An extensive H-3-He-3 study was performed to determine detailed characteris
tics of a regional flow system and a sewage plume over a distance of 4 km i
n a sand and gravel aquifer at Otis Air Base in Falmouth, Massachusetts, H-
3-He-3 ages increase with depth in individual piezometer clusters and with
distance along flowpaths, However, the age gradient with depth (Delta t/Del
ta z) is smaller in the plume than that in the regional waters, due to the
intense recharge in the infiltration beds, The 1960s bomb peak of tritium i
n precipitation is archived longitudinally along a flowline through the mai
n axis of the plume and vertically in individual piezometer clusters, On th
e eastern side of the sampling area, where water from Ashumet Pond forces p
lume water deeper into the flow system, H-3-He-3 ages are young at depth be
cause the H-3-He-3 "clock" is reset due to ontgassing of helium in the pond
. A reconstruction of the tritium input functions for the regional and plum
e samples shows that there is no offset in the peak [H-3] + [He-3(trit)] co
ncentrations for the plume and regional water, indicating that the water fr
om supply wells for use on the base is young. The H-3-He-3 ages and deterge
nt concentrations in individual wells are consistent with the beginning of
use of detergents and the time period when their concentrations in sewage w
ould have been greatest. Ages and hydraulic properties calculated using the
H-3-He-3 data compare well with those from previous investigations and fro
m particle-tracking simulations.