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PV = nRT = NkT
Equation of state for an ideal/perfect gas, relating pressure (P), volume (V), temperature (T), number of moles (n), and the ideal gas constant (R) or Boltzmann's constant (k).
U = 3/2nRT = 3/2Nkt
Expression for the internal energy of an ideal gas, indicating that it is directly proportional to the temperature and number of moles or molecules.
dU = dQ + dW, so ΔU = ∫dQ + ∫dW = Q + W
This equation represents the first law of thermodynamics, stating that the change in internal energy (ΔU) of a system is equal to the heat added to the system (dQ) plus the work done on the system (dW).
U is a state function
closed system (n = const.)
dQ|V = CVdT, where CV = (∂U/∂T)V
dQ|V: infinitesimal amount of heat added to a system while the volume is held constant; at constant volume, the system does no mechanical work (dW = pdV = 0) —> dQ = dU and since the change in internal energy at constant volume depends only on temperature —> dU = CVdT
CV = (∂U/∂T)V: The rate at which the system’s internal energy U changes with temperature T at fixed volume.
CV: heat capacity at constant volume; the amount of heat required to raise the system’s temperature by one unit without changing its volume.
Heat capacity of a perfect gas is CV = 3/2nR
dQ|P = CPdT, where CP = (∂H/∂T)P
dQ|P: infinitesimal amount of heat added to a system while the pressure is held constant; at constant pressure, the system generally does mechanical work as it expands or contracts —> dQ = dU + PdV and H = U + PV, its differential is dH = dU + PdV + VdP (at const. pressure dP = 0) —> dH = dQ; since enthalpy at constant pressure depends only on temperature, dH = CPdT
CP = (∂H/∂T)P: The rate at which is the system’s internal energy U changes with temperature T at fixed pressure.
CP: heat capacity at constant pressure; the amount of heat required to raise the system’s temperature by one unit without changing its pressure.
Heat capacity of a perfect gas is CP = 5/2nR
dS = dQrev/T ≥ dQ/T
Entropy is a state function, this change depends only on the initial and final states, not the path.
Definition of entropy/Clausius inequality, expressing the second law of thermodynamics. It relates the change in entropy (S) to heat transfer (Q) and absolute temperature (T), and distinguishes between reversible and irreversible processes. (spontaneous process in closed system)
dQrev: Infinitesimal heat transferred in a reversible process.
dQ: Infinitesimal heat transferred in a general (possibly irreversible) process
T: Absolute temperature at which the heat exchange occurs (in Kelvin)
≥: Indicates that entropy change is greater for irreversible processes than for reversible ones
Interpretation: For a reversible process: dS = dQ/T
For an irreversible process: dS > dQ/T
Entropy of an isolated system never decreases.
dStot = dS + dSsurr ≥ 0
Total entropy change / entropy balance, expressing the second law of thermodynamics. It states that the total entropy change of a system plus its surroundings is never negative. (spontaneous process in closed system)
dStot: Infinitesimal change in total entropy (system + surroundings)
Interpretation: Reversible process: dStot = 0 (in equilibrium)
Irreversible (spontaneous) process: dStot > 0
A process can occur spontaneously only if it increases the total entropy of the universe.
S = klnW
Boltzmann entropy formula, giving the statistical definition of entropy. It relates the macroscopic entropy of a system to the number of accessible microscopic configurations.
k: Boltzmann’s constant
W: Number of micro states of the system consistent with the macroscopic constraints (energy, volume, number of particles)
Interpretation: Entropy increases as the number of possible microscopic arrangements of a system increases. Systems naturally evolve toward macrostates with larger W, corresponding to higher entropy.
dU = -PdV + TdS + ∑iμidni
Fundamental thermodynamic relation, expressing the differential change in internal energy of a system in terms of its natural variables.
-PdV: Mechanical work done by the system
TdS: Energy change associated with heat transfer in a reversible process
μi: Chemical potential of component i
dni: Infinitesimal change in the amount (moles or particles) of component i.
∑iμidni: Energy change due to matter exchange or chemical reactions.
