Supplemental Material: Annu. Rev. Phys. Chem. 2007. 58:267-97 doi: 10.1146/annurev.physchem.58.032806.104607 Localized Surface Plasmon Resonance Spectroscopy and Sensing Willets and Van Duyne SUPPLEMENTAL APPENDIX In the supplemental material, we derive Equations 1 and 3 from the second section of the main text (Theory) in greater detail. DERIVATION OF EQUATION 1 Maxwell’s Equations To begin, we consider a single metal sphere irradiated by y-propagating and zpolarized laser light at wavelength λ. The sphere is embedded in an external medium (viz., vacuum, gas, or liquid) with dielectric constant, εo. The dielectric constant of the sphere is ε1 and is assumed to be independent of the sphere size. The sphere, laser E field, and Cartesian coordinate system are shown in Figure 1A for the case a/λ = 1.0. Figure 1. A sphere with radius a embedded in a dielectric medium (ε0) and irradiated by xpropagating, z-polarized light of wavelength λ. (a) a/λ = 1. (b) a/λ = 0.1 (the quasi-static field case). The laser E field has the general form r E = Ex xˆ + E y yˆ + Ez zˆ , (S.1) where xˆ , yˆ , zˆ are unit vectors along the Cartesian axes x, y, z. The values of Ex, Ey, and Ez are controlled by polarization to be Ex = Ey = 0 and Ez = non-zero for an x-propagating, z-polarized wave: ⎡ ⎛x ⎞⎤ Ez = Ez0 cos ⎢ 2π ⎜ − υ t ⎟ ⎥ . (S.2) ⎠⎦ ⎣ ⎝λ 2π = k and 2πν = ω gives Substituting λ Ez = Ez0 cos(kx − ωt ). S-1 (S.3) Supplemental Material: Annu. Rev. Phys. Chem. 2007. 58:267-97 doi: 10.1146/annurev.physchem.58.032806.104607 Localized Surface Plasmon Resonance Spectroscopy and Sensing Willets and Van Duyne The general solution to this problem involves solving Maxwell’s equations (Equations S.4) to find the time-dependent electric and magnetic fields in all regions of space: ∇⋅E = ρ ε0 c 2∇ × B = ∂E j + ∂t ε 0 (S.4a) ∇×E = − (S.4c) ∇⋅B = 0. ∂B , ∂t (S.4b) (S.4d) Substantial simplification in the mathematics of this situation, while retaining the essence of the physics, can be obtained by making the long wavelength approximation. If we require that λ > 400 nm, then kx << ωt so that Ez = Ez0 cos ωt , (S.5) and if we further require that a/λ < 0.1, the electric field of the laser will be Eo, a vector pointing along the z axis, that can be assumed to be spatially independent for distances on the order of the sphere size. These conditions are depicted in Figure 1B. The external applied field Eo is approximately constant in time so that ∂E ∂B = 0 and = 0. ∂t ∂t Thus Maxwell’s equations reduce to the equations for electrostatics (Equation S.6) and magnetostatics (Equations S.7). Electrostatics: ∇⋅E = ρ ε0 (S.6a) ∇×E = 0 (S.6b) (S.7a) ∇⋅B = 0 (S.7b) Magnetostatics: ∇×B = j ε 0c 2 This means that for static charges and currents, electricity and magnetism are distinct phenomena. The problem we wish to focus on is the solution of the electrostatic equations for the electric field inside and outside the metal sphere. Thus we ignore the magnetostatic equations. The metal sphere is a conductor and has no net charge density (i.e. ρ = 0) so that ∇⋅E = 0 (S.8a) ∇×E = 0. (S.8b) S-2 Supplemental Material: Annu. Rev. Phys. Chem. 2007. 58:267-97 doi: 10.1146/annurev.physchem.58.032806.104607 Localized Surface Plasmon Resonance Spectroscopy and Sensing Willets and Van Duyne In order to calculate the E(x,y,z) field, we need to know the scalar potential, Φ(x,y,z), so that the field can be obtained from E = −∇Φ. (S.9) The scalar potential, Φ(x,y,z), can be obtained from ∇ ⋅∇Φ = 0, (S.10) ∇ 2Φ = 0. (S.11) which gives Laplace’s equation: Laplace’s Equation We start by converting Laplace’s equation in Cartesian coordinates to spherical coordinates using the relationships x = r sin θ cos φ y = r sin θ sin φ r = (x2 + y2 + z2)1/2 θ = cos −1 ⎜ ⎟ ⎛z⎞ ⎝r⎠ and the coordinate system defined in Figure 2: Figure 2. Coordinate axes system for Cartesian and polar coordinates. S-3 z = r cos θ ⎛ y⎞ ⎝x⎠ φ = tan −1 ⎜ ⎟ Supplemental Material: Annu. Rev. Phys. Chem. 2007. 