Open Access Article
Theekshana
Malalagama
abc,
Binghui
Tian
*abc,
R. M. G.
Rajapakse
abd,
Rehan
Gunathilake
abc,
Ling
Feng
abc and
Min
Yang
*abc
aNational Engineering Research Center of Industrial Wastewater Detoxication and Resource Recovery, Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing 100085, China. E-mail: tianbh@rcees.ac.cn; Tel: +86 10 62928390
bUniversity of Chinese Academy of Sciences, Beijing 100049, China
cChina-Sri Lanka Joint Research and Demonstration Center for Water Technology, Ministry of Water Supply, Meewathura, Peradeniya 20400, Sri Lanka
dDepartment of Chemistry, University of Peradeniya, Peradeniya 20400, Sri Lanka
First published on 18th September 2025
Groundwater is a vital water source, providing drinking water to at least 50% of the world's population and accounting for 43% of water used in irrigation. In Sri Lanka, 39.6% of the population rely on groundwater for drinking purposes, with 72% of this group residing in rural areas. In several of these regions, groundwater quality is affected by geogenic contaminants such as excessive fluoride, hardness, and salinity, which are linked to chronic health issues. These ion-related problems highlight the need for selective separation technologies, with electrodialysis (ED) emerging as a promising and sustainable option. However, membrane fouling and scaling remain significant challenges. This study aims to investigate the mechanisms of membrane fouling and scaling in ED systems and develop effective cleaning strategies to restore membrane performance. The fouling process involves two stages: organic fouling dominant in the initial stages, followed by inorganic scaling. Pearson correlation analysis revealed a strong negative correlation of −0.94 for organic fouling and −0.63 for inorganic fouling. A similar two-stage fouling behavior was also observed in a one-year field experiment conducted in Sri Lanka, further supporting these findings. An integrated acid–base cleaning method was developed, with acidic cleaning effectively removing inorganic scales and alkaline cleaning addressing organic fouling. The acid–base cleaning approach stands out as a sustainable solution to tackle fouling in ED systems, making it suitable for decentralized groundwater treatment in Sri Lanka.
Water impactAccess to clean water remains a challenge in rural Sri Lanka, where communities rely on untreated groundwater. Electrodialysis (ED) offers a sustainable solution, but membrane fouling limits performance. This study investigates fouling mechanisms and proposes a simple acid–alkaline cleaning method. By restoring efficiency and extending lifespan, the approach supports wider ED use in rural water treatment, improving health and sustainability. |
Fouling of ion-exchange membranes (IEMs) comes in several forms, each with distinct mechanisms and impacts on membrane performance. These include inorganic fouling, organic fouling, colloidal fouling, and biofouling, as identified in previous studies.5–7 Inorganic fouling occurs when ions such as calcium, magnesium, barium, sulfate, fluoride, and bicarbonate precipitate as insoluble salts, forming scale on the membrane surface. Organic fouling occurs when organic substances such as aromatic compounds, proteins, oils, carbohydrates, humic acids, and anti-foaming agents adhere to the membrane via electrostatic and hydrophobic interactions. Colloidal fouling arises from suspended particles, such as colloidal silica, manganese oxide, aluminum oxide, clay minerals, organic colloids, and iron oxide. These particles accumulate on the membrane surface, blocking the diffusion layer and reducing membrane efficiency. Although biofouling has been less studied in ED, it remains a challenge in other membrane processes, often resulting in the growth of microbial colonies on the membrane surface.5 While substantial research has been conducted on fouling in pressure-driven processes like RO8–10 and NF,11–13 studies focusing on fouling in ED, particularly for groundwater treatment, are relatively limited.
Understanding the mechanisms of membrane fouling in ED and developing effective cleaning strategies are crucial for advancing the sustainability of this technology. Regular cleaning is essential to mitigate fouling and maintain the long-term performance of ED systems, particularly in field applications requiring continuous operation. This study investigates membrane fouling in an ED system treating real groundwater at the laboratory scale, with a focus on understanding the mechanisms of fouling and scaling in Sri Lankan groundwater. The findings were further validated using performance data from a long-term ED plant operated for groundwater treatment. Additionally, it aims to develop and evaluate cleaning procedures to mitigate fouling and restore membrane performance, contributing to more sustainable ED operations. A variety of analytical techniques are utilized to systematically examine membrane morphology, elemental distribution, foulant composition, and scale formation. The effectiveness of chemical cleaning methods in removing foulants and scaling will also be assessed, with the ultimate goal of establishing an optimized cleaning protocol for ED systems in field applications.
