science:gas
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Table of Contents
gas behaviour and equations
Introduction
- most substances become gases once they have become liquids (at their melting point temperature) and then the temperature exceeds their boiling point temperature
- NB. some substances sublime straight from solid to gas
Boiling point
- this is the temperature at which a liquid will form gas bubbles and start to evaporate into its gaseous form
- the vapour pressure of a liquid rises as its temperature increases
- the boiling point temperature is when the liquid's vapour pressure exceeds that of the pressure of the space above it
- the standard boiling point is measured when the space above it is normal atmospheric pressure of 1 atm
- if the pressure of the space above it falls then the boiling point temperature falls (eg. high altitude)
- this is why butane gas stoves can work in freezing conditions at high altitude but not at normal altitudes
- if the pressure of the space above it increases, then the boiling point temperature increases (eg. pressure cooker, LPG bottles)
- vapour pressure of propane is much higher than that of butane and thus propane containers need to be build much stronger
- see comparison of gas options for hiking or camping for more details
The Gas Equation
PV = nRT
- where:
- P = pressure in Pascal (N/m2)
- V = volume of space the gas is contained within measured in m3
- n = number of moles of gas substance in mol
- R = the gas constant = 8.314 J/(mol.K)
- T = temperature in degrees Kelvin K= Celsius temp + 273.15
- NB. if use P in atm, V in litres, then the gas constant is 0.08206 L.atm/(mol.K)
moving gas from one volume space to another volume space
- the PV product above remains constant as you have not lost any gas, hence:
- P2V2 = P1V1
- ie. the new pressure = P1V1 / V2
Gaseous pressure units
- 1 atmosphere (atm) is the standard pressure of earth's atmosphere which equates to:
- 1.01325 bar
- 101.325 kPa
- 760mmHg = 760 Torr
- 14.696 pounds per square inch (psi)
Relative gas densities to air
- in general gas density rises in proportion to its molecular weight for the same temperature and pressure
- the following assumes same temperature and pressure (except for the hot wood fire smoke which is compared to normal ambient air temperature)
- carbon monoxide, like smoke, coming from a stove or heater will initially rise hence smoke alarms and CO alarms should generally be mounted near a ceiling for the earliest warning, later both will mix with air as they cool to air temperatures and smoke may even sink
- underground coal miners are at major risk from:
- pools of carbon dioxide (“black damp”) as it forms from human respiration, the rotting of timber supports, or the slow oxidation of coal
- carbon monoxide poisoning via either:
- “white damp” - CO produced from machinery exhausts or slow coal fires
- “after damp” - CO left behind after a methane or coal dust explosion
- methane asphyxiation “firedamp” from methane trapped within coal seams and rock strata that bleed out when mined
- hydrogen sulphide “stinkdamp” produced by the decomposition of iron pyrites in the presence of moisture or organic breakdown
- NB. fog tends to lie close to ground not because of intrinsic gas density but because it is colder and thus more dense
| Relative density to air | molecular weight (g/mol) | |
|---|---|---|
| hydrogen H2 | 0.07 | 2 |
| helium He | 0.138 | 4 |
| methane (natural gas) CH4 | 0.554 | 16 |
| pure water vapour H2O | 0.62 | 18 |
| hot wood fire smoke (mainly nitrogen, carbon dioxide and water vapor) | 0.6 to 0.8 depending upon temperature | |
| acetylene C2H2 | 0.91 | 26 |
| carbon monoxide CO | 0.97 | 28 |
| nitrogen N2 | 0.97 | 28 |
| dry air | 1.0 | 29 (average of constituents) |
| same temperature wood fire smoke | 1.01-1.05 | |
| oxygen O2 | 1.105 | 32 |
| hydrogen sulphide H2S | 1.19 | 34 |
| carbon dioxide CO2 | 1.53 | 44 |
| propane C3H8 | 1.53 | 44 |
| butane C4H10 | 2.0 | 58 |
science/gas.1788353237.txt.gz · Last modified: 2026/09/02 12:47 by gary1