Systems and apparatuses for regulating a multi-phase fluid stream flowing from a subterranean geological formation, and related methods are described herein. The system and apparatus generally include a conduit defining a flow path for the fluid stream, the conduit further defining a first restriction having a throat portion, and the conduit further defining a first return path including an inlet positioned downstream of the first restriction and an outlet positioned upstream of the inlet of the first return path. Related methods include placing the apparatus or system within a wellbore conduit defined by a wellbore.