Skip to main content Accessibility help
×
Hostname: page-component-848d4c4894-5nwft Total loading time: 0 Render date: 2024-05-20T01:55:36.759Z Has data issue: false hasContentIssue false

2 - Real gas compression

from Part 1 - Physics, mathematics, statistics, anaesthetic apparatus

Published online by Cambridge University Press:  13 August 2009

Sylva Dolenska
Affiliation:
William Harvey Hospital, Kent
Get access

Summary

Forces of adhesion in the gas lessen the impact on the container. The result is that the pressure measured is less than that predicted by the universal gas equation. The effect is magnified in a smaller volume.

Also, the molecules are not negligible in size; their total volume lessens the volume of the container, decreasing the distance of travel; a correction for the volume of the molecules (Vo) has to be applied.

When gas is compressed at a sufficiently low temperature, the forces of adhesion eventually cause its liquefaction (i.e. the forces of attraction overcome the random thermal motion).

Isothermic compression – decompression

Figure 3 shows slow compression of nitrous oxide under various temperature conditions. Because compression is slow, there is sufficient time for temperature equilibration with the surroundings. This pressure–volume change is called isothermic.

The top isotherm for 50 ℃ behaves as an ideal gas isotherm. At 36.5 ℃ the isotherm just touches the lightly shaded area in the graph, which represents the gas and liquid phase. This temperature is the critical temperature of nitrous oxide, above which the gas cannot be liquefied at any pressure. At lower temperatures, here 20 ℃, the gas can be liquefied. If compression is slow to allow temperature to remain constant, the pressure in the container remains constant until all gas is liquefied: the decrease in volume of the container is matched by a decrease in volume of the gaseous phase (which is now called vapour) as it is being liquefied.

Type
Chapter
Information
Publisher: Cambridge University Press
Print publication year: 2006

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

Save book to Kindle

To save this book to your Kindle, first ensure coreplatform@cambridge.org is added to your Approved Personal Document E-mail List under your Personal Document Settings on the Manage Your Content and Devices page of your Amazon account. Then enter the ‘name’ part of your Kindle email address below. Find out more about saving to your Kindle.

Note you can select to save to either the @free.kindle.com or @kindle.com variations. ‘@free.kindle.com’ emails are free but can only be saved to your device when it is connected to wi-fi. ‘@kindle.com’ emails can be delivered even when you are not connected to wi-fi, but note that service fees apply.

Find out more about the Kindle Personal Document Service.

Available formats
×

Save book to Dropbox

To save content items to your account, please confirm that you agree to abide by our usage policies. If this is the first time you use this feature, you will be asked to authorise Cambridge Core to connect with your account. Find out more about saving content to Dropbox.

Available formats
×

Save book to Google Drive

To save content items to your account, please confirm that you agree to abide by our usage policies. If this is the first time you use this feature, you will be asked to authorise Cambridge Core to connect with your account. Find out more about saving content to Google Drive.

Available formats
×