Interpretation: This equation combines the first and second laws of thermodynamics and shows how internal energy changes due to; volume work, entropy (heat) changes, and changes in composition.
H = U + PV and dH = VdP + TdS + ∑iμidni
Definition and differntial form of enthalpy, a thermodynamic potential useful for processes at constant pressure.
PV: Pressure-volume energy associated with system expansion
VdP: Energy change due to a change in pressure
TdS: Energy change associated with entropy (heat) transfer
μi: Chemical potential of component i
dni: Infinitesimal change in the amount of component i.
∑iμidni: Energy change due to changes in composition.
Interpretation: Enthalpy is a natural thermodynamic potential with natural variables (S, P, {ni}). At constant pressure and composition, dH = TdS = dQrev. It is a state function that represent the total energy content of a system that is useful for describing processes occuring at constant pressure.
At constant P (dP = 0): dHP = dQ
A = U -TS and dA = -PdV -SdT + ∑iμidni
Definition and differntial form of the Helmholtz free energy, a thermodynamic potential useful for processes at constant temperature and volume.
A: Maximum (free) work that can be done by the system during an isothermal process.
TS: Energy unavailable to do useful work at temperature T.
-PdV: mechanical work term
-SdT: Change in free energy due to temperature variation
μi: Chemical potential of component i
dni: Infinitesimal change in the amount of component i.
∑iμidni: Energy change due to changes in composition.
interpretation: The Helmholtz free energy has natural variables (T, V, {ni}). At constant temperature and volume dA ≤ 0 (spontaneous process), with equality for reversible processes.
G = H - TS and dG = VdP - SdT + ∑iμidni
Definition and differential form of the Gibbs free energy, the thermodynamic potential most useful/the energy in a system available to do useful work for/at processes at constant temperature and pressure.
G: State funcion and also called free enthalpy
TS: Energy unavailable to do useful work at temperature
VdP: Change in free energy due to pressure variation
-SdT: Change in free energy due to temperature variation
μi: Chemical potential of component i
dni: Infinitesimal change in the amount of component i.
∑iμidni: Energy change due to changes in composition.
Interpretation: The Gibbs free energy has natural variables (T, P, {ni}). At constant temperature and pressure, dG ≤ 0 (spontaneous process), with equality for reversible processes.
At constant temperature and pressure, a process is spontaneous if the Gibbs free energy decreases. At equilibrium, G is minimized and dG = 0.
ΔrG = (∂G/∂ξ)P,T = ΔrG° + RTlnQ with Q = Πiaivi
ΔrG: Gibbs free energy change of the reaction at the current conditions
(∂G/∂ξ)P,T: Change in Gibbs free energy with respect to the extent of reaction ξ, at constant pressure and temperature
ξ: Extent of reaction, a measure of reaction progress
ΔrG°: Standard Gibbs free energy change of reaction, defined for standard-state conditions
Q: Reaction quotient, describing the current composition of the system
ai: Activity of species i (effective concentration)
vi: Soichiometric coefficient of species i (positive for products, negative of reactants)
Πi: Product over all species in the reaction
Interpretation: ΔrG < 0: reaction proceeds spontaneously in the forward direction
ΔrG = 0: reaction is at equilibrium
ΔrG > 0: reaction is non-spontaneously in the forward direction
The Gibbs free energy change of a reaction depends on its standard free energy change and on how far the system’s current composition is from equilibrium.
ΔrG° = -RTlnK with K = (Πiaivi )eq
Standard Gibbs free energy change-equilibrium relation, linking thermodynamics with chemical equilibrium.
ΔrG°: Standard Gibbs free energy change of reaction, defined for standard-state conditions
K: Equilibrium constant of the reaction
ai: Activity of species i
vi: Soichiometric coefficient of species i (positive for products, negative of reactants)
Πi: Product over all species in the reaction
(…)eq: Evaluated at equilibrium
Interpretation: K > 1 —> ΔrG° < 0: products favored at equilibrium
K = 1 —> ΔrG° = 0: neither side favored
K < 1 —> ΔrG° > 0: reactants favored
The standard Gibbs free energy change of a reaction determines the position of equilibrium: the more negative ΔrG° is, the larger the equilibrium constant and the more product-favored the reaction.
