing atmospheric carbon dioxide (CO 2 ) by sequestering carbon as carbonate minerals. These rocks are commonly characterized by a high content of divalent cations, including nickel (Ni 2 + ), whose behavior and mobility during mineral carbonation remain insufficiently understood. This issue is critical, as the large-scale application of mineral carbonation may pose ecotoxicological risks by mobilizing specific metallic elements naturally occurring in ultramafic rocks. To elucidate possible Ni mobility during single-stage aqueous mineral carbonation, 15 g of powdered serpentinized peridotite was carbonated in a batch-type reactor for 96 hours at 185°C and a P CO₂ of 100 bar. The experiment resulted in the dissolution of forsterite and the extensive crystallization of magnesite, demonstrating that the serpentinized peridotite is a highly effective natural material for permanent CO 2 storage in the single-stage carbonation processes. Nickel released during the dissolution of forsterite (approximately 50 % of the whole Ni budget) was mainly incorporated in newly formed Ni-rich phyllosilicates (more than 98 %) and a small portion was mobilized into the post-carbonation fluid (less than 2 %), reaching a concentration of approximately18 mg/kg after 96 hours. The presence of Ni in newly crystallized magnesite crystals has not been detected. These results suggest that the behavior of Ni during single-stage mineral carbonation is complex and requires careful monitoring to prevent potential negative impacts on the natural environment. • Serpentinized peridotite was carbonated to investigate Ni mobilization. • Forsterite was identified as the primary source of Ni²⁺ release. • Magnesite constituted 46 wt% of post-carbonation solid products. • More than 98 % of the mobilized Ni was incorporated into Ni-phyllosilicates. • After 96 h of carbonation, the Ni content in the fluid reached 18 mg/kg.

Journal of CO2 UtilizationVol. 97
Wrocław University of Science and Technology (PL), British Geological Survey (GB), Warsaw University of Life Sciences (PL), Geological Institute (RU), Institute of Geological Sciences (UA), AGH University of Krakow (PL)
Openalex Percentile: Top 12%
CO2 Sequestration and Geologic Interactions
2.40
AI Navigator

Ask Laika to Summarize, Analyze, and Connect papers live on the map.

Summarize Papers & Methodologies

Extract key findings, datasets, and comparative methods across publications.

Benchmark Rankings & Visual Analytics

Rank top research institutions, authors, funders, topics, and journals by Field-Weighted Citation Impact (FWCI) and paper volume with instant charts.

Connect Distant Disciplines

Bridge topological clusters on the map to find hidden collaborative intersections.