st 1 scenario MEASUREMENT OF WATER REFRACTIVE INDEX GRIGORIOS P. ZYGOURAS PHYSICIST MELISSIA LYCEUM , ATTICA , HELLAS PURPOSE OF EXERCISE • To understand that light changes direction passing through different transparent materials (optical media) • To calculate the refractive index of a liquid by using diffraction grating • To calculate the refractive index of a liquid by processing two photos, using SalsaJ software • To confirm Snell's law of refraction. THEORETICAL APPROACH • When light passes from one optical medium to another changes direction • This phenomenon is called refraction. Measuring the deviation of the light ray , we calculate the medium’ s refractive index • These measurements are made by editing taken photos , which show the different path of light when it passes from air into water • Two different setups are used to take the appropriate images: 1. with diffraction grating 2. without diffraction grating and changing the angle of incident ray at the boundary between the two media • Two different refraction index calculations are made using : 1. Snell's law and 2. The theory that fringe patterns of the same order have the same integer wavelength multiple distance from the central fringe pattern either light is transmitted in the air or in another medium (water). REQUIRED EQUIPMENT • • • • • • • Diffraction grating (200 - 500 lines per mm) Bubble Laser, or Laser pointer Transparent bowl Adhesive tape Scissors Translucent paper Pegs as a means of support, in case of Laser pointer use • NOTE: The experiment performance is better using Bubble Laser device than Laser pointer, because the images are sharper. REQUIRED EQUIPMENT TAKING PHOTOS 1. 2. 3. For best results use : A dark room to get better definition Long exposures without flash A tripod to avoid shaky pictures emerge. CALCULATION OF THE REFRACTIVE INTEX WITHOUT DIFFRACTION GRATING • Using two images of the light ray : One falling vertically to the boundary of air - water and one forming a small angle with it. In the second case the light path changes as it goes from air to water. • We convert the two pictures in one using the software SalsaJ - as described below - and then we measure the deviation of the two lateral light rays from vertical. • We calculate the refractive index of water from the relations derived on the basis of the theoretical approach to the phenomenon. 1ST MEASUREMENT METHOD WITH COMPOSITION OF TWO PHOTOS (Without diffraction grating) • We pour water in the bowl. • We stick the translucent paper on one side of the bowl. • We keep the source of light (Laser beam) at the opposite side perpendicular to the surface. One half the beam has to pass through the water and the other half through the air. • Because the light ray is perpendicular to the boundary of the two media there is no difference between them. • We take a photo. PHOTOS OF EXPERIMENTAL SETUP THE DIFFERENCE IS DINSTINCTIVE IN THE DARK PHOTO IN WHICH THE LIGHT RAY IS PERPENDICULAR TO THE BOUNDARY OF THE TWO MEDIA THERE IS NO DEVIATION OF LIGHT RAY PASSING THROUGH THE AIR AND THE WATER • We turn slightly the source of the light so that the light ray strikes with a very small angle of incidence (to be consistent with the approach that sinφ=tanφ) • We can now observe the divergence of the light ray when it passes through the water from the footprint of the translucent paper • We take a photo again IMAGE IN WHICH THE LIGHT RAY STRIKES WITH A VERY SMALL ANGLE OF INCIDENCE WE OBSERVE THAT THE LIGHT RAY PASSING THROUGH THE WATER HAS LESS DEVIATION THAN THAT PASSING THROUGH THE AIR PHOTOS PROCESSING • • Open the images with software SalsaJ. We convert images in 8 bit mode to be editable , following the next steps in the menu Image > format > 8 bit, as shown in the picture below. • • Then from the same menu select image > adjust > Brightness/contrast. We suggest the option auto. As we can see on the photo below. UNIFICATION OF THE TWO PHOTOS To measure the deviation of the light rays in the water and in the air, we unify the two images obtained following the steps that are shown in the picture below. In the menu click, manipulation> computer images> add PUTTING THE TWO PREVIOUS IMAGES TOGETHER SCHEMATIC