Phosphorus transformations in the epilimnion of humic lakes: abiotic interactions between dissolved humic materials and phosphate

SUMMARY. 1. Sephadex gel filtration of filtered water from small, Finnish forest lakes demonstrated abiotic movement of ³³P from added PO₄ to two higher molecular weight fractions. This movement was most pronounced in waters with high humic content which also had high iron content. The two fractions which took up ¹³P had nominal molecular weights of > 100,000 and 10,000-20,000.
2. An equilibrium existed between free PO₄ and the two fractions. However, one fraction, at least, appeared to exist in two phases, with one phase in rapid equilibrium with free PO₄ but the other in only slow equilibrium.
3. Additions of ferric iron up to 1 mg Fe l⁻¹ to the filtered lake water stimulated movement from free PO₄, provided high concentrations of humic materials were present. In the absence of humic materials even 0.1 mg Fe 1⁻¹ would precipitate all added ³³PO₄.
4. The high molecular weight P was only partially reactive with standard molybdate reagents. Exposure of the high molecular weight P to sunlight caused a small release of PO₄ under the experimental conditions employed.
5. Possible implications for biological phosphorus demand of such sequestration of free PO₄ by humic materials in combination with iron are discussed.