ΔrG = -νFE, so E = E° -(RT/νF)lnQ
Thermodynamic-electrochemical relation (Nernst equation), linking the Gibbs free energy change of a redox reaction to the cell potential.
ΔrG: Gibbs free energy change of the electrochemical reaction
ν: Number of moles of electrons transferred in the reaction
F: Faraday constant, change per mole of electrons
E: Cell (electrode) potential under non-standard conditions
E°: Standard cell potential
Q: Reaction quotient, expressed in terms of activities of reactants and products
Interpretation: ΔrG < 0 —> E > 0: reaction is spontaneous (galvanic cell)
ΔrG = 0 —> E = 0: system at equilibrium
ΔrG > 0 —> E < 0: reaction is non-spontaneous
At equilibrium (Q = K), E° = (RT/vF)lnK.
dW = -Pext.dV + dW’ and dW’max = (dG)P,T and dW’ = Edq
Work decomposition and maximum non-expansion work, relating mechanical work, GIbbs free energy and electrical work.
dW: Total infinitesimal work done by the system
Pext: External pressure
-PextdV: Expansion (pressure-volume) work
dW’: Non-expansion work (e.g. electrical, surface, magnetic work)
dW’max: Maximum non-expansion work obtainable from the system
(dG)P,T: Change in Gibbs free energy at constant pressure and temperature —> at constant P and T: dW’max: -dG
E: Electrical potential (cell voltage)
dq: Infinitesimal electric charge transferred
dW’ = Edq: Electrical work done by the system
Interpretation:
Total work is the sum of expansion work and non-expansion work
At constant temperature and pressure, Gibbs free energy determines the maximum useful (non-PV) work
In electrochemical systems, this useful work appears as electrical work, directly related to the cell potential
μi = (∂G/∂ni)P,T,nj≠i = (∂A/∂ni)V,T,nj≠i = (∂H/∂ni)P,S,nj≠i = (∂U/∂ni)V,S,nj≠i
Definition of the chemical potential, expressing how the energy of a system changes when the amount of a component is varied.
μi: Chemical potential of component i; the partial molar Gibbs free energy
ni: Amount (moles or particles) of component i
nj≠i: Amounts of all other components, held constant
Interpretation of each expression:
(∂G/∂ni)P,T,nj≠i: Change in Gibbs free energy when one adds component i at constant pressure and temperature. (Most commonly used definition, especially in chemistry and phase equilibrium)
(∂A/∂ni)V,T,nj≠i: Change in Helmholtz free energy at constant volume and temperature.
(∂H/∂ni)P,S,nj≠i: Change in enthalpy at constant pressure and entropy.
(∂U/∂ni)V,S,nj≠i: Change in internal energy at constant volume and entropy.
The chemical potential measures the tendency of a species to enter or leave a system.
GP,T = Πiμini
Euler equation for Gibbs free energy, expressing the total Gibbs free energy of a system at constant pressure and temperature in terms of chemical potentials.
GP,T: Gibbs free energy of the system at fixed pressure and temperature.
μi: Chemical potential of component i
ni: Amount (moles or particles) of component i
∑i: Sum over all components in the system
Forms the basis for equilibrium conditions: minimizing G at constant P, T determines chemical and phase equilibrium
Leads directly to the Gibbs-Duhem equation when differentiated
ΔidealmixS = -nR(xAln(xA)+xBln(xB))
Entropy of mixing for an ideal binary mixture, giving the increase in entropy when two ideal substances are mixed.
ΔSidealmix: Entropy change upon mixing.
n: Total number of moles in the mixture.
xA,xB: Mole fractions of components A and B.
Interpretation: This formula applies to ideal mixtures (ideal gases or ideal solutions), where interactions between unlike and like particles are equivalent. Because 0 < xi < 1, each lnxi < 0, making the overall entropy change positive: ΔidealmixS > 0
Mixing increases entropy because particles become more randomly distributed, increasing the number of accessible microstates.
