The nonlinear surface susceptibility chi(S)(2) is generally referred t
o the system of Cartesian coordinates of the sample. However, since ac
tual measurements take place with respect to the laboratory system of
coordinates, appropriate transformation of chi(S)(2) is necessary to d
educe the underlying susceptibility-components. We demonstrate this by
analyzing the second-harmonic signal generated by an inclined sample
upon rotation around the s-axis of the laboratory system of coordinate
s. The sample consists of two Langmuir-Blodgett-type monolayers of rot
ational symmetry around the sample normal, the two layers being separa
ted by a plane-parallel flat of 1 mm thickness. The occurrence of a ''
symmetry-forbidden'' I(ss)2omega-signal is discussed in detail.