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Table A1 Chemical characteristics of natural waters

From: Aqueous solutions

Environment

pH range

Eh range (V)

Major ions (in order of abundance)

Dissolved organic carbon (mg/l)

Rainwater

    

 Continental

4–6

Oxic

SO2− 4, Ca2+, Cl− NO− 3, Na+, K+, NH+ 4, Mg2+

?

 Marine and coastal

5–6

Oxic

Cl−, Na+, SO2− 4, Mg2+, Ca2+, K+, NO− 3, NH+ 4

?

Rivers

5–9

0.3–0.5

HCO− 3, Ca2+, H4SiO4, SO2− 4, Cl−, Na+, Mg2+, K+

<1–>30

Lakes

    

 Fresh

5–9

−0.1–0.5

HCO− 3, Ca+ 2, H4SiO4, SO2− 4, Cl−, Na+, Mg2+, K+

<1–>100

 Saline

5–10

−0.1–0.5

Cl−, Na+, SO2− 4, HCO− 3, Mg2+, K+, Ca+ 2, H4SiO4

<1–>100

Shallow groundwater

6–8.5

−0.1–0.45

HCO− 3, SO2− 4, Ca2+ Na+, Cl−, Mg2+, K+, Ca2+,H4SiO4, K+

<1–20

Marine

7.5–8.4

0.2–0.4

Cl−, Na+, SO2− 4, Mg2+, Ca2+, K+

<0.1–3

Evaporative marine

7.5–9.0

Oxic or anoxic

As for marine then inc. Mg2+ with mineral ppt.

?

Brackish marine

7.5–8.4

Oxic or anoxic

As for marine

?

Deep connate groundwater

6.0–8.0

−0.25–0.4

Cl−, Na+, K+, SO2− 4, Ca2+, Mg2+,

<10–4500

  1. Data from Baas-Becking et al., 1960; Berner and Berner, 1987; Boggs, 1992; Collins, 1975; Millero and Schreiber, 1982.