Fresnel equations

When light strikes the interface between a medium with refractive index and a second medium with refractive index , both reflection and refraction of the light may occur. The Fresnel equations give the ratio of the reflected wave's electric field to the incident wave's electric field, and the ratio of the transmitted wave's electric field to the incident wave's electric field, for each of two components of polarization. (The magnetic fields can also be related using similar coefficients.) These ratios are generally complex, describing not only the relative amplitudes but also the phase shifts at the interface. The equations assume the interface between the media is flat and that the media are homogeneous and isotropic. The incident light is assumed to be a plane wave, which is sufficient to solve any problem since any incident light field can be decomposed into plane waves and polarizations. S and P polarizations There are two sets of Fresnel coefficients for two different linear polarization components of the incident wave. Since any polarization state can be resolved into a combination of two orthogonal linear polarizations, this is sufficient for any problem. Likewise, unpolarized (or "randomly polarized") light has an equal amount of power in each of two linear polarizations. The s polarization refers to polarization of a wave's electric field normal to the plane of incidence (the direction in the derivation below); then the magnetic field is in the plane of incidence. The p polarization refers to polarization of the electric field in the plane of incidence (the plane in the derivation below); then the magnetic field is normal to the plane of incidence. The names "s" and "p" for the polarization components refer to German "senkrecht" (perpendicular or normal) and "parallel" (parallel to the plane of incidence). Although the reflection and transmission are dependent on polarization, at normal incidence () there is no distinction between them so all polarization states are governed by a single set of Fresnel coefficients (and another special case is mentioned below in which that is true). == Configuration ==

In the diagram, an incident plane wave in the direction of the ray strikes the interface between two media of refractive indices and at point . Part of the wave is reflected in the direction , and part refracted in the direction . The angles that the incident, reflected and refracted rays make to the normal of the interface are given as , and , respectively. The relationship between these angles is given by the law of reflection:\theta_\mathrm{i} = \theta_\mathrm{r},and Snell's law:n_1 \sin \theta_\mathrm{i} = n_2 \sin \theta_\mathrm{t}. The behavior of light striking the interface is explained by considering the electric and magnetic fields that constitute an electromagnetic wave, and the laws of electromagnetism, as shown below. The ratio of waves' electric field (or magnetic field) amplitudes are obtained, but in practice one is more often interested in formulae which determine power coefficients, since power (or irradiance) is what can be directly measured at optical frequencies. The power of a wave is generally proportional to the square of the electric (or magnetic) field amplitude. == Power (intensity) reflection and transmission coefficients ==

We call the fraction of the incident power that is reflected from the interface the reflectance (or reflectivity, or power reflection coefficient) , and the fraction that is refracted into the second medium is called the transmittance (or transmissivity, or power transmission coefficient) . Note that these are what would be measured right at each side of an interface and do not account for attenuation of a wave in an absorbing medium following transmission or reflection. The reflectance for s-polarized light is R_\mathrm{s} = \left|\frac{Z_2 \cos \theta_\mathrm{i} - Z_1 \cos \theta_\mathrm{t}}{Z_2 \cos \theta_\mathrm{i} + Z_1 \cos \theta_\mathrm{t}}\right|^2, while the reflectance for p-polarized light is R_\mathrm{p} = \left|\frac{Z_2 \cos \theta_\mathrm{t} - Z_1 \cos \theta_\mathrm{i}}{Z_2 \cos \theta_\mathrm{t} + Z_1 \cos \theta_\mathrm{i}}\right|^2, where and are the wave impedances of media 1 and 2, respectively. We assume that the media are non-magnetic (i.e., ), which is typically a good approximation at optical frequencies (and for transparent media at other frequencies). Then the wave impedances are determined solely by the refractive indices and : Z_i = \frac{Z_0}{n_i}\,, where is the impedance of free space and . Making this substitution, we obtain equations using the refractive indices: R_\mathrm{s} = \left|\frac{n_1 \cos \theta_\mathrm{i} - n_2 \cos \theta_\mathrm{t}}{n_1 \cos \theta_\mathrm{i} + n_2 \cos \theta_\mathrm{t}}\right|^2 = \left|\frac {n_1 \cos \theta_{\mathrm{i}} - n_2 \sqrt{1 - \left(\frac{n_1}{n_2} \sin \theta_{\mathrm{i}}\right)^2}} {n_1 \cos \theta_{\mathrm{i}} + n_2 \sqrt{1 - \left(\frac{n_1}{n_2} \sin \theta_{\mathrm{i}}\right)^2}} \right|^2\!, R_\mathrm{p} = \left|\frac{n_1 \cos \theta_\mathrm{t} - n_2 \cos \theta_\mathrm{i}}{n_1 \cos \theta_\mathrm{t} + n_2 \cos \theta_\mathrm{i}}\right|^2 = \left|\frac {n_1 \sqrt{1 - \left(\frac{n_1}{n_2} \sin \theta_\mathrm{i}\right)^2} - n_2 \cos \theta_\mathrm{i}} {n_1 \sqrt{1 - \left(\frac{n_1}{n_2} \sin \theta_\mathrm{i}\right)^2} + n_2 \cos \theta_\mathrm{i}} \right|^2\!. The second form of each equation is derived from the first by eliminating using Snell's law and trigonometric identities. As a consequence of conservation of energy, one can find the transmitted power (or more correctly, irradiance: power per unit area) simply as the portion of the incident power that isn't reflected: T_\mathrm{s} = 1 - R_\mathrm{s} and T_\mathrm{p} = 1 - R_\mathrm{p} Note that all such intensities are measured in terms of a wave's irradiance in the direction normal to the interface; this is also what is measured in typical experiments. That number could be obtained from irradiances in the direction of an incident or reflected wave (given by the magnitude of a wave's Poynting vector) multiplied by for a wave at an angle to the normal direction (or equivalently, taking the dot product of the Poynting vector with the unit vector normal to the interface). This complication can be ignored in the case of the reflection coefficient, since , so that the ratio of reflected to incident irradiance in the wave's direction is the same as in the direction normal to the interface. Although these relationships describe the basic physics, in many practical applications one is concerned with "natural light" that can be described as unpolarized. That means that there is an equal amount of power in the s and p polarizations, so that the effective reflectivity of the material is just the average of the two reflectivities: R_\mathrm{eff} = \frac{1}{2}\left(R_\mathrm{s} + R_\mathrm{p}\right). For low-precision applications involving unpolarized light, such as computer graphics, rather than rigorously computing the effective reflection coefficient for each angle, Schlick's approximation is often used. Special cases Normal incidence For the case of normal incidence, , and there is no distinction between s and p polarization. Thus, the reflectance simplifies to R_0 = \left|\frac{n_1 - n_2 }{n_1 + n_2 }\right|^2\,. For common glass () surrounded by air (), the power reflectance at normal incidence can be seen to be about 4%, or 8% accounting for both sides of a glass pane. Brewster's angle At a dielectric interface from to , there is a particular angle of incidence at which goes to zero and a p-polarised incident wave is purely refracted, thus all reflected light is s-polarised. This angle is known as Brewster's angle, and is around 56° for and (typical glass). Total internal reflection When light travelling in a denser medium strikes the surface of a less dense medium (i.e., ), beyond a particular incidence angle known as the critical angle, all light is reflected and . This phenomenon, known as total internal reflection, occurs at incidence angles for which Snell's law predicts that the sine of the angle of refraction would exceed unity (whereas in fact for all real ). For glass with surrounded by air, the critical angle is approximately 42°. 45° incidence Reflection at 45° incidence is very commonly used for making 90° turns. For the case of light traversing from a less dense medium into a denser one at 45° incidence (), it follows algebraically from the above equations that equals the square of : R_\text{p} = R_\text{s}^2 This can be used to either verify the consistency of the measurements of and , or to derive one of them when the other is known. This relationship is only valid for the simple case of a single plane interface between two homogeneous materials, not for films on substrates, where a more complex analysis is required. Measurements of and at 45° can be used to estimate the reflectivity at normal incidence. The "average of averages" obtained by calculating first the arithmetic as well as the geometric average of and , and then averaging these two averages again arithmetically, gives a value for with an error of less than about 3% for most common optical materials. This is useful because measurements at normal incidence can be difficult to achieve in an experimental setup since the incoming beam and the detector will obstruct each other. However, since the dependence of and on the angle of incidence for angles below 10° is very small, a measurement at about 5° will usually be a good approximation for normal incidence, while allowing for a separation of the incoming and reflected beam. == Complex amplitude reflection and transmission coefficients ==