58:267-97 doi: 10.1146/annurev.physchem.58.032806.104607 Localized Surface Plasmon Resonance Spectroscopy and Sensing Willets and Van Duyne Thus we can rewrite Equation S.11 ∇ 2 (r ,θ , φ )Φ(r , θ , φ ) = 0. (S.12) Recall that in spherical coordinates, ∇ 2 (r ,θ , φ ) = 1 ∂2 1 r+ 2 2 r ∂r r ⎡ 1 ∂ ⎛ ∂ ⎞ 1 ∂2 ⎤ + sin θ ⎜ ⎟ ⎢ ⎥, ∂θ ⎠ sin 2 θ ∂φ 2 ⎦ ⎣ sin θ ∂θ ⎝ (S.13) or the equivalent form ∇ 2 (r ,θ , φ ) = 1 ∂ ⎛ 2 ∂ ⎞ 1 ⎜r ⎟+ r 2 ∂r ⎝ ∂r ⎠ r 2 ⎡ 1 ∂ ⎛ 1 ∂2 ⎤ ∂ ⎞ sin . θ + ⎟ ⎢ sin θ ∂θ ⎜ ∂θ ⎠ sin 2 θ ∂φ 2 ⎥⎦ ⎝ ⎣ (S.14) We now can separate the variables into radial and angular components. Radial and Angular Separation of Variables Assume the solution is of the form Φ(r ,θ , φ ) = F (r )Y (θ , φ ), (S.15) and substitute Equation S.15 into S.12 to give ∇ 2 (r , θ , φ ) [ F (r )Y (θ , φ ) ] = I + II + III = 0, (S.16) where (using Equation S.13) 1 ∂2 [rF (r )Y (θ , φ )] r ∂r 2 (S.17a) 1 ∂ ⎛ ∂[ F (r )Y (θ , φ )] ⎞ ⎜ sin θ ⎟ ∂θ r sin θ ∂θ ⎝ ⎠ (S.17b) I= II = 2 III = 1 ∂ 2 [ F (r )Y (θ , φ )] . ∂φ 2 r 2 sin 2 θ (S.17c) Because the r-dependent operators act only on F(r) and the θ , φ operators act only on Y (θ , φ ) , we can separate terms and rewrite Laplace’s equation as S-4 Supplemental Material: Annu. Rev. Phys. Chem. 2007. 58:267-97 doi: 10.1146/annurev.physchem.58.032806.104607 Localized Surface Plasmon Resonance Spectroscopy and Sensing Willets and Van Duyne ⎡ ∂ 2 F (r ) 2 ∂F (r ) ⎤ I + II + III = Y (θ , φ ) ⎢ + + 2 r ∂r ⎥⎦ ⎣ ∂r F (r ) ⎡ 1 ∂ ⎛ ∂Y (θ , φ ) ⎞ ⎤ F (r ) ⎡ 1 ∂ 2Y (θ , φ ) ⎤ = 0. ⎜ sin θ ⎟ + 2 ⎢ 2 r 2 ⎢⎣ sin θ ∂θ ⎝ r ⎣ sin θ ∂φ 2 ⎥⎦ ∂θ ⎠ ⎥⎦ (S.18) Now do the following to Equation S.18: (a) rearrange to get all the F(r) terms on one side of the equation and all the Y (θ , φ ) terms on the other side and (b) divide both sides first by Y (θ , φ ) followed by F(r)/r2 to get r 2 ⎡ ∂ 2 F (r ) 2 ∂F (r ) ⎤ 1 ⎡ 1 ∂ ⎛ 1 ∂ 2Y (θ , φ ) ⎤ ∂Y (θ , φ ) ⎞ sin θ + = − + ⎜ ⎟ ⎢ ⎥ ⎢ ⎥. F (r ) ⎣ ∂r 2 r ∂r ⎦ Y (θ , φ ) ⎣ sin θ ∂θ ⎝ ∂θ ⎠ sin 2 θ ∂φ 2 ⎦ (S.19) The only way to maintain this equality is for each side of this expression to be equal to a constant. We arbitrarily call this constant G. As a result Laplace’s equation is now separated into two equations, one dealing with the radial dependence (Equation S.20a) and one with the angular dependence (Equation S.20b): r 2 ⎡ ∂ 2 F (r ) 2 ∂F (r ) ⎤ + ⎢ ⎥=G F (r ) ⎣ ∂r 2 r ∂r ⎦ (S.20a) ⎧ 1 ∂ ⎛ 1 ∂ 2Y (θ , φ ) ⎫ ∂Y (θ , φ ) ⎞ sin + θ ⎨ ⎬ = −GY (θ , φ ). ⎜ ⎟ ∂θ ⎠ sin 2 θ ∂φ 2 ⎭ ⎩ sin θ ∂θ ⎝ (S.20b) Separating Polar and Azimuthal Angles A second separation of variables is required to isolate the θ - and φ - dependent parts of Laplace’s equation. For this, we assume Y (θ , φ ) = P(θ )Q(φ ). (S.21) Substituting Equation S.21 into Equation S.20b yields ⎧ 1 ∂ ⎛ 1 ∂ 2 [ P (θ )Q (φ )] ⎫ ∂[ P (θ )Q (φ )] ⎞ sin + θ ⎨ ⎬ = −G [ P (θ )Q (φ ) ] . (S.22) ⎜ ⎟ 2 ∂θ ∂φ 2 ⎠ sin θ ⎩ sin θ ∂θ ⎝ ⎭ ∂2 ∂ Because only operates on P(θ) and operates only on Q(φ ), we have ∂θ ∂φ 2 S-5 Supplemental Material: Annu. Rev. Phys. Chem. 2007. 58:267-97 doi: 10.1146/annurev.physchem.58.032806.104607 Localized Surface Plasmon Resonance Spectroscopy and Sensing Willets and Van Duyne ⎪⎧ Q(φ ) ∂ ⎨ ⎩⎪ sin θ ∂θ ⎛ ∂ [ P (θ ) ] ⎞ P(θ ) ∂ 2 [Q(φ ) ] ⎫⎪ θ sin ⎬ = −G [ P(θ )Q(φ )] . ⎜ ⎟+ ∂θ ⎠ sin 2 θ ∂φ 2 ⎪⎭ ⎝ (S.23) Divide through both sides by Q(φ ) , then by P(θ), and multiply by sin2 θ to get 2 ∂ [ P(θ ) ] ⎞ sin 2 θ ∂ [ Q(φ ) ] ⎪⎫ ⎪⎧ sin 2 θ ∂ ⎛ 2 + sin θ ⎨ ⎬ = −G sin θ . ⎜ ⎟ 2 2 ∂θ ⎠ Q(φ ) sin θ ∂φ ⎪⎩ P(θ ) sin θ ∂θ ⎝ ⎪⎭ (S.24) Now rearrange to get all θ on the left-hand side and all φ on the right-hand side to get ⎪⎧ sin θ ∂ ⎨ ⎪⎩ P(θ ) ∂θ 2 ⎛ ∂ [ P(θ ) ] ⎞ ⎪⎫ 1 ∂ [Q(φ ) ] 2 sin θ sin θ . G + = − ⎜ ⎟⎬ Q(φ ) ∂φ 2 ∂θ ⎠ ⎪⎭ ⎝ (S.25) This is only true for all θ , φ if both sides equal a constant arbitrarily called D so that ⎧ sin θ ∂ ⎛ ∂[P(θ )] ⎞⎫ 2 ⎜ sin θ ⎟⎬ + G sin θ = D ⎨ ∂θ ⎠⎭ ⎩ P(θ ) ∂θ ⎝ 2 1 ∂ [Q(φ ) ] − = D. Q(φ ) ∂φ 2 (S.26b) SUMMARY OF SEPARATION OF VARIABLES Radial Equation : Polar Equation : Azimuthal Equation : (S.26a) r 2 ⎡ ∂ 2 F (r ) 2 ∂F (r ) ⎤ + ⎢ ⎥=G F (r ) ⎣ ∂r 2 r ∂r ⎦ ⎧ sin θ ∂ ⎛ ∂[P(θ )] ⎞⎫ 2 ⎜ sin θ ⎟⎬ + G sin θ = D ⎨ ∂θ ⎠⎭ ⎩ P(θ ) ∂θ ⎝ 1 ∂ 2 [Q(φ )] − =D Q(φ ) ∂φ 2 S-6 Supplemental Material: Annu. Rev. Phys. Chem. 2007. 