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Components of the thermal water from the Kochbrunnen spring

 

Temperature: 65.8°C

PH: 6.35/ 50°C

Radon 0.62nCi/l corresponding to 1.7 M.E.

 

 

Components: Sodium-Chloride spring

 

 

Cations:

Milligramme

Mval    

Mval %

Lithium  ions (Li+)

4.13

0.5970

 0.43

Sodium ions (NA+)

2633

114.5

 82.35

Potassium ions (K+)

87.5

2.237

 1.61

Rubidium ions (Rb+)

0.52

0.0061

 0.004

Caesium ions (Cs+)

0.32

0.0024

 0.002

Ammonium ions (NH4+)

5.41

0.2999

 0.22

Magnesium ions (Mg2+)

46.8

3.850

 2.77

Calcium ions (Ca2+)

342.3

17.08

 12.28

Strontium ions (Sr2+)

14.1

0.3218

 0.23

Barium ions (Ba2+)

0.85

0.0124

 0.009

Aluminium ions (Al3+)

0.026

0.0029

 0.002

Manganese (II) ions (Mn2+)

0.70

 0.0255

 0.018

Iron (II) ions (Fe2+)

2.83

 0.1013

 0.073

Nickel ions (Ni2+)

0.003

 0.0001

 -

Copper ions (Cu2+)

0.002

 0.00006

 -

Silver ions (Ag+)

0.003

 0.00003

 -

Zinc ions (Zn2+)

0.014

 0.0004

 -

Lead ions (Pb2+)

0.006

 0.00006

 -

Tin ions (Sn2+)

0.006

 0.0001

 -

 

 

 139.04

 100.00

 

 

Anions:

 

 

 

Flouride ions (F-)

0.54

0.0284

0.020

Chloride ions (Cl-)

4540

128.1

92.13

Bromide ions (Br-)

3.64

0.0455

0.033

Iodine ions (J-)

0.095

0.00075

0.001

Sulphate ions (SO42-)

65.2

1.357

0.98

Nitrate ions (NO3-)

0.58

0.0094

0.007

Hydrogen phosphate ions (HPO42-)

0.04

0.0008

0.001

Hydrogen arsenate ions (HA2O42-)

0.14

0.0020

0.001

Hydrogen carbonate ions (HCO3-)

579.7

9.50

6.83

 

8329

139.04

100.00

  

 

Undissociated components

 

Millimole

 

Silicic acid (metal) (H2SiO3)

73.5

0.9411

 

Titanic acid (metal) (H2Ti3)

0.005

0.005

 

Boric acid (metal) (HBO2)

3.94

0.0899

 

 

8406

 

 

 

 

Gaseous components

 

 

 

Free carbon dioxide (CO2)+

332

7.54

 

 

8738

 

 

 

Traces are also present of: Germanium (Ge4+) some 0.0002 mg/kg. Molybdenium (Mo4+) some 0.0009 mg/kg. Hydrogen sulphide (HS) (H2S) some 0.005 mg/kg.

No trace was found of Nitrate ions (NO2-) corresponds to 168 ml at 0°C and 760 Torr).





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