Clear-cutting reduces nitrate leaching in a pine plantation of high natural N status |
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Authors: | R L Parfitt G J Salt L F Hill |
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Institution: | Landcare Research, Manaaki Whenua, Private Bag 11052, Palmerston North, New Zealand |
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Abstract: | Following the tree harvest, the biogeochemistry of a catchment is modified by changes in soil temperature and moisture, and nutrient cycling. We monitored soil-solution and stream-water chemistry, and soil properties in a Pinus radiata D. Don plantation in New Zealand before and after clear-cutting and replanting in 1997. The annual rainfall during the study was 1440–1860 mm. The soil was a 1800-year-old pumice soil of high natural N status; the catchment had received large inputs of volcanic N in rain, probably over the 1800 years since the pumice had been deposited. The leaching loss of nitrate-N was 28 kg ha?1 yr?1 in 1996, and then decreased sharply after clear-cutting to 3 kg ha?1 yr?1 in 1998 and <1 kg ha?1 yr?1 in 1999. Weed growth and soil microbial biomass increased during this time, and would have removed much of the N from soil solution in the upper soil layers. Although the catchment was small (8.7 ha), there was a 2-year lag until N decreased in stream-water; the losses of dissolved organic N to stream-water were low. There was no change in soil pH over the 4 years, but spring-water pH appeared to increase, which was consistent with the increase in bicarbonate that accompanied grass/weed growth. The export of cations (mmolc l?1) in the spring-water was Na>Ca>Mg=K as expected for rhyolitic pumice, and the total concentration was probably controlled by the accompanying anions. The export of anions was NO3=Cl>SO4=HCO3 before harvest and HCO3=Cl>SO4=NO3 after harvest. |
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Keywords: | Andisol Ammonium Clear-felling DOC Nitrification |
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