Researchers Frantisek Cacho, Jakub Masac and Andrej Kudry report in the open-access journal Results in Chemistry a flow-through coulometric titration method that determines iodides directly in water samples with very high chloride content, including seawater. The central challenge they tackled is one that plagues nearly every electroanalytical technique: interference. Chlorides, sulfates, bromides and fluorides coexist with iodide in real matrices and can distort or swamp the analytical signal. Seawater, with an average chloride concentration of nearly 20 grams per liter, represents perhaps the worst-case scenario for iodide determination. Conventional approaches, such as high-performance liquid chromatography or gas chromatography with mass spectrometry, typically require a time-consuming derivatization step in which iodine species are converted to detectable derivatives. Ion chromatography, while simpler, suffers from low sensitivity. Spectrophotometric methods based on the Sandell-Kolthoff reaction, in which iodine catalyzes the reduction of yellow cerium(IV) ions by arsenic, demand careful kinetic control. The new method sidesteps much of this complexity by exploiting a clever two-step electrochemical strategy inside a porous electrode.

The heart of the instrument is a compact flow cell equipped with a cylindrical working electrode made of porous glassy carbon, also known as reticulated vitreous carbon, with a porosity of 100 pores per inch, 4 millimeters long and 10 millimeters in diameter. A platinum auxiliary electrode and a saturated silver/silver chloride reference electrode complete the three-electrode arrangement. The measurement unfolds in two distinct phases. First, a 4-milliliter sample or standard is pumped through the system, filling the pores of the working electrode at a resting potential of 200 millivolts, where no interfering electrochemistry occurs. Then the potential is stepped up to 960 millivolts and held for 30 seconds, during which iodide ions are electrochemically oxidized to iodine within the electrode volume. In the second phase, a constant reduction current of minus 8 microamperes is applied, converting the generated iodine back to iodide while the instrument records the resulting signal.

Why bother with this oxidation-then-reduction round trip instead of simply oxidizing iodide directly? The answer lies in signal quality. The reduction of iodine proceeds at a more negative potential, where the signal-to-noise ratio is substantially higher and the detection limit correspondingly lower. The authors demonstrated that this two-step mechanism yields markedly better performance than direct oxidation. The signal itself is captured using a memory mapping technique, in which chronopotentiometric data are recorded not as a potential-versus-time wave but as a peak of channel counts plotted against potential. The integrated peak area is directly proportional to the chronopotentiometric transition time of the electrode process, and dividing that area by the sampling frequency of the analog-to-digital converter yields the transition time in seconds. This transition time is the quantity that scales linearly with iodide concentration, forming the basis of quantification.

One of the most compelling aspects of flow coulometry is that it can function as an absolute, calibration-free method. Under appropriate conditions, the analytical result is obtained by direct calculation from the measured signal using Faraday’s law, meaning the outcome depends only on physical constants and directly measured quantities rather than on reference materials. In the thin-layer configuration used here, operated galvanostatically, the relationship between transition time and analyte concentration is practically linear as long as the solution layer within the electrode does not exceed the thickness of the diffusion layer and the current density remains below roughly 1 microampere per square centimeter. At higher currents, diffusion limitations begin to distort the response. When the pore diameter of the electrode matches the diffusion layer thickness, the analyte concentration is essentially uniform throughout the electrode, and the potential directly reflects the concentration within its volume, cleanly marking the endpoint of electrolysis.

The team systematically optimized every operating parameter. The oxidation potential was scanned from 800 to 980 millivolts in 20-millivolt steps, with the maximum signal reached at 960 millivolts; beyond that, the electrode material itself began to oxidize, shortening its lifetime. The oxidation duration was varied from 10 to 60 seconds, and 30 seconds emerged as the sweet spot, providing near-maximal conversion to iodine without prolonging each measurement or stressing the electrode at the high applied potential. The reduction current was tested between minus 3 and minus 10 microamperes, with minus 8 microamperes giving the strongest response. Even the carrier electrolyte, a mixture of 0.1 molar sulfuric acid and 0.001 molar hydrochloric acid, was scrutinized: hydrochloric acid concentrations spanning six orders of magnitude were evaluated, and the optimum sat at 0.001 molar, with higher concentrations showing no effect on the signal.

