There are two types of lakes in the vicinity of the nuclear fuel cycle faci
lities in Rokkasho-mura. One is a brackish lake, Obuchinuma Lake, and the o
ther is a freshwater lake, Takahokonuma Lake. Tritium concentrations in Obu
chinuma Lake had a good negative correlation with salinity at any sampling
point and period. We consider that the water of Obuchinuma Lake has been on
ly slightly influenced by precipitation depending on the ratio of seawater
and river water of the Futamata River. Tritium concentrations in Takahokonu
ma Lake ranged from 0.6 to 1.5 Bq.l(-1), and were higher than that in preci
pitation in Rokkasho-mura. Tritium concentration in rivers flowing into the
lakes ranged from 0.7 to 2 Bq.l(-1). and were higher than that in the prec
ipitation. It is assumed that ground waters with higher levels of tritium i
nflow into the rivers.