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Table 4 Chemical analysis and saturation indices of groundwater in the urban area and the wilderness area around the Open-Air Museum (mg/L)

From: Urban sprawl analysis of Akhmim city (Egypt) and its risk to buried heritage sites: insights from geochemistry and geospatial analysis

Sample

1

2

3

4

5

Latitude

26°33′57.83ʺN

26°33′27.82ʺN

26°34′3.71ʺN

26°34′17.63ʺN

26°33′29.713ʺN

longitude

31°44′46.16ʺE

31°44′34.53ʺE

31°44′37.17ʺE

31°45′35.26ʺE

31°43′25.385ʺE

Class

Urban area

Urban area

Urban area

Wilderness area

Wilderness area

TDS

993

889

959

408

438

HCO3

384

444

383

251

278

NH3

14

0.01

0.01

22.5

14.51

Ca

77.15

59.83

72.45

52.29

57.06

K

4

8

6

7

3

Mg

31

17.7

19.07

21

22

Na

188

200

183

42

50

Cl

134.0

113.32

122.52

27.48

34

NO3

18.23

7.72

125.8

0.21

1.14

So4

166

119.8

94.61

39

42

PO4

 < 0.2

 < 0.2

 < 0.2

3.4

0.22

Saturation index (SI)*

Dolomite

− 8.07

− 9.18

− 8.48

− 10.30

− 9.84

Calcite

1.24

0.96

1.15

0.83

0.90

Aragonite

1.19

0.92

1.11

0.80

0.87

Gypsum

− 0.61

− 0.68

− 0.55

− 0.90

− 0.84

Anhydrite

− 0.76

− 0.85

− 0.71

− 1.11

− 1.04

Halite

4.06

4.75

4.29

5.76

5.47

  1. *A positive value indicates supersaturation, meaning the mineral is more likely to precipitate, while a negative value indicates undersaturation, meaning the mineral is more likely to dissolve