Hidden Hexavalent Chromium in Turkish Mining Waters Exposes Flaw in Standard Water Testing

In the mountainous watersheds of eastern Türkiye, where ancient ocean floor rocks have been thrust skyward and mined for their chromium riches, an invisible chemical drama is unfolding in the rivers and streams. A new study from Munzur University, published in Environmental Geochemistry and Health, reveals that the way scientists and regulators routinely measure chromium in water may be hiding the most dangerous form of the metal from view. By tracking two chemically distinct species of chromium across 28 sampling stations in the Pülümür and Ovacık regions of the Eastern Anatolia Basin between March 2025 and February 2026, the research team has delivered one of the most detailed portraits yet of how this notorious contaminant moves through a mining-influenced landscape, and why total chromium measurements alone can paint a misleading picture of risk.

Chromium is a metal of two faces. In its trivalent form, Cr(III), it is a trace nutrient that humans actually require for glucose metabolism, and it tends to bind tightly to soils and sediments, staying put in the environment. In its hexavalent form, Cr(VI), it is something altogether more sinister: a mobile, highly soluble oxidized anion that is classified as a human carcinogen when inhaled and is associated with serious toxic effects when ingested. The difference between these two species is a matter of a few electrons, but that small electrochemical gap separates an essential nutrient from a poison. Yet most environmental monitoring programs around the world still report only total chromium, a single number that lumps the benign and the hazardous together as if they were the same substance.

The research team, led by Banu Kutlu together with Tarık Baydar, Vesile Yıldırım and Zekeriya Konurhan, set out to test whether species-specific measurements provide genuinely additional information beyond that operational total. Their study area is geologically primed for chromium chemistry. The region sits within the Tunceli Ophiolite, a slab of depleted mantle peridotite hosting chromitite deposits, the kind of ultramafic rock that contains abundant chromium-bearing minerals such as chromite. When these rocks weather naturally, chromium can be released into water, and under the right geochemical conditions, manganese oxides and other oxidants can convert the relatively harmless Cr(III) into the hazardous Cr(VI). This means that in ultramafic terrain, hexavalent chromium is not exclusively an industrial artifact; it can be geogenic, produced by the slow chemistry of rock and water long before any mine arrived.

To disentangle these influences, the researchers collected surface-water samples across the watershed for a full year and measured Cr(III) and Cr(VI) separately using species-specific UV–Visible spectrophotometric methods. The operational total chromium was then defined as the sum of the two separately measured species, a calculated value rather than an independently measured total. The results spanned an enormous range: from below the detection limit up to 578.13 micrograms per liter. For context, the World Health Organization guideline for total chromium in drinking water is 50 micrograms per liter, and the calculated total exceeded that screening benchmark at 14 of the 28 stations. That figure alone is striking, but the species-level data told a far more nuanced story.

Cr(III) predominated throughout most of the watershed, consistent with the reducing, mineral-rich conditions that favor the trivalent form. The highest Cr(VI) concentration occurred at a single localized hotspot, a concentrated pocket of the oxidized species rather than a watershed-wide plume. Yet here lies the study’s central warning: when the team screened the data against Cr(VI)-specific thresholds under an assumed scenario of untreated drinking-water ingestion, multiple stations exceeded those screening levels. In other words, a watershed could pass a total chromium test at some locations while still harboring concentrations of the carcinogenic species that warrant attention. Operational total chromium, the study concludes, did not consistently identify the spatial distribution of Cr(VI)-related potential risk.

The health-risk dimension of the work adds another layer of urgency. Using both deterministic calculations and an empirical bootstrap approach, a probabilistic method that resamples the data thousands of times to capture uncertainty, the team estimated screening-level hazard quotients for adults and children consuming the water untreated. The estimates were consistently higher for children than for adults, a familiar pattern in risk assessment that reflects children’s higher water intake relative to body weight and their greater susceptibility to early-life exposures, a principle the U.S. Environmental Protection Agency has formalized in its guidance on early-life susceptibility to carcinogens. Importantly, the researchers are careful about what their numbers do and do not show: direct untreated consumption of the sampled surface waters was not verified, so the results are screening-level indications of potential risk rather than confirmed exposures.

The mineralogical arm of the investigation brought the rocks themselves into the courtroom. Using X-ray diffraction to identify crystalline phases, scanning electron microscopy with energy-dispersive spectroscopy to examine mineral chemistry at microscopic scales, and Fourier-transform infrared spectroscopy to probe molecular structures, the team characterized the solid phases that control chromium’s fate. These techniques matter because chromium mobility in water is governed by which minerals are dissolving, which surfaces are adsorbing the metal, and which oxidants such as iron-manganese nodules are available to catalyze the conversion of Cr(III) to Cr(VI). Multivariate statistical analyses of the hydrochemical data were then used to trace the fingerprints of different water sources and processes across the watershed.

One of the study’s most honest findings is what it could not determine. Mining-influenced stations generally exhibited higher chromium concentrations than their counterparts elsewhere in the watershed, suggesting that mining activity does contribute to mobilization. But the relative contributions of natural geogenic weathering and mining-related mobilization could not be quantitatively apportioned. This is a genuinely difficult problem in ultramafic terrain, where the ore being mined and the bedrock being weathered are chemically similar, and it underscores why isotopic tracing and other advanced source-apportionment tools remain critical for future work in such settings.

The broader implications reach far beyond eastern Türkiye. Ophiolite belts and ultramafic landscapes ring the Mediterranean, the Balkans, the Middle East and beyond, and natural hexavalent chromium in groundwater interacting with such rocks has been documented from Greece to California. In chromite mining regions, communities often depend on local water supplies, and reviews of drinking-water quality in mining areas have repeatedly flagged heavy-metal contamination as a public health concern. If monitoring programs in these regions rely on total chromium alone, they may systematically miss the spatial pattern of the species that matters most for human health, or conversely, they may raise alarms over stations where the chromium is almost entirely the benign trivalent form.

The message of this study is ultimately a call for smarter measurement. Chromium speciation, the researchers conclude, provided additional environmentally and toxicologically relevant information beyond operational total chromium for evaluating chromium mobility and screening-level potential human health risks in this ultramafic watershed. As analytical methods for species-specific determination become more accessible and validated, the case for building speciation into routine monitoring grows stronger. For the communities living along the rivers of the Pülümür and Ovacık regions, and for millions of others downstream of the world’s ultramafic and mining landscapes, the difference between counting all chromium and counting the right chromium could one day prove decisive for public health.

Subject of Research: Chromium speciation and human health risks in surface waters of an ultramafic mining watershed

Article Title: Hydrogeochemical controls on chromium speciation and potential human health risks in surface waters of an ultramafic mining watershed

Article References: Kutlu, B., Baydar, T., Yıldırım, V., & Konurhan, Z. (2026). Hydrogeochemical controls on chromium speciation and potential human health risks in surface waters of an ultramafic mining watershed. Environmental Geochemistry and Health, 48(14), Article 562. https://doi.org/10.1007/s10653-026-03456-6

Image Credits: AI Generated

DOI: 10.1007/s10653-026-03456-6

Keywords: chromium speciation, Cr(VI), Cr(III), ultramafic rocks, mining watershed, surface water, heavy metal contamination, human health risk assessment, drinking water quality, geogenic chromium, Eastern Anatolia, Environmental Geochemistry and Health