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Table 2 Properties of aquifer sediments at Manda, Mohanpur and Bagmara

From: Safe distances between groundwater-based water wells and pit latrines at different hydrogeological conditions in the Ganges Atrai floodplains of Bangladesh

Location

Depth (m)

Aquifer

Effective grain size (mm)

Uniformity coefficient

Hydraulic conductivity (m/h)

D 10

D 60

Manda

12–15

1ST

0.17

0.21

1.23

7.30

18–21

1ST

0.17

0.28

1.64

5.20

27–30

2ND

0.12

0.24

1.96

3.60

33–36

2ND

0.18

0.4

2.29

7.72

36–39

2ND

0.19

0.6

3.16

11.70

Mohanpur

24–30

1ST

0.18

0.42

2.33

8.20

36–39

2ND

0.16

0.27

1.69

6.40

42–45

2ND

0.17

0.25

1.47

6.20

Bagmara

12–15

1ST

0.08

0.21

2.80

1.40

15–18

1ST

0.16

0.23

1.44

6.45

21–24

1ST

0.18

0.44

2.44

11.66

27–30

1ST

0.22

0.42

1.90

15.70

30–33

1ST

0.20

0.42

2.10

11.52

33–36

1ST

0.18

0.40

2.22

10.50

36–39

1ST

0.18

0.42

2.33

10.50