Permeate fluxes from desalination of brines and produced waters: A reactive transport modeling study

Journal Article · Mon Sep 01 00:00:00 EDT 2025 · Applied Geochemistry

DOI:https://doi.org/10.1016/j.apgeochem.2025.106429· OSTI ID:2569646

Molins, Sergi; Spycher, Nicolas; Dischinger, Sarah M; Nassr, Mostafa; Lee, Ji Yeon; Johnston, Jacob; Tilton, Nils; Gleason, Kristofer L; Freeman, Benny D; Stringfellow, William T; Miller, Daniel J

The increasing interest in the use of membrane systems to desalinate inland brackish water, agricultural drainage, and industrially produced wastewater demands improved means of predicting desalination system performance under variable feedwater compositions. The interaction among water flow, solute transport, and chemical composition in these systems impacts permeate flux evolution. Here, an established multicomponent reactive transport simulator that accounts for these coupled processes is applied to compute osmotic pressure and permeate fluxes in reverse osmosis (RO) systems. The model is first validated by predicting permeate fluxes for a set of benchtop crossflow experiments subject to a range of feed flow rates and compositions, under fouling and non-fouling conditions. Results compare favorably with measured data that show that solutions with similar total dissolved solids concentrations but different compositions result in different permeate fluxes. The model is then applied to predict permeate fluxes from the desalination of produced waters using a commercial spiral wound RO module. For NaCl-dominant brines, at total dissolved salt concentrations (TDS) below about 70 g/L, permeate fluxes are inversely proportional to water mole fraction as the latter is a reasonable approximation of water activity (i.e. ideal mixing). In the case of Ca–Cl-, Na–CO3- and Na–SO4-dominant brines below about 70 g/L TDS, this relationship does not hold as well and tends to overpredict osmotic pressure and thus underpredict permeate fluxes. However, the opposite becomes true at higher TDS values for typical produced waters. The scaling potential of these waters is also computed by allowing the precipitation of minerals above their saturation limit on the RO membrane. This work demonstrates how reactive transport models developed for the analysis of waters from geological systems can be extended to improve process design, optimization, and control in desalination systems from produced waters and beyond.

• Research Organization: Lawrence Berkeley National Laboratory (LBNL), Berkeley, CA (United States)
• Sponsoring Organization: US Department of Energy; USDOE Laboratory Directed Research and Development (LDRD) Program
• Grant/Contract Number: AC02-05CH11231
• OSTI ID: 2569646
• Journal Information: Applied Geochemistry, Journal Name: Applied Geochemistry Vol. 189
• Country of Publication: United States
• Language: English