The above equations relating powers (which could be measured with a photometer for instance) are derived from the Fresnel equations which solve the physical problem in terms of electromagnetic field complex amplitudes, i.e., considering phase shifts in addition to their amplitudes. Those underlying equations supply generally complex-valued ratios of those EM fields and may take several different forms, depending on the formalism used. The complex amplitude coefficients for reflection and transmission are usually represented by lower case and (whereas the power coefficients are capitalized). As before, we are assuming the magnetic permeability, of both media to be equal to the permeability of free space as is essentially true of all dielectrics at optical frequencies. In the following equations and graphs, we adopt the following conventions. For s polarization, the reflection coefficient is defined as the ratio of the reflected wave's complex electric field amplitude to that of the incident wave, whereas for p polarization is the ratio of the waves complex magnetic field amplitudes (or equivalently, the negative of the ratio of their electric field amplitudes). The transmission coefficient is the ratio of the transmitted wave's complex electric field amplitude to that of the incident wave, for either polarization. The coefficients and are generally different between the s and p polarizations, and even at normal incidence (where the designations s and p do not even apply!) the sign of is reversed depending on whether the wave is considered to be s or p polarized, an artifact of the adopted sign convention (see graph for an air-glass interface at 0° incidence). The equations consider a plane wave incident on a plane interface at angle of incidence {{nowrap|1= \theta_\mathrm{i}}}, a wave reflected at angle {{nowrap|1= \theta_\mathrm{r} = \theta_\mathrm{i} }}, and a wave transmitted at angle {{nowrap|1= \theta_\mathrm{t}}}. In the case of an interface into an absorbing material (where is complex) or total internal reflection, the angle of transmission does not generally evaluate to a real number. In that case, however, meaningful results can be obtained using formulations of these relationships in which trigonometric functions and geometric angles are avoided; the inhomogeneous waves launched into the second medium cannot be described using a single propagation angle. Using this convention, \begin{align} r_\text{s} &= \frac{ n_1 \cos \theta_\text{i} - n_2 \cos \theta_\text{t}}{n_1 \cos \theta_\text{i} + n_2 \cos \theta_\text{t}}, \\[3pt] t_\text{s} &= \frac{2 n_1 \cos \theta_\text{i}} {n_1 \cos \theta_\text{i} + n_2 \cos \theta_\text{t}}, \\[3pt] r_\text{p} &= \frac{ n_2 \cos \theta_\text{i} - n_1 \cos \theta_\text{t}}{n_2 \cos \theta_\text{i} + n_1 \cos \theta_\text{t}}, \\[3pt] t_\text{p} &= \frac{2 n_1 \cos \theta_\text{i}} {n_2 \cos \theta_\text{i} + n_1 \cos \theta_\text{t}}. \end{align} For the case where the magnetic permeabilities are non-negligible, the equations change such that every appearance of n_i is replaced by n_i/\mu_i (for both i=1, 2 ). One can see that and . One can write very similar equations applying to the ratio of the waves' magnetic fields, but comparison of the electric fields is more conventional. Because the reflected and incident waves propagate in the same medium and make the same angle with the normal to the surface, the power reflection coefficient is just the squared magnitude of : R = |r|^2. On the other hand, calculation of the power transmission coefficient is less straightforward, since the light travels in different directions in the two media. What's more, the wave impedances in the two media differ; power (irradiance) is given by the square of the electric field amplitude divided by the characteristic impedance of the medium (or by the square of the magnetic field multiplied by the characteristic impedance). This results in: T = \frac{n_2 \cos \theta_\text{t}}{n_1 \cos \theta_\text{i}} |t|^2 using the above definition of . The introduced factor of is the reciprocal of the ratio of the media's wave impedances. The factors adjust the waves' powers so they are reckoned in the direction normal to the interface, for both the incident and transmitted waves, so that full power transmission corresponds to . In the case of total internal reflection where the power transmission is zero, nevertheless describes the electric field (including its phase) just beyond the interface. This is an evanescent field which does not propagate as a wave (thus ) but has nonzero values very close to the interface. The phase shift of the reflected wave on total internal reflection can similarly be obtained from the phase angles of and (whose magnitudes are unity in this case). These phase shifts are different for s and p waves, which is the well-known principle by which