Scaling-induced wettinggreatly limits the application
of membrane
distillation (MD) for the desalination of high-salinity feed. Although
highly soluble salts (e.g., NaCl) have high concentrations in this
water, their scaling-induced wetting remains overlooked. To unravel
the elusive wetting behaviors of highly soluble salts, in this study,
we systematically investigated the scaling formation and wetting progress
by in situ observation with optical coherence tomography (OCT). Through
examining the influence of salt type and vapor flux on the wetting
behavior, we revealed that highly soluble salt-induced wetting, especially
under high vapor flux, shared several unique features: (1) occurring
before the bulk feed reached saturation, (2) no scale layer formation
observed, and (3) synchronized wetting progress on the millimeter
scale. We demonstrated that a moving scale layer caused these interesting
phenomena. The initial high vapor flux induced high concentration
and temperature polarizations, which led to crystallization at the
gas–liquid interface and the formation of an initial scale
layer. On the one hand, this scale layer bridged the water into the
hydrophobic pores; on the other hand, it blocked the membrane pores
and reduced the vapor flux. In this way, the decreased vapor flux
mitigated the concentration/temperature polarizations, and consequently
led to the dissolution of the feed-facing side of the scale layer.
This dissolution prevented the membrane pores from being completely
blocked, facilitating the transportation and crystallization of salts
at the distillate-facing side of the scale layer (i.e., the gas–liquid
interface), thus the proceeding of the wetting layer.