58:267-97 doi: 10.1146/annurev.physchem.58.032806.104607 Localized Surface Plasmon Resonance Spectroscopy and Sensing Willets and Van Duyne Solving the Azimuthal Equation Because the azimuthal equation (Equation S.26b) is a function of φ only, replace partial derivatives by ordinary derivatives and rearrange to get d 2Q(φ ) + DQ(φ ) = 0. dφ 2 (S.27) Solutions to this equation have the form Q(φ ) = e imφ only if (S.28) m2 = D . (S.29) This can be checked by direct substitution: dQ(φ ) = imeimφ and dφ d 2Q(φ ) 2 2 imφ = i m e = − m 2 eimφ . dφ 2 (S.30) − m 2 e imφ + De imφ = 0 if and only if m2 = D. (S.31) Therefore, The boundary condition on Q (φ ) is Q(φ ) must be single-valued and continuous over 0 ≤ φ ≤ 2π so that Q(φ ) = Q(φ + π ) . Substituting Q(φ ) = e imφ into the boundary condition, we get e imφ = e im (φ + 2π ) . This reduces to 1 = eim2π = cos2πm + i sin 2πm, • for m = 0; cos0 = 1 and sin0 = 0 ∴ ei2π(0) = 1 • for m = ±1; cos ±2π = 1 and sin ± 2π = 0 ∴ ei2π(±1) = 1 • for m = 2±; cos ± 4π = 1 and sin ±π = 0 ∴ ei2π(±2) = 1. So the final result is Qm (φ ) = e imφ where m2 = D and m = 0, ±1; ±2; ±3; …. S-7 (S.32) Supplemental Material: Annu. Rev. Phys. Chem. 2007. 58:267-97 doi: 10.1146/annurev.physchem.58.032806.104607 Localized Surface Plasmon Resonance Spectroscopy and Sensing Willets and Van Duyne Solving the Polar Equation Because the polar equation (Equation S.26a) is a function of θ only, replace partial derivatives by ordinary derivatives and substitute m2 = D to get ⎪⎧ sin θ d ⎨ ⎪⎩ P(θ ) dθ ⎛ d [ P(θ ) ] ⎞ ⎪⎫ 2 2 ⎜ sin θ ⎟ ⎬ + G sin θ = m . θ d ⎝ ⎠ ⎪⎭ (S.33) Divide both sides by sin2 θ, multiply through by P(θ) and rearrange to get d [ P(θ ) ] ⎞ ⎛ 1 d ⎛ m2 θ + − sin G ⎜ ⎟ ⎜ sin θ dθ ⎝ sin 2 θ dθ ⎠ ⎝ ⎞ ⎟ P(θ ) = 0. ⎠ (S.34) Carry out the indicated derivatives and then substitute x = cos θ and use the appropriate trigonometric relationships to get (1 − x 2 ) d 2 P (θ ) dP (θ ) ⎛ m2 ⎞ − + − 2 x G P(θ ) = 0. ⎜ 2 ⎟ − (1 ) dx 2 dx x ⎝ ⎠ (S.35) Equation S.35 is the associated Legendre equation. The solution of this equation is summarized below: G = l(l+1); where l = 0, 1, 2, 3, … and P (θ ) = 2l + 1 (l − | m |)! |m| Pl (cos θ ). 2 (l + | m |)! (S.36) Combining the Azimuthal and Axial Solutions Now we are in a position to combine the results for the polar and azimuthal equations to give the total angular dependence. By our original assumption, Y (θ , φ ) = P(θ )Q(φ ) (from S.21) where: Qm (φ ) = e imφ (from S.32) with m = 0, ±1, ±2, ±3, …. S-8 Supplemental Material: Annu. Rev. Phys. Chem. 2007. 58:267-97 doi: 10.1146/annurev.physchem.58.032806.104607 Localized Surface Plasmon Resonance Spectroscopy and Sensing Willets and Van Duyne 2l + 1 (l − | m |)! |m| Pl (cos θ ) 2 (l + | m |)! and Pi|m| (θ ) = with l = 0, 1, 2, 3, …. so that: Y1,m (θ , φ ) = with l = 0, 1, 2, 3, …. and m = -l, –l + 1 , … 0, 1, 2, … l – 1, l. 2l + 1 (l − | m |)! |m| Pl (cos θ )e imφ 4π (l + | m |)! (from S.36) (S.37) These are the NORMALIZED SPHERICAL HARMONICS. The table on the following page shows these relationships for varying values of l and m. S-9 Supplemental Material: Annu. Rev. Phys. Chem. 2007. 58:267-97 doi: 10.1146/annurev.physchem.58.032806.104607 Localized Surface Plasmon Resonance Spectroscopy and Sensing Willets and Van Duyne Table of Yl,m(θ,ф) The first few normalized spherical harmonics, Yl,m(θ,ф) Y00 = 1 2(π )1 / 2 Y10 = 1⎛ 3⎞ ⎜ ⎟ 2⎝π ⎠ 1/ 2 cos θ 1⎛ 3 ⎞ Y1±1= m ⎜ ⎟ 2 ⎝ 2π ⎠ Y20 = 1⎛ 5⎞ ⎜ ⎟ 4⎝π ⎠ 1/ 2 sin θ exp(±iφ ) 1/ 2 (3 cos 2 θ − 1) 1 ⎛ 15 ⎞ Y2±1= m ⎜ ⎟ 2 ⎝ 2π ⎠ Y2±2= 1 ⎛ 15 ⎞ ⎟ ⎜ 4 ⎝ 2π ⎠ Y30 = 1⎛ 7⎞ ⎜ ⎟ 4⎝π ⎠ 1/ 2 sin θ cos θ exp(±iφ ) 1/ 2 sin 2 θ exp(±2iφ ) 1/ 2 (5 cos 3 θ − 3 cos θ ) 1 ⎛ 21 ⎞ Y3±1 = m ⎜ ⎟ 8⎝ π ⎠ 1 ⎛ 105 ⎞ Y3±2 = ⎟ ⎜ 4 ⎝ 2π ⎠ 1/ 2 (5 cos 2 θ − 1) sin θ exp(±1φ ) 1/ 2 sin 2 θ cos θ exp(±2iφ ) 1/ 2 1 ⎛ 35 ⎞ Y3±3 = m ⎜ ⎟ sin 3 θ exp(±3iφ ) 8⎝ π ⎠ ___________________________________________________________ S-10 Supplemental Material: Annu. Rev. Phys. Chem. 2007. 