total internal reflection is used to effect polarization transformations. Alternative forms In the above formula for , if we put n_2=n_1\sin\theta_\text{i}/\sin\theta_\text{t} (Snell's law) and multiply the numerator and denominator by , we obtain r_\text{s}=-\frac{\sin(\theta_\text{i}-\theta_\text{t})}{\sin(\theta_\text{i}+\theta_\text{t})}. If we do likewise with the formula for , the result is easily shown to be equivalent to r_\text{p}=\frac{\tan(\theta_\text{i}-\theta_\text{t})}{\tan(\theta_\text{i}+\theta_\text{t})}. These formulas are known respectively as ''Fresnel's sine law and Fresnel's tangent law''. Although at normal incidence these expressions reduce to 0/0, one can see that they yield the correct results in the limit as . == Multiple surfaces ==

When light makes multiple reflections between two or more parallel surfaces, the multiple beams of light generally interfere with one another, resulting in net transmission and reflection amplitudes that depend on the light's wavelength. The interference, however, is seen only when the surfaces are at distances comparable to or smaller than the light's coherence length, which for ordinary white light is few micrometers; it can be much larger for light from a laser. An example of interference between reflections is the iridescent colours seen in a soap bubble or in thin oil films on water. Applications include Fabry–Pérot interferometers, antireflection coatings, and optical filters. A quantitative analysis of these effects is based on the Fresnel equations, but with additional calculations to account for interference. The transfer-matrix method, or Rouard's recursive method can be used to solve multiple-surface problems. == History ==

In 1808, Étienne-Louis Malus discovered that when a ray of light was reflected off a non-metallic surface at the appropriate angle, it behaved like one of the two rays emerging from a doubly-refractive calcite crystal. He later coined the term polarization to describe this behavior. In 1815, the dependence of the polarizing angle on the refractive index was determined experimentally by David Brewster. But the reason for that dependence was such a deep mystery that in late 1817, Thomas Young was moved to write: In 1821, however, Augustin-Jean Fresnel derived results equivalent to his sine and tangent laws (above), by modeling light waves as transverse elastic waves with vibrations perpendicular to what had previously been called the plane of polarization. Fresnel promptly confirmed by experiment that the equations correctly predicted the direction of polarization of the reflected beam when the incident beam was polarized at 45° to the plane of incidence, for light incident from air onto glass or water; in particular, the equations gave the correct polarization at Brewster's angle. The experimental confirmation was reported in a "postscript" to the work in which Fresnel first revealed his theory that light waves, including "unpolarized" waves, were purely transverse. Details of Fresnel's derivation, including the modern forms of the sine law and tangent law, were given later, in a memoir read to the French Academy of Sciences in January 1823. That derivation combined conservation of energy with continuity of the tangential vibration at the interface, but failed to allow for any condition on the normal component of vibration. The first derivation from electromagnetic principles was given by Hendrik Lorentz in 1875. In the same memoir of January 1823, The verification involved • calculating the angle of incidence that would introduce a total phase difference of 90° between the s and p components, for various numbers of total internal reflections at that angle (generally there were two solutions), • subjecting light to that number of total internal reflections at that angle of incidence, with an initial linear polarization at 45° to the plane of incidence, and • checking that the final polarization was circular. Thus he finally had a quantitative theory for what we now call the Fresnel rhomb — a device that he had been using in experiments, in one form or another, since 1817 (see Fresnel rhomb §History). The success of the complex reflection coefficient inspired James MacCullagh and Augustin-Louis Cauchy, beginning in 1836, to analyze reflection from metals by using the Fresnel equations with a complex refractive index. Four weeks before he presented his completed theory of total internal reflection and the rhomb, Fresnel submitted a memoir in which he introduced the needed terms linear polarization, circular polarization, and elliptical polarization, and in which he explained optical rotation as a species of birefringence: linearly-polarized light can be resolved into two circularly-polarized components rotating in opposite directions, and if these propagate at different speeds, the phase difference between them — hence the orientation of their linearly-polarized resultant — will vary continuously with distance. Thus Fresnel's interpretation of the complex values of his reflection coefficients marked the confluence of several streams of his research and, arguably, the essential completion of his reconstruction of physical optics on the transverse-wave hypothesis (see Augustin-Jean Fresnel). == Derivation ==