PRESENTATION OF LIGHT RAYS PASSING THROUGH AIR AND WATER Διάγραμμα διάδοσης του φωτός στον αέρα Diagram propagation of light in air φ1 Central beam ΔΧα 1st beam Distance between light source and translucent paper Διάγραμμα Diagram propagation διάδοσης του of light φωτός in water στο νερό Φ2 Απόσταση Distance between πηγής light φωτός source και διαφανούς and translucent χαρτιού paper Central Κεντρική δέσμη beam ΔΧν 1st beam d MATHEMATICAL EQUATIOS USED FOR OUR CALCULATION • From the geometry of the figure we see that tan 1 and tan 2 • • • a d for the path of light in air, v for the path of light in water. d We know that for small φ angle values we have : sin tan From Snell's Law na sin 1 n sin 2 where ηα= refractive index of air and nv = refractive index of water. We know that the refractive index of air has a value equal to 1. So calculating the prices of tanφ and using the equation sin tan we can calculate the refractive index nv of water from Snell's law : a n sin 1 sin 1 tan 1 n d sin 2 sin 2 tan 2 d Where Δχα και Δχν are the distances in number of pixels to be calculated from the image processing PROCESS OF FINDING VALUES After you get the result of adding the two images, we can find the deviation of each beam from the central. We use the linear option from the menu (see picture below). During this process, we press the shift key down to keep the line horizontal. We draw a line as shown below, and then following the steps in the menu analysis> chart distribution, we get the graph from which we calculate the deviation of the light rays. The deviation is measured in number of pixels. We use the results of the measurements for our calculation MEASURING THE DISTANCES BETWEEN LIGHT RAYS Moving the cursor on the taken graph, we find the positions of light rays (See picture below). The deviation (distance between them) is measured in number of pixels. We use the results of the measurement for our calculation Price of χ Cursor REFRACTIVE INDEX & MEASUREMENT VALUES Coordinates of the beams AIR CENTRAL χ Distances of the side beams from the central WATER 1140 972 AIR Δχα = χ - χ1α = 900 WITH ANGLE χ1 240 WATER Δχν = χ - χ1ν = 686 286 According to the relationship that we have in our theoretical calculations and our measurements the refractive index of water has a value = 1.312. As we can see the price is too close to real which is 1.333 2nd MEASUREMENT METHOD USING DIFFRACTION GRATING • • • • • • • We pour water in the bowl up to a level We stick the translucent paper on one side of the bowl We stick the diffraction grating on the opposite side so that it covers both visual media. We put the source of light (Laser beam) in front of the diffraction grating perpendicular to the surface. We take care of half the beam passes through the water and the other half from the air. Due to the vertical incidence of the beam , the central fringe pattern in water and in the air are on the same line. The rest, however, have different deviations. We take a photo. We use the first and second fringe pattern for our calculations FINDING THE REFRACTIVE INTEX WITH DIFFRACTION GRATING • In this method we use a photo of the beam, when it strikes vertically to the boundary of air - water. • In this case the light follows a different path in water than in air. • We convert the image using the software SalsaJ, as described below, and then measure the deviation of the two lateral beams from vertical. • From the relations derived on the basis of the theoretical approach to the phenomenon, we calculate the refractive index of water. PHOTOS USING THE DIFFRACTION GRATING COURSE OF LIGHT RAYS PASSING THROUGH AIR AND WATER 1st fringe pettern Diagram propagation of light in air φ1 Central fringe pattern ΔΧα 1st fringe pattern Distance between light source and translucent paper 1st fringe pattern Diagram propagation of light in water Φ2 Central fringe pattern ΔΧν 1st fringe pattern Distance between light source and translucent paper d MATHEMATICAL EQUATIONS USED FOR CALCULATION • From the geometry of figure we have and • • • tan 2 v d tan 1 a d in the air, in the water. We know that for small φ angle values we have sin tan Snell's Law gives na sin 1 n sin 2 where ηα= refractive index