General form (multicomponent system):
ΔSidealmix = −nR∑ixilnxi
(∂V/∂T)P,W’,ni = -(∂S/∂P)T,W’, ni
Maxwell relation (from the Gibbs free energy), linking how volume changes with temperature to how entropy changes with pressure.
W′ : Other non-expansion work variables held constant (e.g. electrical work).
ni: Amounts of each component, held constant.
Origin: Starting from the differential of the Gibbs free energy,
dG = VdP−SdT+∑iμidni + (other work terms), the equality of mixed second derivatives of G leads to this relation.
Physical interpretation:
(∂V/∂T)P describes thermal expansion at constant pressure.
−(∂S/∂P)T describes how entropy decreases under compression.
Xi = (∂X/∂ni)P,T,nj≠i
Partial molar quantity, describing the contribution of component i to an extensive property of a mixture.
Xi: Partial molar value of the extensive property X for component i
X: Any extensive thermodynamic property (e.g. V,U,H,S,G)
ni: Amount (moles) of component i
P, T: Pressure and temperature held constant.
nj≠i: Amounts of all other components held constant.
The partial molar quantity tells how much the total property X changes when a small amount of component i is added to a large mixture at fixed P and T.
∑jnjdμj = 0
Gibbs-Duhem equation, expressing a fundamental constraint between the chemical potentials in a multicomponent system.
nj: Amount (moles) of component j.
μj: Chemical potential of component j.
dμj: Infinitesimal change in chemical potential.
This form applies at constant temperature and pressure.
Interpretation: Because the Gibbs free energy is an extensive property, GP,T = Πiμini. Differentiating at constant T and P gives ∑jnjdμj = 0.
Physical meaning: The chemical potentials in a mixture are not independent: if one chemical potential changes, at least one other must adjust to satisfy this constraint.
Pj = xjPj*
Raoult’s law for ideal solutions, relating the partial pressure of component j to its mole fraction in the liquid phase.
Pj: Partial pressure of component j in the vapor.
xj: Mole fraction of component j in the liquid
Pj*: Vapor pressure of pure component j at the same temperature
In an ideal solution, each component contributes to the vapor pressure in proportion to its mole fraction.
Pj = yjP
Dalton’s law, relating the partial pressure of a gas to its mole fraction in the vapor phase.
Pj: Partial pressure of component j
yj: Mole fraction of component j in the vapor
P: Total pressure of the gas mixture
Each gas in a mixture exerts a fraction of the total pressure proportional to its mole fraction.
PB = xBKB
Henry’s law for dilute solutions, describing the behavior of a solute at low concentration.
PB: Partial pressure of solute B in the vapor.
xB: Mole fraction of solute B in the liquid.
KB: Henry’s law constant for solute B (depends on temperature and solute-solvent pair)
At low concentrations, the vapor pressure of a solute is proportional to its mode fraction, but with a proportionality constant different from the pure-component vapor pressure.
(∂µβ/∂P)T − (∂µα/∂P)T = ∆trsV
Pressure dependence of chemical potential/phase transition relation, expressing how the difference in chemical potentials between two phases changes with pressure.
µα, µβ: Chemical potentials of a substance in phases α and β (e.g. solid and liquid).
(∂µ/∂P)T: Change in chemical potential with pressure at constant temperature
∆trsV: Volume change of transition between two phases: ΔtrsV = Vβ − Vα
Explains why increasing pressure favors the phase with smaller molar volume.
Forms part of the Clapeyron equation.
Used to analyze phase equilibria and pressure-induced phase transitions.
(∂µβ/∂T)P − (∂µα/∂T)P = −∆trsS
Temperature dependence of chemical potential/phase transition relation, expressing how the difference in chemical potentials between two phases changes with temperature.
µα, µβ: Chemical potentials of a substance in phases α and β (e.g. solid and liquid).
(∂µ/∂T)P: Change in chemical potential with temperature at constant pressure
∆trsS: Entropy change of transition between two phases: ΔtrsS = Sβ − Sα
Explains why increasing temperature favors the phase with higher entropy.
Together with the pressure relation, leads to the Clapeyron equation.
