A one year field trial was carried out on three adjacent unfertilised plots; an 18 year old grassland, a 14 year old established
Miscanthus crop, and a 7 month old newly planted
Miscanthus crop. Measurements of N
2O, soil temperature, water filled
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A one year field trial was carried out on three adjacent unfertilised plots; an 18 year old grassland, a 14 year old established
Miscanthus crop, and a 7 month old newly planted
Miscanthus crop. Measurements of N
2O, soil temperature, water filled pore space (WFPS), and inorganic nitrogen concentrations, were made every one to two weeks. Soil temperature, WFPS and NO
3− and NH
4+ concentrations were all found to be significantly affected by land use. Temporal crop effects were also observed in soil inorganic nitrogen dynamics, due in part to C
4 litter incorporation into the soil under
Miscanthus. Nonetheless, soil N
2O fluxes were not significantly affected by land use. Cumulative yearly N
2O fluxes were relatively low, 216 ± 163, 613 ± 294, and 377 ± 132 g·N·ha
−1·yr
−1 from the grassland, newly planted
Miscanthus, and established
Miscanthus plots respectively, and fell within the range commonly observed for unfertilised grasslands dominated by perennial ryegrass (
Lolium perenne). Higher mean cumulative fluxes were measured in the newly planted
Miscanthus, which may be linked to a possible unobserved increase immediately after establishment. However, these differences were not statistically significant. Based on the results of this experiment, land-use change from grassland to
Miscanthus will have a neutral impact on medium to long-term N
2O emissions.
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