The Effects of Land Use and Landscape Position on Soil Physicochemical Properties in a Semiarid Watershed, Northern Ethiopia
Table 3
Mean values ± SE of soil bulk density, total porosity, and soil moisture in different land use types across altitudinal gradients.
Soil variables
Land use types
Altitudinal gradients
Average
Lower
Middle
Upper
Bulk density (g cm−3)
Barren land
—
1.34 ± 0.03
1.40 ± 0.03
1.37a±0.10
Cultivated land
1.09 ± 0.03
1.21 ± 0.03
1.32 ± 0.03
1.21b ± 0.10
Grassland
0.98 ± 0.03
1.25 ± 0.03
1.19 ± 0.03
1.14c ± 0.10
Plantation forest
—
1.15 ± 0.03
1.22 ± 0.03
1.19bc ± 0.10
Average
1.04b ± 0.03
1.24a ± 0.03
1.28a ± 0.03
1.23 ± 0.10
Total porosity (%)
Barren land
—
49.68 ± 1.05
47.44 ± 1.05
48.56c ± 1.05
Cultivated land
58.87 ± 1.05
54.50 ± 1.05
50.28 ± 1.05
54.55b ± 1.05
Grassland
63.06 ± 1.05
52.95 ± 1.05
55.24 ± 1.05
57.08a ± 1.05
Plantation forest
—
56.69 ± 1.05
54.20 ± 1.05
55.45ab ± 1.05
Average
60.96a ± 1.05
53.46b ± 1.05
51.79b ± 1.05
53.91 ± 1.05
Soil moisture (%)
Barren land
—
9.08 ± 1.31
9.87 ± 1.31
9.47b ± 1.31
Cultivated land
18.98 ± 1.31
13.66 ± 1.31
14.30 ± 1.31
15.65a ± 1.31
Grassland
22.62 ± 1.31
14.04 ± 1.31
16.37 ± 1.31
17.67a ± 1.31
Plantation forest
—
15.12 ± 1.31
15.55 ± 1.31
15.34a ± 1.31
Average
20.80a ± 1.31
12.98b ± 1.31
14.02b ± 1.31
14.53 ± 1.31
Overall means within columns and rows followed by the same superscript letter(s) are not significantly different ( < 0.05) as influenced by land use and altitude based on Duncan’s test. Values shown are means ± standard error (n = 3).