Here we systematically derive the above relations from electromagnetic premises. Material parameters In order to compute meaningful Fresnel coefficients, we must assume that the medium is (approximately) linear and homogeneous. If the medium is also isotropic, the four field vectors are related by \begin{align} \mathbf{D} &= \epsilon \mathbf{E} \\ \mathbf{B} &= \mu \mathbf{H}\,, \end{align} where and are scalars, known respectively as the (electric) permittivity and the (magnetic) permeability of the medium. For vacuum, these have the values and , respectively. Hence we define the relative permittivity (or dielectric constant) , and the relative permeability . In optics it is common to assume that the medium is non-magnetic, so that . For ferromagnetic materials at radio/microwave frequencies, larger values of must be taken into account. But, for optically transparent media, and for all other materials at optical frequencies (except possible metamaterials), is indeed very close to 1; that is, . In optics, one usually knows the refractive index of the medium, which is the ratio of the speed of light in vacuum () to the speed of light in the medium. In the analysis of partial reflection and transmission, one is also interested in the electromagnetic wave impedance , which is the ratio of the amplitude of to the amplitude of . It is therefore desirable to express and in terms of and , and thence to relate to . The last-mentioned relation, however, will make it convenient to derive the reflection coefficients in terms of the wave admittance , which is the reciprocal of the wave impedance . In the case of uniform plane sinusoidal waves, the wave impedance or admittance is known as the intrinsic impedance or admittance of the medium. This case is the one for which the Fresnel coefficients are to be derived. Electromagnetic plane waves In a uniform plane sinusoidal electromagnetic wave, the electric field has the form {{NumBlk|:|\mathbf{E_k}e^{i(\mathbf{k\cdot r}-\omega t)},|}} where is the (constant) complex amplitude vector, is the imaginary unit, is the wave vector (whose magnitude is the angular wavenumber), is the position vector, is the angular frequency, is time, and it is understood that the real part of the expression is the physical field.  The value of the expression is unchanged if the position varies in a direction normal to ; hence is normal to the wavefronts. To advance the phase by the angle ϕ, we replace by (that is, we replace by ), with the result that the (complex) field is multiplied by . So a phase advance is equivalent to multiplication by a complex constant with a negative argument. This becomes more obvious when the field () is factored as , where the last factor contains the time-dependence. That factor also implies that differentiation w.r.t. time corresponds to multiplication by . If ℓ is the component of in the direction of , the field () can be written .  If the argument of is to be constant,  ℓ must increase at the velocity \omega/k\,,\, known as the phase velocity . This in turn is equal to Solving for gives As usual, we drop the time-dependent factor , which is understood to multiply every complex field quantity. The electric field for a uniform plane sine wave will then be represented by the location-dependent phasor {{NumBlk|:|\mathbf{E_k}e^{i\mathbf{k\cdot r}}.|}} For fields of that form, Faraday's law and the Maxwell-Ampère law respectively reduce to \begin{align} \omega\mathbf{B} &= \mathbf{k}\times\mathbf{E}\\ \omega\mathbf{D} &= -\mathbf{k}\times\mathbf{H}\,. \end{align} Putting and , as above, we can eliminate and to obtain equations in only and : \begin{align} \omega\mu\mathbf{H} &= \mathbf{k}\times\mathbf{E}\\ \omega\epsilon\mathbf{E} &= -\mathbf{k}\times\mathbf{H}\,. \end{align} If the material parameters and are real (as in a lossless dielectric), these equations show that form a right-handed orthogonal triad, so that the same equations apply to the magnitudes of the respective vectors. Taking the magnitude equations and substituting from (), we obtain \begin{align} \mu cH &= nE\\ \epsilon cE &= nH\,, \end{align} where and are the magnitudes of and . Multiplying the last two equations gives {{NumBlk|:|n = c\,\sqrt{\mu\epsilon}\,.|}} Dividing (or cross-multiplying) the same two equations gives , where {{NumBlk|:|Y = \sqrt{\epsilon/\mu}\,.|}} This is the intrinsic admittance. From () we obtain the phase velocity {{nowrap|1=c/n=1\big/\!