Table 1 Saturation index (SI) values simulated at the final concentration factor (CF) obtained in MAC tests performed at different temperatures for the synthetic hypersaline solution before (Syn) and after (BT) the basic treatment (numbers in bold are referred to the species that were actually detected in the solid precipitate by PXRD analysis)

From: Turning mine-tailing streams into sources of water and mineral salts in a membrane-sustained circular scenario

Phase

Formula

Saturation Index

31 °C

44 °C

49 °C

Syn.(a)

BT(b)

Syn.(a)

BT(b)

Syn.(c)

BT(d)

Huntite

CaMg3(CO3)4

6.40

–

6.98

–

7.26

–

Gorgeyite

K2Ca5(SO4)6·H2O

4.69

–

3.74

–

4.54

–

Dolomite

CaMg(CO3)2

3.98

–

4.17

–

4.24

–

Magnesite

MgCO3

1.91

1.93

1.84

1.86

1.84

1.86

Calcite

CaCO3

1.15

–

1.20

–

1.19

–

Aragonite

CaCO3

0.95

–

0.97

–

0.94

–

Anhydrite

CaSO4

0.26

–

0.33

–

0.56

–

Gypsum

CaSO4·2H2O

0.23

–

0.15

–

0.28

–

Halite

NaCl

0.11

0.20

0.08

0.17

0.26

0.37

Sylvite

KCl

−0.37

−0.29

−0.48

−0.40

−0.37

−0.29

Glauberite

Na2Ca(SO4)2

−0.37

–

−0.35

–

0.07

–

Artinite

Mg2CO3(OH)2·3H2O

−1.04

−1.18

−0.44

−0.59

−0.55

−0.74

Thenardite

Na2SO4

–

−1.23

-–

−1.20

–

−0.96

Polyhalite

K2MgCa2(SO4)4·2H2O

−1.31

–

−1.70

–

−1.12

–

Epsomite

MgSO4·7H2O

–

−1.86

–

−2.07

–

−2.05

Hexahydrite

MgSO4·6H2O

–

−1.91

–

−2.02

–

−1.93

Arcanite

K2SO4

−2.11

−2.00

−2.25

−2.14

−2.19

−2.07

Pentahydrite

MgSO4·5H2O

−2.18

−2.05

−2.32

−2.19

−2.23

−2.08

Kainite

KMgClSO4·3H2O

−2.37

−2.14

−2.51

−2.28

−2.23

−1.97

Kieserite

MgSO4·H2O

−2.48

−2.29

−2.36

−2.18

−2.06

−1.85

Bloedite

Na2Mg(SO4)2·4H2O

−2.68

−2.37

−2.85

−2.56

−2.54

−2.21

CF: (a) 1.44, (b) 1.50, (c) 1.57, (d) 1.71