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Ammonia Emissions from Native Soils (and Vegetation)

机译:原生土壤(和植被)的氨气排放

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Unlike previous studies, this study allows for the calculation of direct ammonia emissions from native soils to be based on local meteorology and plant specific data rather than net emission factors from specific measurements. This study allows for the creation of a geographically specific emission inventory for ammonia emissions from native soils that can be modified from year to year whereas previous studies did not take into account changes in temperature from one year to the next. This study found that the apoplastic ratio has the greatest effect on the annual ammonia emission factors from native soils. A change in the apoplastic ratio from 155 to 630 will create an increase in ammonia emissions by a factor of 4. Other than the apoplastic ratio, ambient temperature and solar radiation can also affect the calculation of ammonia emissions from native soils. For example, when comparing 2005 and 2008, the ammonia emissions increased in the S JVAPCD but remained relatively constant in the BAAQMD and in the Sacramento PM_(2.5) nonattainment area. These changes are due to changes in temperature and solar radiation from 2005 to 2008.
机译:与以前的研究不同,该研究允许根据当地气象和植物特定数据而不是特定测量的净排放因子来计算天然土壤中直接氨的排放。这项研究允许为本地土壤的氨气排放量创建一个地理上特定的排放量清单,该清单可以逐年修改,而以前的研究没有考虑一年到下一年温度的变化。这项研究发现,外生比例对原生土壤每年氨气排放因子的影响最大。质外比例从155更改为630将使氨气排放量增加4倍。除了质外率以外,环境温度和太阳辐射也会影响天然土壤中氨气排放的计算。例如,当与2005年和2008年进行比较时,S JVAPCD中的氨气排放量有所增加,但在BAAQMD和萨克拉曼多PM_(2.5)未达标区域中的氨氮排放量则保持相对恒定。这些变化是由于2005年至2008年温度和太阳辐射的变化所致。

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