58:267-97 doi: 10.1146/annurev.physchem.58.032806.104607 Localized Surface Plasmon Resonance Spectroscopy and Sensing Willets and Van Duyne Solving the Radial Equation Since the radial equation (Equation S.20a) is a function of r only, replace partial derivatives by ordinary derivatives and substitute G = l(l + 1) to get r 2 ⎡ d 2 Fl (r ) 2 dFl (r ) ⎤ + ⎥ = l (l + 1) ⎢ Fl (r ) ⎣ dr 2 r dr ⎦ (S.38) Rearrange to a more standard form: d 2 Fl (r ) 2 dFl (r ) F (r ) + − l (l + 1) l 2 = 0. 2 dr r dr r (S.39) Assume a trial solution of the form Fl (r) = r n and calculate the derivatives to get dFl (r ) d [r n ] = = nr n −1 dr dr (S.40a) d 2 Fl (r ) d ⎡ d [r n ] ⎤ d = ⎢ = ⎡⎣ nr n −1 ⎤⎦ = n(n − 1)r n − 2 . ⎥ 2 dr dr ⎣ dr ⎦ dr (S.40b) Now substitute the derivatives (Equations S.40a and S.40b) and the trial function into the radial equation (Equation S.39) to get 2 l (l + 1)r n = 0. n(n − 1)r n − 2 + nr n −1 − r r2 (S.41) n(n − 1)r n − 2 + 2nr n − 2 − l (l + 1)r n-2 = 0. (S.42) Rearrange to get Divide through by rn-2 and simplify to get the quadratic: n 2 + n − l (l + 1) = 0. (S.43) Solve the quadratic for n; this yields two solutions: n = l and n = −(l + 1). Thus there are two solutions to the radial equation S-11 (S.44) Supplemental Material: Annu. Rev. Phys. Chem. 2007. 58:267-97 doi: 10.1146/annurev.physchem.58.032806.104607 Localized Surface Plasmon Resonance Spectroscopy and Sensing Willets and Van Duyne ⎧r l Fl (r ) = ⎨ − (l +1) , ⎩r (S.45) which can be combined to a general solution with coefficients to be determined by the appropriate boundary conditions for the problem: Fl (r ) = Ar l + Br − (l +1) . (S.46) Combining the Radial and Angular Solutions Combine the solutions for radial, polar, and azimuthal equations to give a general solution for Laplace’s Equation in spherical coordinates. So the general solution for ∇ 2 (r , θ , φ )Φ l,m (r , θ , φ ) is (from S.12) Φ l.m (r ,θ , φ ) = Fl (r )Yl ,m (θ , φ ) (S.47a) Φl ,m ( r ,θ , φ ) = ⎡⎣ Al r l + Bl r −( l +1) ⎤⎦ Pl m ( cos θ ) eimφ , (S.47b) with l = 0, 1, 2, … and m = −l, −l + 1, . . . −2, −1, 0, 1, 2, . . . , l − 1, l . Applying Boundary Conditions to the Solution At this point it is useful to go back to the physical picture of the metal sphere in a constant electric field (viz., the long wavelength approximation, Figure 1B) to see the origin of the geometrically derived boundary conditions. It is clear that the geometry of this problem is axially symmetric (Figure 1B/2). Thus there is no dependence on the azimuthal angle, φ. This corresponds to the m = 0 solutions of the azimuthal equation. In general the E field inside the sphere will be different from that outside the sphere. We know that the incident E field will not be affected by the sphere as you move far from the sphere (i.e. r → ∞). We also know that the field at the center of the sphere should have some finite value (i.e. the field will be nonzero). These three conditions can be expressed mathematically as follows: 1) E in ≠ E out 2) as r → ∞ E out → E 0 zˆ E in → finite 3) as r → 0 S-12 Supplemental Material: Annu. Rev. Phys. Chem. 2007. 58:267-97 doi: 10.1146/annurev.physchem.58.032806.104607 Localized Surface Plasmon Resonance Spectroscopy and Sensing Willets and Van Duyne Because we know that m = 0 by axial symmetry, let us examine some solutions of Equations S.46, S.37, and S.47 for specific values of l. ▪ For m = 0, l = 0: B ⎤ ⎡ F0 = ⎢ A0 + 0 ⎥ r ⎦ ⎣ Y00 = 1 , 4π so that Φ 00 = 1 4π B0 ⎤ ⎡ ⎢ A0 + r ⎥ . ⎣ ⎦ (S.48) Evaluating Equation S.48 for r → 0 and r → ∞ we get A0 . 4π Φ 00 (r → 0) = ∞ and Φ 00 (r → ∞) = Because E = −ΛΦ, these solutions correspond to Ein(r → 0) = ∞ and Eout (r → ∞) = 0. These solutions violate the three boundary conditions established above. ∴ A0 = B0 = 0 ▪ For m = 0, l = 1: B ⎤ ⎡ F1 = ⎢ A1r + 21 ⎥ r ⎦ ⎣ Y10 = 3 cos θ . 4π 3 into the constants A1 and B1 to be determined by the boundary 4π conditions, we get If we subsume Φ10 (r , θ ) = A1r cos θ + B1 cos θ . r2 (S.49) Convert to Cartesian coordinates using z = r cos θ and ( r = x2 + y2 + z 2 to get S-13 ) 1/ 2 Supplemental Material: Annu. Rev. Phys. Chem. 2007. 