Table 1 Grain-size distribution, textural classes and smectite properties and proportion.

From: Origin of clay minerals in Early Eocene volcanic paleosols on King George Island, Maritime Antarctica

Profile

Horizon

Depth

Particle size [%]

Textural class

Octahedral occupancy of smectites [%]

Smectite in the parent material [%]

 

[cm]

Clay (<2 µ)

Silt (2 µ-63 µ)

Sand (63 µ−2000 µ)

Dioctahedral

Trioctahedral

P1

Bwb1

0–23

15

18

67

Sandy Loam

92

8

 

Bwb2

23–34

15

19

66

Sandy Loam

97

3

 

Bwb3

34–45

14

19

67

Sandy Loam

92

8

 

Parent material

from Bwb3 horizon

    

55

45

28.4

2Abb

45–60

17

21

62

Sandy loam

81

19

 

2Bab

60–73

20

22

58

Sandy clay loam

91

9

 

Parent material

from 2ABb horizon

    

68

32

33.6

3Abb

73+

20

15

65

Sandy clay loam

99

1

 

Parent material

from 3ABb horizon

    

72

28

41.8

P2

Abb

0–20

19

17

64

Sandy clay loam

98

2

 

Bwb1

20–30

15

19

66

Sandy loam

98

2

 

Bwb2

30–53

15

18

67

Sandy loam

99

1

 

Bwb3

53+

15

13

72

Sandy loam

97

3

 

Parent material

from Bwb3 horizon

    

75

25

29.7