Both the dilute and the concentrated chambers were supplied with brackish water sourced from a deep groundwater well. Operational conditions were maintained at higher applied currents and higher flow rates to mimic the conditions intended for implementation in Sri Lankan context for the selective removal of problematic ions such as fluoride and hardness. The initial volume for all three input solutions used was 1000 mL in each batch. During the intermittent desalination experiments, each desalination cycle was conducted for one hour, and the process was repeated until a total of 100 cycles was completed (Fig. S2). A multi-parameter portable meter (HANNA instruments: H198129 Combo pH and EC meter) was used to monitor pH and EC variation in both dilute and concentrate solutions.
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Eqn (2) was used to calculate the water production rate φ (%), where Vf is the volume of feed (m3) and Vd is the volume of dilute produced (m3).14
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The rate of change in removal efficiency of organic and inorganic components between each sampling interval was calculated to characterize the fouling progression. The rate of change of each parameter was calculated using eqn (3).15
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| Fig. 1 (a) Water production rate (%) and (b) variation and reduction of electrical conductivity of ED during intermittent ED testing. | ||
As shown in Fig. 1(a), the water production rate gradually, though slowly, declined over the measured 100 cycles. This reduction in performance can be attributed to several factors, including membrane fouling and scaling.16 Fouling primarily occurs on the membrane's surface and within its pores due to concentration polarization, while scaling predominantly occurred during intermittent system shutdowns. The presence of scale deposits on the membrane's surface and pores can alter membrane hydrophilicity, facilitating the easier passage of water through the membrane.
The EC in the water produced after 38 cycles remained below 679 μS cm−1, signifying a degradation in water quality with increasing treatment cycles. During the first 21 cycles, EC removal efficiency remained high, ranging from 97.06% to 70.3%, with only a slight decline. However, a sharp drop in efficiency was observed over a few cycles, leading to a significant 30% reduction compared to the initial 21 cycles. This sudden decrease indicates the onset of membrane fouling in the system, a trend that is consistent with the findings of Zhang W. et al. in 2022.17 Following this decline, the efficiency appeared to stabilize, showing alternating periods of decrease and increase. This behavior can be attributed to the ongoing processes of membrane fouling and scaling. During the initial cycles, the IEMs were likely free of significant foulants, allowing efficient ion transport. However, as the cycles progressed, foulants and scale gradually built up on the membrane surfaces, restricting ion movement and reducing performance. This accumulation over time caused a notable drop in EC reduction efficiency, emphasizing the challenges of continuous operation and the importance of implementing effective fouling control strategies.
AEMs were covered by a distinct, brown-colored layer (Fig. 2a), whereas this layer was comparatively less pronounced on the CEMs (Fig. 2d). This discoloration is attributed to the deposition of humic substances, which are the predominant components of natural organic matter (NOM) and are typically classified as humic acid (HA), fulvic acid (FA), and humin. Although CEMs exhibited less severe coloration than AEMs, the accumulation of reddish-brown contaminants was still observed, albeit at a lower intensity. Similar findings of relatively reduced fouling in CEMs have been reported in previous studies.18–20 According to these studies, the morphology of fouling appeared similar in both AEMs and CEMs, although the extent differed. Based on these observations, our subsequent analysis primarily focuses on fouling behavior in AEMs.
Fig. 2(a–c) presents a series of images depicting the fouled AEM sheets alongside images of the pristine, untouched AEMs, offering valuable insights into the fouling that occurred on the membranes. The AEM exhibits distinct brown and dark brown colorations, forming well-defined blocks attributed to the creation of water channels across the membrane, demarcated by the spacers. On the outer surfaces of AEMs, which are exposed to the concentrated solution circulation during the ED operation, a thinner layer of fouling is apparent (Fig. 2(c)). A similar fouling pattern was reported by Xia et al., 2018.21 It is worth noting that IEMs did not exhibit a slimy or gelatinous texture, suggesting that the membrane was not significantly affected by biofouling.
