The
stability of organomineral aggregates in soils has a key influence
on nutrient cycling, erosion, and soil productivity. Both clay minerals
with distinct basal and edge surfaces and organic molecules with reactive
functional groups offer rich bonding environments. While clay edges
often promote strong inner-sphere bonding of −COOH-laden organics,
we explore typically weaker, outer-sphere bonding of such molecules
onto basal planes and its significance in organomineral interactions.
In this surface force apparatus study, we probed face-specific interactions
of negatively charged mica basal surfaces in solutions containing
carboxyl-bearing, low-molecular-weight dicarboxylic acids (DAs). Our
experiments provide distance-resolved, nanometer-range measurements
of forces acting between two (001) mica surfaces and simultaneously
probe DA adsorption. We show that background inorganic ions display
crucial importance in nanoscale forces acting between basal mica surfaces
and in DA adsorption: Na+ contributes to strong repulsion
and little binding of dicarboxylic anions, while small amounts of
Ca2+ are sufficient to screen the basal surface charge
of mica, facilitate strong adhesion, and enhance dicarboxylic anion
adsorption by acting as cationic bridges. Despite reversible and weak
adsorption of DAs, we resolve their multilayer binding via assembly
of hydrophobic chains in the presence of Ca2+, pointing
the importance of abundant, less reactive basal clay surfaces in organomineral
interactions.