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. 2018 Sep 19;9:2198. doi: 10.3389/fmicb.2018.02198

Table 1A.

Chemical properties of rhizosphere soils used in this study (n = 3).

Soil P (mg kg-1) K (cmol+ kg-1) pH (H2O) OM (%) Al sat (%) CICE (cmol+ kg-1) ΣΣ basis (cmol(+)kg-1)
1 60.3 ± 0.8a 2.8 ± 0.1a 5.9 ± 0.1a 12.2 ± 0.1d 0.6 ± 0.0c 16.9 ± 0.0a 16.9 ± 0.0a
2 41.5 ± 0.9cd 1.2 ± 0.0b 5.3 ± 0.0b 10.9 ± 0.2d 9.9 ± 0.1a 11.0 ± 0.1c 9.9 ± 0.1c
4 59.8 ± 0.2a 0.6 ± 0.0d 5.7 ± 0.0ab 15.1 ± 0.1a 1.1 ± 0.0b 9.4 ± 0.0d 9.3 ± 0.0c
13 5.6 ± 0.4k 0.9 ± 0.0c 5.6 ± 0.0c 13.5 ± 0.2b 0.5 ± 0.0c 15.7 ± 0.1b 15.6 ± 0.1b

Calculated as Al/cation exchange capacity [ΣΣ (K, Ca, Mg, Na, and Al)] × 100, n =3.

Different letters in the same column denote significant differences (Tukey’s test, P ≤ 0.05).