1998
DOI: 10.1021/la980529y
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An XPS and Scanning Polarization Force Microscopy Study of the Exchange and Mobility of Surface Ions on Mica

Abstract: Potassium mica was treated with different ionic solutions to replace the naturally occurring K+ on the surface by Ca2+, Mg2+, and H+ ions. The extent of the exchange was monitored by variable emergence angle X-ray photoelectron spectroscopy (XPS). Scanning polarization force microscopy (SPFM) was used to measure the mobility of the surface ions as a result of water adsorption when the mica is exposed to different humidity levels.

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Cited by 70 publications
(99 citation statements)
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“…First, the adsorbed Rb þ ions appear surprisingly stable, with the same protrusion often visible in several consecutive line scans. Theory 42 and scanning polarization microscopy measurements of ions mobility on mica 43 suggest that the residence time of adsorbed ions at a given binding site should not exceed microseconds, but our IDM measurements of the residence time of Rb þ ions over a single binding site (Fig. 1c) indicate an average time in the order of 100 ms (see Supplementary Fig.…”
Section: Resultsmentioning
confidence: 86%
“…First, the adsorbed Rb þ ions appear surprisingly stable, with the same protrusion often visible in several consecutive line scans. Theory 42 and scanning polarization microscopy measurements of ions mobility on mica 43 suggest that the residence time of adsorbed ions at a given binding site should not exceed microseconds, but our IDM measurements of the residence time of Rb þ ions over a single binding site (Fig. 1c) indicate an average time in the order of 100 ms (see Supplementary Fig.…”
Section: Resultsmentioning
confidence: 86%
“…Under the condition of no external salt in the solution, the epitaxial binding sites on the mica surface are in equilibrium between the K + -occupied and K + -vacant states (our molecular dynamics simulations indicate that 52.3% of K + sites are open in pure water, in agreement with previous experimental findings), where GAV-9 may readily react (adsorb) onto the K + -vacant sites [for the K + -occupied sites, on the other hand, it needs to go through ion exchange reactions (34,35)]. However, once a high concentration of salt (e.g., MgCl 2 ) is added into the solution, the above equilibrium is shifted toward the K + -occupied states (or Mg 2+ -occupied states) (36,37). This can be clearly seen from the excess cation density on the mica surface in our simulation (Fig.…”
Section: Resultsmentioning
confidence: 99%
“…However, this exchange process is rapid and leads to 100% substitution on timescales that are short compared to the timescale for the X-ray photoelectron spectroscopy (XPS) measurements used to probe this exchange (22). Nonetheless, to be certain this could not be a source of short domains, we incubated mica for overnight (i.e., approximately 21 h) in CaCl 2 solution before exposure to S-layer proteins solutions for 4 h but found no dif- A and B show unprocessed AFM images.…”
Section: Discussionmentioning
confidence: 99%