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Marine Geochemistry - Laboratory Methods



Solubility of different evaporite minerals in pure water @ 25°C

all calculations with PHREEQC (Parkhurst & Appelo), version 2.12.5 (Nov 2005) PITZER dataset.

carbonate equilibria are calculated for a system open to ambient CO2 (pCO2 = 0.0003 ; log pCO2 = -3.52)

the column "@ seawater evaporation" gives the percentage of seawater you have to evaporate until this mineral starts precipitating

the column "sewater content" gives an approximate amount, that may be precipitated from 1 L of seawater

solubility
constant
molar
weight
solubility
@ 25°C
solubility
@ 25°C
equilibrium
pH
@ seawater
evaporation
seawater
content
NAME
composition
log(KT)
g/mol
mol/L
g/L
-log [H+]
%
g/L
kieserite
MgSO4·H2O
-0.12
138.39
6.251
865.0
4.83
99.0
2.2
halite
NaCl
1.57
58.443
6.100
356.5
6.38
90.6
28
sylvite
KCl
0.9
74.555
4.797
357.6
6.87
99.4
0.75
glauberite
Na2Ca(SO4)2
-5.25
278.19
0.426
118.7
7.16
92.4
1.4
anhydrite
CaSO4
-4.36
136.14
2.28·10-2
3.104
7.07
 
 
gypsum
CaSO4·2H2O
-4.58
172.18
1.52·10-2
2.617
7.06
71.0
1.6
celestite
SrSO4
-6.64
183.68
6.25·10-4
0.115
7.01
70.3
0.02
magnesite
MgCO3
-8.41
84.323
8.41·10-4
0.071
8.50
 
 
calcite
CaCO3
-8.41
100.09
5.21·10-4
0.052
8.31
 
 
dolomite
CaMg(CO3)2
-17.08
184.41
2.99·10-4
0.055
8.36
 
0.07

 

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