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Table 1 Geochemistry of groundwater in Mahomet aquifer wells

From: Functional microbial diversity explains groundwater chemistry in a pristine aquifer

Well

Temp. (°C)

pH

sp. Cond. (μS.cm-1)

[SO42-] (mM)a

[CH4]aq(μM)b

[H2]aq(nM)c

DIC (mM)d

DOC (mg.L-1)e

High sulfate (HS) wells

Chm94B

13.7

7.5

707

0.58

< 0.2

25

7.8

2.2

Chm96A

13.8

7.5

663

0.41

1

3

7.2

1.3

Frd94A

14.2

7.5

760

0.98

2

3

7.4

< 0.4

Iro95A

14.3

7.5

943

1.50

1

60

n/a

3.3

Iro96A

12.1

7.5

1254

4.23

1

n/a

n/a

n/a

Iro98B

13.0

7.6

1277

4.68

3

10

6.6

43.0

Iro98D

13.6

7.8

759

0.72

19

180

7.9

1.9

Ver94A

14.4

7.5

1279

4.57

2

n/a

6.7

1.8

Ver94B

13.7

7.3

1893

10.73

1

89

4.8

1.1

Low sulfate (LS) wells

Chm94A

14.1

7.6

651

0.07

4

n/a

8.0

3.6

Chm95A

14.0

7.6

649

0.14

8

4

7.7

2.1

Chm95B

13.8

7.9

670

0.04

30

3

7.9

2.0

Chm95C

13.7

7.7

601

0.11

3

20

6.6

0.5

Frd94B

15.4

7.6

611

0.05

43

9

7.4

< 0.4

Iro98C

13.3

7.4

664

0.04

15

66

7.6

2.3

Ver94C

13.6

7.7

616

0.23

3

46

7.4

1.1

Ver94D

13.9

7.7

621

0.18

10

n/a

7.7

0.8

Negligible sulfate (NS) wells

AnderN

14.8

7.6

617

0.02

91

144

6.6

n/a

AnderS

15.1

7.1

860

0.02

1237

175

25.9

n/a

CardiS

13.6

7.7

645

0.03

454

240

7.5

n/a

Chm95D

14.0

7.8

625

< 0.01

220

12

7.6

1.6

Chm98A

13.7

7.7

714

< 0.01

676

24

7.9

4.2

PklndE

14.6

7.6

678

0.03

221

63

8.7

n/a

PklndW

14.4

7.5

725

0.03

611

100

6.0

n/a

RailRd

14.4

7.7

661

0.02

106

50

6.4

n/a

  1. a The detection limit for sulfate is 0.01 mM.
  2. b The detection limit for dissolved methane is 0.2 μM.
  3. c The detection limit for dissolved hydrogen is 0.5 nM.
  4. d The detection limit for dissolved inorganic carbon is 0.5 mM.
  5. e The detection limit for dissolved organic carbon is 0.4 mg L–1.