atmospheric chemistry

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T = 298.15K

P = 100kPa

T = 273.15K

P =100kPa

SATP

collisions

kinetic energy ∝ temperature

Avogadro's Law

Density

Lots of space between particles

Gas condition

STP

Planetary atmospheres

Atmospheric Composition

Greenhouse Gases

Standard atmospheric conditions

climate change

mol

mole fraction

ratio of moles of one substance vs. total substances in gas mixture

partial pressure

molar mass

g/mol

Molar Constant (R)

Ideal Gas Law

Combined Gas Law

particles are small, spehrical entities

-273.13

Gas is highly condensable, no fixed shape

Charles's Law

Gay-Lussac's law

Boyle's Law

Impacts from particles on surfaces create pressure

particles

Pressure (P)

Temperature (T)

Melting/Fusion

state changes

Liquids

Solid

Particle theory

KMT

States of Matter

Absolute Temperature

number of particles (n)

°C

S.I. Units

K

Pa

L

atmospheric chemistry

Gas

4 Main variables

Volume (V)

Properties

Gas Laws