THE INFLUENCE OF SOIL CHEMISTRY ON FINE ROOT ALUMINUM CONCENTRATIONS AND ROOT DYNAMICS IN A SUB-ALPINE SPODOSOL, WASHINGTON-STATE, USA

The relationship between root Al concentrations and Al fractions in the soil solution was examined in a mature Abies amabilis ecosystem in the Cascade Range of Washington State. The naturally acidic soils in these ecosystems lead to high concentrations of aqueous Al in soil solutions and contribute to the biocycling of Al by the A. amabilis/T. mertensiana stand. Root concentrations of Al were very closely related to aqueous Al3+ activities, but poorly correlated with total aqueous Al concentrations. The solution Al/Ca molar ratios followed a seasonal cycle with low values during the fall and high values during the spring. Ratios remained < 1 throughout the Oa horizon while they varied between 2 and 14 in the E and Bhs horizons. The vertical distribution of roots and the mortality of fine roots may be linked to the soil solution Al/Ca ratio. Root cation exchange capacity ranged between 180 and 225-mu-mol g-1 and the exchangeable Al fraction represented from 12-17% of the total Al content in the root. Evidence for solid-phase co-precipitates of Al with PO4 and oxalate was indicated from selective dissolution of the root tissue. Sufficient quantities of PO4 and oxalate exists in the roots to tie up 20-40% of the Al present in the roots of the Oa and E horizons, but only 9% of that present in the Bhs horizon. Species differences in the distribution of Al between the above-ground and below-ground components may be dictated by these retention processes in the fine roots.