It has become possible in recent years to detect 17O quadrupole resonance signals in polycrystalline solids with the isotope in its natural abundance (0.0037%). The present experimental methods are mostly based on adiabatic demagnetisation, in which the strong magnetic resonance signal from another nucleus present in the sample, usually protons (P) of spin 1 2 , is monitored in high field, and the 17O spin system (Q) irradiated in zero field a short time later. Repetition of the magnetic field cycle together with simultaneous step wise changes in the Q-Crequency produces a plot of the Q quadrupole resonance spectrum in terms of the change in the P polarisation. Two important conditions are necessary for the successful outcome of a double resonance experiment. Firstly the P-spin-lattice relaxation time roust be long, at least of the order of the cycle time. Secondly, in zero-field, the P and Q spin systems must be brought into repeated thermal contact. Ac least four different experimental techniques are available for ensuringchis. The first utilizes the Harcmann-Hahn equation, in which the precessional frequency of the Q-spins about the applied r.f. field in the rotating frame is sec equal to the P-spin frequency in its own local field; frequent phase reversals of the Q irradiation frequency establish almost continuous thermal contact between the two spin systems. The second requires three different types of spin system, one of which is a nucleus such as 35Cl whose nuclear quadrupole resonance in zero field is used to cool-the P system. The third and fourth methods are particularly useful for the study of oxygen either directly bonded or hydrogen-bonded to hydrogen. They depend on ehe “solid-effect”, in which simultaneous P and Q spin flips occur in high r.f. fields when the Q spin states are sufficiently strongly perturbed by a magnetic dipolar interaction with some of the P spins. This is an efficient mechanism for establishing continuous thermal contact: between the P and Q spins provided chac the P spins attached to oxygen are in good thermal contact with the remainder of the protons, the socalled “dipolar bath”. If they are not, two-frequency irradiation must be used, in which two equally incense radiofrequencies are applied to the sample, separated by the dipolar frequencies. Well-resolved dipolar structure is observed, from which the orientation of ehe electric field gradient: censor at. the 17O nucleus can in principle be derived. These new techniques are currently being used in the study of many different kinds of oxygen-containing compound; the review concludes with a brief survey of their application to hydrogen bonded C 17O and C- 17OH groups in many molecules and ions, including Chose containing symmetrical hydrogen bonds.