Abstract. We investigate the drift dissipative instability in a non-uniform magnetized plasma composed of electrons, positive ions, negative ions and negatively charged dust particles. We use a multi-fluid plasma model and derive a dispersion relation for the electrostatic drift waves with frequencies much smaller than the ion gyrofrequencies and wavelengths longer than the ion gyroradii. The presence of the negatively charged, massive dust grains affects the drift wave frequency and the growth rate of the drift dissipative instability. The present results may be relevant to space and laboratory magnetoplasmas containing negative ions and charged dust grains.The low-frequency electrostatic drift wave is one of the fundamental modes of a non-uniform magnetized plasma (e.g. [1][2][3][4]). In the standard theory of the drift dissipative instability, consideration of a non-Boltzmann electron density perturbation owing to electron-ion collisions leads to a phase shift between the electron density perturbation and the wave potential, which in turn produces instability [1][2][3][4][5][6]. Non-thermal drift waves cause cross-field transport [5] of the electrons and ions in an inhomogeneous magnetoplasma. Furthermore, it is well known [7][8][9][10] that dispersive drift waves, driven by the drift dissipative instability, can be responsible for the formation of zonal flows, streamers, and vortical structures. The latter play an important role in tokamaks [11], for example.It has been shown that the properties of the dispersive drift wave [12] can be modified in the presence of charged dust grains [13,14] owing to the modification of the equilibrium quasi-neutrality condition and the dust particle dynamics. Dust charge fluctuations can also modify the properties of electrostatic drift waves [15,16]. The dynamics of the collisional drift wave instability in an electron-ion plasma with stationary dust grains (i.e. dust grains that do not move on the time scale of the instability) has been studied in [17], without presenting, the modification of the instability growth rate and the drift wave frequency owing to the presence of dust. † Permanent address: