The reactivity of calcite, one of the most abundant minerals in the earth’s crust, is determined by the molecular details of its interface with the contacting solution. Recently, it has been found that trace concentrations of NaNO3 severely affect calcite’s (104) surface and its reactivity. Here we combine molecular dynamics (MD) simulations, X-ray reflectivity (XR) and in situ atomic force microscopy (AFM) to probe the calcite (104) – water interface in the presence of NaNO3. Simulations reveal density profiles of different ions near calcite’s surface, with NO3− able to reach closer to the surface than CO32− and in higher concentrations. Reflectivity measurements show a structural destabilisation of the (104) surfaces’ topmost atomic layer...
In-situ atomic force microscopy (AFM) experiments were performed to study the overall process of dis...
John S. Ions and the calcite-water (10.4) interface - investigated with three-dimensional atomic for...
Söngen H, Schlegel SJ, Morais Jaques Y, et al. Water Orientation at the Calcite-Water Interface. The...
The reactivity of calcite, one of the most abundant minerals in the earth’s crust, is determined by ...
Calcite is among the most abundant minerals on earth and plays a central role in many environmental ...
It seems natural to assume that defects at mineral surfaces critically influence interfacial process...
Marutschke C, Walters D, Cleveland J, Hermes I, Bechstein R, Kühnle A. Three-dimensional hydration l...
The interaction of organic molecules with the surface of calcite plays a central role in many geoche...
The physico-chemical mechanisms by which rock-forming minerals dissolve in natural fluids are contro...
When two mineral surfaces are compressed against each other in aqueous environment, surface forces a...
Funding Information: Financial support from the German Research Foundation through grant KU1980/14-1...
Carbonate-bearing rocks in the upper Earth’s crust are prone to continuous changes under influences ...
Calcite–water interactions are important not only in carbon sequestration and the global carbon cyc...
The interactions of trivalent lanthanides and actinides with secondary mineral phases such as calcit...
Lateral Force Microscopy (LFM) studies were carried out on cleaved calcite sections in contact with ...
In-situ atomic force microscopy (AFM) experiments were performed to study the overall process of dis...
John S. Ions and the calcite-water (10.4) interface - investigated with three-dimensional atomic for...
Söngen H, Schlegel SJ, Morais Jaques Y, et al. Water Orientation at the Calcite-Water Interface. The...
The reactivity of calcite, one of the most abundant minerals in the earth’s crust, is determined by ...
Calcite is among the most abundant minerals on earth and plays a central role in many environmental ...
It seems natural to assume that defects at mineral surfaces critically influence interfacial process...
Marutschke C, Walters D, Cleveland J, Hermes I, Bechstein R, Kühnle A. Three-dimensional hydration l...
The interaction of organic molecules with the surface of calcite plays a central role in many geoche...
The physico-chemical mechanisms by which rock-forming minerals dissolve in natural fluids are contro...
When two mineral surfaces are compressed against each other in aqueous environment, surface forces a...
Funding Information: Financial support from the German Research Foundation through grant KU1980/14-1...
Carbonate-bearing rocks in the upper Earth’s crust are prone to continuous changes under influences ...
Calcite–water interactions are important not only in carbon sequestration and the global carbon cyc...
The interactions of trivalent lanthanides and actinides with secondary mineral phases such as calcit...
Lateral Force Microscopy (LFM) studies were carried out on cleaved calcite sections in contact with ...
In-situ atomic force microscopy (AFM) experiments were performed to study the overall process of dis...
John S. Ions and the calcite-water (10.4) interface - investigated with three-dimensional atomic for...
Söngen H, Schlegel SJ, Morais Jaques Y, et al. Water Orientation at the Calcite-Water Interface. The...