barometers and the relationship they have to thermometers? I'm trying to understand how atmospheric pressure effects the resting level of a liquid and I don't feel quite right about how I see it. I'm wondering why temperature doesnt play an equally significant role in barometers, or if it does.
Come on ya'll - - let's teach Mathis a thing or two.
It's hard to picture how they managed to do this in the 17th century without getting air bubbles into the tube, isn't it?Barometer (from http://www.infoplease.com
Barometer (burom'utur) [key], instrument for measuring atmospheric pressure. It was invented in 1643 by the Italian scientist Evangelista Torricelli, who used a column of water in a tube 34 ft (10.4 m) long. This inconvenient water column was soon replaced by mercury, which is denser than water and requires a tube about 3 ft (0.9 m) long. The mercurial barometer consists of a glass tube, sealed at one end and filled with pure mercury. After being heated to expel the air, it is inverted in a small cup of mercury called the cistern. [snip]
Has anyone thought much about what is theoretically contained in such a vaccum? I know that by definition there is nothing, but I think the truth is that there is always a plenum of energy no matter where you are, just a different type.article continued: The mercury in the tube sinks slightly, creating above it a vacuum (the Torricellian vacuum).
In other words; atmospheric pressure stops the mercury from decreasing down the tube to such an extent that it flows out of the cisturn and onto the floor.Atmospheric pressure on the surface of the mercury in the cistern supports the column in the tube
Is that a good way of putting it?
Ok, so they seem to be saying; the higher you go above sea level, the more the mercury level decreases down the tube, and this is because the air weighs less. Because the air weighs less, the mecury is allowed to relax a bit more. The mecury level goes down in the tube, only because the mercury level in the cisturn goes up. Right?The level that the column of mercury is at varies in height according to variations in atmospheric pressure. Hence changes in elevation affect the level that the column of mercury rests at. The column of mercury generally decreases in height as you climb above sea level
Can you go so high up that the cisturn overflows ? Gravity of course would stop it from emptying out completely
Also, at colder temperatures, does a body of liquid like mercury actually shrink in overall resting height?
The reason I ask is because, when I look at a thermometer, the mercury rises when it gets hot. Is this because the body of the mercury as a whole is expanding? And does the mercury decrease when it's cold becaues its body as a whole is constricting, becoming more dense?
Thermometers seem significantly different than barometers because they are totally sealed off and therefore the weight of air cannot cause the mercury to rise or fall.
Am I on the right track here folks?
What I'm further confused about is why the barometer is not seriouly affected by temperature as well as atmospheric weight.
Why does air weigh less when a storm is building up? Why does the air weigh more during times of peace?Standard sea-level pressure is 14.7 lb per sq in. (1,030 grams per sq cm), which is equivalent to a column of mercury 29.92 in. (760 mm) in height; the decrease with elevation is approximately 1 in. (2.5 cm) for every 900 ft (270 m) of ascent.
At a given location a storm is generally anticipated when the barometer is falling rapidly; when the barometer is rising, fair weather may usually be expected.
- Mathis