An analytical registration of P-transport processes in intact sediment cores from the shallow reservoir Radeburg I1 (near Dresden, Saxonia, Germany) was possible by application of KH232P04 and followed by sequential P-fractionation (PSENNER et al. 1984). Under oxygen free conditions and sufficient nitrate supply an activity accumulation was found in the uppermost sediment horizon. Nitrate influences above all the BD-fraction (reductant soluble P), so that an interaction between nitrate and the iron binding system could be proved. It could be shown by means of activated sludge (a model object for microbial polyphosphate accumulation from a lab plant qualified for biological P-and N-elimination) that added KH232P04 was bound within 5 h to about 75 % in the NaOH-fraction. The saturation of iron compounds in the activated sludge took place immediately after KH23*P04 had been added. In the same time the portion of the microbial immobilization of added 32P amounted to 7 % in the high-iron sediment from the Radeburg reservoir, whereas evidently in the heat-and HgCI2-sterilized sediments this portion was additionally ascertained in the BD-fraction, too,