“…However, studies on the contributions of heterogeneous and homogeneous crystallization to membrane scaling and wetting are still very limited, and the results of previous investigations have generally been contradictory. Several studies have proposed that membrane scaling is mainly caused by heterogeneous crystallization on the membrane surface, ,, whereas other researchers have suggested that the deposition of crystals originating from homogeneous crystallization accounts for the water flux decline. − In addition, solutes in the feedwater, such as natural organic matter (NOM), also affect scaling during pressure- or osmosis-driven membrane filtration. , Membrane scaling for RO, nanofiltration (NF), and forward osmosis (FO) can be accelerated by the formation of an organic fouling layer on the membrane surface, − which can be attributed to an increase in concentration polarization. In addition, the functional groups of NOM (e.g., the carboxyl groups) can promote the heterogeneous crystallization of gypsum on the membrane surface. , Different from the above membrane processes, MD is driven by the vapor pressure difference and uses hydrophobic membranes.…”