Jump to content

Inner sphere complex

From Wikipedia, the free encyclopedia
This is an old revision of this page, as edited by Achia UW (talk | contribs) at 03:51, 11 November 2019 (Revised and added formulas with explanations found in wetting of inorganic inner sphere complexes.). The present address (URL) is a permanent link to this revision, which may differ significantly from the current revision.

Inner sphere complex is a type of surface complex that refers to the surface chemistry changing a water-surface interface to one without water molecules bridging a ligand to the metal ion. Formation of inner sphere complexes occurs when ions bind directly to the surface with no intervening water molecules. These types of surface complexes are restricted to ions that have a high affinity for surface sites and include specifically adsorbed ions that can bind to the surface through covalent bonding.

Inner Sphere Complexes

Inner sphere complexes describe active surface sites that are involved in nucleation, crystal growth, redox processes, soil chemistry, alongside other reactions taking place between a cation and surface.[1]

However, inner sphere complexes have surface hydroxyl groups that function as -donor ligands, increasing the coordinated metal ion's electron density.[2] This is an example of competitive complex formation, in which ligands will compete for space on an activation site of a metal ion.

Surface structures are able to reduce and oxidize ligands, whereas transport phenomena do not. Therefore, surface structure serves an important role in surface reactivity, with the coordination environment at the solid-water interface changing intensity or rate of a reaction.[1]

Wetting and Inner Sphere Complexes

One method to achieve inner sphere complexes is through wetting: a phenomenon where one fluid, known as a wetting agent, replaces another medium, like water or air, on a surface. In the case of a solid-water to a solid-liquid interface, the liquid spreads to increase the solid-liquid and liquid-gas interfacial area, and decreases the solid-gas interfacial and solid-water area as a result.

The spreading coefficient of the liquid is described by the Gibb's Free Energy over the area[3]

The Gibb's Free Energy is spontaneous only when S is positive or zero.

Another method of wetting is adhesional wetting, where the liquid makes contact with the solid surface for the first time. However, this initial wetting decreases the liquid-gas interface that can be modeled by the Dupré equation[3]

Or by the revised Dupré-Young equation

Immersional wetting that has a metal ion completely immersed in a liquid ligand solution does not have a change in liquid-gas interface. This reaction can be modeled by

From these models, metal ions can be influenced by contact angle, and as a result, inner sphere complexes are influenced by wetting agents and wetting procedures.[4]

Applications in Soil Chemistry

References

  1. ^ a b Huntsberger, J. R. (May 1, 1975). "Surface Chemistry and Adhesion- A Review of Some Fundamentals". Journal of Adhesion. 7: 289–299.
  2. ^ Stumm, Werner (May 5, 1995). "The Inner-Sphere Surface Complex A Key to Understanding Surface Reactivity". American Chemistry Society Publications. 244: 1–32 – via ACS Publications. {{cite journal}}: line feed character in |title= at position 34 (help)
  3. ^ a b Shaw, Duncan J. (1992). Introduction to Colloid and Surface Chemistry. Great Britain: Butterworth Heinemann. pp. 151–159. ISBN 07506 11820.
  4. ^ Pashley, Richard M.; Karaman, Marilyn E. (2004). Applied Colloid and Surface Chemistry. Great Britain: John Wiley & Sons, Ltd. pp. 8–9. ISBN 0 470 86882 1.