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Geochemical Study Reveals Dirty, Organics-Laden Water in Pompeii's Early Baths

Chemical crusts show scarce well water kept basins stale, then record aqueduct upgrades that increased supply at the cost of higher metal levels.

Overview

  • Researchers from the University of Mainz analyzed calcium‑carbonate deposits from Pompeii’s water system, with findings published in PNAS in January 2026.
  • The deposits indicate bathwater in republican-era facilities contained bath oils, sweat and urine, pointing to very dirty conditions and likely high bacterial loads.
  • Slave‑driven treadwheel pumps lifted only about 1,000 liters of fresh groundwater per day, often insufficient for even one complete daily water change.
  • Later modernization, including the Serino aqueduct and new kettles and pipes, boosted water availability and warmth but introduced lead, zinc and copper into the system.
  • Cyclical chemical patterns in the calcite may reflect fluctuating volcanic CO2 in groundwater before the 79 CE eruption, a tentative interpretation offered by the authors.