The metrological performance is impressive for such a simple setup. The method exhibits a linear range from 0.1 to 40 milligrams per liter with a coefficient of determination of 0.9993. The limit of detection, calculated by the IUPAC-recommended ULA 2 procedure from the lower part of the calibration curve, is 0.03 milligrams per liter, and the limit of quantification is 0.09 milligrams per liter. Repeatability, assessed from ten consecutive measurements of a 5-milligram-per-liter iodide standard, came in at 5.00 plus or minus 0.03 milligrams per liter, a relative standard deviation of just 0.54 percent. Reproducibility, verified in an external laboratory, yielded 4.9 plus or minus 0.1 milligrams per liter with a relative standard deviation of 1.1 percent, confirming that the method travels well beyond the developing lab.

Interference testing was thorough and revealing. Twelve potential interferents, including chloride, bromide, fluoride, sulfate, sulfite, ammonium, potassium, calcium, magnesium, aluminum, boron and iron species, were challenged against iodide at ratios from 1:1 up to 1:100, and for chloride all the way to 1:5000, a range chosen to bracket the chloride level of seawater. Most ions caused no measurable interference. Bromide produced a slight positive bias only at a 1:100 ratio, where the iodide signal rose by 9 percent, a consequence of bromide being co-oxidized to bromine, which is a stronger oxidant than iodine and further drives iodide conversion; such bromide levels are highly unlikely in real samples. Iron(III) was the one significant offender, cutting the iodide signal by 22 percent at a 1:50 ratio and eventually eliminating it, because its reduction overlaps the iodine reduction signal. Iron(II) behaves identically after being oxidized to iron(III) in the first step. Fortunately, this interference can be suppressed simply by passing the sample through a cation exchanger in the sodium cycle.

The real-sample results showcase the method’s practical reach. Bottled Slovak mineral waters Vincentka, Saratica and Cigelka, thermal and sulfur spring waters from Chorvatsky Grob and Dudince, Mediterranean seawater collected at Lloret de Mar in Spain, and iodized table salt were all analyzed after simple pretreatment, typically just boiling to remove bicarbonate. Iodide concentrations determined by calibration curve agreed closely with standard-addition results, passing a Student t-test at the 95 percent confidence level. Vincentka contained 4.6 milligrams per liter, Cigelka 0.78, the Chorvatsky Grob spring 0.16, and seawater 0.13 plus or minus 0.03 milligrams per liter, while the table salt held 25.1 milligrams per kilogram. In the two samples falling below the quantification limit, standard additions were recovered at 101 to 110 percent. With its robust, inexpensive porous carbon electrode, minimal reagent consumption, on-line sample handling capability and green analytical chemistry credentials, the method could readily extend to continuous process monitoring of water quality, offering laboratories a fast, low-cost alternative to chromatographic and spectrometric techniques.

Subject of Research: Electroanalytical determination of iodide in high-chloride water samples by flow-through coulometric titration

Article Title: Determination of iodides in water samples with high chloride content by in-built-electrode coulometric titration using a porous carbon electrode

Article References: Cacho, F., Masac, J., & Kudry, A. (2026). Determination of iodides in water samples with high chloride content by in-built-electrode coulometric titration using a porous carbon electrode. Results in Chemistry, 31, Article 103938. https://doi.org/10.1016/j.rechem.2026.103938

Image Credits: AI Generated

DOI: 10.1016/j.rechem.2026.103938

Keywords: iodide determination, coulometric titration, porous glassy carbon electrode, flow-through analysis, seawater analysis, chloride interference, electrochemistry, iodine deficiency, green analytical chemistry, mineral water, detection limit, WHO iodine intake

