Table 1 Trace element contents in the bottom sediments of the Bratsk Reservoir, versus their content in the natural environment of the Baikal region, as well as calculated anomaly ratio (AR).

From: Composition and physico-chemical properties of bottom sediments in the southern part of the Bratsk Reservoir (Russia)

Element

Content [ppm]

Percentage abundance in the Earth’s crust42 [ppm]

Average content in the natural environment of the Baikal region [ppm]

AR

average

max

min

bedrock22,39

deep (abyssal) silt of Lake Baikal40,41

Be

1.30

2.00

0.80

2.10

2.0

0.63

Co

18.10

28.00

12.20

17.30

9.0

19.00

2.01

Cr

95.30

176.00

45.10

92.00

80.0

120.00

1.19

Cs

2.70

5.00

1.11

4.90

6.2

5.00

0.44

Cu

31.30

44.00

15.70

28.00

29.0

1.08

La

28.30

41.90

14.30

31.00

35.2

58.00

0.80

Mn

717.60

1200.00

424.00

1000.00

685.0

945.00

1.05

Mo

0.80

2.09

0.35

1.10

8.3

1.40

0.10

Ni

68.00

97.00

45.30

47.00

32.0

84.00

2.12

Pb

13.80

19.00

8.18

17.00

11.0

19.00

1.25

Rb

42.60

100.00

16.00

84.00

42.80

80.00

1.00

Sc

10.70

20.30

4.70

14.00

11.00

13.00

0.97

Sr

140.40

250.00

45.00

320.00

210.0

320.00

0.67

Th

5.70

8.90

1.20

10.50

3.8

10.00

1.49

V

83.90

138.00

49.00

97.00

62.0

160.00

1.35

Y

18.00

29.00

11.50

21.00

22.5

0.8

Zn

89.50

108.00

62.80

67.00

41.0

88.00

2.18

  1. Explanation: (−) – data is not available.