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Title: Transformations of aluminum in waters draining podzolic forest soils

Thesis/Dissertation ·
OSTI ID:5163813

In this study, I undertook a combined laboratory and field investigation of the chemistry and transformations of soluble aluminum-ligand complexes prevalent in podzolic soils. Three biogeochemically important ligands (silicate, phosphate, and fulvate) were tested in laboratory studies. Silicate and phosphate formed a series of soluble mono- and di-nuclear aluminum complexes exhibiting pH dependent conditional stabilities consistent with mixed hydroxy-Al-ligand species. Equilibrium constants were estimated for a soluble mononuclear aluminum-silicate (AlH{sub 3}SiO{sub 4}{sup 2+}) and a series of hydroxy-aluminum-phosphate complexes. Binding between Al and fulvate was consistent with 1:1:0, 1:1:1 and 1:1:2 Al:fulvate:OH combining ratios, and a pH dependent form of a two-site Scatchard model was developed to model the experimental data. Field studies were conducted in three watersheds overlain by podzolic soils: Hubbard Brook Experimental Forest, New Hampshire; the North Branch of Moose River, New York State: and Jamieson Creek Watershed, British Columbia. Aluminum-organic complexes dominated the chemistry of soluble aluminum in each study watershed. A simple, accurate predictive model of aluminum speciation was developed based on pH titration data of surface water samples.

Research Organization:
Syracuse Univ., NY (USA)
OSTI ID:
5163813
Resource Relation:
Other Information: Thesis (Ph. D.)
Country of Publication:
United States
Language:
English