| Particles naturally form a cone-shape on a flat surface. |
| Slope ange is called the "angle of repose". |
When sand or some other granular material with particles of nearly the same size and shape is poured onto a flat surface, it begins to mound up. As the pile grows, particles move down the slope and away from the center. The result is a pile with the general shape of a cone.
The pile has a characteristic slope that depends upon several factors, including the size and the shape of the granules. The angle of this slope is called the angle of repose.
When a mixture of two granular materials with particles of different angles of repose is poured, something more can happen. The particles often separate according to size, with larger particles ending up at the bottom of the slope. Sometimes the two materials will also arrange themselves in layers. In this activity we will explore some different examples.
First, let’s investigate the angle of repose for individual granular materials with grains of different sizes and shapes. Then we can investigate how mixtures of different granular materials might separate when they are poured.
To observe and measure the angle of repose consistently, we will pour the granular material into a Hele-Shaw cell, a box with two parallel sheets of rigid transparent material a few millimeters apart. You can make such a cell from a CD case and three pencils, or from other materials. Click here for the instructions.
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