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. 2018 Dec 20;8:18006. doi: 10.1038/s41598-018-36324-0

Table 3.

Origin of cowpea isolates used in this study, and soil chemical properties of the sampling sites.

Country Region/Province Location Latitude Longitude pH (H2O) B C Ca Fe K Mg Mn Na P N
(mg.kg−1) (%) cmol(+).kg mg.kg−1 (mg.kg−1) cmol(+).kg−1 (mg.kg−1) (mg.kg−1) (mg.kg−1) (%)
Ghana Northern NyankpalaG 9.389 −1.006 5.9 0.27 0.40 1.06 59.15 68 0.39 79.22 8 6 0.023
DamongoG 9.043 −1.814 4.3 0.23 0.31 1.13 53.73 90 0.49 54.96 7 10 0.04
Upper East GaruF 10.929 −0.125 5.3 0.25 0.55 1.74 40.32 38 0.46 39.09 9 5 0.048
South Africa Mpumalanga KlipplaatdriftF (Middleveld region) −25.233 29.033 6.0 0.23 0.30 3.03 36.80 135 1.19 56.14 11 56 0.29
NelspruitG (Lowveld region) −25.474 30.970 4.9 0.09 0.26 0.74 38.16 43 0.38 39.90 12 32 0.029

Note: FRhizobia trapped by direct planting of Kersting’s bean in the fields, GRhizobia trapped in the glasshouse from sampled field soils.