B. Vanraij, BIOAVAILABLE TESTS - ALTERNATIVES TO STANDARD SOIL EXTRACTIONS, Communications in soil science and plant analysis, 29(11-14), 1998, pp. 1553-1570
Due to the complexity of the soil plant system and in spite of the eno
rmous amount of information available, the search for better methods t
o determine the bioavailability of nutrients to plants continues to be
important. The large number of methods of soil analysis available wor
ldwide in routine soil testing is an unquestionable demonstration of t
he lack of agreement on best alternatives. The question discussed in t
his paper, based on a literature review, is if those methods, consider
ed here as the ''standard methods'' of soil analysis, are the best pos
sible alternatives for the evaluation of bioavailability of elements i
n soil. As alternative non-standard methods, electroultrafiltration (E
UF), the extraction with 0.01 mol calcium chloride (CaCl2) L-1 solutio
n, the extraction with ion-exchange resin and the adsorption of phosph
orus (P) on iron oxide treated paper filter (Pi), were considered. The
se four methods were compared with the standard methods Olsen, Mehlich
1, Bray 1, Mehlich 3, AB-DTPA, Egner, water, ammonium acetate (NH4OAc
), and DTPA. The criterion used to compare the different methods was t
he percent variation (100 r(2)) associated with the correlations of pl
ant indexes of bioavailability, in most cases uptake by plants, and so
il contents of the elements. For P, the extraction with ion-exchange r
esin presented considerable higher values of the percent variation, in
comparison with the standard methods, EUF, and CaCl2, The resin extra
ction is adaptable to all types of soils, including acid and alkaline,
which is not the case for the standard methods. Comparisons for other
elements was impaired by the limited amount of data available, but be
tter alternatives to the standard methods are not yet available. The e
xtraction with resin seems to be feasible for other elements, includin
g potassium (K), calcium (Ca), magnesium (Mg), sulfur (S), nitrogen (N
), molybdenum (Mo), copper (Cu), manganese (Mn), zinc (Zn), cadmium (C
d), and lead (Pb), but there is a need for a practical laboratory tech
nique to determine all those elements and the biological validation wi
th plant experiments. Thus only for P is there a more accurate alterna
tive to evaluate bioavalilabity of nutrients in soils.