Techniques for the study of electron attachment and detachment are reviewed. The rate coefficients for the various processes of aeronomic interest are then discussed. The rates of three-body and dissociative attachment by thermal electrons have been successfully determined by swarm techniques and by high frequency studies of electrons produced by high energy particles and by photoionization. Collisional and associative detachment rates for thermal energy negative ions have been measured using the swarm and flowing afterglow techniques. Radiative attachment rates for some atmospheric negative ions have been calculated from measurements of photodetachment cross sections using crossed photon and ion beam techniques. Electron beam studies and measurements of ion kinetic energy have provided much useful information regarding the dissociative attachment process and the structure of molecular negative ions. Rate coefficients for low energy processes such as the three-body attachment to O,, the radiative attachment to 0 , and the associative detachment of 0-in collisions with various atmospheric gases are reasonably well known. Other possibly important low energy processes, such as dissociative attachment to 0 3 , radiative attachment to O,, and the associative detachment of 02-areless well known.Canadian Journal of Chemistry, 47, 1783 (1969) Introduction Laboratory measurements of the rates of loss of free electrons by collisional attachment to molecular oxygen and radiative attachment to atomic oxygen under conditions of electron energy and gas temperature appropriate to the earth's atmosphere were first reported about 10 years ago. Measurements of photodetachment rates for 0-and 0,-were made at about the same time. Information concerning such processes as of 1963 were reviewed by Branscomb (1). Although progress has been made in refining and understanding these processes, it was not until 1966 that really significant new laboratory data in the area of electron attachment and detachment processes became available in the form of associative detachment coefficients for 0-and 0,-in collisions with atomic oxygen (2). These results, along with the accompanying studies of negative ion -molecule reaction rates ( 2 4 ) have made possible much more realistic models of the electron -negative ion balance at altitudes where atomic oxygen is present (3-5). In keeping with the purposes of this Symposium we will limit our discussion to some of the laboratory techniques and results which form a basis for atmospheric models.Electron attachment and detachment processes which are considered to be of aeronomic interest