ch 10.1
DESCRIPTION
Ch 10.1. Kinetic Theory: 5 assumptions small particles - far apart Movement random, rapid & continuous Collisions are elastic No attractive/repulsive forces Average kinetic energy depends on temp. Ch 10.1. Properties specific to gases: Expand Compress Low density Fluid - PowerPoint PPT PresentationTRANSCRIPT
1
Ch 10.1
• Kinetic Theory: 5 assumptions1. small particles - far apart
2. Movement random, rapid & continuous
3. Collisions are elastic
4. No attractive/repulsive forces
5. Average kinetic energy depends on temp.
2
Ch 10.1• Properties specific to gases:
– Expand– Compress– Low density– Fluid– Diffuse: [↑]to [↓] until equal
• Rate depends on, speed, diameter, attractive force
• Calculated by v1 m2
• v2 m1
• Effuse: force through small opening.– Joule Thomas effect
3
Ch 10.2
– Note: the lower the temp of a gas the more “ideal” it is
– Pressure = caused by the collisions of gas particles against it’s container.
– Standard Pressure units• 101.3 kPa=• 760mmHg or Torr for Torricilli (barometer)• 1 ATM
– STP = standard temp and pressure
4
Ch 10.2
• Standard Temperature– 0 oC or 273 K
• Temp is a measure of kinetic energy
• Kinetic energy = mv2 / 2
• Absolute zero is where (theoretically) all particle motion ceases.-273 oC or 0 K
5
Ch 10.3
• In 1662 Robert Boyle: If amount and temp remain the same then,
• Boyle’s Law = P1V1 = P2V2
• Inverse proportion: As one goes up the other goes down.
6
Ch 10.3
• 1787 Jacques Charles showed that the volume of a gas varied directly with Kelvin temp
• Charles’ Law: V1 = V2
• T1 T2
• K= oC + 273
• *** always calculate in Kelvin for gases***
7
Ch 10.3
• 1802 Joseph Gay-Lussac recognized that for each 1oC increase the volume would increase by 1/273.
• Therefore at -273oC a gas would have no volume or disappear BUT ALL gases turn to liquid before this happens.
• He also noticed : P1 = P2
• T1 T2
8
Ch 10.3
• The Combined Gas Law:
P1V1 = P2V2
T1 T2
9
Ch 10.3
• John Dalton found that in the absence of a chem rxn the pressure of a gas mixture is the sum of the individual gas pressures.
• The partial pressure is the pressure of one gas in a mixture so it’s only part of the total pressure!
• P total = P gas + P other gases
• P gas = P total – P other gases
10
CH 10.3
• When a gas is collected through water displacement –The left over water vapor pressure exerts a pressure that must be accounted for.
• Use a water vapor chart (pg 899)
• Pgas = Patm – PH2O at what ever temp
•
11
CH 10.3
• A sample of Oxygen gas is collected in a 175ml container over water at 15oC and the barometer read 760 torr. What volume will the dry gas occupy at 770torr and 15oC.
• Adjusting for the water vapor 760 torr - 12.8 torr = 747.2 torr should be used instead of 760 torr.
12
IDEAL GAS Law
• Ideal Gas equation is derived at by combining all 4 variables concerned with the physical characteristics of gases (volume, temperature, pressure & # of particles)
13
IDEAL GAS Law
• Ideal Gas Equation: PV=nRT
• R is a constant used in calculations involving the ideal gas equation
• R= .0820 L•Atm
• mol•K
• R = (1atm)(22.4L)/ (1mol)(273K)
• n = number of moles
14
Molecular Mass and Density
• The calculation of the molecular mass (M) and Density (D) can be determined using the ideal gas equation.
• M = mRT D= MP
PV RT
This is important in determining the formulas and structures of unknown compounds.