The historical setting is critical to the study’s power. In the late 1990s, Ethiopia sourced most of its iodized salt from Eritrea. When the border between the two countries closed in May 1998 amid escalating conflict, that supply line was severed, and iodized salt effectively disappeared from Ethiopian markets for an extended period. Because the disruption hit some areas and birth cohorts harder than others, it created a stark contrast between children who enjoyed months of exposure to iodized salt in utero and during infancy and those who had little or none. The researchers exploited this variation using an event-study design combined with difference-in-differences comparisons across space and time, a quasi-experimental approach that approximates the rigor of a randomized trial without exposing anyone to harm.

Iodine’s biological role explains why the timing of exposure matters so much. The thyroid gland concentrates iodine to synthesize the hormones thyroxine and triiodothyronine, which regulate basal metabolism and, crucially, drive fetal brain development. During pregnancy and early infancy, maternal thyroid hormones and the infant’s own emerging thyroid function govern neuronal migration, myelination, and synapse formation. Severe deficiency produces cretinism, but even moderate deficits impair cognition, hearing, and motor function. The World Health Organization has long endorsed universal salt iodization as one of the most cost-effective public health interventions available, yet coverage remains uneven globally, and programs that collapse can undo decades of progress.

To measure the consequences of Ethiopia’s supply shock, the team assembled an unusually rich set of data sources. They used the 2015/2016 Ethiopian National Micronutrient Survey to infer urinary iodine status among children and women of reproductive age, the 2000 and 2005 waves of the Ethiopia Demographic and Health Survey to analyze birthweight, child survival, and physical growth, and nearly two decades of records from the Ethiopian Higher Education Entrance Examination spanning 2003 to 2019 to assess academic achievement. A distinctive feature of the analysis was its integration of environmental geochemistry. Working with collaborators at Rothamsted Research and the University of Nottingham, the team mapped district-level soil and cereal grain concentrations of iodine and selenium across Ethiopia, allowing them to distinguish regions where diets naturally supply adequate iodine from regions wholly dependent on fortified salt.

The results on child survival are sobering. Rural children with fewer months of early-life exposure to iodized salt experienced excess mortality that emerged during infancy and persisted through early childhood. The pattern held in comparisons of birth cohorts born just before and just after the 1998 border closure, and the excess deaths were concentrated precisely where environmental iodine was lowest. This gradient is the study’s central strength: children living in districts with iodine-rich soils and crops had a physiological buffer against the loss of fortified salt, while children in iodine-poor districts bore the full brunt of the deficiency. Earlier intervention trials in severely deficient regions, including studies of oral iodine supplementation and iodinated irrigation water in China, had suggested that iodine could improve infant survival, but population-scale causal evidence of this kind has been scarce.

The educational findings extend the harm deep into adolescence. Students from rural cohorts with reduced early-life iodine exposure scored significantly lower on standardized secondary-school entrance examinations, with the deficit most pronounced in low-iodine districts. The dose-response relationship was graded and consistent: the more months of iodized salt a child’s first years encompassed, the better their later exam performance, and the effect strengthened with naturally low environmental iodine. Because the exams gate access to Ethiopian higher education, the measured deficits translate into lost opportunity at a formative juncture, suggesting that a temporary nutritional disruption in infancy imposes lifelong costs on human capital formation.

The methodological machinery behind these conclusions deserves attention. By modeling exam scores and mortality as event studies aligned by year of birth, the researchers could verify that outcomes diverged only for cohorts whose critical developmental windows overlapped the salt disruption, remaining flat for cohorts exposed before or after. Including selenium in the spatial analysis helped rule out confounding by correlated soil chemistry, and the team controlled for other shocks of the era, including the Ethiopian-Eritrean conflict, droughts, and changes in safety-net programs. All analysis code was released publicly on GitHub, and soil and grain nutrient data are archived in the Rothamsted Research repository, an unusually transparent package for a study of this scale.

