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States of matter
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kinetic theory of matter
all matter consists of tiny particles that are in constant, random motion
kinetic energy
energy of motion (depends on the mass and speed of particles)
temperature
measure of the average KE of the particles in a substance
kinetic theory of gases
gas particles have negligible volume and are very far apart
gas particles are in constant, random motion
gas particles have elastic collisions (no energy is lost and no attractive forces)
gas pressure
the result of gas particles colliding (with walls of a container)
more collisions = more pressure
causes: more particles, decreased volume, higher temperature
pressure
atmospheric pressure is caused by the force (weight) of air due to gravity
standard atmospheric pressure
air pressure at sea level
equal to 1 atm, 760 mmHg, or 101.3 KPa
0C and 1atm
intermolecular forces
forces of attraction between molecules (not as strong as intramolecular forces)
london dispersion forces
attractive forces caused by uneven distribution
diople-diople forces
attractive forces between polar molecules
hydrogen bonding
special type of diople-diople forces occurring between hydrogen and an electronegative element (O, N, F)
evaporation
transition of particles from liquid to gas at a temperature below the boiling point (temp of remaining liquid decreases as evaporation occurs)
criteria for evaporation
must be at the surface of the liquid and must have enough energy to break IMFs
vapor pressure
pressure exerted by gas particles above a liquid (result of evaporation)
vapor pressure and IMFs
the weaker the attractive forces, the higher the vapor pressure (more volatile liquid)
boiling
rapid phase transition from liquid to gas (vapor)
bubbles form due to vapor pressure being equal to atmospheric pressure
normal boiling point
the temperature liquid will boil at when the vapor pressure above the liquid is 1 atm (760 mmHg)
melting point
the temperature a solid changes into a liquid
strong IMFs lead to higher melting points
vibrations between particles need to become strong enough to overcome attractions
freezing point
the temperature a liquid changes into a solid
melting point = freezing point
at this temp, liquid and solid phases are in equilibrium
amorphous solids
lack an ordered internal structure (atoms are randomly arranged)
crystal structure
particles are arranged in a crystal lattice
unit cell
the smallest group of particles within a crystal that retain the geometric shape (determines the overall crystal shape)
allotropes
2 or more different molecular structures of the same element
each allotrope has different physical properties due to its different structure
only a few elements have allotropes (phosphorous, sulfur, oxygen, boron, antinomy)
gas
low density, indefinite shape and volume, weak IMFs
liquid
high density, indefinite shape but definite volume, moderate IMF
solid
high density, definite, shape and volume, strong IMFs
water
water does not follow the normal trend for density of solids, liquids and gases
solid ice is less dense than liquid water
unique that water is a liquid at room temperature (due to H-bonding) other molecular substances with similar molar masses are gases at room temperature
melting
solid to liquid (endothermic = particle absorb energy)
freezing
liquid to solid (exothermic = particles release energy)
boiling (vaporation)
liquid to gas (endothermic)
condensation
gas to liquid (exothermic)
sublimation
solid directly to gas
deposition
gas directly to solid
phase diagram
shows the phase of a substance at different temperatures and pressures
the curves are lines of equilibrium (2 phases at once)
critical point
the temp. and pressure at which the gas and liquid phrases of a substance become identical
triple point
the temperature and pressure at which all 3 phrases are in equilibrium (all 3 exist at the same time)
supercritical fluid
a substance held at or above its critical temperature and pressure
has properties of both gas liquid