Ions dissolved in solution are known to interact in remarkable ways with charged Langmuir monolayers. The organic monolayer can be used as a molecular template for ordered nucleation of inorganic crystals (biomineralization) and functional nanoparticles. However, the clear majority of experiments demonstrating these behaviors have been performed with divalent ions. Trivalent ions are present in several important processes that are unique from previously studied divalent systems. We will demonstrate that trivalent ions under floating monolayers can model two important systems: charge inversion and liquid-liquid solvent extraction. Using in situ synchrotron x-ray scattering and emission methods, we can make direct, nanoscale observations of the interactions between ion and monolayer. Charge inversion is a fascinating phenomenon in which small ions of an opposite charge to some large object (colloidal particle, DNA molecule, etc.) will attach to and reverse the object’s charge, rather than simply neutralizing it. There are many experimental systems demonstrating this behavior and an enormous body of theoretical work to explain it. Two classes of explanation exist for how charge inversion may occur, “chemical” and “physical” mechanism. Using grazing incidence diffraction (GID), we have found that ions can form an ordered lattice which is incommensurate to a floating, charged monolayer. Because the ions are incommensurate, they cannot be specifically attached to molecules in the monolayer and must be, therefore, held in place by “physical” means. Solvent extraction can be an extremely complex procedure, so our approach to studying it is to simplify the system into a basic model. Ordinarily, two immiscible liquids – an aqueous phase containing some desired species and other impurities and an organic phase, which sometimes contains extractant molecules that improve efficiency – are mixed together and allowed to separate again. While the liquids are being mixed together, the target species from the aqueous phase is pulled across the interface into the organic phase. The mechanism by which the transfer occurs is very poorly understood and very difficult to study directly since it is a very dynamic process and obscured by the bulk of the liquids. Here we propose that the air-water interface is a model of the liquid-liquid interface; in our model, the hydrophobic “organic” phase is the air above the water. This lets us make direct observations of the interactions between ions dissolved in the aqueous phase and the extractant molecules in the organic phase with x-rays, something which would be impossible in an ordinary solvent extraction experiment. We observed a sharp transition in ordering as the atomic weight of the ion dissolved in solution is increased. One would expect a continuous variation, since the size of the ions varies continuously. Second, using x-ray fluorescence, we find that heavier lanthanides are much more strongly attracted to the monolayer than light ones. The unexpected nature of our results emphasizes the need for bottom-up approaches to understanding these systems rather than the top-down method used for the last century. In addition, our results demonstrate that it is, indeed, possible to overcome the experimental difficulties and make the types of measurements necessary for this approach.

Last modified

• 01/09/2019

Creator

• Mitchell Miller

DOI

• https://doi.org/10.21985/N23F32

Subject

• Physics and Astronomy

Keyword

• John Ketterson

Date created

• 2017-01-01

Resource type

• Dissertation

Rights statement

• In Copyright