Central to understanding phase stability and phase diagrams.
P = P*exp(Vm∆P/RT)
Pressure dependence of vapor pressure, describing how the vapor pressure of a condensed phase changes with pressure at constant temperature.
P: Vapor pressure of the substance at pressure P* + ΔP.
P*: Vapor pressure at a reference pressure (usually the saturation vapor pressure at the same temperature).
Vm: Molar volume of the condensed phase (liquid or solid)
Interpretation: This equation shows that increasing the pressure on a condensed phase increases its vapor pressure exponentially. The effect is usually small for liquids and solids because their molar volumes are small.
Assumptions: Constant Vm and T, Vapor behaves ideally
dP/dT =∆trsS/∆trsV = ∆trsH/T∆trsV
Clapeyron equation, describing the slope of a phase boundary in a pressure-temperature phase diagram.
dP/dT: Slope of the phase equilibrium line between two phases
ΔtrsS: Entropy change of the phase transition.
ΔtrsV: Volume change of the phase transition.
ΔtrsH: Enthalpy change (latent heat) of the phase transition.
Predicts how phase equilibrium shifts with temperature and pressure.
Explains unusual behavior such as the negative melting curve slope of ice (because ΔtrsV < 0)
dlnP/dT ≈ ∆trsH/RT2
Clausius-Clapeyron equation (approximate form), describing how the vapor pressure depends on temperature during a phase transition involving a gas (typically vaporization or sublimation).
P: Vapor pressure of the substance
ΔtrsH: Enthalpy change of transition (e.g. enthalpy of vaporization or sublimation)
Assumptions:
The vapor behaves as an ideal gas
The molar volume of the condensed phase is negligible compared to that of the vapor.
ΔtrsH is approximately constant over the temperature range
Physical interpretation: The vapor pressure of a substance increases rapidly with temperature, with the rate of increase governed by the enthalpy of the phase transition.
Integrated form (commonly used):
lnP = -(ΔtrsH/R) (1/T) + C
or, between two temperatures,
ln (P2/P1) = −(ΔtrsH/R) (1/T2 − 1/T1)
∆T = (RT*2/∆trsH)xB
Boiling-point elevation (ideal dilute solution)
ΔT: Increase in boiling temperature of the solution relative to the pure solvent.
T*: Boiling temperature of the pure solvent.
ΔtrsH: Enthalpy of vaporization of the solvent.
xB: Mole fraction of the solute B.
Interpretation: Adding a nonvolatile solute lowers the vapor pressure of the solvent, so a higher temperature is required for boiling
lnxB = ∆fusH/R[1/Tfus − 1/T]
Freezing-point depression (ideal solution)
xB: Mole fraction of solute B in the liquid phase.
ΔfusH: Enthalpy of fusion of the solvent.
Tfus: Freezing (melting) temperature of the pure solvent.
T: Freezing temperature of the solution.
Interpretation: The presence of solute stabilizes the liquid phase, lowering the temperature at which solid-liquid equilibrium occurs.
For very dilute solutions, this leads to the familiar linear freezing-point depression: ΔTfus ∝ xB
µi = µi° + RTlnai = µi° + RTlnxi + RTlnγi
Chemical potential in terms of activity, describing real (non-ideal) solution behavior.
μi: Chemical potential of component i
μi°: Standard chemical potential of component i (defined by the chosen standard state)
ai: Activity of component i, a measure of its effective concentration.
xi: Mole fraction of component i
γi: Activity coefficient of component i, accounting for deviations from ideality.
Key relations: ai = xiγii
For an ideal solution: γi = 1, so μi = μi° + RTlnxi
For a non-ideal solution: γi ≠ 1, and the additional term RTlnγi quantifies intermolecular interaction effects.
Activity replaces mole fraction to account for non-ideal interactions between particles.
µi = µi° + RTlnai = µi° + RTln(bi/b°) + RTlnγi
Chemical potential in terms of activity and molality, used for real solutions (especially electrolytes).
