Evaluation of the Mehlich 3 soil extractant for upland Malawi soils

Abstract

The Mehlich 3 (M3) universal soil extraction method was compared with the ammonium acetate (AA), Bray 1, and DPTA extraction procedures for the analysis of calcium (Ca), magnesium (Mg), potassium (K), phosphorus (P), zinc (Zn), copper (Cu), manganese (Mn), and iron (Fe). Upland Malawi soils from 112 smallholder farmers’ fields of the Alfisol, Ultisol, and Oxisol soil orders were analyzed by the four procedures. Calcium, Mg, and K extracted by the M3 and AA procedures were highly correlated (r² = 0.98, 0.98, and 0.99 for the respective elements). The M3 extractant also correlated well with the DPTA procedure for Zn and Cu (r² = 0.88 for both elements) and the Bray 1 method for P (r² = 0.80). Amounts of Mn and Fe extracted by M3 and DPTA were poorly correlated (r² = 0.28 and 0.47, respectively), with both elements testing high in all soils. The high levels suggest that Mn and Fe deficiencies are likely to be rare, and that analysis for these elements is not generally necessary. Special precautions for Zn and Cu analyses are advised due to the low conentrations of these elements in the M3 extract and various laboratory sources of Zn contamination. The use of soil pH along with M3‐extractable Zn is recommended in the identification of potentially Zn‐deficient soils. The preference for expressing analytical results on a volume rather than weight basis is discussed. Based on a review of literature relating to the M3 extractant, the following critical M3 soil test values are tentatively recommended for maize on upland Malawi soils: Ca, 50 mg/dm³; Mg, 75 mg/dm³ and Mg:Ca ratio >0.067; K, 70 mg/dm³; P, 20 mg/dm³; Zn, 1.0 mg/dm³; and Cu, 0.5 mg/dm³. These suggested values should not preclude in‐country correlation studies. Because the M3 procedure is well correlated with the AA, DPTA, and Bray 1 methods, and because it is a rapid procedure, the M3 method can be highly recommended as a replacement for the three current procedures for Malawi upland soils. Caution is advised in extending the results to Malawi lowland soils, which are characterized by higher pH values.

Notes

Research funded by the Rockefeller Foundation, P. O. Box 30721, Lilongwe 3, Malawi, in cooperation with the Malawi Ministry of Agriculture.