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Table 1 Chemical and isotopic composition of the groundwaters. Concentrations of chemical elements and ions are given in mg L−1 except for Cs which is in μg L−1. The 18O/16O ratio (δ18O) is reported via the δ notation “per mil” as a deviation from the Standard Mean Ocean Water (SMOW)

From: Potential for hydrogen-oxidizing chemolithoautotrophic and diazotrophic populations to initiate biofilm formation in oligotrophic, deep terrestrial subsurface waters

 

KA2198Aa

KF0069A01b

Med

Min-max

Med

Min-max

pH

7.5

7.4–7.5

7.8

7.2–7.8

Na

1465

1430–1530

3085

3040–3130

Mg

138

121–148

32

31–32

K

40

32–42

14

13–16

Ca

189

186–269

3870

3760–3980

Cl

2780

2683–3050

13400

10810–14600

SO4 2−

280

280–337

673

637–703

DOC

6.4

6.4–6.4

bdc

bd–bd

HCO3

212

202–220

6.5

5.5–6.8

δ18O

−7.5

−7.8 to −7.4

−12.4

−12.4 to −12.4

Fe-total

1.7

1.5–1.7

0.037

0.011–0.063

Fe2+

1.6

1.2–1.7

0.06

db–0.06

Mn

0.71

0.70–0.97

0.23

0.23–0.23

HS

0.05

0.01–0.08

0.01

bd–0.07

NH4 +_N

2.4

2.3–3.1

0.01

0.01–0.02

PO4 3−_P

0.0071

0.0006–0.0136

bd

bd–bd

NO3

bd

bd–bd

bd

bd–bd

NO2

0.00055

0.0005–0.0006

bd

bd–bd

Cs

4.6

4.5–4.8

4.2

4.2–4.2

  1. a1–8 measurements in 2002–2009
  2. b1–15 measurements in 2003–2008
  3. cbd, below detection limit