μii: Chemical potential of component i
μi°: Standard chemical potential of component i
ai: Activity of component i
bi: Molality of component i (mol*kg−1)
b°: Standard molality (1 mol*kg−1)
γi: Activity coefficient on the molality scale.
Key relation: ai = γi(bi/b°)
For an ideal dilute solution: γi = 1, so µi = µi° + RTln(bi/b°)
For a non-ideal solution: γi ≠ 1, and the additional term RTlnγi quantifies intermolecular or ionic interaction effects
Central to solution thermodynamics and phase equlibrium.
Essential for describing electrolytes and real solutions.
Activity corrects molality to reflect the true thermodynamic “escaping tendency” of a component
F = C − P + 2
Gibbs phase rule, giving the number of independent variables required to describe a system at equilibrium.
F: Degrees of freedom —> Number of independent intensive variables (e.g. temperature, pressure, composition) that can be changed without altering the number of phases in equilibrium
C: Number of components —> Minimum number of chemically independent species needed to describe the composition of all phases
P: Number of phases —> Physically and chemically uniform, mechanically separable parts of the system (e.g. solid, liquid, gas)
2: The two fundamental intensive variables, temperature and pressure
Fundamental to phase diagrams.
Predicts the maximum number of phases that can coexist.
As the number of phases increases, the number of variables that can be independently adjusted decreases.
Examples:
Single-phase system (P = 1): F = C + 1
Two-phase equilibrium (P = 2): F = C
Triple point of a one-component system (C = 1, P = 3): F = 0 (No freedom: both T and P are fixed)
nαlα = nβlβ
Lever rule, used in phase diagrams to relate the amounts of coexisting phases in a two-phase region.
nα: Amount (moles or mass) of phase α
nβ: Amount (moles or mass) of phase β
lα: Length of the tie-line segment opposite phase α in the phase diagram
lβ: Length of the tie-line segment opposite phase β
Allows calculation of phase amounts in binary phase diagrams.
Widely used in liquid-liquid, solid-liquid, and solid-solid equilibria.
γ± = (γp+γq−)1/(p+q)
Mean ionic activity coefficient, used to describe the non-ideal behavior of electrolytes.
γ±: Mean ionic activity coefficient of the electrolyte
γ+: Activity coefficient of the cation
γ−: Activity coefficient of the anion
p: Stoichiometric coefficient of the cation
q: Stoichiometric coefficient of the anion
Physical interpretation: For an electrolyte that dissociates as ApBq → pA+ + qB−, individual ionic activity coefficients cannot be measured independently. Instead, their combined effect is represented by the mean ionic activity coefficient.
Central to electrolyte thermodynamics.
Used in equilibrium constants, electrochemistry, and colligative properties.
Appears in models such as Debye-Hückel theory
Special case (1:1 electrolyte): For NaCl (p = q = 1): γ± = √γ+γ−
logγ± = −|z+z−|A√I
Debye-Hückel limiting law, describing the activity coefficients of electrolytes in very dilute solutions.
γ±: Mean ionic activity coefficient
log: Base-10 logarithm
z+: Charge number of the cation
z−: Charge number of the anion
|z+z−|: Product of ionic charges (absolute value)
A: Debye-Hückel constant (depends on temperature and solvent)
I: Ionic strength of the solution
Physical interpretation: As ionic strength increases, electrostatic interactions between ions become stronger, causing deviations from ideal behavior and reducing the activity coefficient below 1.
Fundamental equation in electrolyte thermodynamics.
Explains why electrolyte solutions are non-ideal, even at low concentrations.
Used in calculating equilibrium constants, cell potentials and activities.
Higher ionic strength —> stronger ion-ion interactions —> smaller γ±
I = 1/2∑i zi2(bi/b°)
Ionic strength (molality scale), measuring the total electrostatic effect of ions in a solution.
I: Ionic strength of the solution.
∑i: Sum over all ionic species in solution.
zi: Charge number of ion i
bi: Molality of ion i (mol*kg−1).
b°: Standard molality (1 mol*kg−1).
1/2: Factor accounting for double counting of ion–ion interactions.
Central parameter in electrolyte thermodynamics.
Appears in Debye-Hückel equation for activity coefficients.