58:267-97 doi: 10.1146/annurev.physchem.58.032806.104607 Localized Surface Plasmon Resonance Spectroscopy and Sensing Willets and Van Duyne Φ10 ( x, y, z ) = A1 z + B1 z ( x2 + y2 + z 2 ) 3/ 2 . (S.50) Now calculate the E field from E(x,y,z) = −ΛΦ10(x,y,z) recalling that ∇ = ∇ x xˆ + ∇ y yˆ + ∇ z zˆ and ∇x = ∂ , ∂x ∇y = ∂ , ∂y ∇z = ∂ . ∂z Thus, ⎛∂ ∂ ∂ ⎞ E( x, y, z ) = −⎜⎜ xˆ + yˆ + zˆ ⎟⎟Φ10 ( x, y, z ) ∂y ∂z ⎠ ⎝ ∂x ⎡ ⎤ ⎛ ∂ B1 z ∂ ∂ ⎞⎢ ⎥. E ( x, y, z ) = − ⎜ xˆ + yˆ + zˆ ⎟ A1 z + 3 ⎥ ⎢ 2 2 2 2 ∂ ∂ ∂ x y z ⎝ ⎠⎢ ( x + y + z ) ⎥⎦ ⎣ (S.51) Compute E(x,y,z) by taking the partial derivatives for each component of the field separately and applying the chain rule as needed to get ⎡ ⎤ 3z ( xxˆ + yyˆ + zzˆ ) ⎥ zˆ ⎢ ˆ . − E ( x, y, z ) = − A1z − B1 3 5 ⎥ ⎢ 2 2 2 2 2 2 2 2 x y z x y z + + + + ( ) ( ) ⎢⎣ ⎥⎦ (S.52) Now we must solve for A1 and B1 using the boundary conditions at the surface of the sphere (viz., r = a). Remember that r = ( x2 + y 2 + z 2 ) . 1/ 2 Summary of boundary conditions Inside vs. outside of sphere Condition 1A: Sphere surface (r = a) Condition 2A: E out ( x, y, z ) → E 0 zˆ as r → ∞ Condition 1B: ε in E r ,in = ε out E r ,out (radial BC) Condition 2B: E in ( x, y, z ) → finite as r → 0 Eθ and Eφ are continuous (tangential BC) S-14 Supplemental Material: Annu. Rev. Phys. Chem. 2007. 58:267-97 doi: 10.1146/annurev.physchem.58.032806.104607 Localized Surface Plasmon Resonance Spectroscopy and Sensing Willets and Van Duyne ▪ Applying condition 1A to Equation S.52: E out ( x, y, z ) → E 0 zˆ as r → ∞ ⎡ zˆ 3z ( xxˆ + yyˆ + zzˆ ) ⎤ E out ( x, y, z ) = − A1,out zˆ − B1,out ⎢ 3 − ⎥⎦ . r5 ⎣r (S.53) Term in [ ] goes to 0 as r → ∞. Thus, − A1,out = E0 . (S.54) ▪ Applying condition 1B: E in ( x, y, z ) → finite as r → 0 ⎡ zˆ 3z ( xxˆ + yyˆ + zzˆ ) ⎤ E in ( x, y, z ) = − A1,in zˆ − B1,in ⎢ 3 − ⎥⎦ r5 ⎣r (S.55) Term in [ ] goes to ∞ as r → 0. Thus to keep the field finite, B1,in = 0. (S.56) ▪ Applying condition 2A: ε in E r ,in = ε out E r ,out (radial BC) First we must compute the radial components of E. The relationship between the spherical coordinate components of E and the Cartesian coordinate components of E is given by (see D. Fitts, Vector Analysis in Chemistry, McGraw-Hill, NewYork, 1974, pp. 124--25) E( x, y, z ) = E x xˆ + E y yˆ + E z zˆ (S.57a) and E ( r ,θ , φ ) = Er rˆ + Eθ θˆ + Eφ φˆ . (S.57b) To get Er, Eθ, and Eф from Ex, Ey, and Ez, use the following: Er = sinθcosφEx + sinθsinφEy + cosθEz Eθ = cosθcosφEx + cosθsinφEy – sinθEz Eφ = −sinφEx + cosφEy, as well as the following relationships between the unit vectors: φˆ ⋅ xˆ = − sin φ rˆ ⋅ yˆ = sin θ sin φ θˆ ⋅ xˆ = cos θ cos φ θˆ ⋅ yˆ = cos θ sin φ rˆ ⋅ zˆ = cos θ θˆ ⋅ zˆ = − sin θ φˆ ⋅ zˆ = 0 . rˆ ⋅ xˆ = sin θ cos φ S-15 φˆ ⋅ yˆ = cos φ Supplemental Material: Annu. Rev. Phys. Chem. 2007. 58:267-97 doi: 10.1146/annurev.physchem.58.032806.104607 Localized Surface Plasmon Resonance Spectroscopy and Sensing Willets and Van Duyne So we see that these can be combined to give E r = rˆ ⋅ xˆ E x + rˆ ⋅ yˆ E y + rˆ ⋅ zˆ E z E = θˆ ⋅ xˆ E + θˆ ⋅ yˆ E + θˆ ⋅ zˆ E θ x y z Eφ = φˆ ⋅ xˆ E x + φˆ ⋅ yˆ E y + φˆ ⋅ zˆ E z . Now rearrange Ein(x,y,z) into the form Ein ( x, y, z ) = Ex ,in xˆ + E y ,in yˆ + Ez ,in zˆ . (S.58) And rearrange Equation S.55 to match the form of Equation S.58: ⎡ 3B z 2 B ⎤ ⎡ 3B zx ⎤ ⎡ 3B zy ⎤ Ein ( x, y, z ) = ⎢ 1,in5 ⎥ xˆ + ⎢ 1,in5 ⎥ yˆ + ⎢ 1,in5 − 1,3in − A1,in ⎥ zˆ . (S.59) r ⎣ r ⎦ ⎣ r ⎦ ⎣ r ⎦ Thus, using the unit vector relationships, we get ⎡ 3B zx ⎤ ⎡ 3B zy ⎤ Er ,in = (sin θ cos φ ) ⎢ 1,in5 ⎥ + (sin θ sin φ ) ⎢ 1,in5 ⎥ + ⎣ r ⎦ ⎣ r ⎦ 2 ⎡ 3B z ⎤ B (cos θ ) ⎢ 1,in5 − 1,3in − A1,in ⎥ , r ⎣ r ⎦ (S.60) and similarly from Equation S.53, ⎡ 3B zx ⎤ ⎡ 3B zy ⎤ + (sin θ sin φ ) ⎢ 1,out Er ,out = (sin θ cos φ ) ⎢ 1,out ⎥ ⎥+ 5 5 ⎣ r ⎦ ⎣ r ⎦ 2 ⎡ 3B z ⎤ B1,out A − − (cos θ ) ⎢ 1,out 1, out ⎥ . 5 r3 ⎣ r ⎦ (S.61) Evaluate Equation S.60 using B1,in = 0 determined from the boundary condition 1B: Er ,in = − A1,in cos θ . (S.62) Now evaluate Equation S.61 using A1,out = −E0: ⎡ 3B zx ⎤ ⎡ 3B zy ⎤ + (sin θ sin φ ) ⎢ 1,out Er ,out = (sin θ cos φ ) ⎢ 1,out ⎥ ⎥+ 5 5 ⎣ r ⎦ ⎣ r ⎦ 2 ⎡ 3B z ⎤ B1,out E − + (cos θ ) ⎢ 1,out 0 ⎥. 