Table 1 Pre-injection conditions, elemental concentrations (from Alfredsson et al.7) and Ca isotope ratios

From: Rapid CO2 mineralisation into calcite at the CarbFix storage site quantified using calcium isotopes

Borehole

Sample

Sampling date

Depth

T (°C)

pH

Na (μg/ml)

Si (μg/ml)

Ca (μg/ml)

Sr (ng/ml)

Li (ng/ml)

Calcite SI

δ44/40Ca

2 s.e.

HK-7b

08HAA08

08/07/2008

Shallow

12.4

7.65

9.17

12.0

11.3

20.1

 

−1.13

  

HN-4

08HAA01

01/07/2008

Deep

32.3

9.43

48.6

25.1

1.64

1.62

0.40

0.12

1.95

0.05

HK-34

08HAA03

04/07/2008

Deep

25

9.63

49.6

22.7

2.17

3.98

    

HK-31

08HAA05

04/07/2008

Deep

17.4

9.29

41.8

20.7

3.75

11.9

0.31

0.29

2.04

0.04

HK-26

08HAA06

04/07/2008

Deep

18.8

8.44

72.5

17.8

5.72

28.3

    

HK-26

09HAA17

29/05/2009

Deep

16.5

8.51

77.0

16.7

5.36

26.5

0.59

0.02

1.22

0.05

HK-12

09HAA18

29/05/2009

Shallow

5.3

8.33

8.82

8.63

8.39

14.8

0.16

−0.78

1.11

0.05

HK-31

09HAA19

29/05/2009

Deep

18.9

9.41

48.6

21.1

3.69

11.9

0.44

0.37

1.91

0.05

HK-25

09HAA20

29/05/2009

Shallow

7.4

8.09

8.00

9.0

8.02

13.9

0.28

−1.00

1.09

0.04

HK-34

09HAA21

29/05/2009

Deep

27.5

9.79

55.0

24.6

1.30

1.74

0.23

0.15

2.04

0.03

rpt

           

1.98

0.06

HK-7b

09HAA22

29/05/2009

Shallow

11.7

7.67

12.2

13.0

21.7

38.9

0.31

−0.50

1.14

0.03

HN-1

09HAA23

29/05/2009

Deep

24.7

9.26

43.5

14.1

5.37

18.1

0.16

0.51

2.07

0.04

HN-4

09HAA24

05/06/2009

Deep

34.5

9.56

55.6

25.2

1.32

1.27

0.27

0.10

1.89

0.04

HK-26

10HAA26

25/06/2010

Deep

17.2

8.65

74.5

16.6

5.25

26.1

0.32

0.05

1.62

0.04

HK-31

10HAA28

25/06/2010

Deep

16.9

9.55

48.6

23.1

3.61

12.0

0.41

0.42

1.91

0.06

HN-4

10HAA29

25/06/2010

Deep

30.4

9.69

54.7

30.6

1.29

1.14

    

HK-34

10HAA30

25/06/2010

Deep

28.0

9.88

51.0

27.1

1.21

1.67

0.24

0.03

1.75

0.03

  1. Borehole names are the same as in Figs. S1–3. The shallow wells, HK-7b, HK-12, and HK-25, draw water from the dominate aquifers in the upper system, whereas the deeper wells, HN-2, HN-4, HK-34, HN-1, HK-31, and HK-26, draw water from the highest discharge aquifers below 400 m since these wells are cased down to that depth7