
%0 Journal Article
%A Hailes, K. J. 
%A Aitken, R. L. 
%A Menzies, N. W. 
%T Magnesium in tropical and subtropical soils from north-eastern Australia. I. Magnesium fractions and interrelationships with soil properties
%J Soil Research
%D 1997/05/06
%V 35
%N 3
%P 615-628
%K acid-extractable, deficiency, exchangeable, mineral, organic carbon, total.
%R https://doi.org/10.1071/S96081
%U https://www.publish.csiro.au/paper/S96081 
%X The magnesium (Mg) status of 52 highly weathered, predominantly acidic, surface soils from tropical and subtropical north-eastern Australia was evaluated in a laboratory study. Soils were selected to represent a range of soil types and management histories. Exchangeable Mg concentrations were generally low (median value 0&#183;37 cmol(+)/kg), with deficient levels (&#60;0&#183;3 cmol(+)/kg) being measured in 22 of the soils, highlighting the potential for Mg deficiency as a limitation to plant growth in the region. Furthermore, acid-extractable Mg concentrations, considered a reserve of potentially available Mg, were generally modest (mean and median values, 1&#183;6 and 0&#183;40 cmol(+)/kg, respectively). The total Mg content of the soils studied ranged from 123 to 7894 mg/kg, the majority present in the mineral pool (mean 71%), with smaller proportions in the acid-soluble (mean 11%) and exchangeable (mean 17%) pools, and a negligible amount associated with organic matter (mean 1%). A range of extractant solutions used to displace exchangeable Mg was compared, and found to yield similar results on soils with exchangeable Mg &#60;4 cmol(+)/kg. However, at higher exchangeable Mg concentrations, dilute extractants (0&#183;01 M CaCl2, 0&#183;0125 BaCl2) displaced less Mg than concentrated extractants (1 M NH4Cl, 1 M NH4OAc, 1 M KCl). The concentrated extractants displaced similar amounts of Mg, thus the choice of extractant is not critical, provided the displacing cation is sufficiently concentrated. Exchangeable Mg was not significantly correlated to organic carbon (P &#62; 0&#183;05), and only 45% of the variation in exchangeable Mg could be explained by a combination of pHw and clay content. 
