Capillary action
Capillary action means either of two things:
- When liquid moves through thin tubes.
- When liquid moves through something that is full of little holes (like a sponge).
Capillary action is a result of the surface tension of liquids.
An example of capillary action is what happens inside a drinking straw left in a cup of water. The force of adhesion which holds the water together and to the straw is a little stronger than gravity, so the water will rise inside the straw a little higher than the rest of the water.
Another example is what happens when putting a sponge in a puddle of water. The little bubbles in the sponge work like many straws gathered together. When the sponge is dipped in water, the water starts to go into the holes, and the bubbles that are inside the sponge pull on the water that they touch.
Capillary action also takes place inside the human body. For example, it removes tears from the eyes.
Capillary Action Media
Capillary water flow up a 225 mm-high porous brick after it was placed in a shallow tray of water. The time elapsed after first contact with water is indicated. From the weight increase, the estimated porosity is 25%.
Moderate rising damp on an internal wall
Capillary flow experiment to investigate capillary flows and phenomena aboard the International Space Station
Water height in a capillary plotted against capillary diameter
Capillary flow in a brick, with a sorptivity of 5.0 mm·min−1/2 and a porosity of 0.25.
Capillary rise of water between two glass plate. The product of layer thickness (d) and elevation height (h) is constant (d·h = constant), the two quantities are inversely proportional. The surface of the water between the planes is hyperbola.
Capillary rise of water between two glass plate. The product of layer thickness (d) and elevation height (h) is constant (d·h = constant), the two quantities are inversely proportional. The surface of the water between the planes is hyperbola.
Capillary rise of water between two glass plate. The product of layer thickness (d) and elevation height (h) is constant (d·h = constant), the two quantities are inversely proportional. The surface of the water between the planes is hyperbola.
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