Ja. Stanturf et El. Stone, LOSS OF NITROGEN AND BASES AFTER FERTILIZATION OF 2ND-GROWTH HARDWOODFOREST SOILS, Forest ecology and management, 65(2-3), 1994, pp. 265-277
Soils at five New York sites of a nitrogen fertilization study in seco
nd-growth mixed deciduous forests were sampled to determine the fate o
f applied N and possible adverse chemical changes from its application
. Organic layer and mineral soil (0-10 cm) samples were collected 10 o
r 11 years after the initial application from plots receiving a total
of 0, 672 and 1344 kg-N ha-1 in two equal-sized applications 5 years a
part. Nitrogen was applied as ammonium nitrate, except the first appli
cation at one location was urea. Treatments had little effect on the N
and C pools of the forest floor and surface soil, indicating no appre
ciable retention of added N in the upper soil. Concentration and mass
of cations in the mineral soil decreased with added N, as did pH, in a
ccord with an hypothesis of nitrate leaching. The estimated loss of ba
se cations was modest ( 1 2.4 kmol ( + ) ha-1) relative to the anions
added in the highest single application of N (24 kmol ( - ) ha-1). On
such soils, N added in excess of plant uptake capacity is not immobili
zed by long-term storage in soil organic matter despite its wide C:N r
atio. The reduction in pH entails a loss of effective cation exchange
capacity in addition to the associated loss of base cations.