Genesis and Classification of Termite-Mediated Soils along Toposequences in a Semiarid Area of Southeast Ethiopia
Table 4
Selected soil physicochemical properties of the termite mounds (TM, n = 3, ± standard deviation) and reference pedons across toposequences in Ilala-Sara and Silala, southeast Ethiopia.
Horizons
Depth (cm)
Sand (>63 μm)
Silt (2–63 μm)
Clay (<2 μm)
Texture class
Silt : clay ratio
pH (1 : 2.5 H2O)
CCE (g kg−1)
EC (mS cm−1)
OC (g kg−1)
Avail. P (mg kg−1)
CEC (cmolc kg−1)
g kg−1 of fine Earth
Pedon D01, Ilala-Sara, ∼ gently undulating summit
A
0–12
680
60
260
Sandy clay loam
0.23
5.74
1.49
12.48
4.81
5.20
AB
12–30
500
80
420
Sandy clay
0.19
5.95
1.83
13.26
4.26
10.00
Bw
30–73
440
120
440
Clay
0.27
5.49
1.29
11.70
9.17
10.60
BC
73–140
510
130
360
Sandy clay
0.36
5.92
1.34
8.780
8.62
9.00
Cr
140–200+
720
140
140
Sandy loam
1.0a0
6.06
1.99
6.630
5.57
6.00
TM
—
480 ± 1.15
140 ± 2.00
380 ± 2.31
Sandy clay
0.37
6.83 ± 0.31
13.21 ± 0.02
22.88 ± 0.24
9.13 ± 0.96
32.67 ± 2.19
Pedon D02, Ilala-Sara site, ∼ gently undulating back slope
A
0–7
780
80
140
Sandy loam
0.57
5.69
0.92
11.70
7.92
5.20
AB
7–95
580
80
340
Sandy clay loam
0.24
5.21
0.80
11.70
6.7
7.60
Bw
95–140
360
20
620
Clay
0.03
6.03
1.08
9.75
6.54
4.80
BC
140–170
480
60
460
Sandy clay
0.13
5.4
0.68
2.34
6.7
9.20
Cr
170–200+
540
100
360
Sandy clay
0.28
5.1
0.62
3.90
6.4
8.60
TM
—
527 ± 1.33
180 ± 2.00
293 ± 1.76
Sandy clay loam
0.61
6.28 ± 0.13
46.14 ± 0.17
20.41 ± 0.40
11.97 ± 1.11
28.67 ± 0.88
Pedon D03, Ilala-Sara site, ∼ nearly levelled toe slope