5 r3 ⎣ r ⎦ Rearrange Equation S.63 and substitute the following: S-16 (S.63) Supplemental Material: Annu. Rev. Phys. Chem. 2007. 58:267-97 doi: 10.1146/annurev.physchem.58.032806.104607 Localized Surface Plasmon Resonance Spectroscopy and Sensing Willets and Van Duyne sin θ cos φ = x , r sin θ sin φ = z y , and cos θ = r y to give Er ,out ⎡ − cos θ 3 ⎛ 2 zy 2 zx 2 ⎞ ⎤ = E0 cos θ + B1,out ⎢ + 5 ⎜ z cos θ + + ⎟⎥ . 3 r ⎝ r r ⎠⎦ ⎣ r (S.64) We are now ready to use boundary condition 2A: ε in E r ,in = ε out E r ,out ; inserting Equations S.62 and S.64 into the boundary condition: −ε in A1,in cos θ = ε out E0 cos θ − ε out B1,out cos θ r3 + (S.65) 3ε out B1,out ⎛ 2 zy 2 zx 2 ⎞ + ⎜ z cos θ + ⎟. r5 r r ⎠ ⎝ Divide through by cosθ and substitute z = rcosθ to give −ε in A1,in = ε out E0 − ε out B1,out r3 + 3ε out B1,out ⎛ 2 zy 2 zx 2 ⎞ + ⎜z + ⎟. r5 z z ⎠ ⎝ (S.66) Recall that r2 = (x2 + y2 + z2) so Equation S.66 can be simplified to −ε in A1,in = ε out E0 − ε out B1,out r 3 + 3ε out B1,out r 5 (r 2 ). (S.67) Canceling r2, combining terms, and factoring out εout gives 2B ⎤ ⎡ −ε in A1,in = ε out ⎢ E0 + 1,3out ⎥ . r ⎦ ⎣ (S.68) Letting r = a as we are interested in the surface of the sphere, 2B ⎤ ⎡ −ε in A1,in = ε out ⎢ E0 + 1,3out ⎥ . a ⎦ ⎣ (S.69) We cannot simplify this expression any further, so we now turn to our next boundary condition. ▪ Applying condition 2B: Eθ and Eφ are continuous (tangential BC) S-17 Supplemental Material: Annu. Rev. Phys. Chem. 2007. 58:267-97 doi: 10.1146/annurev.physchem.58.032806.104607 Localized Surface Plasmon Resonance Spectroscopy and Sensing Willets and Van Duyne Consider the axial case where Eθ ,in = Eθ ,out Recall Eθ = θˆ ⋅ xˆ Ex + θˆ ⋅ yˆ E y + θˆ ⋅ zˆ Ez . (S.70) Using Equation S.59 and the unit vector relationships, we get ⎡ 3B1,in zy ⎤ ⎡ 3B1,in zx ⎤ Eθ ,in = (cos θ cos φ ) ⎢ θ φ (cos sin ) + ⎢ ⎥+ ⎥ 5 5 ⎣ r ⎦ ⎣ r ⎦ ⎤ ⎡ 3B1,in z 2 B1,in A (− sin θ ) ⎢ − − 1,in ⎥ 5 r3 ⎦⎥ ⎣⎢ r and similarly from Equation S.53 in analogy to Equation S.71 above: ⎡ 3B zx ⎤ ⎡ 3B zy ⎤ Eθ ,out = (cos θ cos φ ) ⎢ 1,out + (cos θ sin φ ) ⎢ 1,out ⎥ ⎥+ 5 5 ⎣ r ⎦ ⎣ r ⎦ ⎡ 3B1,out z 2 B1,out ⎤ − 3 − A1,out ⎥ . ( − sin θ ) ⎢ 5 r ⎣ r ⎦ (S.71) (S.72) Evaluate Equation S.71 using B1,in = 0 (Equation S.56) determined from boundary condition 1B: Eθ ,in = A1,in sin θ . (S.73) Now evaluate Equation S.72 using A1,out = -E0 (Equation S.54) determined from boundary condition 1A: ⎡ 3B zx ⎤ ⎡ 3B zy ⎤ Eθ ,out = (cos θ cos φ ) ⎢ 1,out + (cos θ sin φ ) ⎢ 1,out ⎥ ⎥+ 5 5 ⎣ r ⎦ ⎣ r ⎦ ⎡ 3B z 2 B1,out ⎤ − 3 − E0 ⎥ . ( − sin θ ) ⎢ 1,out 5 r ⎣ r ⎦ Rearrange Equation S.74 to get Eθ ,out = − E0 sin θ + 3B1,out zy cos θ sin φ r5 B1,out sin θ + 3B1,out z 2 sin θ − r3 r5 3B1,out zx cos θ cos φ r5 S-18 (S.74) + (S.75) . Supplemental Material: Annu. Rev. Phys. Chem. 2007. 58:267-97 doi: 10.1146/annurev.physchem.58.032806.104607 Localized Surface Plasmon Resonance Spectroscopy and Sensing Willets and Van Duyne Equate Eθ,in (Equation S.73) and Eθ,out (Equation S.75) according to boundary condition 2B and divide by sinθ to get A1,in = − E0 + Substitute B1,out r 3 − 3B1,out z 2 r 5 x = cos φ r sin θ + 3B1,out zy cos θ sin φ r sin θ 5 + 3B1,out zx cos θ cos φ r 5 sin θ . (S.76) y = sin φ into Equation S.76 and simplify to r sin θ and get A1,in = − E0 + B1,out r3 − 3B1,out z 2 r5 + 3B1,out zy 2 cos θ r 6 sin 2 θ + 3B1,out zx 2 cos θ r 6 sin 2 θ . (S.77) Substitute z = rcos θ into Equation S.77 and simplify to get A1,in = − E0 + B1,out r3 − 3B1,out z 2 r5 + 3B1,out cos 2 θ r 5 sin 2 θ ( x 2 + y 2 ). (S.78) Substitute (x2 + y2) = r2 sin2 θ and simplify to get A1,in = − E0 + B1,out r3 − 3B1,out z 2 r5 + 3B1,out r 2 cos 2 θ r5 . (S.79) Substitute z2 = r2 cos2 θ to get A1,in = − E0 + B1,out r3 − 3B1,out z 2 r5 + 3B1,out z 2 r5 . (S.80) And this finally simplifies to A1,in = − E0 + B1,out r3 . (S.81) . (S.82) Let r = a to yield the final result: A1,in = − E0 + B1,out a3 Solving for the Final E Field Expressions (Equation 1) We now have two equations in two unknowns to solve for A1,in and B1,out, i.e. Equations S.69 and S.82 reproduced below: S-19 Supplemental Material: Annu. Rev. Phys. Chem. 2007. 