Used in equilibrium, electrochemistry and colligative property calculations
Ionic strength weights each ion by the square of its charge, so highly charged ions contribute much more strongly than singly charged ions.
Ionic strength increases with both ion concentration and ion charge.
A = (F3/(4πNAln10)) (ρb°/2e3R3T3)1/2
Debye-Hückel constant A, appearing in the Debye-Hückel limiting law for electrolyte solutions. It determines how strongly ionic activity coefficients depend on ionic strength.
A: Debye-Hückel constant (depends on temperature and solvent)
F: Faraday constant
NA: Avogadro constant
ρ: Density of the solvent
b°: Standard molality (1 mol*kg-1)
ε0: Permittivity of free space
εr: Relative permittivity (dielectric constant) of the solvent
Physical interpretation: The constant A reflects how effectively the solvent screens electrostatic interactions between ions. A high dielectric constant (large εr) weakens ion-ion interactions, reducing deviations from ideality.
Depends only on solvent properties and temperature, not on the electrolyte.
Pin = Pout + 2γ/r
Laplace’s equation/Kelvin equation for a curved interface
Pin: Pressure inside a droplet or bubble
Pout: Pressure outside the droplet or bubble
γ: Surface tension of the liquid (N/m)
r: Radius of curvature of the droplet or bubble.
Physical interpretation: The pressure inside a curved surface (droplet or bubble) is higher than outside due to surface tension. Smaller droplets/bubbles have higher internal pressure because Pin - Pout ∝1/r
Explains phenomena like capillarity, bubble formation and emulsion stability
P = ρgh
Hydrostatic pressure
P: Pressure at depth h in a fluid
ρ: Density of the fluid
g: Acceleration due to gravity
h: Height (depth) of the fluid column
Pressure increases linearly with depth in a static fluid.
Fundamental to fluid statics and capillary phenomena.
Often combined with Laplace’s equation to study curved interfaces under gravity
wad = γsg + γlg − γsl
Work of adhesion/wetting equation, describing the thermodynamic of a liquid spreading on a solid surface.
wad: Work of adhesion (energy required to separate unit area of the solid-liquid interface)
γsg: Surface tension of the solid–gas interface.
γlg: Surface tension of the liquid–gas interface.
γsl: Surface tension of the solid–liquid interface.
Physical interpretation:
Determines wettability of a liquid on a solid surface.
If wad > 0, the liquid spreads on the solid (good wetting)
If wad < 0, the liquid beads up (poor wetting)
Predicts whether liquids will spread, form droplets or stick to surfaces.
γsg = γsl + γlgcosΘc
Young’s equation, describing the contact angle of a liquid droplet on a solid surface.
γsg: Surface tension of the solid–gas interface.
γlg: Surface tension of the liquid–gas interface.
γsl: Surface tension of the solid–liquid interface.
Θc: Contact angle of the liquid droplet on the solid surface
Physical interpretation:
Relates surface tensions to the shape of a droplet on a solid surface.
The contact angle Θc indicates wettability: Θc < 90° —> good wetting and Θc > 90° —> poor wetting
If Θc = 0, the liquid spreads completely
Used to calculate work of adhesion:
wad = γlg(1 + cosΘc)
ni/N = (exp(-εi/kT))/q with q = ∑iexp(-εi/kT) and <X> = N<x> = N∑ixi(ni/N)
ni/N = (exp(-εi/kT))/q: Boltzmann distribution —> Gives the fraction of particles in a particular energy state at temperature T
q = ∑iexp(-εi/kT): Partition function —> Encodes the statistical properties of the system
<X> = N<x> = N∑ixi(ni/N): Average value of an arbitrary quantity X of the entrie system at a certain temperature —> GIves the expected total value of a property over the system
ni: Number of particles in state i
N: Total number of particles.
εi: Energy of state i.
k: Boltzmann constant.
T: Absolute temperature.
q: Partition function; normalizes the probabilities of each state.
⟨X⟩: Ensemble average of property X over the system.
⟨x⟩: Average value of x per particle.
xi: Value of property x for a particle in state i.