The findings carry pointed lessons for policy. Salt iodization costs only a few cents per person per year, yet this study demonstrates that its absence is not a neutral state but an active harm, visible in death certificates and exam halls alike. Ethiopia itself illustrates both sides of the story: after the disruption, the country rebuilt its program through central iodized facilities, and coverage recovered substantially by the mid-2010s. But the episode reveals how fragile fortification systems can be when they depend on a single supply chain, and how quickly biological gains can reverse. The authors’ results align with a broader economics literature linking iodization to cognition and earnings in the United States, Switzerland, Tanzania, Denmark, and China, but they add a mortality dimension that those studies could rarely quantify.

For global health planners, the message is twofold. First, sustaining existing iodization programs matters as much as launching new ones, and supply chains deserve the same scrutiny as fortification standards. Second, environmental context should shape targeting: where soils are iodine-poor, populations have no dietary fallback, making uninterrupted fortification a matter of survival. As climate change, conflict, and trade disruptions increasingly stress food systems, Ethiopia’s experience stands as a warning written in the fates of two cohorts of children, and as proof that one of the cheapest interventions in public health is also one of the most consequential.

Subject of Research: Effects of disrupted salt iodization on child mortality and academic achievement in Ethiopia

Article Title: Loss of salt iodization harmed child survival and academic achievement in Ethiopia

Article References: Alemu, R., Tafere, K., Gashu, D., Joy, E. J. M., Bailey, E. H., Lark, R. M., Broadley, M. R., & Masters, W. A. (2026). Loss of salt iodization harmed child survival and academic achievement in Ethiopia. Nature Food. https://doi.org/10.1038/s43016-026-01408-y

Image Credits: AI Generated

DOI: 10.1038/s43016-026-01408-y

Keywords: iodine deficiency, salt iodization, Ethiopia, child mortality, cognitive development, micronutrients, public health, quasi-experimental study, school achievement, thyroid hormones, food fortification, environmental geochemistry

The interruption at the heart of the study was not a slow policy drift but a sudden break. For a period beginning in May 1998, iodized salt stopped flowing into Ethiopian households, meaning that iodine intake dropped back to whatever trace amounts occurred naturally in local foods and water. Because iodine concentrations in soil and crops vary dramatically across landscapes, this exposed children to a geographic lottery: in districts where environmental iodine was abundant, the consequences were muted; where soils and staple grains carried little iodine, children and pregnant women were effectively returned to a state of deficiency.

The biological stakes of iodine are well established. Iodine is an essential component of the thyroid hormones thyroxine and triiodothyronine, which regulate basal metabolism and, critically, drive brain development in the fetus and infant. Severe deficiency during pregnancy causes cretinism, marked by profound intellectual disability, while milder prenatal and early-childhood deficiency depresses intelligence quotient scores, school performance and even survival through mechanisms that include hypothyroidism and impaired immune function. Because the window of maximum vulnerability closes early—largely before a child enters school—deficiency during gestation and infancy inflicts losses that later nutrition cannot fully repair.

Against that backdrop, the Ethiopian interruption offered researchers a rare opportunity. Randomized trials that withhold iodine from pregnant women and children would be unethical, and many earlier studies of iodization relied on coarse baseline measures of deficiency, such as regional goiter rates recorded decades earlier. The Ethiopian case is different: the loss of iodized salt was sudden, affected the whole country, and coincided with rich new data on how much iodine naturally occurs in Ethiopian soils and grains. The study leverages the GeoNutrition survey work, published in Nature in 2021, which mapped the geospatial variability of nutritional quality in Ethiopian and Malawian cereals and provided a district-level measure of naturally occurring iodine.

