# Difference between revisions of "Course:Total internal reflection"

Main article: brilliance

Total Internal Reflection, or TIR as it is often abbreviated, is a very unique optical phenomenom. Although many aspiring gemologist struggles with this topic, it is fairly easy to understand aslong as you keep a few basic rules in mind.

When light travels through air and reaches an object with a different refractive index (like for instance water, with a RI of about 1.3), two things happen: the light refracts (or bends) inside that object (the water) while other parts of the light will reflect off the water.

In the previous example, the light is traveling from air with an RI of 1, to water with an RI of 1.3.
We could also say that light is traveling from an optically rarer medium (the air) to an optically denser medium (the water).

 Optically rarer means that the medium (material) has a lower refractive index compared to another medium, the material with the higher RI is called the optically denser medium

Although what we discussed up till now doesn't have anything to do with TIR, it is important to know that light traveling from an optically rarer medium to an optically denser medium will always both refract and reflect.

When we let the light travel from the optically denser material (the water) to an optically rarer medium (the air), that always rule is not valid anymore. Light traveling from the denser to the rarer medium will either:

• Completely reflect back inside (with no refraction out)
• Partially refract out and partially reflect back inside
• Continue to travel along the boundary of two media

Which of these paths the light will take depends on the angle the ray of light makes when it hits the boundary between the optically denser and the optically rarer material.
The specific angle, where it will either refract (plus some reflection) or totally reflect (with no refraction), is termed the critical angle. You can think of the critical angle as a turning point.

When the first happens (completely reflect back inside), we talk about total internal reflection.

 The three behaviors a ray of light can exhibit when traveling inside an optically denser medium (like glass) towards an optically rarer medium (as in air)

In the image above the 3 possibilities of light traveling from air into an optically denser material and then towards an optical rarer material (air again) are illustrated. We assume that the hemicylinder (half a cylinder) is glass (RI = 1.54) and the surrounding medium is air (RI = 1).
The dashed line marked "N" and "O" is an imaginary line cutting through the middle of a hemicylinder, this imaginary line is termed the "normal" and from this line the angles are measured. The normal is perpendicular to the flat top of the hemicylinder. A hemicylinder was chosen for illustration as any line going to the center point of a cylinder will reach the outer boundary at 90° as illustrated by the dotted lines. Any ray of light reaching a boundary at 90° will not be refracted.
The critical angle (ca) is the outer limit of the area between the normal and the red line.

The blue ray (left) travels inside the hemicylinder at an angle larger than the critical angle and the light will be internally reflected. The green ray (middle) travels at an angle smaller than the critical angle and will refract out, with some reflection (the dashed-dotted line). The red ray travels at exactly the critical angle and will continue its path along the boundary of the hemicylinder and the surrounding air.

Note: the colored lines are differently colored for illustration purposes, they could all have been blue, or green or red (or any other color).

 Total Internal Reflection can only happen when light is traveling from an optically denser to an optically rarer medium

This theory is very important to understand as it the basic principle behind gemcutting and the refractometer.
In diamond the angles at which the pavillion facets are cut are determined by the critical angle (abbreviated by ca).
The refractometer makes use of this phenomenom by showing which parts of the light on the refractometer's scale are from reflection and which from refraction.

#### Total internal reflection in facetting

Total Internal Reflection in a Diamond.
Light reaching the facet at an angle larger than the critical angle will be reflected.

In 1919 Marcel Tolkowsky published his "Diamond Design - A Study of the Reflection and Refraction of Light in a Diamond" in which he described how to use total internal reflection to get the most light return by a diamond. That was the birth of the modern brilliant cut in which most diamonds are fashioned.

He calculated the angles of the different facets in a way that all light entering through the top (the crown) of the diamond would be internally reflected on the back facets (the pavillion) and guided back to the top, where the light will exit. This causes the brilliance for which the brilliant cut diamonds are famous.

The light enters through the crown (point 1) and reaches a pavillion facet at point 2. As the angle of the incident ray is larger than the critical angle, it will be internally reflected towards point 3. At point 3, the incident ray is also larger than the ca, so again the light ray will be internally reflected. When the light reaches point 4, it reaches the boundary between the diamond and the air at an angle smaller than the critical angle and it will refract out of the stone, following Snell's Law.
In other words, the pavillion facets act like mirrors that send the light back.

Schematic overview of the Total Internal Reflection in different cuts

When the angles are not correct, light may leak out of the side of the brilliant, causing a less attractive diamond that seems to have "windows" in them. Windows are areas where you can almost look through the stone.

When the stone is too shallow, it causes a so-called "fish-eye" when you look through the table of the diamond. This fish-eye is the reflection of the girdle. When cut too deep, it will form a so-called "nail-head", named after the reflection of your head when you look at it through the table.

#### Total internal reflection in a refractometer

The refractometer is one of the most important tools in determative gemology and although you don't need to know how it works in order to operate it, the knowledge will make you much smarter and it is quite satisfactory to the mind if you do understand it.

While we previously talked about light traveling from a gemstone (such as diamond) to an optically rarer medium (air), the theory also works for every other two materials with different refractive indices that are in contact with eachother (such as diamond and glass). The rule that light should travel from the material with the higher refractive index (the denser medium) to a material with a lower refractive index (the rarer medium) still applies. It doesn't work vice versa.

 For every two media in contact in which light is traveling from the denser to the rarer medium, the dividing line where either the ray of light is totally reflected or refracted is fixed and can be calculated. This dividing line is named the critical angle (ca)
Inside the refractometer: Total Internal Reflection

On the left you find an image showing the critical angle as the red line.
When light reaches the boundary of the two materials at an angle larger than this critical angle (the blue line), the ray of light will be totally reflected back into the denser material. Light reaching the boundary at an angle smaller than the critical angle will be refracted out of the denser medium (and a small amount will be reflected) into the rarer medium (the green line). All light traveling precisely on the critical angle will follow the path of the boundary between the two materials.