\sqrt{\mu\epsilon\,}.}} For vacuum this reduces to {{nowrap|1=c=1\big/\!\sqrt{\mu_0\epsilon_0}.}} Dividing the second result by the first gives n=\sqrt{\mu_{\text{rel}}\epsilon_{\text{rel}}}\,. For a non-magnetic medium (the usual case), this becomes {{tmath|1= n=\sqrt{\epsilon_{\text{rel} } } }}. Taking the reciprocal of (), we find that the intrinsic impedance is {{nowrap|1=Z=\sqrt{\mu/\epsilon}.}} In vacuum this takes the value Z_0=\sqrt{\mu_0/\epsilon_0}\,\approx 377\,\Omega\,, known as the impedance of free space. By division, {{nowrap|1=Z/Z_0=\sqrt{\mu_{\text{rel}}/\epsilon_{\text{rel}}}.}} For a non-magnetic medium, this becomes Z=Z_0\big/\!\sqrt{\epsilon_{\text{rel}}}=Z_0/n. Wave vectors In Cartesian coordinates , let the region have refractive index , intrinsic admittance , etc., and let the region have refractive index , intrinsic admittance , etc. Then the plane is the interface, and the axis is normal to the interface (see diagram). Let and (in bold roman type) be the unit vectors in the and directions, respectively. Let the plane of incidence be the plane (the plane of the page), with the angle of incidence measured from towards . Let the angle of refraction, measured in the same sense, be , where the subscript stands for transmitted (reserving for reflected). In the absence of Doppler shifts, ω does not change on reflection or refraction. Hence, by (), the magnitude of the wave vector is proportional to the refractive index. So, for a given , if we redefine as the magnitude of the wave vector in the reference medium (for which ), then the wave vector has magnitude in the first medium (region in the diagram) and magnitude in the second medium. From the magnitudes and the geometry, we find that the wave vectors are \begin{align} \mathbf{k}_\text{i} &= n_1 k(\mathbf{i}\sin\theta_\text{i} + \mathbf{j}\cos\theta_\text{i})\\[.5ex] \mathbf{k}_\text{r} &= n_1 k(\mathbf{i}\sin\theta_\text{i} - \mathbf{j}\cos\theta_\text{i})\\[.5ex] \mathbf{k}_\text{t} &= n_2 k(\mathbf{i}\sin\theta_\text{t} + \mathbf{j}\cos\theta_\text{t})\\ &= k(\mathbf{i}\,n_1\sin\theta_\text{i} + \mathbf{j}\,n_2\cos\theta_\text{t})\,, \end{align} where the last step uses Snell's law. The corresponding dot products in the phasor form () are {{NumBlk|:|\begin{align} \mathbf{k}_\text{i}\mathbf{\cdot r} &= n_1 k(x\sin\theta_\text{i} + y\cos\theta_\text{i})\\ \mathbf{k}_\text{r}\mathbf{\cdot r} &= n_1 k(x\sin\theta_\text{i} - y\cos\theta_\text{i})\\ \mathbf{k}_\text{t}\mathbf{\cdot r} &= k(n_1 x\sin\theta_\text{i} + n_2 y\cos\theta_\text{t})\,. \end{align}|}} Hence: {{NumBlk|:|At  y=0\,,~~~\mathbf{k}_\text{i}\mathbf{\cdot r}=\mathbf{k}_\text{r}\mathbf{\cdot r}=\mathbf{k}_\text{t}\mathbf{\cdot r}=n_1 kx\sin\theta_\text{i}\,.|}} s components For the s polarization, the field is parallel to the axis and may therefore be described by its component in the direction. Let the reflection and transmission coefficients be and , respectively. Then, if the incident field is taken to have unit amplitude, the phasor form () of its -component is {{NumBlk|:|E_\text{i}=e^{i\mathbf{k}_\text{i}\mathbf{\cdot r}},|}} and the reflected and transmitted fields, in the same form, are {{NumBlk|:|\begin{align} E_\text{r} &= r_{s\,} e^{i\mathbf{k}_\text{r}\mathbf{\cdot r}}\\ E_\text{t} &= t_{s\,} e^{i\mathbf{k}_\text{t}\mathbf{\cdot r}}. \end{align}|}} Under the sign convention used in this article, a positive reflection or transmission coefficient is one that preserves the direction of the transverse field, meaning (in this context) the field normal to the plane of incidence. For the s polarization, that means the field. If the incident, reflected, and transmitted fields (in the above equations) are in the -direction ("out of the page"), then the respective fields are in the directions of the red arrows, since form a right-handed orthogonal triad. The fields may therefore be described by their components in the directions of those arrows, denoted by . Then, since , {{NumBlk|:|\begin{align} H_\text{i} &=\, Y_1 e^{i\mathbf{k}_\text{i}\mathbf{\cdot r}}\\ H_\text{r} &=\, Y_1 r_{s\,} e^{i\mathbf{k}_\text{r}\mathbf{\cdot r}}\\ H_\text{t} &=\, Y_2 t_{s\,} e^{i\mathbf{k}_\text{t}\mathbf{\cdot r}}. \end{align}|}} At the interface, by the usual interface conditions for electromagnetic fields, the tangential components of the and fields must be continuous; that is, {{NumBlk|:|\left.\begin{align} E_\text{i} + E_\text{r} &= E_\text{t}\\ H_\text{i}\cos\theta_\text{i} - H_\text{r}\cos\theta_\text{i} &= H_\text{t}\cos\theta_\text{t} \end{align}~~\right\}~~~\text{at}~~ y=0\,.