DISTRIBUTION OF HELIUM AND TRITIUM IN LAKE-BAIKAL

The H-3-He-3 age of a water mass is a measure of the time that has pas sed since the water mass was last in contact with the atmosphere. Betw een 1992 and 1995 a detailed study of H-3-He-3 ages was conducted in L ake Baikal, the deepest and largest lake by volume on Earth, to invest igate deep water renewal in its three major basins. Maximum H-3-He-3 a ges are 14-17 years in the southern basin, 16-18 years in the central basin, and 10-11 years in the northern basin. Rates of renewal of deep water with surface water, deduced from volume-weighted mean H-3-He-3 ages below 250 m depth, are about 10% yr(-1) in the southern and centr al basins and 15% yr(-1) in the northern basin. In the southern basin the mean H-3-He-3 age below 250 m depth increased steadily from 9.6 ye ars in 1992 to 11 years in 1995, indicating a slight diminution in dee p water renewal during this time. Bottom water renewal by large-scale advection was estimated from the mass balance of He-3 in the 200 m thi ck bottom layer of each basin. Bottom water renewal rates in the north ern basin were found to be between 80 and 150 km(3) yr(-1) and in the central basin between 10 and 20 km(3) yr(-1), whereas in the southern basin they were practically zero. Correlating oxygen and dissolved hel ium-4 concentrations with H-3-He-3 age allowed us to determine the mea n hypolimnetic oxygen depletion rate in the water column (4.5 mu mol L -1 yr(-1)), as well as mean helium fluxes from the lake bottom (2.8x10 (11) atoms m(-2) s(-1) in the northern basin, and 1.3x10(11) atoms m(- 2) s(-1) in the central and southern basins). The helium isotope ratio of the terrigenic helium component injected from the lake bottom, det ermined from measurements of water from hydrothermal springs in the vi cinity of the lake, was found to be similar to 2.2 x 10(-7).