Grasslands are the basis for a stable agriculture in the Northeast USA
. However, knowledge of interactive effects of soil drainage and N fer
tilization on grassland production in this region remains scant. Our o
bjective was to quantify the effect of soil drainage on grassland biom
ass production and N accumulation. The study was conducted for 2 yr on
a floodplain site iii central Pennsylvania on two soils selected for
extreme drainage conditions. Perennial ryegrass (Lolium perenne L. cv.
Bastion) was treated with a split application (50% in mid-April, 50%
in mid-July) of 0, 84, 168 and 252 kg, N ha-1 of N-15 depleted NH4NO3.
Biweekly biomass samples were taken starting mid-May of each year and
continuing until the grass headed and all herbage was removed from th
e plots. Plots were re-fertilized and monthly biomass sampling commenc
ed at the end of August and continued until the end of October 31. Fer
tilizer nitrogen recovery was greatest in the first harvest after fert
ilization, irrespective of soil type or season. Peak fertilizer N reco
very for spring growth was 50% on the well-drained soil and 32% on the
poorly drained soil. In the summer-fall growth period, peak fertilize
r N recovery was 26% on the well-drained and 18% on the poorly drained
soil. Biomass on the poorly drained soil was 26% less in the spring a
nd 8% less in the summer-fall periods compared with that of the well-d
rained soil. Overall, poor soil drainage conditions resulted in a 39%
reduction in fertilizer N recovery and a 21% reduction in yield of per
ennial ryegrass.