Hkj. Powell et al., FREE ALUMINUM AND RELATED PARAMETERS IN SOIL SOLUTION FROM A SOUTH ISLAND (NEW-ZEALAND) HIGH COUNTRY SITE UNDER CONTRASTING S AND P FERTILIZATION, Australian Journal of Soil Research, 35(1), 1997, pp. 175-181
Soil solution samples were taken from 7 plots of varying Hieracium inf
estation at the AgResearch (NZ) Mt John trial site, Lake Tekapo. The s
oils, which had been fertilised, oversewn, and graced, were analysed f
or free (reactive) Al, total Al, pH, NOM (natural organic matter), and
phosphate. The plots had received annual fertiliser combinations of 0
-100 kg P and 0-20 kg S/ha . year. Soil solution pH was in the range 4
.33-5.76 and total Al concentrations were in the range 13-68 mu M. Fre
e Al concentrations were in the range 0.48-4.8 mu M. The pH dependence
of log(free[Al]) (slope: -0.69+/-0.37) indicated control of soluble A
l by NOM rather than Al(OH)(3) solubility. Soil solution phosphate con
centrations depended strongly on P application rate, reaching over 100
mu M. At high P concentrations, the product [Al3+][PO43-] indicated a
pproximate saturation with respect to variscite. One comparison indica
ted that effects on pH and NOM in the upper 5 cm were due to the prese
nce or absence of gracing.