unit 2: liquids and solids, solubility, equilibrium will barkalow and price ryan
TRANSCRIPT
Unit 2: Liquids and solids, solubility, equilibrium
Will Barkalow and Price Ryan
Intermolecular forces
• In order from weakest to strongest– London Dispersion – non-polar/non-polar– Dipole-Dipole – polar/polar– Hydrogen Bond – ultra polar/ultra polar• H with N,O,F
– metallic– ionic– Covalent Bond (network) – certain C-family
elements and compounds
Cubic crystal structure
– Simple Cubic (1 atom)• V = e3 = 8r3
– Body-Centered Cubic (2 atoms)• 4r = e• V = e3 =(4r/ )3
– Face-Centered Cubic (4 atoms)• V = e3 = (4r/ )3
Phase Changes
– Matter exists as solids, liquids, or gases– Matter changes between these three phases
based on temperature or atmospheric pressure
Phase diagramPhase Diagrams – show which state matter exist at certain temp and pressure
Triple Point (T) – all three phases are at equilibrium Critical Point (C) – highest temp of pressure where a distinct gas and liquid phase can existSupercritical Fluid (SCF) – liquid and gas phases are indistinguishable
Solubility
• The amount of substance that can be dissolved in a solvent at a given temperature (g/L)
• Some Simple Solubility Rules– NO3
- is always soluble
– C2H3O2- is always soluble
– OH- is insoluble with everything except alkali metals, NH4
+, Ca2+, Sr2+, and Ba2+
– PO43- is insoluble with everything except alkali metals
and NH4+
Equilibrium
• aA + bB cC + dD• Occurs when opposing reactions proceed at equal rates with
constant concentrations• KC = equilibrium constant
– KC = {[C]c[D]d}/{[A]a[B]b}– No Solids and Liquids included in equation
• Q = Reaction Quotient– Q = {[C]c[D]d}/{[A]a[B]b}– When not at equilibrium– Q < K Shift Right, Q > K Shift Left, Q = K Equilibrium Established
• No solids or liquids included in equation
Equilibrium continued
• KP = KC(RT)-n
• or same expression as Kc, but using pressures
• KSP = solubility product constant, this indicates how soluble a solid is in water– KSP = (C)c(D)d
– Reactants are Solids so they are not included in the equation
LeChâtlier’s Principle • A system in equilibrium, when disturbed, will shift to
the extent necessary to restore equilibrium• Example:– N2 + 3H2 2NH3 + 94K• Disturbance add N2: reactant is increased so product is
increased, shift right• Disturbance increase temp: tries to lower energy, lower
products, shift left• Disturbance increase pressure: will favor side with fewer moles,
fewer moles on product side, increase products, shift right• Disturbance add catalyst: reaction goes faster but no change to
each side, no shift
Predicting Formation of precipitates based on Ksp
– Knet = Ksp x Kf
• Kf = formation constant
– Used in reactions with complex ions– Lower Ksp means it’s less soluble. The combination
with a complex ion makes it more soluble (the Kf value times the Ksp value is much larger than the original Ksp value).
Concentration Units
– Cmolar = nsolute/Vsolution
– Cmolal = nsolute /msolvent (kg)
– Mass Percent = msolute /msolution
– Mole Fraction = nsolute /nsolution
– Volume Fraction = Vsolute /Vsolution
– Parts Per Million (PPM) = msolute (mg) / msolvent (kg) ≈ msolute (mg) / msolution (kg) when mass of solute is small enough
Henry’s Law
– Sg = kHPg
– The solubility of gas increases in direct proportion to the partial pressure above the solution
Colligative Properties
– Boiling Point Elevation: Tb = iCmolalKb
• i = Van’t Hoff Factor – when dissolved , # of particles the molecule breaks into (Ex. NaCl = 2)• Kb = Boiling point elevation constant• solutes make it harder for water molecules to vaporize,
thus requiring more energy to boil– Freezing Point Depression: Tf = iCmolalKf
• Kf = freezing point depression constant• solutes make it harder for water molecules to form an
orderly crystalline structure
Raoult’s Law (Vapor Pressure)
– PA = XAPOA
– PA = solution vapor pressure
– XA = mole fraction of solvent (nsolvent/nsolution)
– POA = solvent vapor pressure
– Adding a non-volatile solute to a solution will lower the vapor pressure, thus raising the boiling point
Osmosis
– V = nRT– = nRT/V = CmolarRT• = osmotic pressure • R = 8.314 if pressure is in Pascals (Pa). R = 0.08206 if
pressure is in atm
– Pressure required to prevent osmosis by a solvent toward a solution with a higher solute concentration