L. Khiari et al., A soil phosphorus saturation index decreasing scooped weight effect in Mehlich-3 procedure, COMM SOIL S, 30(15-16), 1999, pp. 2157-2168
The Mehlich-3 method extracts a quantity of phosphorus (P-M3) well correlat
ed with crop yield in acid soils, and a quantity of aluminum (Al-M3) well c
orrelated with P sorption capacity of mineral soils. Phosphorus fertility l
evels in soils are generally determined on a volume basis, while soil sorpt
ion capacity for P and P saturation of the soil sorption capacity are asses
sed on a weight basis. However, scooped weights vary widely among tested so
ils. The purpose of this paper was to test the stability of a constructed r
atio of P-M3/Al-M3 across a range of soil:solution ratios using 24 soils. T
wenty-four surface soils of different genetical and textural groups were ex
tracted for P-M3 and Al-M3 without replication. Scooped weights varied betw
een 3.21 and 4.17 g per 3-mL scooped volume. Reproducibility of volumetric
test (3 mL of soil per 30 mL of Mehlich-3 solution) was within 3% for P-M3,
Al-M3, and 100 P-M3/Al-M3 using two contrasting soils with two replication
s. Extracted P-M3 and Al-M3 expressed on a weight basis decreased across th
e 24 soils as sample weight increased between 1.50 and 5.00 g, by steps of
0.50 g, per 30 mL of extracting solution. The 100P(M3)/Al-M3 ratio was less
variable than P-M3 or Al-M3 taken alone using a wide range of sample weigh
ts. In contrast with P-M3 and Al-M3 values taken alone, the 100P(M3)/Al-M3
ratio produced stable data across the entire range of sample weights corres
ponding to scooped weights between 0.50 and 1.67 g mL(-1), as shown by a po
wer test. The 100P(M3)/Al-M3 ratio could be used simultaneously as a P satu
ration index for assessing environmental risk, and as a P fertility index f
or making fertilizer recommendations.