Table 4 Groundwater compositions of seawater, rivers, mid-ocean ridges (MORs), groundwater archetypes

From: Large-scale groundwater flow and sedimentary diagenesis in continental shelves influence marine chemical budgets

CONCENTRATIONS (mmol/L)

Ca2+

K+

Mg2+

Na+

Cl−

Source(s)

Seawater

10.3

10.3

53.4

47.0

547

6

Groundwater archetypes

Cold seeps

34.2

66.0

28.2

2640

2890

24,26,52

Clastic-derived

30.0

5.23

18.7

366

448

53,54

Deep CaCl2 brines

1130

212

275

2100

5130

28a

Carbonate-derived

34.3

23.3

101

1160

1310

56

Modified concentrations

Modified cold seeps

−3.82

2.21

−48.0

31.2

0

-

Modified clastic-derived

26.0

−3.76

−29.7

−21.6

0

-

Modified deep CaCl2 brines

110

12.3

−23.9

−246

0

-

Modified carbonate-derived

4.03

−0.574

−11.0

14.9

0

-

Modified MORs

28.9

28.1

−52.7

−39.5

0

6

Modified rivers

0.329

0.033

0.122

0.085

0

6

  1. aTable 8.
  2. Modified concentrations have been normalized relative to modern seawater to indicate net contributions to seawater chemistry (see Section 4.4 and Supplementary Table 1 for methods).