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Table 1 Chemical properties of a C. papaya L. rhizospheric soil under both conventional and organic farming systems

From: Crop management as a driving force of plant growth promoting rhizobacteria physiology

Chemical characterization

Conventional

Organic

P value

pH

5.5

6.6*

0.041

P (mg dm−3)

355.3

382.7n.s.

0.643

K (mg dm−3)

189.0

116.0*

0.032

Ca (cmolc dm−3)

4.4

4.4n.s.

0.812

Mg (cmolc dm−3)

0.6

0.9n.s.

0.073

Na (cmolc dm−3)

0.1

0.2n.s.

0.056

C (%)

1.4

1.3

0.104

MO (g dm−3)

23.3

22.4n.s.

0.138

Cu (mg dm−3)

2.8

8.6***

0.00014

Zn (mg dm−3)

22.6

14.0**

0.0085

Mn (mg dm−3)

10.0

23.0**

0.0012

S (mg dm−3)

127.5

35.3***

0.00001

B (mg dm−3)

0.9

1.4*

0.0193

Fe (mg dm−3)

26.8

21.2*

0.045

H + Al (cmolc dm−3)

2.3

0.8*

0.014

BS (cmolc dm−3)

5.6

5.7n.s.

0.569

T (cmolc dm−3)

7.9

6.5*

0.027

t (cmolc dm−3)

5.6

5.7n.s.

0.452

V (%)

70.7

87.3*

0.017

  1. H + Al, potential acidity; BS, sum of bases; T, cation exchange capacity (CEC) at pH 7.0; t, effective cation exchange capacity (eCEC); V, saturation percentage for bases; n.s, means are not significantly different by Student’s t test at P ≤ 0.05
  2. * Means are statistically different by Student’s t test at P ≤ 0.05, ** P ≤ 0.01 and *** P ≤ 0.001