Xj. Wang et al., NITROGEN FLUXES IN SURFACE SOILS OF 1-2-YEAR-OLD EUCALYPT PLANTATIONSIN TASMANIA, Australian Journal of Soil Research, 36(1), 1998, pp. 17-29
To improve our understanding of nitrogen (N) supply in eucalypt planta
tions in Tasmania, N fluxes were determined in surface soils (0-10 cm)
at 4 sites supporting 1-2-year-old plantations of E. nitens. Net N mi
neralisation, nitrification, leaching, and uptake were measured by an
in situ soil-core technique. Soils were derived from basalt (3 sites)
or mudstone (1 site). Average rates of net N mineralisation ranged fro
m 18 to 91 kg N/ha . year, and most mineralised N was nitrified and le
ached. There were significant linear relationships among net N mineral
isation, nitrification, and leaching (r = 0.61-0.83). Annual rates of
net N mineralisation varied as much within sites as between them, and
rates in individual plots were significantly correlated with anaerobic
ally mineralisable N (r = 0.82) or total N (r = 0.66), but were not co
rrelated or only weakly correlated with C:N ratio, loss-on-ignition, o
rganic C, water content, or temperature. Leaching was weakly correlate
d with effective rainfall (rainfall minus evaporation, r = 0.39). Soil
contained most mineral N during February-April (i.e. late summer-earl
y autumn) and least during October-November (i.e. late spring). We con
cluded that available N at these sites was highly variable spatially a
nd temporally, and at a plot scale was closely related to concentratio
ns of mineralisable substrate and not to soil water or temperature.