of air and nv = refractive index of water We know that the refractive index of air has a value equal to 1. So calculating the prices of tanφ and using the equation sin tan we can calculate the refractive index nv of water from the Snell's law : a n sin 1 sin 1 tan 1 n d sin 2 sin 2 tan 2 d Where Δχα and Δχν are the distances in number of pixels to be calculated from the image processing FIND THE POSITIONS OF THE FRINGE PATTERN We use the linear option from the menu (see picture below). We draw a line along the photo to find the positions of the fringes, as described below. During this process, we press the shift key down to keep the line horizontal. Following the procedure described in the previous case , we get the graph from which we calculate the distances. MEASUREMENT OF THE POSITION OF THE FRINGE PATTERN • Moving the cursor on the line we draw , the position of the fringe pattern appears as in the picture below. Central fringe pattern 1st left fringe pattern 2nd left fringe pattern 1st right fringe pattern 2nd right fringe pattern • Price of χ 1ST MEASUREMENT using SNELL’S LAW • We measure the positions of the first two fringe patterns and the central and then we calculate the distances from the central, when light is passing through air and water. • The values of positions in number of pixels are listed in the table : AIR • WATER Central (χ) 2189 2176 1st Left (χ1) 1490 1641 1st Right (χ2) 2887 2694 2nd Left (χ3) 971 1246 2nd Right (χ4) 3398 3071 Subtracting the values of each fringe from the central we find their distances. We use these values in the final equation of Snell’s law to calculate the refractive index of water.. Table showing distances of the lateral fringes pattern from the central AIR WATER χ - (χ1) = Δ(χ1α) 699 χ - (χ1) = Δ(χ1ν) 535 χ - (χ3) = Δ(χ3α) 1218 χ - (χ3) = Δ(χ3ν) 930 (χ2) – χ = Δ(χ2α) 698 (χ2) – χ = Δ(χ2ν) 518 (χ4) – χ = Δ(χ4α) 1209 (χ4) – χ = Δ(χ4ν) 895 We use these values in the final equation of Snell’s law to calculate the following refractive index values η1 = 1,306 η2 = 1,347 η3 = 1,309 η4 = 1,350 With an average value of n = 1.328, which is very close to actual value n = 1.333 Another group of measurements listed in the table below show the distances between central and lateral fringe pattern , giving good results as we see. AIR η1 = 1,329 WATER χ - (χ1) = Δ(χ1α) 718 χ - (χ1) = Δ(χ1ν) 540 η2 = 1,355 χ - (χ3) = Δ(χ3α) 1273 χ - (χ3) = Δ(χ3ν) 952 η3 = 1,337 (χ2) – χ = Δ(χ2α) 709 (χ2) – χ = Δ(χ2ν) 523 η4 = 1,322 (χ4) – χ = Δ(χ4α) 1213 (χ4) – χ = Δ(χ4ν) 917 Average value n = 1.335, which is close to the actual value of the refractive index of water n = 1.333 These values are obtained as above, using the diffraction grating and Snell’s law COURSE OF LIGHT RAYS PASSING THROUGH AIR AND WATER FOR THE 2nd MESUREMENT METHOD 1st fringe pettern Diagram propagation of light in air φ1 Central fringe pattern ΔΧα 1st fringe pattern Distance between light source and translucent paper 1st fringe pattern Diagram propagation of light in water Φ2 Central fringe pattern ΔΧν 1st fringe pattern Distance between light source and translucent paper d 2nd MEASUREMENT METHOD FROM THE POSITION OF FRINGE PATTERNS • We derive to the same results using the equation that calculates the distance of the fringe patterns from the central in the air or in the water: and , Ν: the same integer number for the first fringe pattern in the air and in the water. • From the geometry of the figure above tan 1 tan 2 tan 2 d d . From the above equation tan 2 d tan 1d d and and finally (1) and • From the definition of the refractive index n c c: light speed in u vacuum or in the air and u light speed in another optical medium. • From the basic wave speed equation c f we finally have: n • f f (2) From equations (1) and (2) n Calculating Δχα and Δχν we can derive to the calculation of the refractive index of water or any other medium. • As mentioned values are similar to those we used before, thus results are the same. CALCULATION OF MEASUREMENT ERROR THEORETICAL VALUE WITH DIFFRACTION GRATING 1,333 WITHOUT DIFFRACTION GRATING 1,333 MEASUREMENT VALUE ERROR % 1st MEASUREMENT 1,328 1st MEASUREMENT 0,38 2nd MEASUREMENT 1,335 2nd MEASUREMENT 0,15 1,312 1,58