Acoustic reciprocity theorems have proved their usefulness in the stud
y of forward and inverse scattering problems. The reciprocity theorems
in the literature apply to the two-way (i.e. total) wavefield, and ar
e thus not compatible with one-way wave theory, which is often applied
in seismic exploration. By transforming the two-way wave equation int
o a coupled system of one-way wave equations for downgoing and upgoing
waves it appears to be possible to derive 'one-way reciprocity theore
ms' along the same lines as the usual derivation of the 'two-way recip
rocity theorems'. However, for the one-way reciprocity theorems it is
not directly obvious that the 'contrast term' vanishes when the medium
parameters in the two different states are identical. By introducing
a modal expansion of the Helmholtz operator, its square root can be de
rived, which appears to have a symmetric kernel. This symmetry propert
y appears to be sufficient to let the contrast term vanish in the abov
e-mentioned situation. The one-way reciprocity theorem of the convolut
ion type is exact, whereas the one-way reciprocity theorem of the corr
elation type ignores evanescent wave modes. The extension to the elast
odynamic situation is not trivial, but it can be shown relatively easi
ly that similar reciprocity theorems apply if the (non-unique) decompo
sition of the elastodynamic two-way operator is done in such a way tha
t the elastodynamic one-way operators satisfy similar symmetry propert
ies to the acoustic one-way operators.