Soil and lodgepole pine foliar responses to two fertilizer sulphur forms in the Sub-Boreal Spruce zone, central interior British Columbia.

摘要

Sulfur (S) fractions, total nitrogen (N) concentrations, and cumulative net S mineralization of forest floors and surface mineral soils (0-20 cm) were measured 13 years after an S-deficient lodgepole pine (Pinus contorta var. latifolia) stand was fertilized (100 kg S ha-1+400 kg N ha-1) in 1990. The study site is located in Prince George, British Columbia (Canada), within the Stuart Dry Warm variant of the Sub-Boreal Spruce biogeoclimatic zone. The predominant Brunisolic Gray Luvisolic soils have formed an undulating to rolling morainal deposit with loam to sandy loam textures. Fertilizer treatments compared two S sources: elemental S (S0) and ammonium sulfate (AS). Total S and ester sulfate-S (SO4-S) concentrations and cumulative net S mineralization in forest floors were significantly higher in the S0 treatment than in the control and AS treatment. Except for a slight elevation of extractable SO4-S, such differences were absent in the mineral soils. Total S and SO4-S concentrations in current-year (2002) pine foliage from the S0 treatment were significantly higher than in foliage from the control and AS treatment, while foliar N concentrations indicated that all treatments had caused a return to N-deficiency. These results indicate that prolonged amelioration of S deficiencies in lodgepole pine stands in central interior British Columbia may be possible with single applications of S0..