octopus
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eaglesaquarium said:FM... your videos scare me. Not that they are scary in their own right, but the fact that such things exist (and that you can find them) frightens me a little.
majerah1 said:Atmospheric pressure.
Fishmanic said:more details needed I believe
It's the Brenulli Effect.. Where gravity in conjunction with hydrolic pressures interact and gets the fluid in motion.. The fluid will continue to stay in motion until the fluid pressure is equal, or something like that..majerah1 said:Yeah but I don't remember exactly how to explain it, so Ill let someone else take that honor
HAMBONE said:
It's the Brenulli Effect.. Where gravity in conjunction with hydrolic pressures interact and gets the fluid in motion.. The fluid will continue to stay in motion until the fluid pressure is equal, or something like that..Yeah but I don't remember exactly how to explain it, so Ill let someone else take that honor
http/science.howstuffworks.com/siphon-info.htmHow A Siphon Works
Siphons operate by atmospheric pressure. The container from which the liquid is siphoned must therefore be open to the air. When the tube is filled, the liquid will run out of the lower end. (The greater weight of the liquid in the arm outside the container determines the direction of flow of the liquid.) As the liquid starts to flow, the fluid pressure at the top of the tube is lowered. A liquid always flows from an area under higher pressure to an area of lower pressure. The liquid in the container (under atmospheric pressure) flows up into the tube (an area of lowered pressure). This liquid in turn will flow out the outside end of the tube, again lowering the pressure at the top of the tube.
Once the flow has begun, it will continue if undisturbed as long as the inside end of the tube remains below the surface of the liquid. The flow can be cut off by raising the outside end of the tube above the level of the surface of the liquid in the container.
One limit to the use of siphons is imposed by the height to which atmospheric pressure can lift a given liquid. At sea level, atmospheric pressure can raise water to a height of about 30 feet (9 m). At higher altitudes the pressure is less, as is the height to which the water can be raised. Liquids heavier than water cannot be raised as high as water. Thus at sea level, mercury can only be raised about 30 inches (760 mm).