Research Article

Effectiveness of Community-Based Soil and Water Conservation in Improving Soil Property in Damota Area, Southern Ethiopia

Table 3

Pearson coefficient of correlation between soil physicochemical properties.

Sand (%)Clay (%)Silt (%)BD (g·cm−3)pH (H2O)OC (%)TN (%)Av. P (ppm)CEC and exch. Basis (cmol (+)kg−1)
CECNaKCa2+Mg2+

Sand (%)1−0.7340.076−0.140−0.242−0.158−0.243−0.306−0.234−0.044−0.1470.0380.121
Clay (%)1−0.6080.0180.2580.4800.6960.3880.7830.1860.2480.1260.090
Silt (%)10.157−0.0850.125−0.459−0.1320.1340.0270.2690.0640.036
BD (g cm−3)10.0700.672−0.044−0.0960.0700.201−0.0700.0450.586
pH (H2O)10.2930.3720.1320.2710.1720.2260.050.002
OC (%)10.7790.1400.4320.0390.0690.6400.126
TN (%)10.1060.5740.0480.1530.2060.147
Av. P (ppm)10.0300.1410.0700.150−0.136
CEC (cmol(+) kg−1)10.0190.2250.1510.158
Exch. basis (cmol(+) kg−1)Na10.1770.2980.264
K10.2140.074
Ca2+1−0.021
Mg2+1

BD, bulk density; pH, soil reaction; OC, organic carbon; TN, total nitrogen; AV. P, available phosphorous; CEC, cation exchange capacity. Na, K, Ca2+, and Mg2+ are exchangeable sodium, potassium, calcium, and magnesium, respectively; and implies the mean correlation between soil properties significant at and 0.01 levels, respectively.