The predominant components of the fouling layer are calcium (Ca) and magnesium (Mg), with both elements forming significant scale deposits. EDS confirms the presence of Ca and Mg, which are primarily identified as calcium carbonate (CaCO3) and magnesium carbonate (MgCO3), respectively (section 2.1 in the SI). XRD analysis further identified multiple crystalline phases of CaCO3, including calcite, vaterite, and aragonite as well as crystalline MgCO3, providing a detailed picture of the scaling (section 2.2 in the SI). Silica (Si) was also a major contributor, with silicon dioxide (SiO2) present in significant quantities. XPS confirmed the presence of S–O bonds, indicating that silica is a dominant foulant, likely originating from the groundwater (section 2.4 in the SI). Furthermore, organic fouling is observed through FTIR spectroscopy, which detects characteristic bands associated with organic compounds, particularly proteins and polysaccharides (section 2.3 in the SI). These organic foulants are found to be adhered to the membrane surface, contributing to the overall fouling composition. An et al. (2023)22 also reported that low molecular weight (LMW) organic matter tends to accumulate more readily on membrane fouling where significant concentrations of LMW organic compounds are found in raw water (Fig. S1) due to the unique nature of Sri Lankan groundwater.
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| Fig. 5 FTIR absorbance values at 1670 cm−1 over time, indicating the progression of organic fouling (a) and EDS elemental composition analysis showing calcium weight % on the membrane over time (b). | ||
As shown in Fig. 5(a), organic fouling is quantified using FTIR-based principal component analysis (PC1), which explained 98.7% of the spectral variance. The dominant loadings in PC1 were associated with amide functional groups (1670 cm−1), indicating proteinaceous or organic material accumulation. Organic fouling increased rapidly in the early treatment cycles: absorbance rose from 78.85 at cycle 20 to 85.97 by cycle 100. The highest rate of increase was between cycles 20 and 30. During this period, the rate of change in absorbance was calculated at 0.369 absorbance units per cycle, suggesting a rapid initial fouling stage. After cycle 30, the fouling rate slowed to 0.049 absorbance units per cycle, indicating a near-steady-state phase. This behavior is consistent with stage 1 fouling, where a thin organic layer forms quickly and then stabilizes, reducing membrane performance by obstructing ion transport.
Fig. 5(b) presents the progression of inorganic fouling, as measured by energy-dispersive spectroscopy (EDS). The first principal component (explaining 95.2% of the variance) showed strong loadings for calcium (Ca), confirming the role of calcium-based scaling. During early operation (cycles 20 and 30), calcium deposition remained low at 0.1 wt%, and the rate of change was negligible. However, a gradual but steady increase in Ca content was observed between cycle 30 and 100, reaching 0.5 wt% at cycle 100, with a corresponding deposition rate of 0.0057 wt% per cycle. This trend indicates the onset of stage 2 fouling, where the pre-established organic layer likely promotes the nucleation and growth of inorganic scale (e.g., CaCO3).
These two datasets together support a sequential fouling model:
Stage 1: early organic accumulation driven by electrostatic and hydrophobic interactions.
Stage 2: later-stage inorganic scaling facilitated by the organic layer and operating conditions.
Although the proposed two-stage fouling model is based on post-operation analysis of lab-scale membranes and is not predictive in real time, it offers a valuable mechanistic foundation for understanding fouling progression. To enable early-stage identification during ED operation, future work should incorporate real-time monitoring tools—such as resistance tracking, voltage fluctuations, or current efficiency trends—as potential operational indicators. These could be further enhanced by advanced electrochemical signal monitoring techniques, as demonstrated by Zhang et al. (2024),23 which show strong potential for early detection and differentiation of fouling stages.
Future studies should aim to validate this two-stage fouling model in pilot-scale ED systems, integrating online monitoring tools (e.g., EIS) to enable real-time identification and mitigation of both organic and inorganic fouling stages.