|}} When we substitute from equations () to () and then from (), the exponential factors cancel out, so that the interface conditions reduce to the simultaneous equations {{NumBlk|:|\begin{align} 1 + r_\text{s} &=\, t_\text{s}\\ Y_1\cos\theta_\text{i} - Y_1 r_\text{s}\cos\theta_\text{i} &=\, Y_2 t_\text{s}\cos\theta_\text{t} \,, \end{align}|}} which are easily solved for and , yielding {{NumBlk|:|r_\text{s}=\frac{Y_1\cos\theta_\text{i}-Y_2\cos\theta_\text{t}}{Y_1\cos\theta_\text{i}+Y_2\cos\theta_\text{t}}|}} and {{NumBlk|:|t_\text{s}=\frac{2Y_1\cos\theta_\text{i}}{Y_1\cos\theta_\text{i}+Y_2\cos\theta_\text{t}}\,.|}} At normal incidence , indicated by an additional subscript 0, these results become {{NumBlk|:|r_\text{s0}=\frac{Y_1-Y_2}{Y_1+Y_2}|}} and {{NumBlk|:|t_\text{s0}=\frac{2Y_1}{Y_1+Y_2}\,.|}} At grazing incidence , we have , hence and . p components For the p polarization, the incident, reflected, and transmitted fields are parallel to the red arrows and may therefore be described by their components in the directions of those arrows. Let those components be (redefining the symbols for the new context). Let the reflection and transmission coefficients be and . Then, if the incident field is taken to have unit amplitude, we have {{NumBlk|:|\begin{align} E_\text{i} &= e^{i\mathbf{k}_\text{i}\mathbf{\cdot r}}\\ E_\text{r} &= r_{p\,} e^{i\mathbf{k}_\text{r}\mathbf{\cdot r}}\\ E_\text{t} &= t_{p\,} e^{i\mathbf{k}_\text{t}\mathbf{\cdot r}}. \end{align}|}} If the fields are in the directions of the red arrows, then, in order for to form a right-handed orthogonal triad, the respective fields must be in the -direction ("into the page") and may therefore be described by their components in that direction. This is consistent with the adopted sign convention, namely that a positive reflection or transmission coefficient is one that preserves the direction of the transverse field the field in the case of the p polarization. The agreement of the other field with the red arrows reveals an alternative definition of the sign convention: that a positive reflection or transmission coefficient is one for which the field vector in the plane of incidence points towards the same medium before and after reflection or transmission. So, for the incident, reflected, and transmitted fields, let the respective components in the -direction be . Then, since , {{NumBlk|:|\begin{align} H_\text{i} &=\, Y_1 e^{i\mathbf{k}_\text{i}\mathbf{\cdot r}}\\ H_\text{r} &=\, Y_1 r_{p\,} e^{i\mathbf{k}_\text{r}\mathbf{\cdot r}}\\ H_\text{t} &=\, Y_2 t_{p\,} e^{i\mathbf{k}_\text{t}\mathbf{\cdot r}}. \end{align}|}} At the interface, the tangential components of the and fields must be continuous; that is, {{NumBlk|:|\left.\begin{align} E_\text{i}\cos\theta_\text{i} - E_\text{r}\cos\theta_\text{i} &= E_\text{t}\cos\theta_\text{t}\\ H_\text{i} + H_\text{r} &= H_\text{t} \end{align}~~\right\}~~~\text{at}~~ y=0\,.|}} When we substitute from equations () and () and then from (), the exponential factors again cancel out, so that the interface conditions reduce to {{NumBlk|:|\begin{align} \cos\theta_\text{i} - r_\text{p}\cos\theta_\text{i} &=\, t_\text{p}\cos\theta_\text{t}\\ Y_1 + Y_1 r_\text{p} &=\, Y_2 t_\text{p} \,. \end{align}|}} Solving for and , we find {{NumBlk|:|r_\text{p}=\frac{Y_2\cos\theta_\text{i}-Y_1\cos\theta_\text{t}}{Y_2\cos\theta_\text{i}+Y_1\cos\theta_\text{t}}|}} and {{NumBlk|:|t_\text{p}=\frac{2Y_1\cos\theta_\text{i}}{Y_2\cos\theta_\text{i}+Y_1\cos\theta_\text{t}}\,.|}} At normal incidence indicated by an additional subscript 0, these results become {{NumBlk|:|r_\text{p0}=\frac{Y_2-Y_1}{Y_2+Y_1}|}} and {{NumBlk|:|t_\text{p0}=\frac{2Y_1}{Y_2+Y_1}\,.|}} At , we again have , hence and . Comparing () and () with () and (), we see that at normal incidence, under the adopted sign convention, the transmission coefficients for the two polarizations are equal, whereas the reflection coefficients have equal magnitudes but opposite signs. While this clash of signs is a disadvantage of the convention, the attendant advantage is that the signs agree at grazing incidence. Power ratios (reflectivity and transmissivity) The Poynting vector for a wave is a vector whose component in any direction is the irradiance (power per unit area) of that wave on a surface perpendicular to that direction. For a plane sinusoidal wave the Poynting vector is , where and are due only to the wave in question, and the asterisk denotes complex conjugation. Inside a lossless dielectric (the usual case), and are in phase, and at right angles to each other and to the wave vector ; so, for s polarization, using the and components of and respectively (or for p polarization, using the and components of and ), the irradiance in the direction of is given simply by , which is in a medium of intrinsic impedance . To compute the irradiance in the direction normal to the interface, as we shall require in the definition of the power transmission coefficient, we could use only the component (rather than the full component) of or or, equivalently, simply multiply by the proper geometric factor, obtaining . From equations () and (), taking squared