Pregled bibliografske jedinice broj: 1122548
Unseeded, spontaneous nucleation of spherulitic magnesium calcite
Unseeded, spontaneous nucleation of spherulitic magnesium calcite // Journal of colloid and interface science, 593 (2021), 359-369 doi:10.1016/j.jcis.2021.03.002 (međunarodna recenzija, članak, znanstveni)
CROSBI ID: 1122548 Za ispravke kontaktirajte CROSBI podršku putem web obrasca
Naslov
Unseeded, spontaneous nucleation of spherulitic
magnesium calcite
Autori
Prus, Marzena ; Li, Chunhui ; Kedra-Krolik, Karolina ; Piasecki, Wojciech ; Lament, Karolina ; Begović, Tajana ; Zarzycki, Piotr
Izvornik
Journal of colloid and interface science (0021-9797) 593
(2021);
359-369
Vrsta, podvrsta i kategorija rada
Radovi u časopisima, članak, znanstveni
Ključne riječi
Magnesium calcite, Spherulites, Molecular simulations, Solid transformation, Precipitation-dissolution, Growth rate
Sažetak
Most of the sedimentary carbonates deposited in the marine environments are composed of calcium carbonate minerals with varying amounts of incorporated Mg2+. However, understanding how interactions of impurities with carbonate and their incorporation affect sediments behavior remains a challenge. Here, a new insight is obtained by monitoring solution composition, morphology, and electrokinetic potential of carbonate particles formed in a spontaneous unseeded batch precipitation experiment using electrochemical and scanning electron microscopy methods. The solid composition and growth rate are extracted from changes in the bulk composition and fitted to chemical affinity rate law, revealing that the precipitation pathway consists of second-order dissolution and first-order precipitation. The molecular dynamics simulations show that the lattice strain induced by randomly substituting Ca2+ by Mg2+ stabilizes spherical nanoparticles and reduces their surface area and volume. Combining kinetics and thermodynamics insight, we conclude that variation in the carbonate bulk and interfacial energies, along with the solution supersaturation, lead to the dissolution-precipitation transformation pathway from Mg-rich to Mg-poor carbonate phase that preserves spherulitic morphology. Our findings are relevant for long-standing questions of how impurities influence diagenesis of carbonate sediments and spherulitic carbonate particles’ origin.
Izvorni jezik
Engleski
Znanstvena područja
Kemija
POVEZANOST RADA
Ustanove:
Prirodoslovno-matematički fakultet, Zagreb
Profili:
Tajana Begović
(autor)
Citiraj ovu publikaciju:
Časopis indeksira:
- Current Contents Connect (CCC)
- Web of Science Core Collection (WoSCC)
- Science Citation Index Expanded (SCI-EXP)
- SCI-EXP, SSCI i/ili A&HCI
- Scopus
- MEDLINE