Some effects of applying undiluted silage effluent to grassland

Two small-plot experiments were carried out to assess the influence on herbage dry matter (DM) production, chemical composition and soil fertility status of applying undiluted silage effluent at a range of application rates and intervals after a silage cut. In the first experiment, in 1990, silage effluent was applied at 25, 50, 100, 150 and 200 m³ ha^?1 1, 8, 15 and 22 d after a silage cut in August. In the second experiment, in 1991, silage effluent was applied at 7, 14, 21, 28, 35, 42, 49, 75, 100, 125 and 150 m³ ha^?1 1, 4, 8, 15, 22 and 29 d after silage cuts were taken from different sites in May, July and August. An untreated control and an Inorganic fertilizer treatment were incorporated in both experiments. The immediate effects of the treatments on herbage yield, chemical composition and soil nutrient status were assessed 6–8 weeks after the initial application; residual effects on herbage and soil fertility were measured at a subsequent harvest. Compared with the untreated control, herbage yield increases were obtained with increasing rates of effluent application. Although there was evidence that higher yields could be obtained from earlier applications, up to 50 m³ ha^?1 of effluent could be applied up to 15 d after taking a silage cut with little damage to the sward. Delaying the timing of application, and increasing the application rate, increased the proportion of the sward which was damaged; this reached a maximum of 0·84 when the highest application rates were applied 29 d after a silage cut. The increase in the proportion of dead herbage in the sward, associated with increasing rate of effluent application, reduced the quality of the herbage harvested in Experiment I. In Experiment 2 the N, P and, in particular, the K content of the herbage increased with increasing rate of effluent application, whereas the effect on Mg content was variable with contents generally being less than 2·0 g kg^?1 DM. Apparent recovery of nutrients applied in the effluent was both low and variable ranging from 0·58 to ?0·03 for N, 0·10 to ?0·005 for P, 0·34 to ?0·02 for K and 0·21 to ?0·002 for Mg over both experiments. Effluent had little effect on soil pH, whereas P and, in particular, K contents increased with increasing rate of effluent application. There was evidence that effluent had a beneficial effect on both herbage yield and chemical composition at the residual cut, the extent depending upon rate and time of effluent application.