The mean concentration of soluble organic phosphorus in the 6 major rivers entering Lough Neagh from 1975 to 1979 was 38 μg P 1 −1. Soluble organic phosphorus constituted 16% of the total phosphorus input during this period. The chemical nature and availability for algal growth of soluble organic phosphorus is largely unknown. An adsorption-precipitation technique for concentrating soluble organic phosphorus from 1001. volumes of river water was developed using lanthanum. From the lanthanum-phosphorus precipitate acid-soluble and alkali-soluble concentrated solutions of organic phosphorus were obtained. 25% of the soluble organic phosphorus from 6 river samples was acid-soluble and 40% was subsequently alkali-soluble. These concentrated solutions were subjected to gel filtration chromatography on a preparative scale using Sephadex G-50 and G-75 when soluble organic phosphorus compounds were fractionated by molecular weight. Of the acid-soluble organic phosphorus 40% was of mol. wt> 10,000, 20% was of mol. wt between 10,000 and 1500 and 40% was of mol. wt < 1500. When the alkali-soluble organic phosphorus was fractionated 70% was of mol, wt > 50,000. Although the acid-soluble concentrates were yellow in colour and may have contained fulvic acids, further gel filtration chromatography of the acid-soluble organic phosphorus with mol. wt > 10,000 indicated that the organic phosphorus was itself coloourless. Alkali-soluble concentrates were red-brown in colour and may have contained humic acids. Sufficient of the alkali-soluble organic phosphorus with mol. wt > 50,000 was isolated by precipitation on acidification for elemental analyses and infrared spectroscopy. Elemental analyses (45.9%, C, 6.6% H, 5.7% N, 0.6% P) showed that the composition of the precipitated material was not identical to the composition of soil humic acids being lower in carbon and higher in hydrogen, nitrogen and phosphorus. Infrared absorption spectra were, however, characteristic of humic substances. Phosphorus may be an integral part of the humic acid structure or an organic phosphorus-metal-organic matter complex may exist. Iron was present in the structure but the phosphorus to iron ratio was not constant between river samples. Algal bioassays on the acid-soluble organic phosphorus with mol. wt > 10,000 and the alkali-soluble organic phosphorus with mol. wt > 50,000 showed that 10 and 32% respectively were available for growth under the conditions of the test.
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