Site Menu
 
  Renewing Paradise Advertisement
Tuesday, 07 February 2012
How soon?
Resize Site Text
A+ | A- | Reset
Navigation
Site Menu
About Rainmakers
Credits & Debits
Copyright Notice
FAQs
About New Caledonia
About Conrad Hopman
Contact & Password
Links
Search
OOPS. Your Flash player is missing or outdated.Click here to update your player so you can see this content.
Login for special content
You must be a registered user and log-in before you can view the "restricted" areas of this web-site.

Within the restricted areas, there are also some "special" areas, for which you must contact the author (using the "Contact" link email form) and request a special username & password for access to be sent by email.






Lost Password?
No account yet? Register
We are an ethical, non-profit association and strictly respect your privacy. By registering at this site you accept the condition that you will not deliberately do anything contrary to the interests of the Rainmaker Ozeania Association.

We hope you find the ideas presented here stimulating and thought provoking. Please send your feedback / comments through the 'contact' link.

Related Items
DB function failed with error number 1146
Table 'bazrmo07_joom7.jos_contentprotector_params' doesn't exist SQL=SELECT * FROM jos_contentprotector_params
PDF Print E-mail
Article Index
#1.1 Heating Air
Page 2
Page 3
Page 4
Page 5
Page 6
Page 7
Page 8

Boiling water becomes bigger, but its temperature and pressure do not change

Image

The heat added to the L.H2O between 0 and 100°C can be felt and measured with a thermometer. It is thus called sensible heat (SQ). The Q added to the 100°C water to boil it away is called "latent" because it is stored in the G.H2O and released again when the G.H2O condenses back to L.H2O. LQ is volume Q.

LQ and SQ initially came from the same fire. They differ what the water does with them. Its T rises from 0 to 100°C; its volume increases during the 100°C L.H2O- G.H2O phase transition. Most substances expand as they are heated. The volume of mercury in a thermometer increases slightly as it is warmed. That is why the column lengthens or shortens to show T. Mercury expands when it boils to vapour- as water does. When L.H2O freezes to ice, it becomes bigger and colder at the same time- but its T does not change. The Q removed from L.H2O as it freezes is a sort of negative LQ.

LQ absorption can be used for cooling. This can be observed after swimming on a day when a very hot, dry wind is blowing. One soon becomes so cold that one shivers. The hot dry wind absorbs LQ out of one's body as it dries the water off it. The body, and the hot wind, both have a lower T than before the wind absorbed the moisture and LQ necessary to do this.

This effect is used to measure atmospheric humidity with wet and dry bulb thermometers. The wet bulb is relatively cooler when the air is drier. It is also used to keep water cool in hot, dry climates. The water is put in porous earthenware jars. Water seeping out through the pores sucks heat out of the jars as it evaporates. A sophisticated variant of the same idea is used in absorption chillers. If a warm (e.g. 40°C) dry wind blows over a colder (20°C) sea, both the sea and the wind are T cooled, while the wind absorbs LQ (586 kCal per kg L.H2O evaporated) out of the sea. More LQ is absorbed per kg atmospheric humidity (Φ) evaporating from (20°C) water (586 kCal per kg L.H2O evaporated) than from water boiling at 100°C (539 kCal per kg L.H2O boiled).



 
 
Go to top of page  Site Menu | About Rainmakers | Credits & Debits | Copyright Notice | FAQs | About New Caledonia | About Conrad Hopman | Contact & Password | Links | Search |