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. 2020 Oct 10;17(20):7384. doi: 10.3390/ijerph17207384

Table 3.

Soil P fractions come from field experiment under sequential extractions (mg·kg−1).

Soil Depth Treatment Sol-P Al-P Fe-P Red-P Ca-P Org-P
Surface soil P0 0.10 ef 4.75 d 30.20 ef 16.27 cd 10.96 cd 62.48 a
P1 0.16 def 12.00 cd 45.78 de 20.60 bc 20.86 bcd 63.82 a
P2 0.49 bc 19.61 c 64.66 c 26.64 ab 23.53 bc 65.75 a
P3 0.63 b 34.47 b 92.00 b 27.46 a 26.19 b 59.78 a
P4 1.33 a 83.23 a 139.06 a 28.26 a 39.50 a 57.97 a
Subsurface soil P0 0.07 f 2.88 d 13.39 f 11.95 d 8.20 d 39.90 b
P1 0.15 def 7.83 d 28.71 ef 17.00 cd 9.37 d 34.04 b
P2 0.30 cde 9.64 cd 35.73 e 21.32 bc 18.53 bcd 36.71 b
P3 0.33 cd 11.27 cd 45.03 de 20.60 bc 17.63 bcd 31.03 b
P4 0.32 cd 12.90 cd 53.40 cd 18.66 c 17.87 bcd 33.73 b
Source of variation
Treatment <0.001 <0.001 <0.001 <0.001 <0.01 ns
Soil depth <0.001 <0.001 <0.001 <0.001 <0.01 <0.001
T × S <0.001 <0.001 <0.001 ns ns ns

Note: Values followed by different letters indicate significant difference (p < 0.05) between various treatment in different soil depths. “ns” in ANOVA results indicates no significant difference.