Chapter 3 Coherence A detailed study of the effects due to the finite size and spectral bandwidth of a source requires the more powerful tools provide...
Chapter 3 Coherence A detailed study of the effects due to the finite size and spectral bandwidth of a source requires the more powerful tools provided by coherence theory, which is essentially a statistical description of the properties of the radiation field in terms of the correlation between the vibrations at different points in the field. Comprehensive treatments of coherence theory are to be found in reviews by Mandel and Wolf [1965] and by Troup and Turner [1974], as well as in books by Beran and Parrent [1964], Pefina [1971], Mandel and Wolf [1995] and Born and Wolf [1999].
3.1 Quasi-Monochromatic Light As mentioned in Chapter 2, light from a thermal source is not strictly monochromatic. Accordingly, to evaluate the electric field due to a thermal source emitting over a range of frequencies, we have to sum the fields due to the individual monochromatic components. From Eqs. (2.1) and (2.9) the net electric field is given by the integral /»oo
V(r\t)
= / Jo
a(v) cos[2jrvf - 0(v)]dv,
(3.1)
where a(v) and (v) are the amplitude and phase, respectively, of a monochromatic component of frequency v. Since V^r\t) is a real function, our first step is to develop a complex representation which is a generalization of that used earlier for monochromatic light. For this we make use of the associated function (also real) /•OO
V{i)(t) = / Jo
a(y) sin[27rvf - 0(v)]dv. 35
(3.2)
Chapter 3. Coherence
36 We can then define a complex function
V(0 = V(r)(0 + iV(0(0
-L
00
a(v) exp{i[2;rvf - 0(v)]}dv.
(3.3)
This complex function is called the analytic signal associated with the real function V ( r ) 0); its properties have been discussed in detail by Born and Wolf [1999]. In particular, it can be shown that if v(v) is the Fourier transform of V^r\t), so that oo
/
v(v)exp(-i2itvt)dv,
(3.4)
v(v) exp(-i2nvt)dv.
(3.5)
-00
we have /»00
V(t) = 2 / Jo It can also be shown that
(V(t)V*(t))=2([V(r)(t)]2),
(3.6)
so that, if we ignore a factor of (1/2), as we have done in Eq. (2.15), the optical intensity due to a quasi-monochromatic source is / = {V(t)V*W).
(3.7)
It follows that if the operations on V^r\t) are linear, it is possible to replace it by V(t) and take the real part at the end of the calculation.
3.2 Waves and Wave Groups Monochromatic light corresponds to an infinitely long train of waves, all of which have the same wavelength or frequency. The superposition of infinite trains of waves of slightly different frequencies (as from a quasi-monochromatic source) results in the formation of wave groups. For convenience, we take E = acos(cot — kz), where co = 2nv and k = 2n/X, to represents a monochromatic wave propagating along the z axis. A quasi-monochromatic beam consisting of a number of such waves whose angular
33. Phase Velocity and Group Velocity
37
frequencies lie within a very small interval ± Aco about a mean angular frequency co can then be represented by the relation pcb+Aco
V(z, 0 = /
a(co) cxp[-i(cot - kz)]dco.
(3.8)
J CO— Ad)
If k is the propagation constant for an angular frequency co, Eq. (3.8) can be rewritten as V(z, t) = A(z, t) exp[-i(f - kz)l