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This article in SSSAJ

  1. Vol. 59 No. 4, p. 1081-1085
     
    Received: Dec 21, 1993
    Published: July, 1995


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doi:10.2136/sssaj1995.03615995005900040019x

Comparing Potassium Soil Tests with a Flexible Function and a Modifier Variable

  1. Manuel O. Avellaneda and
  2. Mario A. Jauregui 
  1. Fac. de Ciencias Agrarias, Univ. Nacional de Cuyo, Almirante Brown 500, 5505-Chacras de Coria, Mendoza, Argentina
    PRODETEC FINNIDA, NICABOX 115, P.O. Box 52-7444, Miami, FL 33152-7444

Abstract

Abstract

Selecting the appropriate functional form and using modifier variables are key issues in soil test calibration. Flexible functions capture all the information conveyed by the data, except for stochastic aberrations of local maxima, minima, and inflexion points. The objective of this study was to show that a flexible function can be used for comparing soil tests including the sediment volume (SV) as a modifier variable. Data used in this test were collected from 30 irrigated Torrifluvents in which K availability had been evaluated with the Neubauer method. The dependent variable was total K uptake by ryegrass (Lolium perenne L.). Independent soil K variables corresponded to seven soil test methods: NH4OAc-exchangeable K; HNO3-extractable K; H2CO3-extractable K; soluble K; resin-extractable K; K potential; and K adsorption ratio. The modifier variable, SV, is a quick, inexpensive, and fairly accurate attribute widely used in western Argentina to appraise soil texture. Data were evaluated using the generalized Cobb-Douglas (GCD) function. Explanation of variability in K uptake using the GCD model, with exchangeable K and SV as independent variables, was highly satisfactory (R2 = 0.88). The other six methods of soil testing gave R2 values from 0.55 to 0.76. Contribution of SV as a modifier for the interpretation of K availability was significant (α < 0.01) for all soil K indices. The GCD function captured a positive interaction between the independent variables. This indicates that the higher K buffering capacity of the finer textured soils was an overriding factor that favored K absorption by plants.

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