A method of sampling a subterranean formation fluid may comprise extracting a first fluid sample from a portion of the subterranean formation, altering a temperature of the portion of the subterranean formation, and extracting a second fluid sample from the portion of the subterranean formation having altered temperature. The temperature of the portion of the subterranean formation may be altered based on the relative position of a subterranean formation fluid temperature and the multiphase region envelope in the phase diagram of the subterranean formation fluid. The method may further comprise determining a property of the subterranean formation fluid.