58:267-97 doi: 10.1146/annurev.physchem.58.032806.104607 Localized Surface Plasmon Resonance Spectroscopy and Sensing Willets and Van Duyne 2B ⎤ ⎡ − ε in A1,in = ε out ⎢ E0 + 13,out ⎥ a ⎦ ⎣ A1,in = − E0 + B1,out a3 (S.69) (S.82) . Solve for A1,in first by eliminating B1,out. Multiply both sides of Equation S.82 by −2εout and add to Equation S.69 to get ⎡ 3ε out ⎤ (S.83) − A1,in = ⎢ ⎥ E0 . ⎣ (2ε out + ε in ) ⎦ Now solve for B1,out to get ⎡ ε −ε ⎤ B1,out = a 3 E0 ⎢ in out ⎥ . (S.84) ⎣ (ε in + 2ε out ) ⎦ Recall our previous expressions for Ein(x,y,z) (Equation S.55) and Eout(x,y,z) (Equation S.53). Substituting Equations S.56 and S.83 into Equation S.55, we obtain ⎛ 3ε out ⎞ Ein ( x, y, z ) = ⎜ ⎟ E0 zˆ . ε ε + 2 in ⎠ ⎝ out (S.85) Substituting Equations S.54 and S.84 into Equation S.53, we obtain ⎡ ε −ε ⎤ ⎡ zˆ 3z ⎤ Eout ( x, y, z ) = E0 zˆ − ⎢ in out ⎥ a 3 E0 ⎢ 3 − 5 ( xxˆ + yyˆ + zzˆ ) ⎥ . r ⎣r ⎦ ⎣ ( ε in + 2ε out ) ⎦ (S.86) This is Equation 1 from the main text. DERIVATION OF EQUATION 3 This derivation originates from References 25 and 40 in the main text. We begin by considering the shift in the localized surface plasmon resonance (LSPR) originating from the adsorption of a layer of thickness d and refractive index nA onto the nanoparticle surface. At all distances greater than d from the nanoparticle surface, we assume that there is an external environment with refractive index nE. Thus the distance-dependent refractive index can be written as ⎧n n( z ) = ⎨ A ⎩ nE 0≤ z≤d d <z<∞ . (S.87) We are interested in measuring the wavelength-shift in the LSPR spectrum due to the introduction of the adsorption layer; this can be expressed as follows: S-20 Supplemental Material: Annu. Rev. Phys. Chem. 2007. 58:267-97 doi: 10.1146/annurev.physchem.58.032806.104607 Localized Surface Plasmon Resonance Spectroscopy and Sensing Willets and Van Duyne Δλ = m ⋅ (n final − ninitial ) , (S.88) where m is the bulk refractive index sensitivity of the nanoparticles (in units of energy RIU-1 where RIU is a refractive index unit) and ninitial and nfinal are the refractive indices of the initial state and the final state, respectively. We can define ninitial as the external environment in the absence of the adsorption layer; i.e. ninitial = nE. However, the refractive index of the final state is more complex because it involves some combination of the refractive index of both the adsorbed layer as well as the external environment, as shown in Equation S.87 above. Moreover, the refractive index should be weighted by the distant-dependent intensity of the electromagnetic (EM) field since the fields that probe the local refractive index are more intense closer to the nanoparticle surface (see, for example, Figure 5 in the text). We can approximate the EM field as decaying exponentially with some characteristic length given by ld: E ( z ) = E 0 exp⎛⎜ − z ⎞⎟ . ⎝ ld ⎠ (S.89) Thus, to normalize the refractive index by the relative field intensity (e.g. I/I0), we need to use the EM field squared and our normalization factor becomes 2 ⎡ ⎛ − z ⎞⎤ ⎛ −2 z ⎞ . ⎢⎣ exp ⎜⎝ ld ⎟⎠ ⎥⎦ = exp ⎜⎝ ld ⎟⎠ (S.90) We can now define an effective refractive index, neff, which normalizes the z-dependent refractive index by the intensity factor in Equation S.90: ∞ neff = 2 n ( z ) exp ⎛⎜ −2 z ⎞⎟ dz. ∫ ld ⎠ ⎝ ld 0 (S.91) The factor of 2 normalizes the integral such that neff = nE in the absence of an ld adsorption layer. Inserting Equation S.87 into Equation S.91 and expanding the integral, we get neff = d ∞ 2⎡ ⎛ −2 z ⎞ dz + n exp ⎛ −2 z ⎞ dz ⎤ . exp n ⎜ ⎢ A ∫d E ⎜⎝ ld ⎟⎠ ⎥⎦ ld ⎟⎠ ⎝ ld ⎣ ∫0 (S.92) Evaluating this integral yields the following expression: ⎡ ⎤ neff = nA ⎢1 − exp ⎛⎜ −2d ⎞⎟ ⎥ + nE exp ⎛⎜ −2d ⎞⎟ . l ld ⎠ d ⎠⎦ ⎝ ⎝ ⎣ S-21 (S.93) Supplemental Material: Annu. Rev. Phys. Chem. 2007. 