Chemistry Hobbs

Lecture 1

Phases and Phase Equilibria

3 Phases

Gas

Liquid

Solid

Under given conditions of pressure and temperature a material will be found in one of these states depending on...

Intermolecular forces

Kinetic Energy

A phase is a form of matter that is uniform throughout in chemical composition and physical state

Kinetic energy is directly proportional to temperature

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These are attractive forces within the molecules which fight agents kinetic energy

A phase transition is the spontaneous conversion of one phase to another phase. Occurs at a characteristic temperature for a given pressure

Heating Curves

X-axis

Y-axis

Energy

Temperature

The slope of the line = The inverse specific heat capacity for that phase

Vapour Pressure

the pressure exerted by the vapour at equilibrium with its condensed phase at a given temperature

Intermolecular Forces rise

Temperature rise

Lowers

Rises

Solid - Gas Equilibria

When kinetic energy and the pressure is high enough sublimation occurs

This converts the solid straight to a gas

Phase Diagrams

Critical Point

This is where the gaseous and liquid phase merge together under a great deal of temperature and pressure

Clausius-Clapeyron Equation

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R=Gas Constant

H=Enthalpy of Vaporisation

T=Temperature (Kelvin)

p=Pressure

Lecture 2

Solution

A homogenous mixture, with no boundaries separating it's components

Heterogeneous Mixture

A mixture in which there are boundaries separating its components

Solute

Solvent

minority component

majority component

Concentrations

amount of solute dissolved in a solvent

Molarity (M)

Molality (m)

Molar Fraction

No. of Moles of Solute

L of Solution

No. of Moles of Solute

Mass (Kg) of Solvent

No. of moles of solute

No. of moles of solvent and solute

Solubility

The maximum amount of solute that can dissolve in a solvent at a given temperature

Why do solutions form

a solute will spontaneously dissolve if the formation of a solution leads to the lowering of the total Gibbs Energy

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Entropy

Is the number of ways in which a system can distribute it's energy

A solvent normally has higher entropy than the pure solute and solvent

Solvents are usually entropically favoured

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Dissolving Salts

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The salt needs to be split into positive and negative ions to calculate enthalpy

Ideal and Ideal Dilute Solutions

Rate of Vaporisation = kx

Rate of Condensation = kp

@ equilibrium they equal each other

Raoult's Law

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Pa=Vapor Pressure of Solvent

Xa=Mole Fraction of A

P*a=Vapour Pressure of Pure Solvent A

Ideal Solution is a solution that obey Rault's law throughout the composition range from pure A to pure B

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Ideal Dilute Solutions

Henry's Law

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Solutions which obeys Raoult's Law and the solute obeys Henry's Law

Pressure increases the solubility of gasses

Lecture 4

Colligative Properties

A collative property of a solution depends not on the nature of the chemical species dissolved in the solution but only the amount of solute dissolved in the solute

E.g.

Vapaur Pressure Lowering

Boiling Point Elevation

Freezing Point Elevation

Osmosis

Change in Bp/Fp = (Kb/Kf)(mb)

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Osmatic Pressure is the hydrostatic pressure due to h

Lecture 4

Liquid Vapour Phase Diagrams

click to edit

Lecture 6

Chemical Equilibria

The System must be closed

It's reached spontaneously

It shows no visual change

Found at a certain temperature

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Reaction shifting

Towards Products

Towards Reactants

Q increases

Q Decreases

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Q<K

Q>K

Q=K

@ Equilibrium

increase product formation until eq. is increased

Increase reactant to reach eq.

Gibbs Free Energy

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G<0

G=0

G>0

Spontanious

Equilibrium

Not Sponatnious