For hundreds of years, the Anio Novus aqueduct carried water 87 km (54 miles) from the Aniene River of the Apennine Mountains down into Rome. Built between AD 38 and 52, scholars continue to struggle to determine how much water the Anio Novus supplied to the Eternal City—until now.
By studying limestone deposits that formed from the flowing water within the aqueduct, called travertine, University of Illinois at Urbana-Champaign researchers reported in the Journal of Archaeological Science an actual estimate for the aqueduct’s flow rate of 1.4 m^3/s (± 0.4).
“At this rate, the aqueduct would have supplied the city with 370 gallons of water each second,” said lead author Bruce Fouke, a professor of geology and microbiology and a member of the Carl R. Woese Institute for Genomic Biology at Illinois. “That’s enough water, per second, to take a three-hour shower or to take 7 baths.”
This buildup of travertine within the aqueduct channel indicates the average water level, called the wetted perimeter. According to the wetted perimeter near Roma Vecchia, where the ancient Anio Novus aqueduct and travertine are well preserved, the aqueduct was almost always full of water.
Still, their estimate is significantly lower than previous estimates, which did not account for the travertine. They found that even a small amount of travertine deposit served to significantly reduce the water flow by 25 percent.
Former estimates have tried to reconcile flow rates recorded in AD 97 by Rome’s water commissioner Sextus Julius Frontinus in his classic text entitled De Aquis. “We believe his data should not be used, considering he did not have the means to accurately measure water flux and flow velocity,” Fouke said. “Furthermore, Frontinus’ data contained many discrepancies, which he blamed on measurement error, water theft and fraud in his water department.”