In contrast, the correlation coefficient between removal efficiency and inorganic fouling, as indicated by calcium deposition, is r = −0.63, reflecting a moderate negative correlation. This finding indicates that while inorganic fouling also contributes to the reduction in removal efficiency, its impact is less pronounced in the early stages and becomes more significant in later stages of operation. The moderate correlation reinforces the concept of a secondary fouling mechanism, where inorganic scaling gradually accumulates over time, particularly after organic fouling stabilizes. A summary of the Pearson correlation coefficients is provided in Table 1.
| Correlation pair | Correlation coefficient (r) |
|---|---|
| Removal efficiency vs. organic fouling | −0.94 |
| Removal efficiency vs. inorganic fouling | −0.63 |
A detailed evaluation of removal efficiency, fouling dynamics, rate-of-change calculations, and correlation analysis supports a two-stage fouling model in electrodialysis:
Stage 1 (early phase): organic fouling dominates. This is evident from the sharp increase in FTIR absorbance and its strong negative correlation with removal efficiency. The rapid accumulation of organic deposits significantly impacts membrane performance, with the most noticeable decline occurring within the first 30 cycles.
Stage 2 (later phase): inorganic fouling, particularly calcium scaling, becomes more prominent. This is reflected in a gradual rise in calcium content and a moderate negative correlation between calcium deposition and removal efficiency. Unlike organic fouling, which causes a rapid drop in performance, the effects of inorganic scaling exert a cumulative and slower effect, contributing to a continued but more gradual decline in system performance.
These findings highlight the distinct phases of fouling in ED (Fig. 6) and emphasize the need for targeted mitigation strategies to maintain system performance.
In the first stage, the positively charged surface of the AEM, combined with its hydrophilic nature, creates an ideal environment for organic anions to adhere. AEMs are known to be particularly susceptible to organic foulants (e.g., HA, carbohydrates, and aromatic compounds). This fouling primarily occurs on the membrane surface and within its internal structure owing to electrostatic, van der Waals, and hydrophobic interactions.20 Therefore, these negatively charged organic compounds quickly accumulate on the membrane surface, forming an initial organic fouling layer. This layer creates a rough and uneven surface, which further promotes fouling by trapping additional contaminants.
As the organic layer thickens, it becomes a suitable foundation for inorganic deposition, particularly by divalent cations like calcium (Ca2+). This transition marks the onset of the second fouling stage, characterized by the precipitation of salts such as calcium carbonate (CaCO3). The presence of the organic layer facilitates the attachment and crystallization of inorganic salts, accelerating the fouling process and making it more severe over time.
The electric field in the ED system further intensifies this sequence by driving negatively charged particles toward the AEM, increasing their local concentration and enhancing the likelihood of fouling. Initially, organic fouling reduces membrane efficiency by obstructing ion transport. As inorganic scaling progresses, it exacerbates pore blockage, significantly impairing ion-exchange capacity.
This sequential fouling not only accelerates the deterioration of the membrane's physical structure but also compromises its selective permeability. As both organic and inorganic foulants accumulate, the cumulative impact accelerates membrane degradation, leading to a substantial decline in overall system performance.
These findings highlight the urgency of developing effective cleaning strategies to mitigate fouling to establish ED as a sustainable water treatment solution for Sri Lanka. Although the water production rate remained largely unaffected, prolonged fouling progressively compromises water quality over time, underscoring the need for optimized maintenance protocols to sustain long-term ED performance.