The analytical strategy combined that environmental gradient with household and educational data spanning the interruption. Children who were in utero or in infancy when the iodized salt supply was severed could be compared with siblings and with cohorts born slightly earlier or later, and the severity of exposure could be calibrated by how iodine-poor their home district was. This design allows the researchers to separate the effect of iodine loss from the many other shocks—droughts, conflicts, economic fluctuations—that Ethiopia experienced during the same period.

The results were stark. The authors report a significant drop in child survival following the loss of iodized salt, and a parallel decline in academic achievement among affected cohorts, with both effects concentrated in rural districts with lower environmental iodine concentrations. In places where local foods provided a partial buffer, children fared comparatively better; where the environmental safety net was thin, the loss of fortification translated directly into biological harm. That gradient is important because it makes the causal interpretation far more difficult to dismiss: a purely coincidental shock, such as a regional famine or policy change unrelated to nutrition, would not be expected to track the geography of soil iodine so closely.

To probe that question further, the researchers ran placebo tests—analyses structured to detect effects where none should exist if iodine were the true mechanism. For example, they examined children whose ages meant they were not exposed during the critical developmental window, and districts where environmental iodine was plentiful. These tests confirmed that the losses were not driven by generic hardship but specifically by the absence of iodine during early life, strengthening the case that the interrupted fortification program itself caused the damage.

The findings resonate with a broader body of evidence assembled over decades. A randomized trial in Ethiopia by Mohammed, Marquis, Aboud, Bougma and Samuel, published in Maternal and Child Nutrition in 2020, showed that providing iodized salt to women before pregnancy improved children’s cognitive development—an in-country experimental counterpart to the new observational findings, demonstrating that restoring iodine early in life raises cognitive scores. Earlier work by Feyrer, Politi and Weil on the introduction of salt iodization in the United States documented large cognitive gains, though it relied on coarse baseline deficiency measures that limited precision. In Tanzania, Field, Robles and Torres showed that iodine deficiency depressed schooling attainment across Africa. And a 2021 review by Zimmermann and Andersson in the European Journal of Endocrinology documented that iodized salt coverage worldwide remains uneven and tenuous, with programs vulnerable to supply disruptions, regulatory lapses and declining political attention.

What the Ethiopian study adds is the reverse-direction evidence: not what is gained when iodization begins, but what is lost when it stops. This matters because salt iodization is often treated in global health as a solved problem. In reality, fortification programs depend on continuous supply chains, quality monitoring and enforcement, and the new results suggest that a single interruption lasting long enough to affect a birth cohort can impose lifelong costs in mortality and human capital. The magnitude of the educational losses implies economic consequences as well, since lower achievement translates into reduced productivity and earnings across the affected generation’s working lives.

For policymakers, the message is twofold. First, universal salt iodization programs deserve the same vigilance applied to vaccination campaigns: they must be monitored continuously, and disruptions must be treated as public health emergencies rather than logistical footnotes. Second, the environmental gradient in the findings underscores that fortification is not uniformly protective on its own; in regions where soil iodine is naturally scarce, food systems may need complementary strategies, including diversified fortification or targeted supplementation for women of reproductive age. The Ethiopian cohort that lost its iodized salt in 1998 cannot recover what was taken from it, but the evidence it generated makes a compelling case that the world’s remaining gaps in iodine coverage are not benign—and that closing them, and keeping them closed, is among the most cost-effective investments available in child health and education.

Subject of Research: The impact of interrupted salt iodization on child survival and educational outcomes in Ethiopia

Article Title: Interrupted salt iodization harmed child health and education in Ethiopia

Article References: Interrupted salt iodization harmed child health and education in Ethiopia. (2026). Nature Food. https://doi.org/10.1038/s43016-026-01415-z

Image Credits: AI Generated

DOI: 10.1038/s43016-026-01415-z

Keywords: salt iodization, iodine deficiency, Ethiopia, child mortality, academic achievement, micronutrients, thyroid hormones, nutrition policy, early childhood development, food fortification, environmental iodine, natural experiment