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Atmospheric Science
the study of gases in the atmosphere and the reactions they undergo
Gas Characteristics
No definite shape or vol
Compressible
Low density changing based on temp and V
Units of gas density
g/L
If temperature increases density
density decreases
If volume increases then density
density decreases with the volume
Gases exert
Pressure
Atmospheric pressure
Pressure exerted by the gases in the air on everything inside the earth’s atmosphere
Barometer
device used to measure pressure
Units of pressure
atm
mmHg
torr
Units of pressure conversions
760mmHg=1atm=760torr
4 parameters of gas
Pressure
Volume
Moles
Temp
Directly proportional
As one increases the other increases
(y-x) opposite sides of equation x=y
Inversely proportional
As one increases the other decreases
(y-1/x) same side xy=0
Boyle’s Law relates
Pressure and Volume, constant T and N
Boyle’s law experiment
J-Tube experiment
J-Tube Experiment relationship
inversely, as P increases, V decreases and vice versa
Charle’s Law relates
Volume and Temperature, constant P and N
Charle’s Law Relationship
Direct, as Volume increases T increases
Avogadro’s Law relates
moles of gas to volume, constant T and P
Avogadro’s Law relationship
Directly, as n increases V increases
Ideal Gas equation(only used by GASES)
PV=nRT
Mole fraction (X)
ratio of the moles of a given gas to the total # of moles in a mixture of gases
Kinetic Molecular Theory
Attempts to explain why gases follow the ideal gas law
KMT #1.
G particles are so small that the V of each particle is negligible.
KMT #2.
g particles are in constant motion colliding with walls = pressure
KMT #3.
g particles assert no force on each other
KMT #4.
g particle collision are elastic, no kinetic energy lost
KMT #5.
Avg kinetic energy of a g particle is proportional to T only
Gas particles move by
Diffusion
Two generalizations of gas particles
As size increases, speed decreases
As T increases, speed increases
Random walk Principle
gas particles travel in a straight line until they collide with something, changing the direction
Mean free path
shortest distance between starting and ending points
Liquid characteristics
Definite volume, no shape
Polar liquids used as solvents (H2O)
Solids characteristics
Fixed shape
Fixed Volume
Incompressible
Hydrogen bonding importance
Supports life on earth
Crystalline Solids
regular, repeating 3D arrangements of atoms and/or molecules
Amorphous Solids
disordered structure with no defined pattern
Crystal Lattice/Crystal Structure
points used to denote positions of atoms/molecules
Unit cell
smallest repeating unit of crystal structure
Types of Crystalline solids
Atomic
Ionic
Molecular
Atomic Solids
atoms at lattice points
Metallic Solids
metal atoms held together by clouds of ve-
high melting point, shiny, conductive (Au)
Ionic Solids
Ions at lattice points
brittle, conductive, high melting point
ex. NaCl(s)
Molecular Solids
covalently bonded molecules at lattice points
poor conductivity, low melting point, hard, low density
ex. H2O(S)
Network Covalent Solids
nonmetal atoms at lattice points
poor conductivity, low melting points, very hard
Unit cell lattice points
represent atoms/ions/molecules aka Spheres
Net number of atoms/spheres
total # of atoms contained within the invisible borders of the unit cell
Types of Unit Cells
Simple cubic
Body-centered cubic(bcc)
Face-centered cubic (fcc)
Closest packing structures
arrangement of atoms in a crystalline solid which assumes spheres are as close to each other as possible
Type of packed structres
Hexagonal Closest packed (bcc)(hcp)
Cubic closest packed(fcc)(ccp)
Deposition
gas to solid
sublimation
solid to gas
condensation
gas to liquid
Nonpolar (even electronegativity) means what forces
dispersion
Polar(uneven) compound has what forces
dispersion and dipole
H-F, H-O, H-N
dispersion, dipole, H
C-H bonds only have what force
dispersion
If K > 1, mostly
productsI
If K<1, mostly
reactants