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. 2023 Jun 7;21(2):319–332. doi: 10.1007/s40201-023-00857-y

Table 3.

Pearson correlation coefficients (r) between Cd fractions in the soil (n = 12)

Cultivated soil Uncultivated soil
F1 F2 F3 F4 F5 F1 F2 F3 F4 F5
Cd25
F1 1 -0.685* -0.454 ns 0.636 ns 0.174 ns 1 -0.451 ns -0.876** 0.722* 0.245 ns
F2 1 0.090 ns -0.796* 0.197 ns 1 0.519 ns -0.849** 0.147 ns
F3 1 -0.524 ns -0.331 ns 1 -0.774* -0.120 ns
F4 1 -0.115 ns 1 -0.139 ns
F5 1 1
Cd50
F1 1 -0.803** -0.753* 0.871** -0.129 ns 1 -0.619 ns -0.804** 0.862** 0.120 ns
F2 1 0.558 ns -0.763* -0.153 ns 1 0.815** -0.870** 0.157 ns
F3 1 -0.917** 0.322 ns 1 -0.833** 0.131 ns
F4 1 -0.279 ns 1 0.145 ns
F5 1 1

**, and * show correlation is significant at the probability levels of 0.05, and 0.01 respectively, and ns denotes that the value is not significant. F1, exchangeable; F2, bound to carbonates; F3, bound to organic matter; F4, bound to iron manganese oxides; F5, residual fractions