Organic Carbon Inputs from Lakes and Septic Systems Increase Manganese Exposure Risk in Lakeside Private Wells

Abstract Groundwater manganese (Mn) contamination is a growing global health concern increasingly associated with adverse neurotoxic effects. We investigated the processes controlling Mn release into groundwater in two lake catchments spanning sewered and unsewered residential developments using a multitracer approach integrating hydrogeochemistry, stable isotopes (δ18O, δ2H), and artificial sweeteners as wastewater tracers in 50 private wells. Manganese exceeded the 0.12 mg L–1 health standard in 50% of wells, nearly double the regional average, and in almost all wells (92%) under suboxic–reducing conditions. Elevated Mn concentrations strongly correlated with dissolved organic carbon (DOC), supporting DOC-driven Mn mobilization. Isotopic signatures in nearshore wells indicated lake–groundwater mixing, suggesting a role for lake-derived carbon in Mn mobilization, while littoral sediment porewaters represent a potential groundwater Mn source. Using a novel application of artificial sweeteners, we fingerprint wastewater-derived organic carbon as an overlooked anthropogenic driver of Mn release to groundwater. Artificial sweeteners were detected in 85% of wells, particularly in unsewered areas, and positively correlated with Mn and DOC. Collectively, these findings reveal coupled hydrogeological, biogeochemical, and anthropogenic controls on groundwater quality and underscore the need to account for domestic wastewater inputs and lake water mixing as drivers of Mn contamination in vulnerable residential developments.

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Publication Details

Journal
ACS ES&T Water
Published
2026-10-20
DOI
https://doi.org/10.1021/acsestwater.6c00435
Primary Topic
Groundwater and Isotope Geochemistry
Type
article
Field-Weighted Citation Impact
0.00
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article

Organic Carbon Inputs from Lakes and Septic Systems Increase Manganese Exposure Risk in Lakeside Private Wells

Debra M. Hausladen, James W. Roy, Md. Muhyminul Islam, Janie Masse-Dufresne
ACS ES&T Water
Groundwater and Isotope Geochemistry
article

Organic Carbon Inputs from Lakes and Septic Systems Increase Manganese Exposure Risk in Lakeside Private Wells

Debra M. Hausladen, James W. Roy, Md. Muhyminul Islam, Janie Masse-Dufresne
article en

Abstract

Abstract Groundwater manganese (Mn) contamination is a growing global health concern increasingly associated with adverse neurotoxic effects. We investigated the processes controlling Mn release into groundwater in two lake catchments spanning sewered and unsewered residential developments using a multitracer approach integrating hydrogeochemistry, stable isotopes (δ18O, δ2H), and artificial sweeteners as wastewater tracers in 50 private wells. Manganese exceeded the 0.12 mg L–1 health standard in 50% of wells, nearly double the regional average, and in almost all wells (92%) under suboxic–reducing conditions. Elevated Mn concentrations strongly correlated with dissolved organic carbon (DOC), supporting DOC-driven Mn mobilization. Isotopic signatures in nearshore wells indicated lake–groundwater mixing, suggesting a role for lake-derived carbon in Mn mobilization, while littoral sediment porewaters represent a potential groundwater Mn source. Using a novel application of artificial sweeteners, we fingerprint wastewater-derived organic carbon as an overlooked anthropogenic driver of Mn release to groundwater. Artificial sweeteners were detected in 85% of wells, particularly in unsewered areas, and positively correlated with Mn and DOC. Collectively, these findings reveal coupled hydrogeological, biogeochemical, and anthropogenic controls on groundwater quality and underscore the need to account for domestic wastewater inputs and lake water mixing as drivers of Mn contamination in vulnerable residential developments.

ACS ES&T Water
Western University (CA), Environment and Climate Change Canada (CA), Université de Sherbrooke (CA), Imam Sadiq University (IR), Université Laval (CA), École de Technologie Supérieure (CA)
Openalex Percentile: Top 17%
Groundwater and Isotope Geochemistry
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