Table 2 The Baltic Sea sub-basins used to derive CO2 uptake rates from the atmosphere. Salinity, temperature, and TA data were taken from the BALTSEM model (see Methods)

From: Seafloor alkalinity enhancement as a carbon dioxide removal strategy in the Baltic Sea

Sub-basin

Area (km2)

Mud (km2)

Mean depth (m)

Mean S (-)

Mean T (oC)

TA (µmol kg−1)

pH

O2 (µmol kg−1)

CaCO3 added (Mt yr−1)

CO2 uptake (Mt yr−1)

CaCO3:CO2 (t t−1)

Kattegat (Katt)

22249

8500

24

26.4

7.7

2049

8.01

314

4.0

0.044

89.5

Danish Straits (DS)

19331

2300

15

16.6

7.4

1806

8.00

337

1.1

0.022

49.5

Baltic Proper (BP)

227568

74300

61

7.9

4.7

1576

7.90

378

34.7

1.524

22.7

Bothnian Sea (BS)

67001

8800

64

5.3

3.4

1261

7.90

401

4.1

0.341

12.0

Bothnian Bay (BB)

36559

13300

40

3.2

3.2

862

7.74

410

6.2

0.935

6.6

Gulf of Riga (GoR)

17509

8700

24

5.6

5.2

1884

8.07

383

4.1

0.120

33.7

Gulf of Finland (GoF)

23729

8800

33

5.7

4.5

1435

7.96

389

4.1

0.239

17.2

        

Total

58.2

3.23

 
  1. pH (total scale) was derived from TA assuming the equilibrium of the water boxes with the atmosphere (415 μatm). O2 concentrations denote solubilities at ambient S and T61. Seafloor areas are from Gustafsson et al.27. The CO2 uptake corresponds to the rate after 10 years of calcite addition.