58:267-97 doi: 10.1146/annurev.physchem.58.032806.104607 Localized Surface Plasmon Resonance Spectroscopy and Sensing Willets and Van Duyne If we now substitute neff for nfinal and nE for ninitial in Equation S.88 above, we get the following result: ⎧ ⎡ ⎫ ⎤ Δλ = m ⋅ ( neff − nE ) = m ⋅ ⎨nA ⎢1 − exp ⎛⎜ −2d ⎞⎟ ⎥ + nE exp ⎛⎜ −2d ⎞⎟ − nE ⎬ . ld ⎠ ⎦ ld ⎠ ⎝ ⎝ ⎩ ⎣ ⎭ (S.94) Grouping the nE terms and rearranging, we get ⎡ ⎤ Δλ = m ⋅ ( nA − nE ) ⎢1 − exp ⎛⎜ −2d ⎞⎟ ⎥ . l d ⎠⎦ ⎝ ⎣ (S.95) This is Equation 3 from the main text. It is important to note that this equation reduces simply to Δλ = m ⋅ (n A − n E ) in bulk solvents (where d goes to infinity) where nA is the refractive index of the new solvent and nE is the refractive index of the original bulk medium. Moreover, this approach also works for multilayer systems, as shown in References 25 and 40, following the same derivation. Because this equation is valid for both SPR and LSPR wavelength-shift measurements, we can use it to directly compare the performance of the two types of sensors: ΔλLSPR mLSPR = mSPR ΔλSPR ⎡ ⎛ −2d ⎞⎤ ⎢1 − exp ⎜ ld , LSPR ⎠⎟ ⎥⎦ ⎝ ⎣ . ⎡ ⎛ −2 d ⎞⎤ ⎢1 − exp ⎜ ld , SPR ⎠⎟ ⎥⎦ ⎝ ⎣ (S.96) Here the (nA – nE) terms cancel out because we are comparing sensor performance under identical experimental conditions. From the literature, we know the following relationships (References 25 and 40 from main text): mSPR = 9000 nm RIU-1 and mLSPR = 200 nm RIU-1. This indicates that the SPR outperforms the LSPR sensor for sensing changes in bulk refractive index by a factor of 45. However, as previously stated, the response of the two techniques becomes comparable when measuring short range changes in refractive index due to a molecular adsorption layer. This is due to the difference in the EM-field decay length, i.e. ld,SPR = 200 nm and ld,LSPR = 5 nm. Inserting the values for ld and m into Equation S.96, we can now directly compare the wavelengthshift performance of the two sensors as a function of layer thickness as shown in Figure 3. S-22 Supplemental Material: Annu. Rev. Phys. Chem. 2007. 58:267-97 doi: 10.1146/annurev.physchem.58.032806.104607 Localized Surface Plasmon Resonance Spectroscopy and Sensing Willets and Van Duyne Figure 3. Comparison of the LSPR and SPR wavelength-shift responses using Equation S.96 and values mSPR = 9000 nm RIU-1, mLSPR = 200 nm RIU-1, ld,SPR = 200 nm, and ld,LSPR = 5 nm. As the layer thickness approaches zero, the response of the two sensors becomes nearly identical (i.e, the ratio approaches one). Thus, despite the large difference in the bulk refractive index responses, the two sensors are comparable for thin adsorption layers, which is important for most sensing applications (such as sensing antigen-antibody binding). At this point, we have only considered the bulk refractive index response (m) and the EM-field decay length (ld) for comparing the LSPR and surface plasmon resonance (SPR) sensor response. However, one should also account for the different surface areas of the two substrates by normalizing against the number of adsorbed molecules to get the wavelength-shift response per molecule. We can approximate this by comparing the area occupied by the metal for an SPR thin film with the area occupied by a nanoparticle array. Consider a 10 × 10-μm region of an NSL-fabricated sample. In the case when 500-nm diameter nanospheres are used as a deposition mask, approximately 460 spheres can occupy that space (owing to the fact that it is a hexagonally close-packed array rather than a square array). Thus, one can subtract the area occupied by the spheres (460*π*0.252 = 90.3 μm2) from the area of the region of interest (100 μm2) to get an approximate value of the area occupied by the nanoparticles (9.7 μm2). Compared to a continuous thin film which will occupy all 100 μm2 of the region of interest, the nanoparticles occupy only 9.7 μm2, or 90.3% less area. If we now consider a full-coverage adsorbed monolayer, the LSPR sensor response originates from 90.3% fewer molecules than the SPR sensor. Thus, in terms of sensor response per adsorbed molecule, the LSPR sensor actually outperforms the SPR sensor. As future experiments push toward sensing smaller concentrations (even single molecules), this feature of LSPR sensors will become increasingly important. S-23
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