Variation in Surface Ionization Potentials of Pristine and Hydrated BiVO4
The Journal of Physical Chemistry Letters
|July 21, 2015
Summary
Bismuth vanadate (BiVO4) shows potential for water splitting. Water adsorption increases its ionization potential by stabilizing the valence band, enhancing its use in photoelectrodes.
Area of Science:
- Materials Science
- Surface Science
- Computational Chemistry
Background:
- Bismuth vanadate (BiVO4) is a key material for photoelectrochemical water splitting and photocatalysis.
- Understanding surface properties is crucial for optimizing BiVO4 performance.
Purpose of the Study:
- To evaluate the ionization potentials of the (010) surface termination of BiVO4.
- To investigate the impact of water adsorption on these ionization potentials.
Main Methods:
- First-principles simulations were employed to calculate ionization potentials.
- Static models and molecular dynamics simulations were used to study water adsorption effects.
Main Results:
- The calculated electron removal energy for pristine BiVO4 (010) surface was 7.2 eV, aligning with experimental data.
- Water adsorption was found to stabilize the valence band edge, increasing ionization potentials due to H2O's molecular dipole.
Conclusions:
- Water adsorption significantly influences the electronic properties of BiVO4 surfaces.
- This study provides insights into the role of polar layers on complex oxides for designing efficient photoelectrodes for water splitting.
Related Concept Videos
Precipitation of Ions
31.2K
Predicting Precipitation
The equation that describes the equilibrium between solid calcium carbonate and its solvated ions is:
The equation that describes the equilibrium between solid calcium carbonate and its solvated ions is:
31.2K
Ionization Energy
44.8K
The amount of energy required to remove the most loosely bound electron from a gaseous atom in its ground state is called its first ionization energy (IE1). The first ionization energy for an element, X, is the energy required to form a cation with 1+ charge:
44.8K
Hybridization of Atomic Orbitals I
69.4K
The mathematical expression known as the wave function, ψ, contains information about each orbital and the wavelike properties of electrons in an isolated atom. When atoms are bound together in a molecule, the wave functions combine to produce new mathematical descriptions that have different shapes. This process of combining the wave functions for atomic orbitals is called hybridization and is mathematically accomplished by the linear combination of atomic orbitals. The new orbitals that...
69.4K
Ions as Acids and Bases
27.8K
Salts with Acidic Ions
Salts are ionic compounds composed of cations and anions, either of which may be capable of undergoing an acid or base ionization reaction with water. Aqueous salt solutions, therefore, may be acidic, basic, or neutral, depending on the relative acid-base strengths of the salt’s constituent ions. For example, dissolving the ammonium chloride in water results in its dissociation, as described by the equation:
Salts are ionic compounds composed of cations and anions, either of which may be capable of undergoing an acid or base ionization reaction with water. Aqueous salt solutions, therefore, may be acidic, basic, or neutral, depending on the relative acid-base strengths of the salt’s constituent ions. For example, dissolving the ammonium chloride in water results in its dissociation, as described by the equation:
27.8K
Solubility Equilibria: Ionic Product of Water
2.1K
Pure water is a weak electrolyte; only a small amount ionizes into hydrogen and hydroxide ions. At any given temperature, the concentration of undissociated water is almost constant, so the ionic product of water is the product of the hydrogen and hydroxide ion concentrations, denoted as Kw. The square root of Kw gives the individual ion concentrations.
The ionic product of water varies with temperature, and its value is 1.0 x 10−14 at standard experimental conditions. Per Le...
The ionic product of water varies with temperature, and its value is 1.0 x 10−14 at standard experimental conditions. Per Le...
2.1K
Factors Affecting Activity Coefficient
1.8K
The extended Debye-Hückel equation indicates that the activity coefficient of an ion in an aqueous solution at 25°C depends on three partially interdependent properties: the ionic strength of the solution, the charge of the ion, and the ion size.
The activity coefficient value for an ion is close to one when the solution has almost zero ionic strength, i.e., when the solution shows close to ideal behavior. As the ionic strength of the solution increases from 0 to 0.1 mol/L, a...
The activity coefficient value for an ion is close to one when the solution has almost zero ionic strength, i.e., when the solution shows close to ideal behavior. As the ionic strength of the solution increases from 0 to 0.1 mol/L, a...
1.8K