magnitudes, we find that the reflectivity (ratio of reflected power to incident power) is {{NumBlk|:|R_\text{s}=\left|\frac{Y_1\cos\theta_\text{i}-Y_2\cos\theta_\text{t}}{Y_1\cos\theta_\text{i}+Y_2\cos\theta_\text{t}}\right|^2|}} for the s polarization, and {{NumBlk|:|R_\text{p}=\left|\frac{Y_2\cos\theta_\text{i}-Y_1\cos\theta_\text{t}}{Y_2\cos\theta_\text{i}+Y_1\cos\theta_\text{t}}\right|^2|}} for the p polarization. Note that when comparing the powers of two such waves in the same medium and with the same cosθ, the impedance and geometric factors mentioned above are identical and cancel out. But in computing the power transmission (below), these factors must be taken into account. The simplest way to obtain the power transmission coefficient (transmissivity, the ratio of transmitted power to incident power in the direction normal to the interface, i.e. the direction) is to use (conservation of energy). In this way we find {{NumBlk|:|T_\text{s} =1-R_\text{s} =\,\frac{4\,\text{Re}\{ Y_1 Y_2\cos\theta_\text{i}\cos\theta_\text{t}\}}{\left|Y_1\cos\theta_\text{i}+Y_2\cos\theta_\text{t}\right|^2}|}} for the s polarization, and {{NumBlk|:|T_\text{p} =1-R_\text{p} =\,\frac{4\,\text{Re}\{Y_1 Y_2\cos\theta_\text{i}\cos\theta_\text{t}\}}{\left|Y_2\cos\theta_\text{i}+Y_1\cos\theta_\text{t}\right|^2}|}} for the p polarization. In the case of an interface between two lossless media (for which ϵ and μ are real and positive), one can obtain these results directly using the squared magnitudes of the amplitude transmission coefficients that we found earlier in equations () and (). But, for given amplitude (as noted above), the component of the Poynting vector in the direction is proportional to the geometric factor and inversely proportional to the wave impedance . Applying these corrections to each wave, we obtain two ratios multiplying the square of the amplitude transmission coefficient: {{NumBlk|:|T_\text{s} =\left(\frac{2Y_1\cos\theta_\text{i}}{Y_1\cos\theta_\text{i}+Y_2\cos\theta_\text{t}}\right)^2\frac{\,Y_2\,}{Y_1}\,\frac{\cos\theta_\text{t}}{\cos\theta_\text{i}} =\frac{4Y_1 Y_2\cos\theta_\text{i}\cos\theta_\text{t}}{\left(Y_1\cos\theta_\text{i}+Y_2\cos\theta_\text{t}\right)^2}|}} for the s polarization, and {{NumBlk|:|T_\text{p} =\left(\frac{2Y_1\cos\theta_\text{i}}{Y_2\cos\theta_\text{i}+Y_1\cos\theta_\text{t}}\right)^2\frac{\,Y_2\,}{Y_1}\,\frac{\cos\theta_\text{t}}{\cos\theta_\text{i}} =\frac{4Y_1 Y_2\cos\theta_\text{i}\cos\theta_\text{t}}{\left(Y_2\cos\theta_\text{i}+Y_1\cos\theta_\text{t}\right)^2}|}} for the p polarization. The last two equations apply only to lossless dielectrics, and only at incidence angles smaller than the critical angle (beyond which, of course, ). For unpolarized light: T={1 \over 2}(T_s+T_p) R={1 \over 2}(R_s+R_p) where R+T=1. Equal refractive indices From equations () and (), we see that two dissimilar media will have the same refractive index, but different admittances, if the ratio of their permeabilities is the inverse of the ratio of their permittivities. In that unusual situation we have (that is, the transmitted ray is undeviated), so that the cosines in equations (), (), (), (), and () to () cancel out, and all the reflection and transmission ratios become independent of the angle of incidence; in other words, the ratios for normal incidence become applicable to all angles of incidence. When extended to spherical reflection or scattering, this results in the Kerker effect for Mie scattering. Non-magnetic media Since the Fresnel equations were developed for optics, they are usually given for non-magnetic materials. Dividing () by ()) yields Y=\frac{n}{\,c\mu\,}\,. For non-magnetic media we can substitute the vacuum permeability for , so that Y_1=\frac{n_1}{\,c\mu_0} ~~;~~~ Y_2=\frac{n_2}{\,c\mu_0}\,; that is, the admittances are simply proportional to the corresponding refractive indices. When we make these substitutions in equations () to () and equations () to (), the factor cμ0 cancels out. For the amplitude coefficients we obtain: Similarly, Fresnel's sine law will apply to the p polarization instead of the s polarization, and his tangent law to the s polarization instead of the p polarization. This switch of polarizations has an analog in the old mechanical theory of light waves (see §History, above). One could predict reflection coefficients that agreed with observation by supposing (like Fresnel) that different refractive indices were due to different densities and that the vibrations were normal to what was then called the plane of polarization, or by supposing (like MacCullagh and Neumann) that different refractive indices were due to different elasticities and that the vibrations were parallel to that plane. Thus the condition of equal permittivities and unequal permeabilities, although not realistic, is of some historical interest. == See also ==