TY - JOUR
T1 - Physical Properties of Interfacial Layers Developed on Weathered Silicates
T2 - A Case Study Based on Labradorite Feldspar
AU - Wild, Bastien
AU - Daval, Damien
AU - Micha, Jean Sébastien
AU - Bourg, Ian C.
AU - White, Claire E.
AU - Fernandez-Martinez, Alejandro
N1 - Publisher Copyright:
© 2019 American Chemical Society.
PY - 2019/10/10
Y1 - 2019/10/10
N2 - Amorphous silica-rich surface layers (ASSLs) formed at the interface between silicate materials and reacting fluids are known to strongly influence, at least in some cases, the dissolution rates of silicate phases including soil minerals, glasses, and cements. However, the factors governing the formation of these ASSLs remain largely unknown. Here, we outline a novel approach that uses recent developments in vertical scanning interferometry and in situ synchrotron-based X-ray reflectivity to directly follow the development of ASSLs and the evolution of their physical properties on a representative silicate, labradorite feldspar. Our approach enables independently probing the reactivities of the outer (bulk fluid/ASSL) interface and of the inner (ASSL/pristine mineral) interface in situ, providing a detailed picture of the temporal evolution of the fluid-mineral interface. We investigated the effects of pH, SiO2(aq) concentration, crystallographic orientation, and temperature on the layer thickness, density, and reactivity as well as on the dissolution rate of the primary mineral. The dissolution rate of labradorite crystals increased with temperature according to an apparent activation energy of ∼57 kJ mol-1 and showed no significant difference between crystallographic faces. Both labradorite and ASSL dissolution rates decreased as circum-neutral pH conditions were approached. High SiO2(aq) concentrations resulted in decreased apparent dissolution rates (even though far-from-equilibrium conditions with respect to labradorite were maintained in the bulk fluid) and in an increased ASSL density at least in some conditions (such as low temperature and close-to-neutral pH values). Our results highlight the importance of ASSLs and their complex impact on the dissolution process. In particular, our results provide evidence of a discrepancy between bulk fluid conditions, generally probed and reported, and those actually operating at the interface with the dissolving primary phase, which are of more direct relevance to the dissolution process but are still largely unknown.
AB - Amorphous silica-rich surface layers (ASSLs) formed at the interface between silicate materials and reacting fluids are known to strongly influence, at least in some cases, the dissolution rates of silicate phases including soil minerals, glasses, and cements. However, the factors governing the formation of these ASSLs remain largely unknown. Here, we outline a novel approach that uses recent developments in vertical scanning interferometry and in situ synchrotron-based X-ray reflectivity to directly follow the development of ASSLs and the evolution of their physical properties on a representative silicate, labradorite feldspar. Our approach enables independently probing the reactivities of the outer (bulk fluid/ASSL) interface and of the inner (ASSL/pristine mineral) interface in situ, providing a detailed picture of the temporal evolution of the fluid-mineral interface. We investigated the effects of pH, SiO2(aq) concentration, crystallographic orientation, and temperature on the layer thickness, density, and reactivity as well as on the dissolution rate of the primary mineral. The dissolution rate of labradorite crystals increased with temperature according to an apparent activation energy of ∼57 kJ mol-1 and showed no significant difference between crystallographic faces. Both labradorite and ASSL dissolution rates decreased as circum-neutral pH conditions were approached. High SiO2(aq) concentrations resulted in decreased apparent dissolution rates (even though far-from-equilibrium conditions with respect to labradorite were maintained in the bulk fluid) and in an increased ASSL density at least in some conditions (such as low temperature and close-to-neutral pH values). Our results highlight the importance of ASSLs and their complex impact on the dissolution process. In particular, our results provide evidence of a discrepancy between bulk fluid conditions, generally probed and reported, and those actually operating at the interface with the dissolving primary phase, which are of more direct relevance to the dissolution process but are still largely unknown.
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U2 - 10.1021/acs.jpcc.9b05491
DO - 10.1021/acs.jpcc.9b05491
M3 - Article
AN - SCOPUS:85073005614
SN - 1932-7447
VL - 123
SP - 24520
EP - 24532
JO - Journal of Physical Chemistry C
JF - Journal of Physical Chemistry C
IS - 40
ER -