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We present a combined molecular dynamics (MD) simulation and X-ray absorption fine structure (XAFS) spectroscopic investigation of aqueous iron adsorption on nanoconfined amorphous silica surfaces. The simulation models examine the effects of pore size, pH (surface charge), iron valency, and counter-ion (chloride or hydroxide). The simulation methods were validated by comparing the coordination environment of adsorbed iron with coordination numbers and bond lengths derived from XAFS. In the MD models, nanoconfinement effects on local iron coordination were investigated by comparing results for unconfined silica surfaces and in confined domains within 2 nm, 4 nm, and 8 nm pores. Experimentally, coordination environments of iron adsorbed onto mesoporous silica with 4 nm and 8 nm pores at pH 7.5 were investigated. The effect of pH in the MD models was included by simulating Fe(II) adsorption onto negatively charged SiO2 surfaces and Fe(III) adsorption on neutral surfaces. The simulation results show that iron adsorption depends significantly on silica surface charge, as expected based on electrostatic interactions. Adsorption on a negatively charged surface is an order of magnitude greater than on the neutral surface, and simulated surface coverages are consistent with experimental results. Pore size effects from the MD simulations were most notable in the adsorption of Fe(II) at deprotonated surface sites (SiO−), but adsorption trends varied with concentration and aqueous Fe speciation. The coordination environment of adsorbed iron varied significantly with the type of anion. Considerable ion pairing with hydroxide anions led to the formation of oligomeric surface complexes and aqueous species, resulting in larger iron hydroxide clusters at higher surface loadings.

A quarter of Earth's land surface is covered by porous sedimentary silicate rocks, so silica–water interfaces are critical to the fate and transport of chemical species on a global-scale. However, while the physiochemical properties of unconfined silica–water interfaces are understood reasonably well, these properties have proven to be unpredictable when the interface is confined in nanometer-scale pores within sedimentary rocks. For example, the existing theories struggle to quantitatively predict how the energetics of adsorption reactions and the coordination environment of adsorbed species shift due to nanoconfinement of an interface. Here, we utilized gradual and known variations in the properties of trivalent lanthanide ions to decipher the chemical interactions that cause the nanoconfinement effects on chemistry at the silica–water interfaces. We discovered that the lanthanide's free energy of hydration (ΔGhydr) is a descriptor that can be used to predict the extent to which nanoconfinement will change the thermodynamics and products of interfacial reactions. We show that nanoconfinement promotes inner-sphere complexation between lanthanides and silica surface, as well as the formation of polymeric surface species. In nanoconfined domains lanthanide's ΔGhydr becomes less negative, reducing the energy required to dehydrate the ion during the formation of an inner-sphere surface complex. These nanoconfinement effects on chemistry become more pronounced for ions with lower hydration free energies.

Spatial confinement is prevalent in sedimentary rocks and can lead to changes in the chemical behavior at mineral–water interfaces. This includes both deviations in the physico-chemical properties of confined water, when compared to the bulk liquid phase, and subsequent alterations in adsorption chemistry of ions inside nano-scale mineral pores. Here we document contrasting adsorption mechanisms and differences in local coordination environments of copper (Cu2+), depending on whether the ion is adsorbed on non-porous silica surfaces, versus inside 8 nm and 4 nm pores in silica. X-ray absorption spectroscopy, flow micro-calorimetry, and batch adsorption methods together with molecular modeling are used to thoroughly describe the dependence of these adsorption processes on the pore size. We show that confinement within silica pores promotes Cu–Cu interactions and increases the formation of Cu–Cu polynuclear surface complexes. We also demonstrate that the mechanism of Cu2+ adsorption on non-porous versus porous silica is vastly different. The adsorption of Cu2+ on non-porous silica is an endothermic process, whereby Cu2+ undergoes dehydration prior to surface complexation. In contrast, adsorption within nano-scale pores is preceded by only partial dehydration, and significant formation of Cu–Cu polynuclear complexes, which leads to an overall exothermic signal. Interfacial confinement leads to dramatic changes in the adsorption mechanism and speciation, which in turn controls the fate and transport of chemical species in natural environments.

Being the fourth most abundant element in the Earth's crust, iron (Fe) is a key player in myriad biogeochemical processes. Iron that resides in the structures of nano- to micron-scale clay mineral particles undergoes cycling between Fe(II) and Fe(III). This iron comprises a large redox-active pool in surface environments, controlling the fate and transport of nutrients and contaminants. The mechanism of electron transfer involving this iron species is poorly understood. We observe that Fe(III) in clay minerals does not oxidize arsenic As(III), unless a minor amount of Fe(II) is introduced into the predominantly-Fe(III) structure. These “activated” clay minerals are redox-active both in the presence and absence of oxygen. In the presence of oxygen, Fe(II) catalyzes the production of reactive oxygen species; however, the oxidation pathway in the absence of oxygen is unknown. Here we show that under oxygen-free conditions, the redox-active species in clay minerals is FeII–O–FeIII moieties at the edge sites. We used in situ and ex situ spectroscopic methods, including X-ray absorption, Mossbauer, and diffuse reflectance spectroscopies, as well as ab initio calculations. Our ab initio calculations show that desorption of water from an FeII–O–FeIII site in clay mineral requires less energy, compared to a fully-oxidized FeIII–O–FeIII site. We propose that this lower barrier for the desorption of water increases the apparent kinetics of redox reactions on clay mineral surfaces.

A fluid flow in a nanochannel highly depends on the wettability of the channel surface to the fluid. The permeability of the nanochannel is usually very low, largely due to the adhesion of fluid at the solid interfaces. Using molecular dynamics (MD) simulations, we demonstrate that the flow of water in a nanochannel with rough hydrophilic surfaces can be significantly enhanced by the presence of a thin layer of supercritical carbon dioxide (scCO2) at the water-solid interfaces. The thin scCO2 layer acts like an atomistic lubricant that transforms a hydrophilic interface into a super-hydrophobic one and triggers a transition from a stick- to- a slip boundary condition for a nanoscale flow. This work provides an atomistic insight into multicomponent interactions in nanochannels and illustrates that such interactions can be manipulated, if needed, to increase the throughput and energy efficiency of nanofluidic systems.