O.T. Denmead , R. Leuning , I. Jamie , D.W.T. Griffith
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They included a mass-balance study employing a small test plot approximately 0.05 ha in area in which 14 sheep were grazed, tower-based flux measurements representing areas between 25 ha and 5 km<sup>2</sup> and convective boundary-layer budgets representing regions of order 100 km<sup>2</sup>. The mass-balance study, which was considered to be the most reliable micrometeorological approach, gave an average emission over 8 days of 1.87 g N<sub>2</sub>O–N head<sup>−1</sup> d<sup>−1</sup> corresponding to 11.5% of the nitrogen (N) voided by the animals in urine and dung. However, the data set included two days after rain on which emissions were an order of magnitude larger than on the other days in the study. For the latter, the emission of N<sub>2</sub>O accounted for 3.9% of the N excreted. 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引用次数: 41
摘要
政府间气候变化专门委员会(IPCC)和澳大利亚国家温室气体清单委员会(NGGIC)的估计表明,放牧牧场是氧化亚氮(N2O)的重要人为来源,占全球氧化亚氮总排放量的28%,占澳大利亚的43%。这些估计几乎完全基于圈地试验对野外规模的外推,不确定程度很高。需要通过直接现场测量进行验证。本文报道了在不同空间尺度上对澳大利亚同一地点放牧牧场N2O排放进行的微气象研究。其中包括利用一块面积约为0.05公顷的小试验田进行质量平衡研究,其中放牧了14只羊,基于塔的通量测量面积为25公顷至5平方公里,对流边界层预算面积为100平方公里左右。质量平衡研究被认为是最可靠的微气象方法,其8天的平均排放量为1.87 g N2O-N head - 1 d - 1,相当于动物尿液和粪便中氮(N)的11.5%。然而,数据集包括雨后两天,这两天的排放量比研究中其他日子的排放量大一个数量级。对于后者,N2O的排放量占排泄量的3.9%。尽管由于时间和空间变化较大,不确定性水平仍然很高,但微气象测量表明,N2O排放量可能比NGGIC算法预测的N2O排放量大得多,NGGIC算法使用0.4%的尿液排放因子和1.25%的粪便排放因子,但IPCC算法的预测似乎更接近,两者都使用2%。该研究为提高相关微气象方法的精度指明了途径。
Nitrous oxide emissions from grazed pastures: measurements at different scales
Estimates made by the Intergovernmental Panel on Climate Change (IPCC) and the Australian National Greenhouse Gas Inventory Committee (NGGIC) suggest that grazed pastures are substantial anthropogenic sources of nitrous oxide (N2O), contributing 28% of all anthropogenic N2O emissions globally and >43% for Australia. These estimates are based almost wholly on extrapolations of enclosure experiments to the field scale and uncertainty levels are high. Verification with direct field measurements is needed. This paper reports micrometeorological studies of N2O emissions from Australian grazed pastures made at the same location on a variety of space scales. They included a mass-balance study employing a small test plot approximately 0.05 ha in area in which 14 sheep were grazed, tower-based flux measurements representing areas between 25 ha and 5 km2 and convective boundary-layer budgets representing regions of order 100 km2. The mass-balance study, which was considered to be the most reliable micrometeorological approach, gave an average emission over 8 days of 1.87 g N2O–N head−1 d−1 corresponding to 11.5% of the nitrogen (N) voided by the animals in urine and dung. However, the data set included two days after rain on which emissions were an order of magnitude larger than on the other days in the study. For the latter, the emission of N2O accounted for 3.9% of the N excreted. Although uncertainty levels remain high due to large temporal and spatial variability, the micrometeorological measurements suggested that N2O emissions might be considerably larger than those predicted by NGGIC algorithms which use emission factors of 0.4% for urine and 1.25% for dung, but appear to be predicted more closely by IPCC algorithms which use 2% for both. The study has indicated ways to improve the precision of relevant micrometeorological approaches.