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| Fig. 8 Representative scanning electron microscopy (SEM) images of membrane after cleaning under (a) DW, (b) NaOH, (c) HCl and (d) citric acid. | ||
The scaling observed in the cleaned membrane, as shown by the high proportion of C, O, and Ca elements, suggests that CaCO3 is the predominant component of fouling (Fig. S11–S14). This is observed in the cleaning methods of DW, NaOH, and HCl. However, it was observed that the peak height and area within the FTIR spectrum associated with CaCO3 were comparatively smaller in cleaned membranes (Fig. S14), suggesting that the surface concentration of foulants was effectively lowered. The surfaces of the membranes exhibited a relatively clean appearance in all three reagents, with few variances. The surface morphology of the membrane surface subjected to DW cleaning (Fig. 8(a)) exhibited a noticeable improvement in smoothness. In conjunction with the obtained outcomes, DW partially mitigated scaling; however, a substantial amount remained. Membranes cleaned with NaOH showed evidence of remaining CaCO3 crystals on the surface. This is likely because NaOH is effective at removing organic debris25 but less effective at solubilizing inorganic scale. Enhanced elimination of inorganic foulants can be attained through the application of acidic agents due to the solubilization and chelation reaction that occurs between inorganic ions and acids.24,26 As a result, the presence of the inorganic foulant on the membrane was effectively eliminated with the use of HCl solution.
However, despite the effectiveness of the cleaning process for HAc, the distinctive peaks associated with CaCO3 in FTIR analysis27–29 and the presence of Ca patches in EDS mapping were hardly distinguishable in the HAc-cleaned membrane (Fig. S14). However, the production of a gel layer (Fig. 8(d)) was detected during the HAc process, which was also noted by Wang S. et al. (2023)27 in their research on the VMD desalination process. Even though the Ca and Mg fouling were not evident on the membrane after it had been cleaned with HAc, significant organic fouling was still found, implying that organic fouling formed first and could not be fully removed by acidic cleaning alone.
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| Fig. 9 Fluorescence excitation and emission matrix of the membrane cleaning solutions: (a) DW, (b) NaOH, (c) HCl and (d) citric acid for AEM. | ||
Cleaning with deionized water (DW) revealed the presence of tyrosine-like aromatics (region I) and protein-like substances (region II), suggesting moderate removal efficiency while indicating that some organic matter remained on the membrane. In contrast, NaOH cleaning led to a significant reduction in these regions, highlighting its strong oxidative properties and effectiveness in mitigating biofouling, including the breakdown of high molecular weight humic substances. HCl cleaning had a slight effect on the reduction of aromatic proteins and lower molecular weight humic acids, suggesting its effectiveness in removing inorganic foulants rather than organic matter. Citric acid cleaning was highly effective, as evidenced by significant reductions in fluorescence intensity across regions associated with humic substances. This indicates that citric acid is particularly effective in dislodging complex fouling layers composed of both organic and inorganic components. Overall, the 3D-EEM spectroscopy analysis underscores the differential cleaning efficacy of each reagent, with citric acid emerging as the most efficient in removing both organic and inorganic contaminants from the AEM.
For professional users, a combination of HCl and NaOH is recommended for effective cleaning. These chemicals, commonly used in industrial-scale cleaning, should be handled exclusively by trained professionals following proper safety procedures. Post-chemical cleaning, membranes should be flushed with deionized water (DW) to remove residual contaminants. Although DW flushing effectively removes some foulants through hydraulic action, it is insufficient for insoluble scalants, highlighting the need for chemical cleaning.
For household or decentralized users, the use of HCl is discouraged due to potential health and handling risks. Instead, citric acid offers a safer and equally effective alternative for removing alkaline scaling. DW flushing remains a primary cleaning method for non-professionals, offering a safe way to maintain membranes without chemical exposure.
By adopting user-specific, two-step cleaning protocols, membrane performance can be effectively restored (Fig. S10(b)), ensuring the sustainable operation of ED systems for brackish groundwater treatment.
Our investigation into various cleaning methods revealed that physical cleaning techniques, such as DW and NaOH, were ineffective in removing alkaline scaling. In contrast, acidic solutions, particularly HCl and HAc, show promise in addressing inorganic scaling, with citric acid emerging as a viable option for household-level cleaning applications. Despite their respective strengths, none of the individual cleaning methods was able to fully eliminate all foulants. Based on these findings, we recommend a comprehensive cleaning protocol that combines acid cleaning followed by base cleaning to restore membrane performance and extend the operational lifespan of ED systems. This multi-step approach helps address both organic and inorganic fouling, improves membrane recovery and supports the long-term sustainability of brackish groundwater desalination systems.
The data supporting this article have been included as part of the SI.
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