A hydrochemical investigation was carried out on eight small High Tatr
a mountain lakes (Poland). When comparing recent data with those from
the period 1935-1965, a constant process of acidification of the lakes
is found. The average pH of precipitation is 4.8 in the study area, b
ut the lakes are in two stages of acidification: weak (pH 6.0-6.5) and
intermediate (pH 5.5-5.8). The differences are due to differences in
water sources.