Phases Flashcards
Ideal Gas Law
PV=nRT R=8.314 J/K mol
Simple Mercury Barometer
Patm=ρgh
1 atm = 760 torr = 760 mmHg
Boyle’s Law
PV=constant
P and V inversely proportional at constant T
Charles’ Law
V/T=constant
V and T are proportional at constant P
Avogadro’s Law
V/n=constant
V and n are proportionals at constant T and P
Isovolumetric
No change in volume = no work done
ΔE=q
Adiabatic
No heat exchanged
ΔE=w
Isothermal
No internal energy change
ΔE=0
Standard molar volume
22.4 L
Partial Pressure
P(a)=x(a) P(total) x(a)=mole fraction
Dalton’s Law
P(total)=P(1) + P(2) + P(3) + …
Partial Pressure Equilibrium Constant
K(p)= P(C)^c P(D)^d / P(A)^a P(B)^b
K(p)=K(c)(RT)^Δn
Real Gases
Behave non-ideally w/ high P (above 10 atm) and low T (near boiling pt)
Heat Capacity
The added nrg needed to incfrease the tep of a given substance 1K or 1°C
c=q/ΔT
Heat transfer
measured in calories
1 cal = 4.184 J
1 Cal = 1000 cal = 4184 J
q=cΔT
Specific heat Capactiy
q=mcΔT in J/Kg K or cal/g °C
Phase Changes
Melting, boiling, sublimating: endothermic (+ΔH), increase in entropy (+ΔS), increase volume and molecular motion
Freezing, condensation, deposition: exothermic (-ΔH), decrease in entropy (-ΔS), decrease volume and motion
Critical Point
Molecule both gas and liquid
Triple point:
Equilibrium between the phases
Phase Diagram
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