An experiment was conducted to compare the quality of snow-melt runoff from
fresh or composted manure that had been spread on snow. Sixteen sheet meta
l trays held a layer of snow and either frozen composted or fresh manure. E
ach tray measured 400mm x 400mm x 100mm deep and had two holes to collect r
unoff from the surface and bottom of the tray. Trays were mounted on racks
at a slope of 20 degrees and insulated with rigid polystyrene. Total depth
of compacted snow in the trays was about 90 mm (6 kg). Composted and fresh
manure was spread to give nutrient loading rates in accordance with availab
le manure management guidelines. A factorial experimental design was used w
ith two materials, four arrangements of snow with composted or fresh manure
, two collection openings, two collecting periods, and two replicates of ea
ch. Trays were placed in a temperature-controlled room to simulate a natura
l freeze-thaw cycle. Daily temperatures were set at 8 degrees for 10 hours
and -5 degrees C for 14 hours. Runoff from the snow surface acid from the b
ottom of trays was collected and analyzed for soluble carbon, total nitroge
n, and BOD5. The mean BOD5 level of runoff from composted manure was 45.0 m
g/L compared with 1834 mg/L from unprocessed manure. The snow-material sequ
ence, representing application season, had a significant effect on all anal
ysis parameters from runoff of fresh manure, but no effect on runoff qualit
y of composted manure. Although there were no significant differences betwe
en BOD5 levels of early and late runoff for both fresh and composted manure
and total nitrogen for composted manure, nitrogen, and soluble carbon leve
ls from fresh manure and soluble carbon from composted manure were signific
antly higher in the early runoff. The mean BOD5 level and the concentration
s of soluble carbon from runoff of fresh manure collected from upper openin
g locations were significantly higher than those from lower ones.