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首页> 外文期刊>Journal of Geophysical Research, D. Atmospheres: JGR >Ammonia and methane dairy emission plumes in the San Joaquin Valley of California fromindividual feedlot to regional scales
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Ammonia and methane dairy emission plumes in the San Joaquin Valley of California fromindividual feedlot to regional scales

机译:加利福尼亚圣华金河谷从个体饲养场到区域规模的氨和甲烷奶类排放羽

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摘要

Agricultural ammonia (NH_3) emissions are highly uncertain, with high spatiotemporal variability and a lack of widespread in situ measurements. Regional NH_3 emission estimates using mass balance or emission ratio approaches are uncertain due to variable NH_3 sources and sinks as well as unknown plume correlations with other dairy source tracers. We characterize the spatial distributions of NH_3 and methane (CH_4) dairy plumes using in situ surface and airborne measurements in the Tulare dairy feedlot region of the San Joaquin Valley, California, during the NASA Deriving Information on Surface conditions from Column and Vertically Resolved Observations Relevant to Air Quality 2013 field campaign. Surface NH_3 and CH_4 mixing ratios exhibit large variability with maxima localized downwind of individual dairy feedlots. The geometric mean NH_3:CH_4 enhancement ratio derived from surface measurements is 0.15 ± 0.03 ppmv ppmv~(?1). Individual dairy feedlots with spatially distinct NH_3 and CH_4 source pathways led to statistically significant correlations between NH_3 and CH_4 in 68% of the 69 downwind plumes sampled. At longer sampling distances, the NH_3:CH_4 enhancement ratio decreases 20–30%, suggesting the potential for NH_3 deposition as a loss term for plumes within a few kilometers downwind of feedlots. Aircraft boundary layer transect measurements directly above surface mobile measurements in the dairy region show comparable gradients and geometric mean enhancement ratios within measurement uncertainties, even when including NH_3 partitioning to submicron particles. Individual NH_3 and CH_4 plumes sampled at close proximity where losses are minimal are not necessarily correlated due to lack of mixing and distinct source pathways. Our analyses have important implications for constraining NH_3 sink and plume variability influences on regional NH_3 emission estimates and for improving NH_3 emission inventory spatial allocations.
机译:农业氨气(NH_3)的排放高度不确定,时空变化大,缺乏广泛的现场测量。由于可变的NH_3源和汇以及与其他奶源的示踪剂之间未知的羽状流相关性,使用质量平衡或排放比方法的区域NH_3排放估算是不确定的。我们使用美国航空航天局(NASA)期间从加利福尼亚州圣华金山谷的图莱里奶牛饲养场区域进行的原位表面和空气传播测量来表征NH_3和甲烷(CH_4)奶羽的空间分布。空气质量2013年现场运动。 NH_3和CH_4的表面混合比随单个奶牛饲养场的最大局部顺风表现出较大的变化性。由表面测量得出的几何平均NH_3∶CH_4增强比为0.15±0.03ppmvppmv〜(Δ1)。在空间上不同的NH_3和CH_4源路径下的单个奶牛饲养场,在采样的69个顺风羽流中有68%导致NH_3和CH_4之间具有统计学上的显着相关性。在更长的采样距离下,NH_3:CH_4的增强比降低20–30%,这表明可能将NH_3沉积作为肥育场顺风几公里以内羽流的损失项。即使在将NH_3分配为亚微米颗粒时,乳品区域中表面移动测量正上方的飞机边界层横断面测量也显示出测量不确定性内可比的梯度和几何平均增强比。由于缺乏混合和独特的来源途径,在损失极小的近距离采样的单个NH_3和CH_4羽状流不一定相关。我们的分析对于限制NH_3汇和羽流变异性对区域NH_3排放估算的影响以及改善NH_3排放清单空间分配具有重要意义。

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